{"meta":{"query_hash":"e3f880813a68","filters":{"venue":"Global Biogeochemical Cycles"},"cohort_total":411,"direct_labels_cover":0,"predictions_cover":411,"exported":411,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/e3f880813a68","api":"https://metacan.xera.ac/api/v1/cohort?venue=Global+Biogeochemical+Cycles"},"results":[{"id":"W1480839774","doi":"10.1002/2012gb004519","title":"Distribution, transport, and production of volatile halocarbons in the upper waters of the ice‐covered high Arctic Ocean","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Halocline; Sea ice; Water column; Canada Basin; Arctic; Seawater; Geology; Arctic ice pack; Dimethyl sulfide; Chemistry; Salinity","score_opus":0.004513609558899036,"score_gpt":0.1767323256468808,"score_spread":0.17221871608798175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1480839774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99946624,0.00008767573,0.000017046079,0.000004860894,0.0000016142451,0.0000013446796,0.00016854003,0.0000013492759,0.00025131056],"genre_scores_gemma":[0.9992337,0.000118608965,0.00007714529,0.000008874768,0.000003480225,0.0000029015569,0.00034235796,0.0000013374906,0.00021158656],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999913,0.000010870737,0.0000065313898,0.000021699392,0.000020986632,0.00002695017],"domain_scores_gemma":[0.99975044,0.000028674755,0.000061742205,0.0000069071366,0.000087446264,0.00006482472],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019594186,0.00027090783,0.00023536729,0.0008049107,0.00059014175,0.00067961845,0.00012476966,0.00020351137,0.00028535438],"category_scores_gemma":[0.0002074093,0.00015664264,0.00021360183,0.00068463245,0.00025243234,0.00018231533,0.00027136048,0.00017824631,0.00010384471],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002147418,0.000025905536,0.9726375,0.000031277796,0.00005513743,0.00012349167,0.0005864215,0.00025270163,0.023050033,0.000019588719,0.00006205396,0.0029411789],"study_design_scores_gemma":[0.0000012804577,0.000029145947,0.99885225,0.000003885559,0.0000089872165,0.000023024724,0.00028169306,0.00009851356,0.0005293553,0.0000037905152,0.00016595944,0.0000019923243],"about_ca_topic_score_codex":0.13061127,"about_ca_topic_score_gemma":0.15709186,"teacher_disagreement_score":0.13061127,"about_ca_system_score_codex":0.00083403185,"about_ca_system_score_gemma":0.00071908534,"threshold_uncertainty_score":0.2597021},"labels":[],"label_agreement":null},{"id":"W1480868893","doi":"10.1029/2009gb003658","title":"Recent acceleration of the sea surface <i>f</i>CO<sub>2</sub> growth rate in the North Atlantic subpolar gyre (1993–2008) revealed by winter observations","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; Institut national des sciences de l'Univers; Norges Forskningsråd; Institut Polaire Français Paul Emile Victor; National Aeronautics and Space Administration","keywords":"Ocean gyre; Oceanography; North Atlantic oscillation; Alkalinity; Environmental science; Dissolved organic carbon; Carbon dioxide; North Atlantic Deep Water; Thermohaline circulation; Climatology; Atmosphere (unit); Surface water; Sea surface temperature; Advection; Geology; Chemistry; Geography; Subtropics","score_opus":0.014051738301233591,"score_gpt":0.21885216949399772,"score_spread":0.20480043119276412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1480868893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963852,0.00044642613,0.0004437118,0.00016842765,0.000020749096,0.0000046320015,0.0010534727,0.00004448144,0.0014328663],"genre_scores_gemma":[0.9978097,0.0003424076,0.0004763798,0.000055333454,0.000024301704,0.0000043591044,0.0009477938,0.000008009886,0.00033172162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999658,0.0000024865403,0.0000029209077,0.000013696322,0.000007978029,0.000007109869],"domain_scores_gemma":[0.99965966,0.000030648782,0.00015309185,0.00001795031,0.000098840326,0.00003977],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012252283,0.00025771925,0.00013144527,0.00030130555,0.00023337736,0.00047261696,0.00009610553,0.00023293411,0.00059914944],"category_scores_gemma":[0.00031432588,0.00011388116,0.00017882888,0.00049153605,0.00022677853,0.00026515117,0.00018069115,0.00022502744,0.000110188186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014271084,0.000015685031,0.9647353,0.00006633773,0.0000787098,0.00013023894,0.00023793227,0.0012416362,0.019803945,0.00011921094,0.00087939546,0.012548809],"study_design_scores_gemma":[8.2849294e-7,0.0000059829704,0.998162,0.0000015296091,0.0000063677276,0.000022908007,0.000037625225,0.00031541547,0.0006051115,0.000011302033,0.000829522,0.0000015433653],"about_ca_topic_score_codex":0.07471891,"about_ca_topic_score_gemma":0.12274139,"teacher_disagreement_score":0.07471891,"about_ca_system_score_codex":0.00087337603,"about_ca_system_score_gemma":0.00028985753,"threshold_uncertainty_score":0.14856797},"labels":[],"label_agreement":null},{"id":"W1482267175","doi":"10.1029/2010gb003887","title":"Wetlands, temperature, and atmospheric CO<sub>2</sub>and CH<sub>4</sub>coupling over the past two millennia","year":2011,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Centre for Global Change Science, University of Toronto; Natural Sciences and Engineering Research Council of Canada","keywords":"Ice core; Environmental science; Wetland; Atmospheric sciences; Greenhouse gas; Climate change; Atmosphere (unit); Greenhouse effect; Peat; Biosphere; Climatology; Carbon dioxide; Physical geography; Global warming; Geology; Oceanography; Geography; Ecology; Meteorology","score_opus":0.012330759378583512,"score_gpt":0.22645299051208118,"score_spread":0.21412223113349765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1482267175","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993129,0.00008297933,0.00013379769,0.000034701185,0.0000014839857,6.764248e-7,0.000131009,0.0000038018554,0.00029879154],"genre_scores_gemma":[0.9996649,0.000045838176,0.000092704795,0.0000053143335,0.0000025826293,7.703673e-7,0.00009591355,0.000001518552,0.00009039895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999682,0.000008068344,0.0000013655368,0.000009201973,0.0000045884785,0.000008748795],"domain_scores_gemma":[0.99961865,0.000105361476,0.00016817362,0.000027845153,0.000034168825,0.000045718407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017444234,0.00008500787,0.000058564397,0.00027209392,0.00015523394,0.00027905285,0.000083516185,0.00012518236,0.00085230515],"category_scores_gemma":[0.0006796609,0.00008087573,0.0000865792,0.00030889417,0.0002197048,0.00019234372,0.00022022934,0.00013282314,0.000077274366],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000620198,0.000016948832,0.9903499,0.0000078391495,0.00006426848,0.000035862307,0.000051022173,0.0010811096,0.002743727,0.00019058675,0.0002063574,0.005190373],"study_design_scores_gemma":[6.7871963e-7,0.0000046690734,0.9989874,7.322113e-7,0.000009961612,0.00001937946,0.00002392827,0.00063736807,0.00013100094,0.00005861183,0.0001252357,0.0000010245585],"about_ca_topic_score_codex":0.008136703,"about_ca_topic_score_gemma":0.019251829,"teacher_disagreement_score":0.008136703,"about_ca_system_score_codex":0.00019979349,"about_ca_system_score_gemma":0.00013146257,"threshold_uncertainty_score":0.016178668},"labels":[],"label_agreement":null},{"id":"W1484323760","doi":"10.1029/2006gb002702","title":"Isotope constraints on water, carbon, and heat fluxes from the northern Great Plains region of North America","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; Government of Alberta; Environment and Climate Change Canada; Carleton University; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; National Water Research Institute","keywords":"Transpiration; Environmental science; Soil water; Flux (metallurgy); Atmosphere (unit); Hydrology (agriculture); Atmospheric sciences; Eddy covariance; Stable isotope ratio; Water cycle; Water vapor; Water-use efficiency; Photosynthesis; Ecosystem; Chemistry; Soil science; Ecology; Geology","score_opus":0.009536423299207576,"score_gpt":0.1978816882207403,"score_spread":0.18834526492153272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1484323760","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982212,0.00017433008,0.0002895898,0.000049657683,0.0000017185631,0.000005333681,0.00022862999,0.00001841838,0.0010111076],"genre_scores_gemma":[0.99859804,0.0001557321,0.00057203975,0.00002027181,0.000002663245,0.000009038471,0.00040682414,0.0000064630963,0.00022891552],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986935,0.000015598473,0.0000068012755,0.000050030445,0.000035446694,0.000022829408],"domain_scores_gemma":[0.99986744,0.000029890416,0.000021104612,0.00000960058,0.00005015848,0.000021738068],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027376448,0.00030846096,0.00022828869,0.0005923381,0.00087809726,0.00066257204,0.00033438025,0.00017840718,0.00047243002],"category_scores_gemma":[0.00043820764,0.00022858992,0.00022631674,0.00088657154,0.000458755,0.0002760789,0.0003193914,0.00019495751,0.000054663822],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022559181,0.000050920404,0.87276095,0.00013770029,0.000261239,0.00039980086,0.0019144833,0.013425616,0.08294335,0.0016681158,0.00077267294,0.02543955],"study_design_scores_gemma":[0.0000068221016,0.000005753607,0.9941368,0.0000049472774,0.000023815948,0.000027945924,0.00018287289,0.0038996,0.00079806877,0.00014814231,0.00075551274,0.000009680906],"about_ca_topic_score_codex":0.7520663,"about_ca_topic_score_gemma":0.86239684,"teacher_disagreement_score":0.24793369,"about_ca_system_score_codex":0.0030098553,"about_ca_system_score_gemma":0.0025737185,"threshold_uncertainty_score":0.49878758},"labels":[],"label_agreement":null},{"id":"W1490580799","doi":"10.1029/2005gb002490","title":"Spinning the “Ferrous Wheel”: The importance of the microbial community in an iron budget during the FeCycle experiment","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Microbial Community Ecology and Physiology","field":"Environmental Science","cited_by":163,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Bacterivore; Biogeochemistry; Microbial food web; Biogeochemical cycle; Phytoplankton; Herbivore; Environmental chemistry; Synechococcus; Ferrous; Microbial population biology; Chemistry; Biology; Ecology; Nutrient; Cyanobacteria; Bacteria; Trophic level","score_opus":0.010660669210341419,"score_gpt":0.2514349493751265,"score_spread":0.24077428016478508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1490580799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99740297,0.000116043746,0.0007629094,0.00013322827,0.000036938447,0.000051612835,0.00022234964,0.000049756578,0.0012241342],"genre_scores_gemma":[0.9951617,0.00006705544,0.0012541425,0.0005455745,0.000028269746,0.00017379344,0.00037961826,0.000058541034,0.0023312347],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99966717,0.000069033515,0.000017950426,0.00010309101,0.000060087277,0.00008267393],"domain_scores_gemma":[0.99895144,0.00027216453,0.00011835493,0.00017855984,0.0001420541,0.0003373458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004949239,0.0003249339,0.00061366253,0.00021050399,0.0005348932,0.00072608195,0.00043608344,0.0007330624,0.002294198],"category_scores_gemma":[0.0014259937,0.00026515167,0.00025171446,0.00010555824,0.00045920786,0.0004718144,0.00082762906,0.0010185796,0.00037199576],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003152278,0.00044590878,0.017643908,0.00009744978,0.000028821598,0.00019829067,0.00038702597,0.00014732493,0.9651235,0.00018102828,0.00046579138,0.012128648],"study_design_scores_gemma":[0.00023441206,0.008028506,0.569421,0.000059955968,0.000091473914,0.00031360364,0.00094206975,0.004300601,0.40554994,0.0011963345,0.009734135,0.00012798964],"about_ca_topic_score_codex":0.001953416,"about_ca_topic_score_gemma":0.0032482229,"teacher_disagreement_score":0.002294198,"about_ca_system_score_codex":0.0005031427,"about_ca_system_score_gemma":0.00032178854,"threshold_uncertainty_score":0.0076749325},"labels":[],"label_agreement":null},{"id":"W1491887116","doi":"10.1029/2004gb002300","title":"Influences of boreal fire emissions on Northern Hemisphere atmospheric carbon and carbon monoxide","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":279,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Forest Service","funders":"","keywords":"Boreal; Taiga; Environmental science; Peat; Atmospheric sciences; Northern Hemisphere; Fire regime; Climatology; Carbon monoxide; Southern Hemisphere; Chemistry; Geology; Ecosystem; Forestry; Ecology; Geography","score_opus":0.004247842697735087,"score_gpt":0.20966083553391993,"score_spread":0.20541299283618483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1491887116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986003,0.00021775642,0.0001362842,0.000028280125,0.000007427504,0.0000028557365,0.00026014203,0.000014967642,0.0007319988],"genre_scores_gemma":[0.99938035,0.00007701385,0.0001344482,0.0000117676,0.0000064732567,0.0000025341592,0.00029765783,0.0000043740347,0.00008544899],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978596,0.000053562668,0.0000166726,0.00006832403,0.00003445171,0.000041045918],"domain_scores_gemma":[0.99947673,0.00011540253,0.00018432201,0.000047465644,0.000084892614,0.00009114625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00059435534,0.00043449196,0.00031614862,0.0003858114,0.00034855126,0.00065080565,0.00016713035,0.00020400909,0.0006507266],"category_scores_gemma":[0.0008944192,0.00017144677,0.00043304163,0.00036989103,0.00026716932,0.00032356047,0.00028705515,0.00017532514,0.00006941717],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023471148,0.000037846963,0.9826115,0.000021161517,0.00016961785,0.0001275126,0.00009848816,0.0022754127,0.007950003,0.000087956396,0.00015744039,0.0062284237],"study_design_scores_gemma":[0.000002044123,0.000009577867,0.99908817,0.0000012147777,0.000009479868,0.000026628766,0.000017600842,0.0005580736,0.00015840124,0.000013542374,0.00011292467,0.000002262599],"about_ca_topic_score_codex":0.053471424,"about_ca_topic_score_gemma":0.09591061,"teacher_disagreement_score":0.053471424,"about_ca_system_score_codex":0.00068968185,"about_ca_system_score_gemma":0.00035253807,"threshold_uncertainty_score":0.10632038},"labels":[],"label_agreement":null},{"id":"W1492315926","doi":"10.1029/2006gb002889","title":"Potential glacial‐interglacial changes in stable carbon isotope ratios of methane sources and sink fractionation","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Last Glacial Maximum; Sink (geography); Atmospheric methane; Fractionation; Ice core; Isotopes of carbon; Environmental science; Isotope fractionation; Holocene; Methane; Interglacial; Stable isotope ratio; Environmental chemistry; Glacial period; Carbon cycle; Wetland; Radiocarbon dating; Atmospheric sciences; Greenhouse gas; Chemistry; Geology; Climatology; Oceanography; Ecology; Total organic carbon; Paleontology; Ecosystem","score_opus":0.01419224201511863,"score_gpt":0.24047981071727495,"score_spread":0.22628756870215633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1492315926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949485,0.00032648092,0.0017656091,0.000070961796,0.000013442272,0.0000028987454,0.0007352451,0.00013573094,0.0020011715],"genre_scores_gemma":[0.9988611,0.00010496232,0.00036799186,0.00001607684,0.000004287466,0.0000034444024,0.0004900065,0.000018907103,0.0001332125],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999411,0.000010581165,0.0000048539737,0.00002188524,0.000007846721,0.000013637242],"domain_scores_gemma":[0.9999188,0.000019638106,0.000021353588,0.000015799465,0.000014491449,0.000009814181],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003924299,0.00042095664,0.00022219995,0.00081583584,0.00037315136,0.00067500863,0.00029277152,0.00040548778,0.0019049884],"category_scores_gemma":[0.00055380544,0.00039509035,0.00041178233,0.00065943075,0.0004455863,0.0005066345,0.00040145806,0.00024144404,0.00032686492],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00089258153,0.00008044269,0.77270305,0.00016293398,0.00063569145,0.0002422607,0.00035831603,0.02447401,0.15990081,0.0027992867,0.0010530474,0.036697567],"study_design_scores_gemma":[0.000022125632,0.00005298524,0.97031534,0.000011285685,0.00010785829,0.00011171923,0.000089276655,0.020884356,0.0057048495,0.0011855037,0.0014856784,0.000028929151],"about_ca_topic_score_codex":0.004737259,"about_ca_topic_score_gemma":0.0074594603,"teacher_disagreement_score":0.004737259,"about_ca_system_score_codex":0.00077213784,"about_ca_system_score_gemma":0.00024643203,"threshold_uncertainty_score":0.009419382},"labels":[],"label_agreement":null},{"id":"W1495817180","doi":"10.1029/2009gb003767","title":"Simulating the global distribution of nitrogen isotopes in the ocean","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":236,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; McGill University","funders":"National Science Foundation","keywords":"Denitrification; Water column; Nitrate; Zooplankton; Isotopes of nitrogen; Environmental science; Nitrogen cycle; Nitrogen; Nitrogen fixation; Phytoplankton; Oceanography; Detritus; Environmental chemistry; Ecology; Chemistry; Geology; Nutrient; Biology","score_opus":0.007528051691384113,"score_gpt":0.21691420560076846,"score_spread":0.20938615390938434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1495817180","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9005676,0.00017341037,0.087442406,0.0003847938,0.00009807933,0.000044950262,0.0013088604,0.0007991268,0.009180743],"genre_scores_gemma":[0.9728978,0.00017000338,0.02418994,0.0000931062,0.000017487766,0.00009989619,0.0008042205,0.000082954386,0.001644577],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999411,0.000020752646,0.000002495661,0.000016169515,0.000007979597,0.000011454744],"domain_scores_gemma":[0.99980086,0.000092568174,0.000024121036,0.000028390292,0.000028193252,0.000025820806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002893953,0.00039716993,0.0004643392,0.00016969854,0.0002426607,0.00052724086,0.00074259064,0.0008588225,0.0010913081],"category_scores_gemma":[0.0006644942,0.00034056487,0.0007223743,0.00035730415,0.00040507707,0.00065497775,0.0005499211,0.00053704396,0.00012797292],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022279622,0.000011065497,0.0020095455,0.0000067893434,0.000020545709,0.000018247923,0.0000072956373,0.9957535,0.0006263214,0.0005151797,0.000093567796,0.0009156846],"study_design_scores_gemma":[0.00002019948,0.0000144164505,0.00074109883,0.0000015032289,0.000010266065,0.0000044220883,0.000004901841,0.9983601,0.00018717357,0.00036251167,0.00028919565,0.0000042593047],"about_ca_topic_score_codex":0.02364183,"about_ca_topic_score_gemma":0.015211519,"teacher_disagreement_score":0.02364183,"about_ca_system_score_codex":0.0009710704,"about_ca_system_score_gemma":0.00088280573,"threshold_uncertainty_score":0.047008455},"labels":[],"label_agreement":null},{"id":"W1496142484","doi":"10.1029/2010gb003884","title":"Attributing uncertainties in simulated biospheric carbon fluxes to different error sources","year":2011,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University; Université Laval; Centre de Géomatique du Québec; Environment and Climate Change Canada; University of Waterloo","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Eddy covariance; Environmental science; Shortwave radiation; Carbon cycle; Carbon sink; Atmospheric sciences; Land cover; Shortwave; Satellite; Climatology; Climate change; Meteorology; Ecosystem; Ecology; Geography; Land use; Radiation","score_opus":0.015260641711911547,"score_gpt":0.22028064786455223,"score_spread":0.20502000615264068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1496142484","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85266304,0.0005385137,0.14201415,0.0004910139,0.00006463615,0.00006707714,0.0007982954,0.0004429581,0.0029203608],"genre_scores_gemma":[0.98866874,0.00009015487,0.010693946,0.000046494748,0.00001232503,0.000015097802,0.00029976887,0.000039167895,0.0001342562],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99854124,0.00048136976,0.00009615888,0.00025422103,0.00051844004,0.00010863152],"domain_scores_gemma":[0.9928491,0.004378767,0.0008497014,0.0006894275,0.0011381098,0.00009494072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0043941634,0.00082588656,0.00026491113,0.0012388368,0.00059983396,0.0013875748,0.00083831046,0.000954709,0.00024314938],"category_scores_gemma":[0.016764633,0.00039784334,0.00050964375,0.0012331759,0.0011103436,0.0012507387,0.000954332,0.00059927447,0.000045766043],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007569916,0.00003338145,0.06768878,0.00004552059,0.00015574331,0.000044478158,0.00009556401,0.9138389,0.0017002992,0.0035677105,0.00025139112,0.012502481],"study_design_scores_gemma":[0.00001862108,0.000035324807,0.026851835,0.000044590528,0.00006256341,0.000043645286,0.00009115572,0.9576391,0.005874443,0.008499404,0.00077839755,0.000060914434],"about_ca_topic_score_codex":0.057645448,"about_ca_topic_score_gemma":0.051352203,"teacher_disagreement_score":0.057645448,"about_ca_system_score_codex":0.0029226688,"about_ca_system_score_gemma":0.001651302,"threshold_uncertainty_score":0.11461979},"labels":[],"label_agreement":null},{"id":"W1496465145","doi":"10.1029/2011gb004110","title":"Analysis of seasonality and annual mean distribution of atmospheric potential oxygen (APO) in the Pacific region","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Equator; Seasonality; Middle latitudes; Latitude; Southern Hemisphere; Zonal and meridional; Climatology; Annual cycle; Environmental science; Atmospheric sciences; Trough (economics); Flux (metallurgy); Oceanography; Geology; Biology; Chemistry; Ecology","score_opus":0.00562011297367963,"score_gpt":0.2090603899142647,"score_spread":0.20344027694058509,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1496465145","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986185,0.00003820919,0.00032082936,0.000019115227,0.0000025614459,0.000001973455,0.0007337675,0.000024841413,0.00024015838],"genre_scores_gemma":[0.9981279,0.000029659364,0.00027419353,0.0000037726174,0.0000044923477,0.0000047228655,0.0014984285,0.0000057927155,0.000051056395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999137,0.000012151886,0.000006212285,0.000038347913,0.000016001926,0.000013652235],"domain_scores_gemma":[0.9995983,0.00011175639,0.0001123694,0.000041469564,0.00007679858,0.000059306974],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027426294,0.00014741378,0.00017539939,0.00058838696,0.00015583116,0.00023629887,0.00020155111,0.0001789928,0.00030965224],"category_scores_gemma":[0.0007179716,0.00015295156,0.00018859234,0.00062329177,0.00016513755,0.00017968638,0.00018819518,0.00018311883,0.000057690922],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015997056,0.000049548296,0.9689826,0.000038156148,0.00017073886,0.00018525682,0.00020455474,0.009226506,0.011315132,0.00015477843,0.00056480884,0.008947881],"study_design_scores_gemma":[0.0000062622257,0.00001818163,0.98416823,0.00000292942,0.000018788409,0.000062701525,0.00005560003,0.014669474,0.00048707562,0.000052985157,0.000451352,0.0000064258797],"about_ca_topic_score_codex":0.013150596,"about_ca_topic_score_gemma":0.014784464,"teacher_disagreement_score":0.013150596,"about_ca_system_score_codex":0.00020857959,"about_ca_system_score_gemma":0.00017805929,"threshold_uncertainty_score":0.02614814},"labels":[],"label_agreement":null},{"id":"W1496781974","doi":"10.1029/2004gb002330","title":"Dynamics of biogenic gas bubbles in peat and their effects on peatland biogeochemistry","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":160,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Peat; Biogeochemical cycle; Biogeochemistry; Methane; Environmental science; Buoyancy; Trace gas; Greenhouse gas; Chemistry; Environmental chemistry; Abiogenic petroleum origin; Volume (thermodynamics); Hydrology (agriculture); Soil science; Atmospheric sciences; Geology; Ecology; Oceanography; Mechanics","score_opus":0.00408249890575706,"score_gpt":0.20767981041033756,"score_spread":0.2035973115045805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1496781974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999426,0.000105420266,0.00017173504,0.000013796528,4.78558e-7,0.0000023668558,0.00004804585,0.0000054927177,0.0002266023],"genre_scores_gemma":[0.9996152,0.00007902976,0.00014690853,0.0000036069507,4.0943402e-7,0.000002419014,0.000034955985,0.0000014845959,0.000116060255],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995303,0.000007502493,0.0000023350035,0.000010419956,0.000008659207,0.000017902574],"domain_scores_gemma":[0.99985874,0.0000354426,0.00003960822,0.0000057421507,0.000039331597,0.00002111403],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017049,0.00013511976,0.0001314746,0.0002883281,0.00029672135,0.00039624906,0.00016701323,0.00020659673,0.0003221317],"category_scores_gemma":[0.00030163926,0.00012405396,0.0001049399,0.00016296514,0.00038155844,0.00026642275,0.00015668014,0.00013364742,0.00004874572],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000368495,0.00013148483,0.709673,0.0001538485,0.00007148195,0.0007615759,0.0009607868,0.029102497,0.23047721,0.0007944257,0.00030666712,0.027198529],"study_design_scores_gemma":[0.000005451188,0.00005819976,0.9730338,0.000011785215,0.00001262144,0.00007785887,0.0004004876,0.016941741,0.00866306,0.0002593185,0.00052155135,0.000014110236],"about_ca_topic_score_codex":0.233948,"about_ca_topic_score_gemma":0.32245666,"teacher_disagreement_score":0.233948,"about_ca_system_score_codex":0.001847019,"about_ca_system_score_gemma":0.00066910905,"threshold_uncertainty_score":0.46517253},"labels":[],"label_agreement":null},{"id":"W1498492575","doi":"10.1029/2007gb002994","title":"Pan‐Arctic patterns in black carbon sources and fluvial discharges deduced from radiocarbon and PAH source apportionment markers in estuarine surface sediments","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Arctic; Fluvial; Environmental science; Radiocarbon dating; Estuary; Oceanography; Total organic carbon; Deposition (geology); Physical geography; Flux (metallurgy); Geology; Sediment; Environmental chemistry; Geography; Geomorphology; Paleontology; Chemistry","score_opus":0.005403429437178624,"score_gpt":0.1904019273502383,"score_spread":0.1849984979130597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1498492575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992106,0.00005543006,0.00017036105,0.0000036648755,8.363864e-7,8.637496e-7,0.0002184971,0.0000028529805,0.000336825],"genre_scores_gemma":[0.9985214,0.00013107139,0.0004437781,0.00000423376,0.0000017188618,0.0000031552268,0.0005941149,0.0000046250166,0.00029608153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999905,0.000016692056,0.000008127458,0.000034228455,0.000014419068,0.000021600837],"domain_scores_gemma":[0.9997782,0.00003784364,0.00006407414,0.000016058535,0.00008241929,0.000021321874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022730436,0.00018424883,0.00011729365,0.0007864528,0.00022669727,0.00034744482,0.000069742026,0.00010162034,0.00025036142],"category_scores_gemma":[0.00027803786,0.00015411072,0.00013233491,0.00067327777,0.00016314034,0.0001280569,0.0001854585,0.000108902736,0.00008161944],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027697402,0.000014737128,0.93371534,0.000020614776,0.0000892071,0.00009296626,0.00051771675,0.000583219,0.055339303,0.0002011126,0.000066790984,0.00908198],"study_design_scores_gemma":[0.0000011012091,0.000011071845,0.99750936,0.0000019596403,0.000013491143,0.00003782195,0.000076669654,0.0002575127,0.0018266151,0.000020043857,0.00024251394,0.0000017557273],"about_ca_topic_score_codex":0.017883722,"about_ca_topic_score_gemma":0.031554107,"teacher_disagreement_score":0.017883722,"about_ca_system_score_codex":0.0002904033,"about_ca_system_score_gemma":0.00016064904,"threshold_uncertainty_score":0.035559237},"labels":[],"label_agreement":null},{"id":"W1499035870","doi":"10.1002/2014gb004929","title":"The impact of atmospheric <i>p</i>CO<sub><b>2</b></sub> on carbon isotope ratios of the atmosphere and ocean","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Environment Research Council; McGill University; National Research Foundation of Korea; Sight Research UK; Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Atmosphere (unit); Isotopes of carbon; Dissolved organic carbon; Deep sea; Mixed layer; Carbon dioxide in Earth's atmosphere; Atmospheric sciences; Carbon dioxide; Carbon fibers; Oceanography; Geology; Environmental science; Total organic carbon; Chemistry; Environmental chemistry; Climate change; Meteorology; Materials science; Physics","score_opus":0.007944969120146996,"score_gpt":0.21012141774635068,"score_spread":0.20217644862620368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1499035870","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995706,0.0001340454,0.0014657774,0.0001987743,0.000024308125,0.0000071869003,0.00049489574,0.00010169182,0.0018673909],"genre_scores_gemma":[0.9993581,0.000048993694,0.00028210168,0.000029126522,0.0000028594359,0.000004452199,0.00013397574,0.000020134585,0.00012022526],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99990284,0.000025985002,0.0000049780792,0.000027797982,0.0000135259015,0.000024857378],"domain_scores_gemma":[0.9996295,0.00021967688,0.000039664603,0.00002450379,0.000036193745,0.000050383012],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031938351,0.00073699723,0.00030291706,0.0002277619,0.00038687745,0.0008122493,0.00048008986,0.00087327365,0.0012116423],"category_scores_gemma":[0.00084126444,0.00036803944,0.0007679573,0.00027570358,0.00056202355,0.0005402973,0.0005084991,0.0005595709,0.00014686071],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00056313793,0.00013618493,0.07787218,0.00008437636,0.00027314437,0.00035543245,0.000039509352,0.86532897,0.04968322,0.0010051483,0.0007460746,0.003912573],"study_design_scores_gemma":[0.00008483994,0.00014470045,0.04782876,0.000008291885,0.00010602343,0.000048902184,0.00005240883,0.93837655,0.012386215,0.00045200507,0.00046806197,0.000043310516],"about_ca_topic_score_codex":0.05244799,"about_ca_topic_score_gemma":0.016970117,"teacher_disagreement_score":0.05244799,"about_ca_system_score_codex":0.0010614096,"about_ca_system_score_gemma":0.000622146,"threshold_uncertainty_score":0.10428536},"labels":[],"label_agreement":null},{"id":"W1500576594","doi":"10.1029/2010gb003996","title":"Effects of foliage clumping on the estimation of global terrestrial gross primary productivity","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":411,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"","keywords":"Leaf area index; Primary production; Canopy; Environmental science; Atmospheric sciences; Vegetation (pathology); Remote sensing; Productivity; Boreal ecosystem; Satellite; Flux (metallurgy); Photosynthetic capacity; Taiga; Ecosystem; Photosynthesis; Forestry; Geography; Geology; Ecology","score_opus":0.0066574117178593035,"score_gpt":0.21899578548526186,"score_spread":0.21233837376740256,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1500576594","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888592,0.00031315384,0.01006061,0.0000444414,0.000013131542,0.000012887113,0.00012610927,0.00013196189,0.0004386161],"genre_scores_gemma":[0.99732554,0.00005288457,0.0024118237,0.000021421549,0.0000047019894,0.0000039878596,0.000114621005,0.000024986093,0.000039984632],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989906,0.0004083732,0.000056363082,0.00025820275,0.0001945653,0.000091900976],"domain_scores_gemma":[0.9933878,0.0045436793,0.0010116766,0.000549324,0.0003087603,0.00019881352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024777954,0.0007725298,0.00041081075,0.00035403212,0.00025912045,0.00057276787,0.00042928336,0.00049115624,0.00023870802],"category_scores_gemma":[0.009117569,0.00037495053,0.0005298298,0.00034177303,0.000497073,0.0005524005,0.00050903735,0.00047858575,0.000079328216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005782144,0.0001014633,0.57066476,0.00011308755,0.0003218021,0.00046037548,0.00019963509,0.34991455,0.04343644,0.0004282931,0.00034408164,0.033437286],"study_design_scores_gemma":[0.00003787021,0.0002826532,0.49783167,0.00003594182,0.00015005925,0.0003413737,0.000056497203,0.48297417,0.017426351,0.00038326683,0.0004228825,0.000057234523],"about_ca_topic_score_codex":0.01622563,"about_ca_topic_score_gemma":0.010455644,"teacher_disagreement_score":0.01622563,"about_ca_system_score_codex":0.000710364,"about_ca_system_score_gemma":0.00034951922,"threshold_uncertainty_score":0.032262385},"labels":[],"label_agreement":null},{"id":"W1500717668","doi":"10.1029/2006gb002818","title":"Modeling the soil consumption of atmospheric methane at the global scale","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":220,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Environmental science; Sink (geography); Northern Hemisphere; Methane; Subtropics; Water content; Atmospheric sciences; Soil water; Latitude; Moisture; Atmospheric methane; Climatology; Soil science; Meteorology; Chemistry; Ecology; Geology; Geography","score_opus":0.008925348393192388,"score_gpt":0.2317690841812222,"score_spread":0.2228437357880298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1500717668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8524131,0.00028966108,0.13369037,0.00039564233,0.000057148012,0.0001253964,0.0027436675,0.0006354499,0.009649487],"genre_scores_gemma":[0.98024243,0.00014934385,0.016802363,0.000023050243,0.000012885427,0.00009851943,0.0004162358,0.00005053001,0.0022047248],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999145,0.000016336498,0.000004502484,0.000025600477,0.000019578052,0.000019469],"domain_scores_gemma":[0.9998896,0.000039533963,0.000020831169,0.000014555763,0.000020141528,0.000015293259],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002003259,0.00047302712,0.00042058164,0.00029930915,0.00044415845,0.00047764575,0.0010545407,0.0009489449,0.0014089369],"category_scores_gemma":[0.00053976587,0.00034920566,0.00059075374,0.0004964049,0.00044992295,0.0007833384,0.0005654667,0.00039619242,0.00012893123],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017259115,0.000015774467,0.001805486,0.000020846419,0.00001639913,0.000027759794,0.000018015351,0.9895056,0.003495296,0.003205961,0.00011687009,0.0017546413],"study_design_scores_gemma":[0.00001557313,0.000010889635,0.0011824878,0.0000013652899,0.0000057719585,0.000006515583,0.0000050032804,0.99719536,0.00039367663,0.00083593756,0.00034112204,0.000006371907],"about_ca_topic_score_codex":0.077599786,"about_ca_topic_score_gemma":0.049439732,"teacher_disagreement_score":0.077599786,"about_ca_system_score_codex":0.0017001898,"about_ca_system_score_gemma":0.0011383573,"threshold_uncertainty_score":0.15429622},"labels":[],"label_agreement":null},{"id":"W1504328896","doi":"10.1002/2013gb004764","title":"Influences of glacier melt and permafrost thaw on the age of dissolved organic carbon in the Yukon River basin","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Division of Environmental Biology; National Park Service; U.S. Geological Survey","keywords":"Meltwater; Permafrost; Dissolved organic carbon; Tributary; Glacier; Glacial period; Hydrology (agriculture); Groundwater; Drainage basin; Geology; Peat; Surface water; Environmental science; Physical geography; Oceanography; Geomorphology; Ecology; Geography","score_opus":0.019379835627765244,"score_gpt":0.22890313760564554,"score_spread":0.2095233019778803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1504328896","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997366,0.000034977907,0.000012989394,0.000009498441,5.699673e-7,4.904334e-7,0.000086336586,0.0000016566815,0.00011689451],"genre_scores_gemma":[0.9997925,0.000020237629,0.000013348692,0.0000049949585,3.3619435e-7,7.63916e-7,0.00011388646,9.574674e-7,0.00005295116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999254,0.0000132489595,0.000007151211,0.000019825435,0.000011531563,0.000022876347],"domain_scores_gemma":[0.99979025,0.00005171758,0.000039639173,0.000014714522,0.000058771147,0.0000449145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015188566,0.00011111247,0.00019600539,0.00046291217,0.0004177538,0.000564559,0.0001428204,0.00018404008,0.0006026033],"category_scores_gemma":[0.00033638807,0.00014152682,0.00017835599,0.0005531768,0.00035578271,0.00026890784,0.0003580386,0.0001284605,0.000053527867],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000102182195,0.000013783155,0.99069476,0.00001409198,0.00007879696,0.00007652049,0.00022850593,0.00061401795,0.0050212806,0.000079227524,0.000086456654,0.0029903252],"study_design_scores_gemma":[0.0000015179995,0.0000054916077,0.9993136,0.0000013421107,0.000006939918,0.0000103867915,0.00016305092,0.00025809268,0.00014062825,0.00001219459,0.00008515401,0.000001579039],"about_ca_topic_score_codex":0.11520162,"about_ca_topic_score_gemma":0.22505414,"teacher_disagreement_score":0.8847984,"about_ca_system_score_codex":0.0011580167,"about_ca_system_score_gemma":0.00080183975,"threshold_uncertainty_score":0.22906214},"labels":[],"label_agreement":null},{"id":"W1504648157","doi":"10.1029/2011gb004241","title":"Long‐term C accumulation and total C stocks in boreal lakes in northern Québec","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":116,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Boreal; Trophic level; Sediment; Environmental science; Lake ecosystem; Temperate climate; Total organic carbon; Physical geography; Hydrology (agriculture); Range (aeronautics); Geology; Oceanography; Ecosystem; Ecology; Geomorphology; Geography; Biology; Paleontology","score_opus":0.0130514603526493,"score_gpt":0.23257469198416933,"score_spread":0.21952323163152004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1504648157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985567,0.00015941524,0.00011550332,0.000036402107,0.0000014012,0.0000053760277,0.0005412917,0.00000825193,0.00057566486],"genre_scores_gemma":[0.9988632,0.00006264326,0.00012945445,0.00001915227,0.0000012567476,0.000004553369,0.00041101378,0.0000025746583,0.00050609995],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986565,0.000012417368,0.000006231995,0.000035100253,0.000030730233,0.00004986259],"domain_scores_gemma":[0.9993218,0.00006535175,0.00014457798,0.000024793324,0.0003080033,0.00013546052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024931334,0.00022599244,0.0001970807,0.0007272932,0.0012248252,0.0008736935,0.0003748748,0.00024742365,0.0011755998],"category_scores_gemma":[0.00069879054,0.00014250196,0.00020571338,0.0010514241,0.00039098185,0.000384784,0.00032382924,0.00019649976,0.00009668399],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000097995086,0.000019157203,0.9890695,0.000015541209,0.00008585131,0.00009576457,0.0006159166,0.00094145857,0.0016635555,0.00006535454,0.0004109468,0.0069190417],"study_design_scores_gemma":[0.0000027740764,0.000006315265,0.9985078,0.000004324165,0.000009077874,0.00001799134,0.00021746459,0.0008596775,0.00006798543,0.0000069990197,0.00029497468,0.0000045935767],"about_ca_topic_score_codex":0.9806855,"about_ca_topic_score_gemma":0.9933036,"teacher_disagreement_score":0.019314528,"about_ca_system_score_codex":0.010297171,"about_ca_system_score_gemma":0.0027207355,"threshold_uncertainty_score":0.0747115},"labels":[],"label_agreement":null},{"id":"W1506263099","doi":"10.1029/2008gb003326","title":"British Columbian continental shelf as a source of dissolved iron to the subarctic northeast Pacific Ocean","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; University of Victoria","funders":"Fisheries and Oceans Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Oceanography; Continental shelf; Geology; Upwelling; Downwelling; Isopycnal; Subarctic climate; Submarine pipeline; Water mass","score_opus":0.0046809429271268115,"score_gpt":0.18793282472623368,"score_spread":0.18325188179910687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1506263099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919492,0.00082432036,0.000042425312,0.00018872309,0.0000078974845,0.0000075710354,0.000834205,0.000009336961,0.0061363243],"genre_scores_gemma":[0.9949067,0.0009087615,0.0001899688,0.00007734769,0.0000021897035,0.000006445792,0.00055697566,0.000005145688,0.0033464944],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999236,0.0000054039774,0.0000039813804,0.000017422091,0.00002481876,0.000024907822],"domain_scores_gemma":[0.99973017,0.000017688775,0.000040640265,0.000009239023,0.00014399942,0.00005833064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000112676,0.0001775219,0.00017228285,0.0011074318,0.0014715336,0.0009704327,0.00026882478,0.00015646798,0.0016879741],"category_scores_gemma":[0.00040390814,0.00015635791,0.000067588764,0.0016094905,0.00038004736,0.00017403712,0.00046910928,0.00024379588,0.00015019259],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000107122345,0.000024881252,0.95662093,0.00008321401,0.00005136175,0.00082249206,0.0012302737,0.0004017335,0.0057896124,0.00031793653,0.0024899566,0.03206053],"study_design_scores_gemma":[0.0000026489781,0.0000033733568,0.996463,0.00002243604,0.000010237161,0.00003946241,0.0006908912,0.0001261045,0.00022180499,0.000019555051,0.0023965917,0.0000040140103],"about_ca_topic_score_codex":0.9696474,"about_ca_topic_score_gemma":0.99219525,"teacher_disagreement_score":0.030352592,"about_ca_system_score_codex":0.007812861,"about_ca_system_score_gemma":0.004914261,"threshold_uncertainty_score":0.061062634},"labels":[],"label_agreement":null},{"id":"W1506721913","doi":"10.1002/2014gb004975","title":"Biological and physical controls on N<sub>2</sub>, O<sub>2</sub>, and CO<sub>2</sub> distributions in contrasting Southern Ocean surface waters","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Phytoplankton; Saturation (graph theory); Mixed layer; Hydrography; Dissolved organic carbon; Redfield ratio; Entrainment (biomusicology); Supersaturation; Flux (metallurgy); Atmospheric sciences; Chemistry; Oceanography; Environmental chemistry; Geology; Nutrient","score_opus":0.014097073542934194,"score_gpt":0.21210251069440164,"score_spread":0.19800543715146746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1506721913","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999624,0.00002271465,0.00005257058,0.000008157387,0.0000010563962,0.000001292349,0.00008768221,0.0000041671133,0.00019825404],"genre_scores_gemma":[0.9996207,0.0000201301,0.000082939754,0.000010700104,0.0000022313238,0.0000043093937,0.00017653716,0.000002863358,0.00007960736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999342,0.000009396094,0.0000054120446,0.000027195945,0.00001330673,0.000010485241],"domain_scores_gemma":[0.9998047,0.000035636618,0.0000715295,0.000013562508,0.00003273582,0.000041897234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022492725,0.00027611788,0.00022059144,0.00032314242,0.00028362015,0.00040646244,0.00016572892,0.00027478588,0.0005821477],"category_scores_gemma":[0.00033527534,0.00025765834,0.00027619425,0.00029975435,0.00040505044,0.00034231922,0.00039313553,0.00015948662,0.0001089664],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037662938,0.000038891278,0.82835966,0.00006099877,0.00010836359,0.00015664041,0.0005071717,0.0016034028,0.16511178,0.00008258527,0.00012738346,0.003466471],"study_design_scores_gemma":[0.0000028051413,0.000021950413,0.9983564,0.0000011879539,0.0000052215273,0.0000127756675,0.00008617653,0.0006231128,0.00078960357,0.000022008875,0.00007593167,0.000002795706],"about_ca_topic_score_codex":0.019628558,"about_ca_topic_score_gemma":0.03192765,"teacher_disagreement_score":0.019628558,"about_ca_system_score_codex":0.0004794046,"about_ca_system_score_gemma":0.00030141647,"threshold_uncertainty_score":0.039028585},"labels":[],"label_agreement":null},{"id":"W1508510535","doi":"10.1029/2005gb002659","title":"Belowground carbon turnover in a temperate ombrotrophic bog","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University; McGill University","funders":"","keywords":"Ombrotrophic; Peat; Dissolved organic carbon; Bog; Carbon dioxide; Environmental chemistry; Chemistry; Water table; Respiration; Carbon cycle; Sphagnum; Temperate climate; Ecosystem; Ecology; Botany; Geology; Groundwater; Biology","score_opus":0.007075381754112778,"score_gpt":0.23140386917627492,"score_spread":0.22432848742216216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1508510535","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99979657,0.000034887453,0.000039507675,0.0000018936485,4.707958e-7,7.530344e-7,0.000035017954,0.00000357226,0.00008731446],"genre_scores_gemma":[0.99963045,0.000035165496,0.00012624526,0.000005969164,0.0000012136545,0.0000030118067,0.000106414955,0.000002728216,0.00008890632],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999237,0.000010184941,0.0000049872974,0.000024067378,0.000010582626,0.00002643809],"domain_scores_gemma":[0.99988747,0.00001379103,0.000024943529,0.000008557192,0.000017425815,0.000047869406],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017356119,0.00028060237,0.0002907357,0.00044858258,0.0003422047,0.00040325773,0.00020333253,0.00033617934,0.0003283882],"category_scores_gemma":[0.00019378641,0.00020267443,0.00016903013,0.0001635311,0.00015759307,0.00024787415,0.00029614367,0.00015004014,0.00013325574],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00070472,0.00014882005,0.46493965,0.00009422824,0.00007447544,0.00050799514,0.0006983755,0.0014988051,0.5239843,0.000096357704,0.00007249452,0.007179748],"study_design_scores_gemma":[0.000004881605,0.000057388057,0.9953885,0.0000047391763,0.000009973671,0.00009427977,0.00010626171,0.0017738505,0.002374716,0.000034344925,0.00014592228,0.0000050085428],"about_ca_topic_score_codex":0.010329308,"about_ca_topic_score_gemma":0.014222139,"teacher_disagreement_score":0.010329308,"about_ca_system_score_codex":0.00034941843,"about_ca_system_score_gemma":0.00018631155,"threshold_uncertainty_score":0.02053839},"labels":[],"label_agreement":null},{"id":"W1509162212","doi":"10.1029/2007gb002959","title":"Comprehensive data set of global land cover change for land surface model applications","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Land Use and Ecosystem Services","field":"Environmental Science","cited_by":108,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Office of Science; U.S. Geological Survey","keywords":"Land cover; Land use; Global change; Environmental science; Land use, land-use change and forestry; Grassland; Earth system science; Remote sensing; Land information system; Wetland; Physical geography; Natural (archaeology); Climate change; Land management; Geography; Ecology","score_opus":0.06032826256556116,"score_gpt":0.28353204908996815,"score_spread":0.22320378652440698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1509162212","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.015258255,0.00010331954,0.0013342386,0.00006605491,0.000029217164,0.000092316885,0.9799653,0.0007217232,0.0024296471],"genre_scores_gemma":[0.021217916,0.00008662587,0.0031123261,0.00003168562,0.00001201502,0.00031067923,0.9747285,0.00009303717,0.0004071581],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99930966,0.00006800363,0.00011200864,0.00017950947,0.00025987093,0.00007106603],"domain_scores_gemma":[0.9976749,0.00025444952,0.00033240952,0.0004981865,0.0010576806,0.00018242282],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079572765,0.0012023218,0.00071943353,0.0035225095,0.00050350494,0.00095889735,0.0010165471,0.00082481967,0.005876685],"category_scores_gemma":[0.0026533448,0.00033416867,0.00076775573,0.008748195,0.00020153038,0.0009470248,0.0008105893,0.00086563866,0.00636553],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048746986,0.00060806057,0.18325841,0.0018473215,0.0005941258,0.0007133377,0.00041982438,0.049901374,0.0075540137,0.0048516835,0.651963,0.09780141],"study_design_scores_gemma":[0.00027496132,0.0001599218,0.43848228,0.00026267063,0.00017414031,0.0002755743,0.00064621493,0.029446771,0.007641844,0.003002437,0.5194596,0.00017359579],"about_ca_topic_score_codex":0.0319867,"about_ca_topic_score_gemma":0.030281646,"teacher_disagreement_score":0.0319867,"about_ca_system_score_codex":0.0006894039,"about_ca_system_score_gemma":0.0013826578,"threshold_uncertainty_score":0.06360108},"labels":[],"label_agreement":null},{"id":"W1511682068","doi":"10.1002/2014gb004940","title":"A meta‐analysis of oceanic DMS and DMSP cycling processes: Disentangling the summer paradox","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"Ministerio de Ciencia e Innovación; Centre National de la Recherche Scientifique; Generalitat de Catalunya; Université Laval; National Aeronautics and Space Administration","keywords":"Dimethylsulfoniopropionate; Phytoplankton; Biogeochemical cycle; Sulfur cycle; Environmental science; Seasonality; Oceanography; Abiotic component; Ecology; Chemistry; Environmental chemistry; Sulfur; Biology; Nutrient; Geology","score_opus":0.050484343156442,"score_gpt":0.265698110556657,"score_spread":0.21521376740021497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1511682068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89317226,0.061499286,0.033544183,0.0018003023,0.00023996945,0.00008348479,0.007374172,0.0010404411,0.0012458579],"genre_scores_gemma":[0.98344064,0.0032962703,0.010550379,0.00019299336,0.00006346656,0.000044632976,0.0021379753,0.00011291158,0.00016077628],"study_design_codex":"meta_analysis","study_design_gemma":"meta_analysis","domain_scores_codex":[0.99797875,0.0012775587,0.000106729625,0.0004506415,0.00010601747,0.000080375954],"domain_scores_gemma":[0.9953831,0.0031236948,0.00028762585,0.00076612935,0.0002004881,0.00023890955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0061398605,0.001975511,0.0028648148,0.0041093966,0.0006845679,0.0022910903,0.0014845175,0.00094121107,0.0014376417],"category_scores_gemma":[0.0052597667,0.0008359716,0.010015381,0.004309177,0.00048762956,0.000993061,0.0017742814,0.0010549201,0.00016505505],"study_design_candidate":"meta_analysis","study_design_consensus":"meta_analysis","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020688185,0.00022627298,0.32866347,0.005426345,0.51414603,0.0009313883,0.00038100284,0.073595084,0.03532378,0.0035303687,0.002105488,0.033601973],"study_design_scores_gemma":[0.00042507437,0.0012291516,0.41075796,0.00075797475,0.31998867,0.00047930382,0.0008674595,0.23625378,0.007866662,0.010589828,0.010440435,0.00034378824],"about_ca_topic_score_codex":0.008703469,"about_ca_topic_score_gemma":0.0100019295,"teacher_disagreement_score":0.008703469,"about_ca_system_score_codex":0.0008439798,"about_ca_system_score_gemma":0.0010051194,"threshold_uncertainty_score":0.03247106},"labels":[],"label_agreement":null},{"id":"W1512672845","doi":"10.1002/gbc.20046","title":"Processes affecting greenhouse gas production in experimental boreal reservoirs","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Fisheries and Oceans Canada; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Greenhouse gas; Environmental science; Carbon dioxide; Soil water; Atmosphere (unit); Flux (metallurgy); Carbon cycle; Carbon fibers; Primary production; Methane; Peat; Hydrology (agriculture); Environmental chemistry; Atmospheric sciences; Ecosystem; Chemistry; Soil science; Ecology; Oceanography; Geology","score_opus":0.007640425922201231,"score_gpt":0.22286914102845173,"score_spread":0.2152287151062505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1512672845","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996853,0.000015245899,0.00016263333,0.0000054107386,0.0000017569816,0.00000826191,0.000059565005,0.000007100063,0.00005475744],"genre_scores_gemma":[0.99834955,0.00004590815,0.0010895015,0.000014905175,0.0000020200973,0.000056222794,0.0002684873,0.000009161136,0.0001643929],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998203,0.0000331298,0.000019106046,0.0000501019,0.000030598356,0.000046844627],"domain_scores_gemma":[0.9995734,0.000110352456,0.00013409281,0.000058282018,0.000041281575,0.00008266949],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002608909,0.00035656846,0.0002632584,0.00015387518,0.0003514053,0.00037742828,0.00051885785,0.00033566728,0.00032376568],"category_scores_gemma":[0.00036903986,0.0002510422,0.0005737946,0.0001735329,0.0004241507,0.0003510249,0.00030525724,0.00051271217,0.00003284087],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018995771,0.0006749644,0.022542994,0.00006463176,0.00004954374,0.00014598646,0.00014538347,0.004508113,0.9672427,0.00023263918,0.000068999245,0.0024244136],"study_design_scores_gemma":[0.00050928665,0.0068911803,0.19377151,0.000014105096,0.0002655115,0.00032385738,0.0003328901,0.03913021,0.75641674,0.0005461853,0.0016876849,0.00011080253],"about_ca_topic_score_codex":0.007335701,"about_ca_topic_score_gemma":0.007879491,"teacher_disagreement_score":0.007335701,"about_ca_system_score_codex":0.00071795867,"about_ca_system_score_gemma":0.00033687282,"threshold_uncertainty_score":0.014585972},"labels":[],"label_agreement":null},{"id":"W1512802592","doi":"10.1029/2006gb002897","title":"A 15,800‐year record of atmospheric lead deposition on the Devon Island Ice Cap, Nunavut, Canada: Natural and anthropogenic enrichments, isotopic composition, and predominant sources","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Heavy metals in environment","field":"Environmental Science","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Ice core; Younger Dryas; Geology; Weathering; Enrichment factor; Atmosphere (unit); Deposition (geology); Environmental science; Physical geography; Sediment; Environmental chemistry; Holocene; Oceanography; Geochemistry; Chemistry; Heavy metals; Geography; Geomorphology","score_opus":0.004808978855589591,"score_gpt":0.21026475971723885,"score_spread":0.20545578086164926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1512802592","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99215204,0.00061791134,0.00013615287,0.000059076072,0.0000071395357,0.00001688363,0.0040283673,0.000019802466,0.0029626086],"genre_scores_gemma":[0.99428767,0.0004891773,0.00040692388,0.000038404076,0.0000058637484,0.000011605562,0.0030394874,0.000008168149,0.0017126827],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990964,0.00000407558,0.0000054006414,0.000024801666,0.000028406843,0.000027778638],"domain_scores_gemma":[0.99956006,0.000019360063,0.00004094595,0.00001266121,0.00026431336,0.00010260859],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017580575,0.0002653679,0.0002003064,0.0014617332,0.0012009873,0.0007575791,0.00045749536,0.00020634376,0.00069230975],"category_scores_gemma":[0.00029808944,0.00018150253,0.00015604365,0.0016413907,0.0005027676,0.00017442537,0.00043382996,0.00021779639,0.00015088072],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007174624,0.000018037697,0.9843317,0.00005397793,0.00006899512,0.00021883589,0.00094201055,0.00035047735,0.0040132334,0.00010272813,0.0008049552,0.009023203],"study_design_scores_gemma":[0.000002013592,0.000005789875,0.9978307,0.000013773034,0.000008914769,0.000043957767,0.00027330115,0.00017018159,0.00018472757,0.000008712471,0.0014536706,0.000004132269],"about_ca_topic_score_codex":0.976115,"about_ca_topic_score_gemma":0.99076617,"teacher_disagreement_score":0.023885012,"about_ca_system_score_codex":0.008447779,"about_ca_system_score_gemma":0.005390309,"threshold_uncertainty_score":0.061293244},"labels":[],"label_agreement":null},{"id":"W1514104356","doi":"10.1029/2002gb001890","title":"Air‐sea flux of bromoform: Controls, rates, and implications","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":303,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft; Canadian Bee Research Fund","keywords":"Bromoform; Environmental science; Atmospheric sciences; Flux (metallurgy); Sink (geography); Troposphere; Atmospheric chemistry; Climatology; Oceanography; Meteorology; Ozone; Chemistry; Geology; Geography","score_opus":0.009218870024167835,"score_gpt":0.21695168785150892,"score_spread":0.2077328178273411,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1514104356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9525826,0.031934343,0.003337884,0.0012142883,0.00012032173,0.00003329013,0.002546344,0.00013569703,0.008095078],"genre_scores_gemma":[0.9911277,0.0068386625,0.0007014169,0.0001347035,0.000063528176,0.000012203773,0.00056962227,0.000023915782,0.00052809087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997842,0.00004700359,0.000019075424,0.00008332137,0.00003574702,0.000030710416],"domain_scores_gemma":[0.9994821,0.00019642929,0.00012330683,0.000047263446,0.000107192354,0.00004367696],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096557464,0.0005500026,0.0002890101,0.00073268346,0.00024799778,0.0010641224,0.00033133483,0.0005342593,0.0006533048],"category_scores_gemma":[0.00070076785,0.00024101093,0.0004651268,0.000735467,0.00061198685,0.0010943298,0.00054081826,0.00027415654,0.00018863533],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013062555,0.00013471923,0.74656117,0.0013367414,0.0006892876,0.0004902232,0.0006074962,0.008027853,0.17602585,0.0041885506,0.0015904952,0.059041396],"study_design_scores_gemma":[0.00001995836,0.00008314176,0.9829652,0.00003974303,0.000099315475,0.00007270456,0.00028519714,0.002475076,0.00805261,0.0014807055,0.0044021937,0.000024113968],"about_ca_topic_score_codex":0.013139555,"about_ca_topic_score_gemma":0.0058107493,"teacher_disagreement_score":0.013139555,"about_ca_system_score_codex":0.000759848,"about_ca_system_score_gemma":0.0002553753,"threshold_uncertainty_score":0.026126146},"labels":[],"label_agreement":null},{"id":"W1526859590","doi":"10.1029/2003gb002140","title":"Biological fractionation of silicon isotopes in Southern Ocean surface waters","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":191,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Silicic acid; Equilibrium fractionation; Silicon; Fractionation; Diatom; Isotopes of silicon; Geology; Mass-independent fractionation; Sediment; Isotope; Stable isotope ratio; Isotope fractionation; Surface water; Biogenic silica; Environmental chemistry; Oceanography; Environmental science; Chemistry; Paleontology","score_opus":0.018282084104222728,"score_gpt":0.24841972551687325,"score_spread":0.23013764141265053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1526859590","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99970776,0.000035822402,0.000051665244,0.0000043232053,4.301891e-7,6.319397e-7,0.00003148625,0.000002307927,0.00016537563],"genre_scores_gemma":[0.9995315,0.00007628562,0.00013752957,0.0000062260574,0.000001361694,0.0000022290553,0.00013086046,0.0000021337937,0.000111983194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999616,0.0000051097754,0.000002488041,0.000014329489,0.000010228868,0.0000061878427],"domain_scores_gemma":[0.9999219,0.000016326821,0.000027354436,0.000005583863,0.000016686066,0.000012144409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010317343,0.00019291771,0.00012811089,0.0005201579,0.0002030888,0.0003250938,0.000111039386,0.0001492845,0.00029128976],"category_scores_gemma":[0.000184631,0.00013399783,0.00013704655,0.00031409404,0.0003667117,0.00014463368,0.00021321258,0.0000904091,0.0000753501],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001952868,0.000014667421,0.6152526,0.000041117564,0.00004970886,0.000085308304,0.000430092,0.0012123871,0.37575072,0.00014267962,0.00004054713,0.0067848777],"study_design_scores_gemma":[0.000006792296,0.00006883883,0.98487836,0.0000038522817,0.000015928343,0.000041588417,0.00018207585,0.0017328105,0.012645556,0.00011018946,0.000308811,0.0000052263626],"about_ca_topic_score_codex":0.012324103,"about_ca_topic_score_gemma":0.014811624,"teacher_disagreement_score":0.012324103,"about_ca_system_score_codex":0.0004970507,"about_ca_system_score_gemma":0.00020786407,"threshold_uncertainty_score":0.024504721},"labels":[],"label_agreement":null},{"id":"W1530628957","doi":"10.1029/2011gb004192","title":"A land‐to‐ocean perspective on the magnitude, source and implication of DIC flux from major Arctic rivers to the Arctic Ocean","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":174,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"","keywords":"Arctic; Flux (metallurgy); Oceanography; Canada Basin; Geology; Permafrost; Carbonate; Environmental science; Chemistry","score_opus":0.008478885418098735,"score_gpt":0.21511255517327468,"score_spread":0.20663366975517594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1530628957","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9736564,0.009412575,0.0027857781,0.0008607885,0.00004632731,0.0000072735356,0.0012045228,0.000040621024,0.011985654],"genre_scores_gemma":[0.9922854,0.0047536506,0.0014760485,0.00014913433,0.00003276212,0.000006495384,0.00034372072,0.000016048873,0.0009367208],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991024,0.000025916223,0.000006747208,0.000023810748,0.000015217194,0.000018028366],"domain_scores_gemma":[0.9997185,0.00009058408,0.00004462744,0.000015251553,0.000104153114,0.000026924557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000442044,0.0003744237,0.00032575245,0.001231092,0.0005063745,0.0011229926,0.00020253766,0.00021704884,0.0011067848],"category_scores_gemma":[0.00040927433,0.00017508323,0.00035866327,0.0015215259,0.00055602076,0.0005766909,0.00038082188,0.00030460343,0.00013109103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004893001,0.000027453532,0.81453544,0.0004057058,0.00045663427,0.0012357513,0.0009337139,0.008794968,0.107697025,0.0063349563,0.00075888616,0.058330167],"study_design_scores_gemma":[0.0000065737786,0.000050078987,0.98707795,0.00004334029,0.00013234293,0.00016516511,0.0006951274,0.0026108741,0.003649429,0.001378339,0.004178249,0.0000125135275],"about_ca_topic_score_codex":0.03709058,"about_ca_topic_score_gemma":0.05386289,"teacher_disagreement_score":0.03709058,"about_ca_system_score_codex":0.0011344434,"about_ca_system_score_gemma":0.00043356785,"threshold_uncertainty_score":0.07374936},"labels":[],"label_agreement":null},{"id":"W1532651441","doi":"10.1029/2009gb003721","title":"A first appraisal of prognostic ocean DMS models and prospects for their use in climate models","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Université Laval","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Dimethylsulfoniopropionate; Environmental science; Climatology; Climate model; Forcing (mathematics); Chlorophyll a; Marine ecosystem; Sea surface temperature; Ecosystem; Climate change; Ecosystem model; Biogeochemical cycle; Atmospheric sciences; Oceanography; Phytoplankton; Ecology; Geology; Biology","score_opus":0.01836252912602252,"score_gpt":0.23056404963177055,"score_spread":0.21220152050574803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1532651441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4471354,0.083532184,0.36972225,0.021563102,0.0021021585,0.00037509226,0.0072933976,0.005794335,0.062482122],"genre_scores_gemma":[0.8497292,0.022419631,0.11988609,0.00061791955,0.00057297526,0.0001911307,0.0024899833,0.00039213133,0.0037010529],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99931324,0.0003317383,0.00004754495,0.00006678403,0.00020101632,0.000039745868],"domain_scores_gemma":[0.9972211,0.001179646,0.00013942987,0.00042687354,0.0008874226,0.00014546028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005473013,0.0009849529,0.00064294314,0.00081478467,0.00032541444,0.001432332,0.0016168546,0.0008984665,0.0021085117],"category_scores_gemma":[0.0070967246,0.0005155376,0.00080393575,0.0010045178,0.0005510771,0.0018225203,0.0009288679,0.0008648014,0.00047417489],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061844196,0.00018565204,0.018514987,0.00054226175,0.00029766132,0.000109927656,0.00006952424,0.7580241,0.0039279438,0.022766527,0.007646533,0.18729632],"study_design_scores_gemma":[0.0001306694,0.00040123804,0.0060482207,0.00034068286,0.000119171156,0.000043781667,0.00006939078,0.95543015,0.0024075087,0.012053121,0.022888873,0.00006717022],"about_ca_topic_score_codex":0.009942542,"about_ca_topic_score_gemma":0.005208701,"teacher_disagreement_score":0.009942542,"about_ca_system_score_codex":0.0013481189,"about_ca_system_score_gemma":0.0007587232,"threshold_uncertainty_score":0.028944433},"labels":[],"label_agreement":null},{"id":"W1533727705","doi":"10.1002/gbc.20080","title":"Parameterizing bubble‐mediated air‐sea gas exchange and its effect on ocean ventilation","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":178,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Office of Naval Research; University of Victoria; National Center for Atmospheric Research; National Science Foundation","keywords":"Supersaturation; Bubble; Atmospheric sciences; Saturation (graph theory); Argon; Environmental science; Seawater; Meteorology; Mechanics; Oceanography; Geology; Chemistry; Thermodynamics; Physics","score_opus":0.008529447755466152,"score_gpt":0.2070610391899521,"score_spread":0.19853159143448595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1533727705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9525857,0.0002052448,0.043292746,0.00027238013,0.000032974207,0.00004954019,0.00034741664,0.00019198653,0.0030219958],"genre_scores_gemma":[0.99689215,0.00007111771,0.0027035826,0.000016033617,0.0000058401697,0.00003544109,0.00007200833,0.000026367386,0.00017751328],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998807,0.000049727714,0.000008288821,0.000022427786,0.000012534895,0.000026333078],"domain_scores_gemma":[0.9990748,0.0006425647,0.00011627507,0.00007284237,0.000053876505,0.000039658134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047983436,0.00078015187,0.00042734438,0.00033281266,0.00032229637,0.0007075705,0.0007518693,0.0014082547,0.0007625482],"category_scores_gemma":[0.0026539152,0.00035126225,0.00081103586,0.00025275265,0.0007172638,0.0011472338,0.0008790939,0.0007314504,0.00006637499],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021726903,0.000026419444,0.0028064167,0.000019149456,0.000017707647,0.000033415243,0.0000132783625,0.991678,0.0036303743,0.00087454024,0.000046815137,0.0008321306],"study_design_scores_gemma":[0.000014774562,0.0000206067,0.000630633,0.0000031534023,0.000009422188,0.0000067094843,0.000007967049,0.9974226,0.0013290617,0.0004611623,0.000086429434,0.0000074937916],"about_ca_topic_score_codex":0.0141408285,"about_ca_topic_score_gemma":0.005976697,"teacher_disagreement_score":0.0141408285,"about_ca_system_score_codex":0.00082396256,"about_ca_system_score_gemma":0.0008009975,"threshold_uncertainty_score":0.028117001},"labels":[],"label_agreement":null},{"id":"W1536606969","doi":"10.1029/2005gb002590","title":"Role of methane and biogenic volatile organic compound sources in late glacial and Holocene fluctuations of atmospheric methane concentrations","year":2006,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":166,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Atmospheric methane; Methane; Ice core; Holocene; Trace gas; Last Glacial Maximum; Environmental science; Environmental chemistry; Wetland; Atmospheric sciences; Chemistry; Climatology; Geology; Oceanography; Ecology","score_opus":0.007723273666862259,"score_gpt":0.22687434521784053,"score_spread":0.21915107155097827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1536606969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998563,0.00007664436,0.00031571434,0.00011829559,0.000009346941,0.0000046424084,0.00027512552,0.00004909184,0.0005881376],"genre_scores_gemma":[0.9994628,0.000033869263,0.0002003025,0.000015893413,0.0000032544474,0.0000059797626,0.00016959522,0.000009762927,0.00009850941],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998666,0.000042319003,0.000008539657,0.000036137277,0.000012627333,0.000033720476],"domain_scores_gemma":[0.9997124,0.00012791026,0.000039618626,0.000024694938,0.000029436003,0.0000660037],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004746651,0.00069841766,0.0003415149,0.00045866362,0.0007714163,0.0011040263,0.0007435045,0.0013338856,0.00089936715],"category_scores_gemma":[0.0010398171,0.00058710604,0.000932138,0.0004206997,0.0006369174,0.00068409636,0.0005153644,0.000493517,0.00010505665],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004586489,0.0002585923,0.15270706,0.00004306231,0.00033423057,0.00025087417,0.00012037832,0.8334604,0.007486238,0.0016711338,0.00049382745,0.0027155331],"study_design_scores_gemma":[0.00016924809,0.00013372867,0.06345205,0.000010361811,0.00008568393,0.000031245025,0.000078017365,0.93331677,0.0014563261,0.0007176876,0.00050571124,0.00004326423],"about_ca_topic_score_codex":0.05285033,"about_ca_topic_score_gemma":0.026306942,"teacher_disagreement_score":0.05285033,"about_ca_system_score_codex":0.0015707054,"about_ca_system_score_gemma":0.0008679839,"threshold_uncertainty_score":0.10508543},"labels":[],"label_agreement":null},{"id":"W1538369192","doi":"10.1029/2004gb002325","title":"Spatial and temporal analysis of water chemistry records (1958–2000) in the Huanghe (Yellow River) basin","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":190,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Hydrology (agriculture); Weathering; Total dissolved solids; Drainage basin; Surface runoff; Clastic rock; Dissolved silica; Sedimentary rock; Dilution; Spatial variability; Loess; Geology; Environmental science; Chemistry; Geochemistry; Geomorphology","score_opus":0.008051266480710202,"score_gpt":0.20719175135267445,"score_spread":0.19914048487196426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1538369192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99955124,0.00004869857,0.00004931516,0.000010273864,9.019011e-7,0.000002136746,0.0002099264,0.0000031262985,0.00012431761],"genre_scores_gemma":[0.99907136,0.000060806753,0.00012996042,0.000005814243,0.0000033416165,0.000006271181,0.00057032844,8.4482934e-7,0.00015121879],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999908,0.0000097080665,0.000010550394,0.000036039062,0.000017934335,0.000017829881],"domain_scores_gemma":[0.9995834,0.000076147764,0.00014866982,0.00003746264,0.00009024076,0.000064036314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002849743,0.00012716642,0.00017206286,0.0011069541,0.00022443413,0.0003051752,0.0001797779,0.0002223468,0.0003142111],"category_scores_gemma":[0.00060363486,0.00014516506,0.0001278902,0.0012147536,0.00029633206,0.00026616405,0.00041667238,0.0001140284,0.00005215967],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058078655,0.00001988902,0.9825524,0.000037619964,0.00008320954,0.00021559666,0.0007410097,0.0009178653,0.005568412,0.00008866247,0.00017992864,0.009537351],"study_design_scores_gemma":[0.000002289161,0.000010002727,0.9987255,0.0000026598304,0.000009880725,0.000023237306,0.00009170519,0.0005292369,0.00020943394,0.000008762424,0.00038461993,0.0000026968282],"about_ca_topic_score_codex":0.04081114,"about_ca_topic_score_gemma":0.06506967,"teacher_disagreement_score":0.04081114,"about_ca_system_score_codex":0.00062447117,"about_ca_system_score_gemma":0.00032841452,"threshold_uncertainty_score":0.081147194},"labels":[],"label_agreement":null},{"id":"W1539293059","doi":"10.1029/2006gb002733","title":"What determines the magnitude of carbon cycle‐climate feedbacks?","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate variability and models","field":"Environmental Science","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Concordia University","funders":"","keywords":"Carbon cycle; Environmental science; Climate change; Carbon dioxide in Earth's atmosphere; Atmospheric sciences; Climate model; Carbon fibers; Climatology; Carbon dioxide; Runaway climate change; Ecosystem; Global warming; Effects of global warming; Ecology; Geology; Biology","score_opus":0.011392966927707028,"score_gpt":0.2522948492302938,"score_spread":0.2409018823025868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1539293059","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9709788,0.003520405,0.01098148,0.0032096275,0.00015416014,0.00004380602,0.0003590556,0.0002268271,0.010525766],"genre_scores_gemma":[0.9986197,0.00041555156,0.0005784063,0.0001173406,0.0000343228,0.000007589417,0.000029120049,0.000019409552,0.00017871772],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995704,0.00014445462,0.000028301338,0.00009490339,0.000079873615,0.00008196882],"domain_scores_gemma":[0.99595875,0.0025799114,0.00059144315,0.00017391222,0.00036676027,0.00032912003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016910294,0.00036126343,0.00050762884,0.00056872494,0.00036903616,0.001501812,0.00045845535,0.00093480444,0.0027721492],"category_scores_gemma":[0.009974186,0.00042988698,0.0003125762,0.00036330268,0.00069758354,0.0022203657,0.000613614,0.0005285343,0.00037809304],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00080961996,0.00034755113,0.44954255,0.0020857255,0.001531618,0.0008747056,0.00085140136,0.15855595,0.16903166,0.024981063,0.004841241,0.18654697],"study_design_scores_gemma":[0.00016354863,0.00029040198,0.61977696,0.00031892047,0.00057989464,0.0008656971,0.0017459681,0.2823575,0.016547345,0.06805121,0.009108492,0.00019404439],"about_ca_topic_score_codex":0.0025831368,"about_ca_topic_score_gemma":0.0029553517,"teacher_disagreement_score":0.0027721492,"about_ca_system_score_codex":0.0005683117,"about_ca_system_score_gemma":0.00048614995,"threshold_uncertainty_score":0.0092737675},"labels":[],"label_agreement":null},{"id":"W1540137853","doi":"10.1029/2011gb004157","title":"Decadal changes in the aragonite and calcite saturation state of the Pacific Ocean","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":208,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"U.S. Department of Energy","keywords":"Aragonite; Oceanography; Ocean gyre; Calcite; Saturation (graph theory); Ocean acidification; Seawater; Geology; Shoaling and schooling; Carbonate; Ocean current; Environmental science; Subtropics; Mineralogy; Chemistry; Ecology","score_opus":0.010837122642436357,"score_gpt":0.22626325674164965,"score_spread":0.2154261340992133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1540137853","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983802,0.00011336737,0.00011304208,0.00006228059,0.0000072496005,0.0000019658003,0.00052548246,0.000010632428,0.00078577176],"genre_scores_gemma":[0.9992716,0.00007058498,0.000066355526,0.000020558098,0.0000041025955,0.000002508043,0.00037049374,0.000002295009,0.00019168755],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999528,0.000008620981,0.0000045440506,0.000015743624,0.00000728124,0.000011008888],"domain_scores_gemma":[0.999653,0.000046010322,0.00012599587,0.000028788298,0.000094996714,0.000051250063],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023630833,0.00012596691,0.00009242554,0.0005129659,0.00015701963,0.00035057025,0.00009903093,0.00022006352,0.00072935387],"category_scores_gemma":[0.00078593666,0.00011250498,0.00012042092,0.0005091407,0.00021422144,0.0002214791,0.00023632277,0.0002284544,0.000115628995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029317263,0.000035542074,0.97866416,0.000028331046,0.00014124447,0.000071097464,0.00026208072,0.0009918753,0.009040957,0.0001569324,0.00058518053,0.009729511],"study_design_scores_gemma":[0.0000023586308,0.000015288151,0.99867225,0.0000016290696,0.00001089572,0.000020877162,0.00007333219,0.00039470303,0.0002621815,0.000036173296,0.0005071661,0.0000031120512],"about_ca_topic_score_codex":0.011202438,"about_ca_topic_score_gemma":0.018057022,"teacher_disagreement_score":0.011202438,"about_ca_system_score_codex":0.00029818952,"about_ca_system_score_gemma":0.00011744274,"threshold_uncertainty_score":0.022274435},"labels":[],"label_agreement":null},{"id":"W1541740378","doi":"10.1029/2006gb002879","title":"A high‐resolution survey of DMS, CO<sub>2</sub>, and O<sub>2</sub>/Ar distributions in productive coastal waters","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; University of British Columbia","funders":"","keywords":"Hydrography; Sampling (signal processing); Environmental science; Chlorophyll a; Resolution (logic); Atmospheric sciences; Spatial variability; Image resolution; Oceanography; Chemistry; Geology; Physics; Statistics; Mathematics","score_opus":0.012748290712053191,"score_gpt":0.21025667872638037,"score_spread":0.19750838801432719,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1541740378","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986155,0.00005405343,0.00013939533,0.000018553847,8.3065777e-7,0.000008426576,0.000638546,0.000012627552,0.00051203417],"genre_scores_gemma":[0.9978492,0.000099397774,0.00078682584,0.000023872944,0.000002647901,0.000013465657,0.00078266923,0.0000030664912,0.00043895352],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998958,0.000006055342,0.000005230865,0.000030417543,0.000035472352,0.000026903896],"domain_scores_gemma":[0.9997024,0.000029142533,0.000061511324,0.000020149242,0.00010882071,0.00007798187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001064714,0.00032742193,0.00017436103,0.0007928952,0.0009014381,0.0005157052,0.0003456998,0.00033236813,0.00061483163],"category_scores_gemma":[0.00032316372,0.00024573118,0.00014626913,0.001692239,0.00041111006,0.0002173916,0.00047278093,0.00023144619,0.00014783311],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012877308,0.000042328313,0.9391495,0.00006736344,0.00005889693,0.00030064816,0.0007880803,0.00077678106,0.041788034,0.000039924158,0.00048797688,0.01637167],"study_design_scores_gemma":[0.000002832605,0.000013512883,0.998628,0.0000033584715,0.000006630972,0.00003522185,0.00022849643,0.00032931674,0.0004819311,0.0000052124083,0.00026163762,0.000003901279],"about_ca_topic_score_codex":0.72046995,"about_ca_topic_score_gemma":0.87855864,"teacher_disagreement_score":0.72046995,"about_ca_system_score_codex":0.0017817894,"about_ca_system_score_gemma":0.0019070102,"threshold_uncertainty_score":0.5623525},"labels":[],"label_agreement":null},{"id":"W1542028906","doi":"10.1002/gbc.20017","title":"Inter‐ and intra‐annual variability of vegetation in the northern hemisphere and its association with precursory meteorological factors","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Remote Sensing in Agriculture","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ministry of Education, Science and Technology; Korea Meteorological Administration","keywords":"Empirical orthogonal functions; Environmental science; Advanced very-high-resolution radiometer; Climatology; Phenology; Vegetation (pathology); Leaf area index; Northern Hemisphere; Evergreen; Atmospheric sciences; Precipitation; Latitude; Deciduous; Physical geography; Meteorology; Geography; Geology; Ecology","score_opus":0.004804250181959177,"score_gpt":0.1949557023003664,"score_spread":0.19015145211840723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1542028906","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985758,0.00012104933,0.00024373291,0.000017890367,0.000003143181,0.0000021847118,0.00028356575,0.0000117677955,0.0007408456],"genre_scores_gemma":[0.9992842,0.00005379701,0.00013329193,0.0000047637445,0.0000057976567,0.0000040895216,0.0003554582,0.0000031627062,0.0001554523],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981207,0.00003671864,0.000012044832,0.000061670034,0.00003944545,0.000038064565],"domain_scores_gemma":[0.9994783,0.00016060156,0.00015344334,0.000064800646,0.00007689589,0.00006601839],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041912796,0.00013604917,0.00017766871,0.0005252017,0.00026187304,0.0005562768,0.00015832492,0.00015230667,0.00066620624],"category_scores_gemma":[0.00083063217,0.00011028763,0.00020004722,0.0007927865,0.00019798156,0.00023223512,0.00022928734,0.00017042823,0.00011522461],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038756178,0.000016301632,0.9915719,0.000009146585,0.00004421905,0.000059106656,0.00020075068,0.00042119416,0.0017554896,0.000082467224,0.00013488924,0.00566585],"study_design_scores_gemma":[3.0511913e-7,0.0000024200122,0.9995709,8.616402e-7,0.0000023757548,0.0000103895245,0.000035172157,0.00026132978,0.000026150094,0.000014831823,0.00007443396,8.268992e-7],"about_ca_topic_score_codex":0.016673848,"about_ca_topic_score_gemma":0.026732143,"teacher_disagreement_score":0.016673848,"about_ca_system_score_codex":0.00028707075,"about_ca_system_score_gemma":0.00024874872,"threshold_uncertainty_score":0.033153594},"labels":[],"label_agreement":null},{"id":"W1546468654","doi":"10.1029/2011gb004074","title":"Benthic and pelagic sources of carbon dioxide in boreal lakes and a young reservoir (Eastmain‐1) in eastern Canada","year":2011,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Hypolimnion; Benthic zone; Water column; Environmental science; Pelagic zone; Profundal zone; Hydrology (agriculture); Oceanography; Carbon dioxide; Ecosystem respiration; Hydrobiology; Respiration; Primary production; Environmental chemistry; Ecology; Ecosystem; Eutrophication; Geology; Chemistry; Nutrient; Biology","score_opus":0.010319102068746663,"score_gpt":0.18538217230852416,"score_spread":0.1750630702397775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1546468654","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99918777,0.000059914815,0.000029032737,0.0000103166085,9.040993e-7,0.00000667257,0.0002752488,0.0000034628727,0.0004265032],"genre_scores_gemma":[0.99906796,0.00007013898,0.00013331648,0.000013079709,6.427837e-7,0.000005318397,0.00026000364,0.0000025202817,0.00044712515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997981,0.000008231101,0.000010444375,0.000042847918,0.00006564937,0.00007465109],"domain_scores_gemma":[0.9994272,0.000030240597,0.00007816439,0.0000126518025,0.00028180444,0.00017000566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016513834,0.0003379042,0.0003051484,0.0008687493,0.0020354388,0.00097226596,0.00050291547,0.00025550363,0.00051883014],"category_scores_gemma":[0.0004001542,0.00036878244,0.00022746416,0.0014713716,0.00058679783,0.00029560688,0.00055528834,0.00022230993,0.000089985755],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013343865,0.00003245585,0.9817856,0.000032896514,0.000053248634,0.00033115386,0.0023189192,0.00030634349,0.010433799,0.00005583012,0.00019029739,0.004326013],"study_design_scores_gemma":[0.0000013247201,0.0000067750825,0.9986248,0.0000030509689,0.0000070237998,0.00003255431,0.0007770131,0.00018232751,0.0002174289,0.0000036300667,0.00013995383,0.0000040365144],"about_ca_topic_score_codex":0.9740703,"about_ca_topic_score_gemma":0.9947326,"teacher_disagreement_score":0.02592969,"about_ca_system_score_codex":0.011610646,"about_ca_system_score_gemma":0.0065374994,"threshold_uncertainty_score":0.08424151},"labels":[],"label_agreement":null},{"id":"W1549545390","doi":"10.1029/2004gb002222","title":"Historical burn area in western Canadian peatlands and its relationship to fire weather indices","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":169,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Canadian Forest Service","funders":"","keywords":"Peat; Bog; Environmental science; Physical geography; Fire regime; Hydrology (agriculture); Boreal; Geography; Climatology; Ecology; Geology; Ecosystem; Archaeology","score_opus":0.010732006285526348,"score_gpt":0.21672154294237414,"score_spread":0.2059895366568478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1549545390","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99760795,0.00030117505,0.000083114,0.000023859433,0.000002233439,0.0000022953175,0.0011563599,0.0000070748774,0.0008159529],"genre_scores_gemma":[0.99826425,0.00016393518,0.00008663305,0.000006729404,0.0000015693578,0.0000023897715,0.001035594,0.0000028662985,0.00043610221],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983346,0.000008692382,0.00000961009,0.000031030624,0.000054326356,0.000062806736],"domain_scores_gemma":[0.9994765,0.0000602926,0.00011542143,0.000030036063,0.00020428885,0.000113360744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025388878,0.00011977067,0.0001354443,0.0010082393,0.0005041557,0.00054223667,0.00024809453,0.00014104479,0.00088284607],"category_scores_gemma":[0.0010851837,0.00012405525,0.000115412106,0.0014295821,0.00026340075,0.00016122895,0.00019122096,0.00018598231,0.00009501152],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042943226,0.0000083048235,0.99337786,0.000007746204,0.000038414113,0.00003382909,0.00016700165,0.00052509824,0.00028118616,0.00004994731,0.00035073384,0.0051169386],"study_design_scores_gemma":[4.886675e-7,0.000002096713,0.999373,0.0000027044612,0.000005026645,0.000018554998,0.000086496926,0.00022502171,0.000033270877,0.0000069938164,0.0002449843,0.0000013829645],"about_ca_topic_score_codex":0.952001,"about_ca_topic_score_gemma":0.983648,"teacher_disagreement_score":0.047999024,"about_ca_system_score_codex":0.004135692,"about_ca_system_score_gemma":0.0018727874,"threshold_uncertainty_score":0.09656334},"labels":[],"label_agreement":null},{"id":"W1552407022","doi":"10.1029/2010gb003942","title":"Relationships between net primary productivity and forest stand age in U.S. forests","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":210,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Primary production; Biomass (ecology); Environmental science; Productivity; Carbon cycle; Ecosystem; Terrestrial ecosystem; Leaf area index; Forest ecology; Forest inventory; Ecology; Forest management; Agroforestry; Biology","score_opus":0.01519595266160412,"score_gpt":0.2219613854709439,"score_spread":0.2067654328093398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1552407022","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99792165,0.00031512903,0.000174601,0.00003794686,0.000007240855,0.0000028313416,0.0008291843,0.000011610835,0.0006998942],"genre_scores_gemma":[0.9983199,0.00015724718,0.00020018684,0.00003302448,0.000006955375,0.0000052578634,0.0010925401,0.0000029473133,0.00018200156],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999,0.000021367405,0.000012640683,0.000028403805,0.000018948407,0.000018618435],"domain_scores_gemma":[0.99861515,0.00050602877,0.00040651523,0.000061672145,0.00028049853,0.00013014399],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058380933,0.00019402176,0.0001483853,0.00081089785,0.00021078436,0.0003242216,0.0001212133,0.00016423446,0.0009482196],"category_scores_gemma":[0.0015311927,0.00011040822,0.00022336995,0.0009275736,0.00012326744,0.00029420108,0.00017280669,0.00021940921,0.00019181226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017075157,0.000012904268,0.99674785,0.0000045211837,0.00003059558,0.000021390018,0.00003388932,0.00041945215,0.00013796779,0.00003826042,0.00021537367,0.0023207269],"study_design_scores_gemma":[0.0000010828854,0.000009567852,0.99892247,0.0000020303812,0.000007012692,0.000027517322,0.000032650092,0.0007860317,0.000027615513,0.000045035005,0.00013739754,0.000001639643],"about_ca_topic_score_codex":0.028103212,"about_ca_topic_score_gemma":0.08593159,"teacher_disagreement_score":0.028103212,"about_ca_system_score_codex":0.0003569004,"about_ca_system_score_gemma":0.00025238036,"threshold_uncertainty_score":0.055879235},"labels":[],"label_agreement":null},{"id":"W1553627189","doi":"10.1029/2011gb004031","title":"The role of terrestrial vegetation in atmospheric Hg deposition: Pools and fluxes of spike and ambient Hg from the METAALICUS experiment","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University; University of Toronto; Fisheries and Oceans Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Deposition (geology); Vegetation (pathology); Environmental science; Terrestrial ecosystem; Environmental chemistry; Atmospheric sciences; Chemistry; Geology; Ecosystem; Ecology; Geomorphology; Biology; Sediment","score_opus":0.009740434194621712,"score_gpt":0.24643427274968854,"score_spread":0.23669383855506684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1553627189","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994824,0.0000097054335,0.00012265173,0.0000069723847,7.3450974e-7,0.000011418336,0.00014939468,0.000009250742,0.00020752022],"genre_scores_gemma":[0.99768984,0.0000334796,0.0010229981,0.000041627747,0.0000018830918,0.00005254688,0.0005999379,0.000015298227,0.0005423949],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998616,0.000018479937,0.0000070177994,0.000044467448,0.00004376527,0.000024641644],"domain_scores_gemma":[0.99976534,0.00003781718,0.000040639912,0.0000272065,0.00006765356,0.000061356775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021646418,0.0002496211,0.00029535222,0.00025205236,0.0006718609,0.00040340138,0.00041608675,0.00023182298,0.00066610536],"category_scores_gemma":[0.0002276818,0.00015504993,0.00025107377,0.0002977131,0.00030667812,0.00020898688,0.00035977914,0.0003384618,0.00008065446],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026197517,0.0004215927,0.1975887,0.00006209675,0.000108400425,0.00017627777,0.0006374882,0.0008203063,0.78860676,0.00016835805,0.0001905988,0.008599659],"study_design_scores_gemma":[0.000051797317,0.0008529979,0.9285036,0.0000038146552,0.000050568196,0.000058572597,0.00027749667,0.002622662,0.06659324,0.00006373804,0.0009055159,0.000016155062],"about_ca_topic_score_codex":0.17472714,"about_ca_topic_score_gemma":0.3267554,"teacher_disagreement_score":0.17472714,"about_ca_system_score_codex":0.0018333652,"about_ca_system_score_gemma":0.0013375933,"threshold_uncertainty_score":0.34742022},"labels":[],"label_agreement":null},{"id":"W1555156827","doi":"10.1029/2001gb001550","title":"Trends in North American net primary productivity derived from satellite observations, 1982–1998","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":183,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Center for Atmospheric Research; National Aeronautics and Space Administration","keywords":"Primary production; Precipitation; Environmental science; Productivity; Ecosystem; Vegetation (pathology); Woodland; Growing season; Spring (device); Ecoregion; Climate change; Physical geography; Latitude; Climatology; Geography; Ecology; Meteorology","score_opus":0.012936442396718035,"score_gpt":0.2007568576882351,"score_spread":0.18782041529151705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1555156827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9761195,0.00036243547,0.00026617714,0.000102955004,0.0000128471975,0.0000074743693,0.020048894,0.000056646775,0.0030231471],"genre_scores_gemma":[0.9621984,0.00072994636,0.0011168568,0.000060344923,0.000031287105,0.00006345347,0.03347696,0.000016729045,0.002305989],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999325,0.0000069422094,0.000007233807,0.000021762946,0.000021924558,0.000009564747],"domain_scores_gemma":[0.99954385,0.00005289192,0.0001567753,0.000019423105,0.00019655855,0.000030368466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019808653,0.00023746995,0.00014430443,0.00089250586,0.0002474345,0.0003235682,0.00016516336,0.00015570076,0.0011857789],"category_scores_gemma":[0.0005000946,0.00014945313,0.00011513345,0.0016837375,0.00007525754,0.00024945434,0.00016799582,0.0002207324,0.00034757156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011543034,0.000055515386,0.9700912,0.00012739463,0.000111341404,0.000094001676,0.0003858632,0.0019195526,0.0016078601,0.0001742946,0.008225244,0.017092207],"study_design_scores_gemma":[0.0000032997389,0.0000066763632,0.9963624,0.000006251863,0.000013384873,0.000026101254,0.000057230016,0.0007584002,0.00011037647,0.000024255696,0.00262924,0.0000024124142],"about_ca_topic_score_codex":0.08748815,"about_ca_topic_score_gemma":0.2298041,"teacher_disagreement_score":0.08748815,"about_ca_system_score_codex":0.000711568,"about_ca_system_score_gemma":0.00035975652,"threshold_uncertainty_score":0.17395782},"labels":[],"label_agreement":null},{"id":"W1557582538","doi":"10.1029/2003gb002133","title":"Photochemistry and nature of organic matter in Arctic and Antarctic snow","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":143,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Snow; Organic matter; Arctic; Environmental science; Oceanography; The arctic; Environmental chemistry; Geology; Earth science; Chemistry; Geomorphology","score_opus":0.004088672586171051,"score_gpt":0.20016214293769316,"score_spread":0.19607347035152212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1557582538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983444,0.00047792593,0.0000965979,0.000008471411,0.000003069851,0.000005126844,0.00020059154,0.0000020359034,0.0008617176],"genre_scores_gemma":[0.998033,0.00066982035,0.00030538664,0.000016596578,0.000007487173,0.0000055642813,0.0004761607,0.0000029756027,0.00048298732],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999473,0.000008133036,0.000002323251,0.000011760382,0.000015892083,0.000014723305],"domain_scores_gemma":[0.9999157,0.000017095317,0.000023359333,0.000003137425,0.000020566094,0.000020003936],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011341505,0.00019909066,0.00009005503,0.0006920567,0.00041320897,0.0002998807,0.00009138169,0.0001549543,0.0005515539],"category_scores_gemma":[0.000103339335,0.00009893946,0.00010736646,0.00048227707,0.00021082012,0.00012259939,0.00011148967,0.00010208819,0.00008803698],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042888097,0.000033889395,0.1628299,0.00013714097,0.000070416005,0.00020989384,0.00038650914,0.00041113383,0.82811695,0.0001861611,0.000071764174,0.007117315],"study_design_scores_gemma":[0.000008869143,0.00016784377,0.913649,0.000013862438,0.00003057403,0.0001847164,0.0004336094,0.00050907943,0.083795674,0.000117103125,0.00108298,0.0000066502744],"about_ca_topic_score_codex":0.011483289,"about_ca_topic_score_gemma":0.026238909,"teacher_disagreement_score":0.011483289,"about_ca_system_score_codex":0.00035121152,"about_ca_system_score_gemma":0.0002530864,"threshold_uncertainty_score":0.02283287},"labels":[],"label_agreement":null},{"id":"W1558318529","doi":"10.1029/2012gb004341","title":"Dissolved organic matter composition of winter flow in the Yukon River basin: Implications of permafrost thaw and increased groundwater discharge","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dissolved organic carbon; Permafrost; Biogeochemical cycle; Groundwater; Environmental science; Organic matter; Hydrology (agriculture); Drainage basin; Total organic carbon; Environmental chemistry; Subarctic climate; Groundwater flow; Discharge; Groundwater discharge; Oceanography; Chemistry; Geology; Aquifer","score_opus":0.01713124682135867,"score_gpt":0.23475490893958767,"score_spread":0.217623662118229,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1558318529","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99985075,0.0000322119,0.000027265865,0.000004719157,4.202398e-7,8.705362e-7,0.000048374193,0.0000013911008,0.000033867065],"genre_scores_gemma":[0.99967396,0.000036975413,0.000065970635,0.000008403927,6.3244164e-7,0.000002309985,0.00016145592,0.0000010208653,0.000049390546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991345,0.000012228005,0.000009432485,0.000028453369,0.000014198173,0.000022207783],"domain_scores_gemma":[0.99989164,0.000018474308,0.000030066252,0.000005543534,0.00002911099,0.000025184718],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014822057,0.00020240658,0.0002740951,0.00043118303,0.0005382087,0.0005152369,0.0001702379,0.00029691716,0.00023722574],"category_scores_gemma":[0.00019438582,0.00016133738,0.00024279194,0.00058792223,0.00033604444,0.00028591455,0.00027625507,0.0001277839,0.000029246481],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008069108,0.000027065684,0.9785866,0.000026104062,0.000068559064,0.0001268396,0.00038707463,0.00046908154,0.016192306,0.00003353113,0.000039854156,0.00396213],"study_design_scores_gemma":[0.0000017927906,0.000014816147,0.9986487,0.0000017442469,0.000010213421,0.000026408961,0.00021893893,0.00062548416,0.0003753479,0.000012606516,0.000060863393,0.000003134334],"about_ca_topic_score_codex":0.07928126,"about_ca_topic_score_gemma":0.118738644,"teacher_disagreement_score":0.9207187,"about_ca_system_score_codex":0.0010343662,"about_ca_system_score_gemma":0.0006834565,"threshold_uncertainty_score":0.15763962},"labels":[],"label_agreement":null},{"id":"W1559066630","doi":"10.1029/2008gb003412","title":"Integrating peatlands and permafrost into a dynamic global vegetation model: 1. Evaluation and sensitivity of physical land surface processes","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":336,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Office of Science; University of Bristol; Natural Environment Research Council; Sight Research UK; U.S. Department of Energy","keywords":"Permafrost; Peat; Environmental science; Soil carbon; Soil water; Active layer; Vegetation (pathology); Precipitation; Soil science; Vegetation type; Hydrology (agriculture); Water table; Atmospheric sciences; Shrub; Geology; Groundwater; Ecology; Chemistry","score_opus":0.006856409209611631,"score_gpt":0.2652301059980046,"score_spread":0.258373696788393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1559066630","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99173486,0.00007888902,0.006798179,0.00006567386,0.000015000882,0.000037240803,0.0002410305,0.00008485863,0.00094431126],"genre_scores_gemma":[0.9960181,0.00004679568,0.0035347363,0.000013943968,0.0000058642254,0.00003197058,0.00015025043,0.00001634995,0.0001820671],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99972624,0.00012433525,0.000018712526,0.00005634324,0.000030912408,0.000043503525],"domain_scores_gemma":[0.99906725,0.0006136523,0.00007250498,0.000081317354,0.00009249752,0.000072765164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010628063,0.00074728305,0.0007408497,0.00038008537,0.00036347035,0.000826247,0.00093724584,0.0009000015,0.0006616567],"category_scores_gemma":[0.0029025823,0.0005468623,0.00066322595,0.0004396801,0.00043179508,0.0009851519,0.0007475979,0.00064629473,0.0000820114],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008151707,0.000040159117,0.0071822717,0.000011676497,0.00004041619,0.000026589209,0.000013768855,0.9899463,0.00068580033,0.00017257969,0.000029638682,0.0017692439],"study_design_scores_gemma":[0.000020222362,0.000027679414,0.0016520846,0.000001664683,0.000013378854,0.000004297238,0.0000049923237,0.9977786,0.00032633377,0.000114904506,0.000049629845,0.000006163533],"about_ca_topic_score_codex":0.035937134,"about_ca_topic_score_gemma":0.018641593,"teacher_disagreement_score":0.035937134,"about_ca_system_score_codex":0.0010540456,"about_ca_system_score_gemma":0.000697675,"threshold_uncertainty_score":0.071455896},"labels":[],"label_agreement":null},{"id":"W1571975636","doi":"10.1002/2014gb004825","title":"Radium isotopes as a tracer of sediment‐water column exchange in the North Sea","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Killam Trusts; Nederlandse Organisatie voor Wetenschappelijk Onderzoek","keywords":"Water column; Benthic zone; Oceanography; Sediment; Radium; Environmental science; Sediment–water interface; Geology; Water mass; Bottom water; Biogeochemistry; Surface water; Hydrology (agriculture); Chemistry; Geomorphology","score_opus":0.007996578177411456,"score_gpt":0.19927739212842524,"score_spread":0.1912808139510138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1571975636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983903,0.00018030849,0.00076419243,0.000018533643,0.0000033190604,0.0000017902375,0.00010646046,0.000018068002,0.00051700475],"genre_scores_gemma":[0.9986085,0.00010756686,0.000849943,0.0000113560545,0.0000024285337,0.0000041072226,0.00011194426,0.000008275324,0.00029599894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999175,0.00002169045,0.000006804834,0.000026231859,0.00001934467,0.00000846927],"domain_scores_gemma":[0.9998833,0.000031514548,0.000042705477,0.000011075843,0.000021916476,0.000009454509],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029106712,0.0002682206,0.0002190735,0.0004937923,0.00018822406,0.0003947726,0.00023831347,0.0002706334,0.0003212772],"category_scores_gemma":[0.00027241785,0.00019872045,0.00018422495,0.0005223124,0.00022382617,0.00044353798,0.0002940261,0.00020403674,0.000094938885],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075593474,0.000074657335,0.58409023,0.00013716913,0.00025501597,0.00021154937,0.00035429085,0.009041563,0.3813203,0.0006378382,0.0002524327,0.022869047],"study_design_scores_gemma":[0.000042792733,0.00023495482,0.9344041,0.000016799895,0.00008940615,0.000084878106,0.00022098584,0.023683205,0.03945651,0.00037307444,0.0013617855,0.000031643092],"about_ca_topic_score_codex":0.007318502,"about_ca_topic_score_gemma":0.01189386,"teacher_disagreement_score":0.007318502,"about_ca_system_score_codex":0.0004144101,"about_ca_system_score_gemma":0.00023894553,"threshold_uncertainty_score":0.014551818},"labels":[],"label_agreement":null},{"id":"W1574392304","doi":"10.1029/2011gb004209","title":"Data‐based estimates of suboxia, denitrification, and N<sub>2</sub>O production in the ocean and their sensitivities to dissolved O<sub>2</sub>","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":253,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Denitrification; Water column; Environmental science; Nitrogen; Sediment; Oxygen; Hydrology (agriculture); Oceanography; Chemistry; Geology; Geomorphology","score_opus":0.016497957583973415,"score_gpt":0.21663707676373373,"score_spread":0.20013911917976032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1574392304","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96273893,0.00042041476,0.027376363,0.00013463304,0.000024818775,0.000030590505,0.0039124736,0.00031207583,0.00504973],"genre_scores_gemma":[0.9750344,0.00030537354,0.02023993,0.00005074849,0.000008240565,0.000053225667,0.0038502794,0.00007123469,0.00038649523],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997602,0.000039750415,0.0000241591,0.00006464638,0.00009688305,0.000014292732],"domain_scores_gemma":[0.99932635,0.00015056097,0.00023224218,0.00011790064,0.00015480671,0.000018149753],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069141894,0.00053599325,0.0002506435,0.0006852764,0.00017895339,0.00046958218,0.0005358725,0.00034430018,0.0006790878],"category_scores_gemma":[0.0017592475,0.00027778774,0.0003608397,0.0008763549,0.00025805068,0.0006400778,0.0007124311,0.00025330702,0.00019716736],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012560174,0.00012527134,0.80032957,0.00027896595,0.00039463834,0.00007633011,0.00017344748,0.0811756,0.06305227,0.0011288121,0.0009887789,0.052150697],"study_design_scores_gemma":[0.00006125972,0.000044141565,0.88159007,0.000040119357,0.00013794312,0.00006859736,0.00014329089,0.075947866,0.035789452,0.001403451,0.0047180685,0.000055842862],"about_ca_topic_score_codex":0.01627407,"about_ca_topic_score_gemma":0.03610079,"teacher_disagreement_score":0.01627407,"about_ca_system_score_codex":0.0006451869,"about_ca_system_score_gemma":0.00046696357,"threshold_uncertainty_score":0.032358706},"labels":[],"label_agreement":null},{"id":"W1574959524","doi":"10.1029/2008gb003421","title":"Using tracer observations to reduce the uncertainty of ocean diapycnal mixing and climate–carbon cycle projections","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"","keywords":"Environmental science; Mixing (physics); TRACER; Carbon cycle; Greenhouse gas; Atmospheric sciences; Climatology; Climate model; Climate change; Ocean current; Geology; Oceanography; Physics","score_opus":0.018793067491423253,"score_gpt":0.2561183750374895,"score_spread":0.23732530754606626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1574959524","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.74328846,0.0007197203,0.25140524,0.00076568616,0.000045863995,0.000038075417,0.0007366665,0.0004413352,0.0025588435],"genre_scores_gemma":[0.96432984,0.00016638763,0.034960657,0.000037000304,0.000013853033,0.000021027241,0.00033043098,0.000025245685,0.00011543475],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99924785,0.00032951927,0.000067240166,0.00017243237,0.0001195603,0.000063354455],"domain_scores_gemma":[0.99580175,0.0021405022,0.000975352,0.0006573086,0.0002956899,0.00012943186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00458505,0.0007826907,0.0006174763,0.0009435077,0.00038696374,0.0014494717,0.00084745674,0.001349066,0.00048984756],"category_scores_gemma":[0.016148727,0.0006684691,0.00063781976,0.0008235462,0.00087814534,0.0030829064,0.001681413,0.0009968893,0.000080196674],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032780418,0.000108598266,0.08807354,0.0001417664,0.00038596385,0.000055403278,0.00025312902,0.8318479,0.015854586,0.015538196,0.00029767505,0.04711543],"study_design_scores_gemma":[0.00003705609,0.00004078662,0.022218723,0.000036928308,0.0000575019,0.000015099834,0.00004781335,0.95540994,0.006860158,0.014478474,0.000744949,0.000052638447],"about_ca_topic_score_codex":0.011911451,"about_ca_topic_score_gemma":0.008380513,"teacher_disagreement_score":0.011911451,"about_ca_system_score_codex":0.000987185,"about_ca_system_score_gemma":0.00085897755,"threshold_uncertainty_score":0.024248302},"labels":[],"label_agreement":null},{"id":"W1576551213","doi":"10.1029/2010gb003877","title":"Quantifying spatial and temporal Holocene carbon accumulation in ombrotrophic peatlands of the Eastmain region, Quebec, Canada","year":2011,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec en Abitibi-Témiscamingue; Université du Québec à Montréal","funders":"","keywords":"Peat; Ombrotrophic; Holocene; Physical geography; Boreal; Bog; Deglaciation; Radiocarbon dating; Climate change; Geology; Greenhouse gas; Carbon sink; Environmental science; Climatology; Atmospheric sciences; Hydrology (agriculture); Oceanography; Ecology; Geography; Paleontology","score_opus":0.027078167523053188,"score_gpt":0.2350125518852463,"score_spread":0.2079343843621931,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1576551213","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994155,0.00047528718,0.00042078184,0.000046270558,0.0000033951956,0.000026145706,0.003477599,0.000022028402,0.0013735883],"genre_scores_gemma":[0.99603575,0.00020550661,0.00073294056,0.000021214104,0.0000016136921,0.000016528336,0.0018691284,0.0000060541197,0.0011110823],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986255,0.000006146444,0.000006311753,0.0000444708,0.000028235028,0.000052300406],"domain_scores_gemma":[0.99939287,0.00005266128,0.00008373763,0.000017187542,0.00034535254,0.000108167136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023268795,0.0003004576,0.00018520243,0.0012575826,0.0010836388,0.00080680865,0.0005681937,0.00025278566,0.001124262],"category_scores_gemma":[0.00061542523,0.0001336078,0.00020700786,0.0017965998,0.0002735954,0.00021700455,0.0002597418,0.00017727494,0.00015640623],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000108577566,0.00003512497,0.9669808,0.000060034432,0.00008683728,0.00012714308,0.0009548604,0.0019108295,0.0048719384,0.000108389584,0.0010649683,0.023690458],"study_design_scores_gemma":[0.0000021086219,0.0000056564995,0.99723935,0.000012454705,0.000012386123,0.000014651148,0.00034614818,0.0013590205,0.00026446884,0.0000069159755,0.000732025,0.0000046995383],"about_ca_topic_score_codex":0.9935928,"about_ca_topic_score_gemma":0.9978927,"teacher_disagreement_score":0.012694391,"about_ca_system_score_codex":0.012694391,"about_ca_system_score_gemma":0.006559329,"threshold_uncertainty_score":0.09210467},"labels":[],"label_agreement":null},{"id":"W1582294909","doi":"10.1029/2009gb003689","title":"Oceanic distribution of inorganic germanium relative to silicon: Germanium discrimination by diatoms","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Marsden Fund; Deutsche Forschungsgemeinschaft; Australian Research Council; University of Canberra; Royal Society; Natural Sciences and Engineering Research Council of Canada; National Institute of Water and Atmospheric Research","keywords":"Germanium; Silicon; Fractionation; Analytical Chemistry (journal); Seawater; Materials science; Mineralogy; Geology; Chemistry; Environmental chemistry; Oceanography; Chromatography; Optoelectronics","score_opus":0.005130241231960185,"score_gpt":0.21231482421337608,"score_spread":0.2071845829814159,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1582294909","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992317,0.000057579473,0.00013434836,0.000003829025,5.271564e-7,0.000001252704,0.00014882756,0.0000034377667,0.00041863183],"genre_scores_gemma":[0.99886394,0.0000898532,0.00029949844,0.0000076709175,6.60155e-7,0.0000039789134,0.00031258416,0.0000043399623,0.00041744794],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992764,0.000004890527,0.0000058397354,0.000034547673,0.000012673974,0.00001442857],"domain_scores_gemma":[0.9998759,0.000036003352,0.000025737429,0.000006997443,0.000027968212,0.00002728536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010118559,0.00026157062,0.00021477978,0.00058337854,0.00024777374,0.00038404413,0.00013259423,0.00019241031,0.0005396293],"category_scores_gemma":[0.0001927526,0.0002400782,0.00016303912,0.00045025462,0.00024313803,0.00015541079,0.0004420651,0.0001718153,0.0001315974],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003713501,0.0000191808,0.5811035,0.000066179535,0.000072181254,0.00009477015,0.00044895476,0.0006215163,0.40901938,0.00011892487,0.000042185027,0.008021843],"study_design_scores_gemma":[0.000004907114,0.000102538725,0.9765802,0.0000048416537,0.000023752993,0.00006853788,0.00031103025,0.0009708932,0.021427672,0.000035630743,0.00046147555,0.000008491162],"about_ca_topic_score_codex":0.008855333,"about_ca_topic_score_gemma":0.011386153,"teacher_disagreement_score":0.008855333,"about_ca_system_score_codex":0.00033130703,"about_ca_system_score_gemma":0.00017474333,"threshold_uncertainty_score":0.01760757},"labels":[],"label_agreement":null},{"id":"W1587310363","doi":"10.1029/2007gb003167","title":"Changes in the North Atlantic Oscillation influence CO<sub>2</sub> uptake in the North Atlantic over the past 2 decades","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":162,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"North Atlantic oscillation; Atlantic multidecadal oscillation; Climatology; Environmental science; Oceanography; North Atlantic Deep Water; Ocean current; Temperate climate; Atlantic Equatorial mode; Thermohaline circulation; Ocean gyre; Sea surface temperature; Subtropics; Geology; Ecology","score_opus":0.012143814656280874,"score_gpt":0.20802532721007047,"score_spread":0.1958815125537896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1587310363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982089,0.00013293776,0.00017661296,0.0001313603,0.000011690153,0.0000025134193,0.00018084362,0.000016312053,0.001138904],"genre_scores_gemma":[0.99956733,0.00010513545,0.00008006709,0.00001746092,0.0000039389774,0.0000016834774,0.000071489136,0.000003820446,0.00014907177],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993193,0.00002214804,0.000006638503,0.000015338574,0.0000079410665,0.000015959407],"domain_scores_gemma":[0.99977094,0.000077914076,0.00007883775,0.000011883212,0.00002319723,0.000037252823],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022139782,0.00017060594,0.00013943118,0.00016554588,0.0002153747,0.0005739461,0.0001950925,0.00033977925,0.0013600845],"category_scores_gemma":[0.0010406902,0.00019088906,0.0004048605,0.00023951211,0.00021969934,0.0002840515,0.00036557624,0.00020623775,0.00011910487],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022258576,0.00007879345,0.89478445,0.00008018393,0.00030452723,0.000294883,0.000146622,0.08125676,0.011338274,0.0008086659,0.0010130415,0.009671226],"study_design_scores_gemma":[0.00003802905,0.00005822083,0.8740659,0.000016442327,0.00016065693,0.000054800177,0.00025098026,0.122566015,0.0009902276,0.0004804289,0.0013016209,0.000016638207],"about_ca_topic_score_codex":0.054619696,"about_ca_topic_score_gemma":0.07530093,"teacher_disagreement_score":0.054619696,"about_ca_system_score_codex":0.00069694995,"about_ca_system_score_gemma":0.0005407628,"threshold_uncertainty_score":0.10860354},"labels":[],"label_agreement":null},{"id":"W1592742956","doi":"10.1029/2005gb002481","title":"Acquisition of iron bound to strong organic complexes, with different Fe binding groups and photochemical reactivities, by plankton communities in Fe‐limited subantarctic waters","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":155,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Research Council Canada; Natural Sciences and Engineering Research Council of Canada; National Science Council; National Science Foundation","keywords":"Plankton; Chemistry; Environmental chemistry; Photochemistry; Bioavailability; Dissociation (chemistry); Phytoplankton; In situ; Oceanography; Biology; Organic chemistry; Nutrient; Geology","score_opus":0.009722824030393902,"score_gpt":0.19961878745111233,"score_spread":0.18989596342071843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1592742956","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998066,0.00003745543,0.000040442854,0.0000046675973,2.966245e-7,0.0000015531907,0.0000097807715,0.0000010536529,0.00009830168],"genre_scores_gemma":[0.9992675,0.00009570742,0.00029770343,0.000010181072,7.9833495e-7,0.0000059232043,0.00004356816,0.0000015399982,0.00027699882],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99991703,0.0000089996975,0.0000054138927,0.000030811283,0.000017828888,0.000019964416],"domain_scores_gemma":[0.9998982,0.00001946625,0.00002762146,0.0000072976654,0.000022684353,0.00002470794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011269943,0.00024977443,0.00024707287,0.00025095028,0.0003280972,0.00031916678,0.00016219994,0.00028693586,0.00034377322],"category_scores_gemma":[0.00017821029,0.00021843109,0.00015261969,0.00017444335,0.00027549625,0.0002898125,0.000308827,0.00020218668,0.00008810896],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013317962,0.00002199096,0.037102085,0.000047115496,0.00001308178,0.00007417668,0.00038577506,0.00007720764,0.9593833,0.000025768926,0.0000111207155,0.0027252655],"study_design_scores_gemma":[0.000027893571,0.0009705698,0.8354928,0.000011672223,0.000053870663,0.00042909864,0.0015293005,0.0012373083,0.15930283,0.00015197795,0.00077604904,0.000016602837],"about_ca_topic_score_codex":0.0043670093,"about_ca_topic_score_gemma":0.007499194,"teacher_disagreement_score":0.0043670093,"about_ca_system_score_codex":0.00037569425,"about_ca_system_score_gemma":0.00017983705,"threshold_uncertainty_score":0.008683205},"labels":[],"label_agreement":null},{"id":"W1592827673","doi":"10.1029/2010gb003955","title":"The supply of excess phosphate across the Gulf Stream and the maintenance of subtropical nitrogen fixation","year":2011,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Ocean gyre; Isopycnal; Redfield ratio; Oceanography; Environmental science; Nutrient; Subtropics; Photic zone; Geology; Ecology; Phytoplankton; Biology","score_opus":0.00910251328994765,"score_gpt":0.2052587277171497,"score_spread":0.19615621442720205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1592827673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99935085,0.00012386871,0.00009837642,0.000031791224,0.000001111812,8.3579727e-7,0.000032776366,0.000002473893,0.00035801364],"genre_scores_gemma":[0.99970657,0.00009399831,0.00009221688,0.000008820101,0.000002024773,6.981518e-7,0.00002927145,9.599597e-7,0.000065404965],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996674,0.0000058656897,0.0000027448891,0.000009763361,0.000008396173,0.000006563243],"domain_scores_gemma":[0.9998499,0.000021669755,0.00007160823,0.00000882145,0.000024735606,0.00002311014],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011920974,0.0001769416,0.00009634585,0.00034440766,0.0002921208,0.00034608116,0.00017662233,0.00015711023,0.0005057137],"category_scores_gemma":[0.00045705598,0.00010549805,0.00008943663,0.00032647717,0.00034539492,0.00034109206,0.0004343774,0.000119946686,0.000038169586],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015869693,0.000019329353,0.94545275,0.000042807627,0.00009197084,0.0003123058,0.00028485357,0.003110371,0.040637236,0.00049548305,0.00009579264,0.009298476],"study_design_scores_gemma":[0.000003635337,0.000015914002,0.9955052,0.0000041639614,0.000015568858,0.000062261475,0.00015415566,0.0023298163,0.0014230018,0.00026572027,0.00021767481,0.0000027979947],"about_ca_topic_score_codex":0.027546074,"about_ca_topic_score_gemma":0.05635877,"teacher_disagreement_score":0.027546074,"about_ca_system_score_codex":0.0005259246,"about_ca_system_score_gemma":0.0003769211,"threshold_uncertainty_score":0.054771483},"labels":[],"label_agreement":null},{"id":"W1593082376","doi":"10.1029/2009gb003471","title":"Global atmospheric As and Bi contamination preserved in 3000 year old Arctic ice","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Heavy metals in environment","field":"Environmental Science","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Ice core; Snow; Younger Dryas; Ice sheet; Environmental science; Moraine; Physical geography; Geology; Oceanography; Arctic; Cryosphere; Greenland ice sheet; Climate change; Earth science; Climatology; Sea ice; Glacier; Geography; Geomorphology","score_opus":0.006947522074070873,"score_gpt":0.23623043475853886,"score_spread":0.229282912684468,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1593082376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955586,0.00031664802,0.00010970743,0.000019753674,0.0000056489266,0.0000014436343,0.0025926942,0.000013481695,0.0013819614],"genre_scores_gemma":[0.99509287,0.00042427555,0.0003344024,0.000018248307,0.000010321775,0.000005658596,0.0033820714,0.000008338239,0.00072381384],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996674,0.0000028709787,0.0000017391127,0.000014065329,0.000006014476,0.0000086169175],"domain_scores_gemma":[0.9999318,0.000004937976,0.00002068906,0.0000065908125,0.00002420954,0.000011656135],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013155385,0.0002035461,0.00013065302,0.0006271528,0.0002703157,0.00037869025,0.00008733161,0.00014012786,0.0005017868],"category_scores_gemma":[0.00009809145,0.00006831425,0.00011426862,0.0006470763,0.00017263903,0.00016277008,0.00020843108,0.00011743488,0.0002070434],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043059708,0.000037500275,0.9173059,0.00006551751,0.0001603067,0.00035789804,0.00052151416,0.0010247793,0.06037856,0.000374328,0.0010566156,0.018286496],"study_design_scores_gemma":[0.0000012114468,0.000017251343,0.9954464,0.0000047765284,0.000022888908,0.00006885286,0.00012339852,0.00025977314,0.0019664224,0.000055059387,0.0020298057,0.0000041562926],"about_ca_topic_score_codex":0.02353987,"about_ca_topic_score_gemma":0.027925564,"teacher_disagreement_score":0.02353987,"about_ca_system_score_codex":0.00040198673,"about_ca_system_score_gemma":0.00025066762,"threshold_uncertainty_score":0.04680568},"labels":[],"label_agreement":null},{"id":"W1596663257","doi":"10.1029/2009gb003749","title":"Sulphur deposition causes a large‐scale growth decline in boreal forests in Eurasia","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Scots pine; Taiga; Environmental science; Boreal; Climate change; Dendrochronology; Physical geography; Productivity; Ecology; Ecosystem; Atmospheric sciences; Geography; Biology; Geology; Botany; Pinus <genus>","score_opus":0.008594456758577665,"score_gpt":0.24399058386576014,"score_spread":0.23539612710718247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1596663257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992793,0.00021996588,0.0001478451,0.000020508403,0.0000031277468,0.0000017010813,0.00010152342,0.000010860999,0.00021525145],"genre_scores_gemma":[0.999451,0.00010504705,0.00015229052,0.000012368263,0.0000038466956,0.0000022179006,0.00013724138,0.0000025590014,0.0001334839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985814,0.000019975694,0.000015311603,0.000060589875,0.000025119782,0.0000209055],"domain_scores_gemma":[0.99975747,0.0000373478,0.00010041585,0.00001783337,0.00004984921,0.000037071928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005287971,0.0002850955,0.0002638713,0.00033100176,0.00023503452,0.0003082114,0.0002768982,0.0002033651,0.00034785777],"category_scores_gemma":[0.00035445104,0.0001431883,0.00044784983,0.00031499812,0.00029098307,0.0002472845,0.00021881859,0.00015487555,0.00006735604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019824272,0.000055212215,0.9545551,0.000064237225,0.00017608228,0.00034489742,0.00032692944,0.0016843682,0.03257015,0.00007262397,0.00013273097,0.00981954],"study_design_scores_gemma":[0.0000022201255,0.000036683898,0.9982967,0.0000023847335,0.000018525932,0.000047009537,0.00006032484,0.0010924662,0.0002754556,0.000023178185,0.00014226565,0.0000028798672],"about_ca_topic_score_codex":0.0398248,"about_ca_topic_score_gemma":0.05694711,"teacher_disagreement_score":0.0398248,"about_ca_system_score_codex":0.00050116016,"about_ca_system_score_gemma":0.00039713207,"threshold_uncertainty_score":0.07918596},"labels":[],"label_agreement":null},{"id":"W1597746381","doi":"10.1029/2006gb002764","title":"Regulation of atmospheric CO<sub>2</sub> by deep‐sea sediments in an Earth system model","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":236,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Canada Research Chairs; Natural Environment Research Council; Sight Research UK; Japan Agency for Marine-Earth Science and Technology; Royal Society; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Deep sea; Carbonate; Atmosphere (unit); Geology; Sedimentary rock; Sediment; Carbonate minerals; Carbon cycle; Weathering; Carbon dioxide; Total organic carbon; Mineralogy; Environmental chemistry; Oceanography; Geochemistry; Chemistry; Paleontology; Calcite; Meteorology","score_opus":0.008090156655440911,"score_gpt":0.22510526679460613,"score_spread":0.21701511013916522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1597746381","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92887294,0.0004566067,0.039626934,0.0015687695,0.000158167,0.000059772854,0.0035795753,0.0006896969,0.02498748],"genre_scores_gemma":[0.9890309,0.0002757863,0.0050492734,0.00015972479,0.000039437575,0.000118154705,0.0008540549,0.00006740938,0.0044052517],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990284,0.000031150466,0.0000047611106,0.000028198225,0.000013361501,0.000019648376],"domain_scores_gemma":[0.9997873,0.00007206212,0.00003089184,0.00002166216,0.000051406496,0.000036815836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026309758,0.00054906897,0.0006392944,0.00027901004,0.00049707346,0.001184377,0.0011017853,0.0015398184,0.0024407986],"category_scores_gemma":[0.0007160406,0.00048069458,0.00080448715,0.00040065212,0.0006697337,0.0008142658,0.0007663428,0.0008650714,0.00040818963],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003255295,0.000012738622,0.0021353175,0.00001031726,0.000031903506,0.00005231593,0.000026876056,0.99335796,0.000634251,0.0027566182,0.00033333772,0.0006158212],"study_design_scores_gemma":[0.00003689017,0.000015886566,0.0015626197,0.0000028312024,0.000022901106,0.0000075680246,0.00001500046,0.9966486,0.000106268766,0.00092354545,0.00064750714,0.000010410412],"about_ca_topic_score_codex":0.07819696,"about_ca_topic_score_gemma":0.038425032,"teacher_disagreement_score":0.07819696,"about_ca_system_score_codex":0.0014213895,"about_ca_system_score_gemma":0.0011440695,"threshold_uncertainty_score":0.15548354},"labels":[],"label_agreement":null},{"id":"W1601901570","doi":"10.1002/gbc.20026","title":"The contribution of nitrogen deposition to the photosynthetic capacity of forests","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; Natural Sciences and Engineering Research Council of Canada; Oak Ridge National Laboratory; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Microsoft Research; Canadian Foundation for Climate and Atmospheric Sciences; Natural Resources Canada; Université Laval; U.S. Department of Energy; National Science Foundation","keywords":"Evergreen; Environmental science; Deciduous; Canopy; Deposition (geology); Photosynthetic capacity; Carbon sequestration; Eddy covariance; Temperate rainforest; Carbon sink; Photosynthesis; Temperate climate; Atmospheric sciences; Temperate forest; Climate change; Ecosystem; Ecology; Botany; Carbon dioxide; Biology; Geology","score_opus":0.00466587158271715,"score_gpt":0.1927013173694295,"score_spread":0.18803544578671236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1601901570","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961539,0.0013767624,0.0007606123,0.000024093451,0.0000047649946,0.0000018101031,0.00046618373,0.000011081313,0.0012007584],"genre_scores_gemma":[0.9987159,0.000369641,0.00024525527,0.000011423384,0.000004750305,0.0000030039735,0.00044397588,0.0000049145706,0.00020125149],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998777,0.000024002782,0.000007425227,0.00005219651,0.000024763389,0.000013860116],"domain_scores_gemma":[0.9997446,0.000101077494,0.00006223369,0.00004012602,0.000033520664,0.000018506997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034524084,0.00026752794,0.00022604155,0.00027561552,0.00017144498,0.00035674594,0.00016729535,0.00017157514,0.0006285635],"category_scores_gemma":[0.000675201,0.00013358855,0.00017780956,0.00040241997,0.00023181723,0.0003341954,0.00029095393,0.00013136132,0.00018308635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019063076,0.000024881188,0.8919795,0.00014754775,0.00024792898,0.0001168892,0.00010110169,0.0040247934,0.07370127,0.00036778278,0.0002422058,0.028855434],"study_design_scores_gemma":[0.0000012172271,0.000009441506,0.9964211,0.000004913202,0.0000143882735,0.00006807382,0.000015459642,0.0013172005,0.0015086477,0.00019922765,0.00043696133,0.0000034047296],"about_ca_topic_score_codex":0.0036685108,"about_ca_topic_score_gemma":0.0050379126,"teacher_disagreement_score":0.0036685108,"about_ca_system_score_codex":0.00028972077,"about_ca_system_score_gemma":0.00014227345,"threshold_uncertainty_score":0.007294357},"labels":[],"label_agreement":null},{"id":"W1602663322","doi":"10.1029/2007gb002998","title":"Atmospheric Sb in the Arctic during the past 16,000 years: Responses to climate change and human impacts","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Heavy metals in environment","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Snow; Ice core; Arctic; Peat; Environmental science; Glacier; Physical geography; Atmospheric sciences; Groenlandia; Flux (metallurgy); Environmental chemistry; Geology; Chemistry; Climatology; Oceanography; Geography; Archaeology; Ice sheet; Geomorphology","score_opus":0.020279653201541025,"score_gpt":0.25571653955314005,"score_spread":0.23543688635159904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1602663322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981515,0.00047115886,0.00008487453,0.000044129734,0.000011483408,0.0000019912873,0.00082215614,0.0000070529095,0.00040547835],"genre_scores_gemma":[0.99803716,0.0005652587,0.00018675468,0.000018153274,0.000019723448,0.0000044066583,0.00089382444,0.000003168698,0.0002716394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989057,0.00001506939,0.000009433691,0.00003131005,0.00002883372,0.00002475969],"domain_scores_gemma":[0.9997185,0.0000190218,0.00008130551,0.000010435151,0.00012914251,0.00004154858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003126167,0.00028309601,0.00020984269,0.00088371756,0.00048781853,0.00060833216,0.0001668711,0.00030238848,0.00030565972],"category_scores_gemma":[0.00036562278,0.00016438204,0.0002606977,0.0012809583,0.00023975749,0.00019829685,0.00029298934,0.00017402552,0.0001060952],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021498583,0.00001989416,0.9879005,0.000046006826,0.00013825874,0.00013111564,0.00043470724,0.00048474243,0.002878272,0.000037604543,0.00022577406,0.0074881627],"study_design_scores_gemma":[0.0000011259598,0.000016528842,0.99864763,0.000004480756,0.000017311639,0.000050109615,0.00021776465,0.00023237702,0.00019261039,0.000011424675,0.00060611626,0.0000025473912],"about_ca_topic_score_codex":0.26689458,"about_ca_topic_score_gemma":0.33514348,"teacher_disagreement_score":0.26689458,"about_ca_system_score_codex":0.0010139404,"about_ca_system_score_gemma":0.00069914357,"threshold_uncertainty_score":0.53068215},"labels":[],"label_agreement":null},{"id":"W1603709026","doi":"10.1002/2014gb004998","title":"Processes controlling the distributions of Cd and PO<sub>4</sub> in the ocean","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Science Foundation","keywords":"Geotraces; Thermohaline circulation; Oceanography; Deep sea; North Atlantic Deep Water; Surface water; Seawater; Dissolved organic carbon; Phytoplankton; Water column; Deep ocean water; Nutrient; Environmental science; Geology; Chemistry","score_opus":0.012261825836099392,"score_gpt":0.20858894964087232,"score_spread":0.19632712380477294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1603709026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978788,0.00007551543,0.0009806916,0.0000562077,0.000005057039,0.000006163781,0.00021696874,0.00003243873,0.00074816594],"genre_scores_gemma":[0.99915016,0.000064722255,0.00029716725,0.000012711152,0.000002426977,0.00000427004,0.00013881113,0.000011956771,0.00031795708],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994385,0.0000063317407,0.000004590516,0.00002066874,0.000012658754,0.000011835838],"domain_scores_gemma":[0.99985623,0.000041618317,0.000034773242,0.00001140094,0.000036733498,0.00001922642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017160198,0.0002611348,0.00022179226,0.00032731643,0.00020074657,0.0006588026,0.00019897509,0.00029226285,0.0005883303],"category_scores_gemma":[0.0004236852,0.0003815279,0.0002648591,0.00024836528,0.00035823853,0.000541222,0.0004965324,0.00028849256,0.00015306419],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039166637,0.000067417284,0.4887562,0.00015646745,0.00013060446,0.00044048546,0.00027468984,0.048137788,0.44636378,0.002171135,0.00045742234,0.012652268],"study_design_scores_gemma":[0.00005572803,0.00012686997,0.83221954,0.00001447207,0.00006512769,0.00008735794,0.00038592148,0.13362798,0.030013992,0.0017507054,0.0016192954,0.000033042463],"about_ca_topic_score_codex":0.023509847,"about_ca_topic_score_gemma":0.011417349,"teacher_disagreement_score":0.023509847,"about_ca_system_score_codex":0.0010688977,"about_ca_system_score_gemma":0.0005171071,"threshold_uncertainty_score":0.046746016},"labels":[],"label_agreement":null},{"id":"W1604416319","doi":"10.1029/2003gb002197","title":"Greenhouse gas emissions from reservoirs of the western United States","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":152,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"GDG Environnement; Université du Québec à Montréal","funders":"","keywords":"Greenhouse gas; Carbon dioxide; Methane; Flux (metallurgy); Chemistry; Environmental science; Atmosphere (unit); Atmospheric sciences; Mineralogy; Analytical Chemistry (journal); Hydrology (agriculture); Environmental chemistry; Geology; Meteorology","score_opus":0.007689415591108419,"score_gpt":0.21494308412762744,"score_spread":0.20725366853651903,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1604416319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979534,0.00015569349,0.00010471334,0.000045730383,0.0000025610486,0.0000047071394,0.00033541647,0.0000073798974,0.0013902116],"genre_scores_gemma":[0.9981717,0.0001880815,0.00037882343,0.000030602256,0.0000015642308,0.00000853736,0.0006575046,0.0000028391873,0.0005604478],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999007,0.00001762312,0.0000071473532,0.000019006951,0.00003672914,0.000018831039],"domain_scores_gemma":[0.9997781,0.000031300737,0.00006696513,0.000011681773,0.00008914964,0.000022856188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014632396,0.00016348653,0.0001231186,0.0004377035,0.000369818,0.00057238067,0.0001399353,0.00016884471,0.00051111757],"category_scores_gemma":[0.00039323693,0.00015135811,0.00012547431,0.0012491988,0.00015064553,0.0003578987,0.00052916363,0.00016516606,0.00006706154],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002421784,0.00007350993,0.95815724,0.00006545614,0.000106877094,0.00055231806,0.0007168344,0.003267549,0.013523539,0.00017748319,0.000988315,0.02212862],"study_design_scores_gemma":[0.00001463613,0.00007630193,0.9823616,0.000035019693,0.000062674415,0.00015778057,0.0012062441,0.0065028383,0.0035586208,0.00009099579,0.0059151812,0.00001809221],"about_ca_topic_score_codex":0.17262803,"about_ca_topic_score_gemma":0.3625888,"teacher_disagreement_score":0.17262803,"about_ca_system_score_codex":0.0009003934,"about_ca_system_score_gemma":0.0005407546,"threshold_uncertainty_score":0.34324646},"labels":[],"label_agreement":null},{"id":"W1609953258","doi":"10.1029/2006gb002715","title":"Response of peatland carbon dioxide and methane fluxes to a water table drawdown experiment","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":201,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Peat; Water table; Environmental science; Carbon dioxide; Carbon cycle; Hydrology (agriculture); Greenhouse gas; Carbon fibers; Permafrost; Geology; Ecology; Ecosystem; Groundwater; Oceanography","score_opus":0.006774184747306186,"score_gpt":0.24129470392936206,"score_spread":0.23452051918205588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1609953258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997143,0.000008609478,0.00008438669,0.00000766847,0.000006596383,0.000019962805,0.00007777254,0.000008296868,0.00007236634],"genre_scores_gemma":[0.9980877,0.00003533986,0.00049880677,0.00006738208,0.00000782689,0.00014510806,0.00038658368,0.000013966174,0.0007573567],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99984014,0.000021303173,0.0000129850905,0.000047340025,0.000025017389,0.000053155618],"domain_scores_gemma":[0.99929976,0.00013271358,0.00014834739,0.0000705096,0.000070962866,0.0002776931],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002007569,0.00043273065,0.00050895195,0.00016217286,0.00033877476,0.0003858666,0.00037289568,0.0005356187,0.00091292814],"category_scores_gemma":[0.00037289888,0.00032473294,0.0003749114,0.00016665692,0.00037244626,0.0002899471,0.000391467,0.0011360402,0.000116347015],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009167191,0.0027381033,0.007930184,0.00003436244,0.000047134006,0.0001064473,0.00014982684,0.00049537636,0.9776095,0.000033946628,0.000061162,0.0016268475],"study_design_scores_gemma":[0.00075343566,0.03347306,0.28076112,0.00001068524,0.00016180311,0.000104917934,0.000393644,0.007124061,0.6755987,0.00018831436,0.0013571357,0.00007310245],"about_ca_topic_score_codex":0.004616355,"about_ca_topic_score_gemma":0.0070205894,"teacher_disagreement_score":0.004616355,"about_ca_system_score_codex":0.0005449415,"about_ca_system_score_gemma":0.00044564749,"threshold_uncertainty_score":0.0091789365},"labels":[],"label_agreement":null},{"id":"W1614912833","doi":"10.1029/2006gb002705","title":"From Miami to Madison: Investigating the relationship between climate and terrestrial net primary production","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Oak Ridge National Laboratory; National Aeronautics and Space Administration","keywords":"Primary production; Environmental science; Photosynthetically active radiation; Biome; Terrestrial ecosystem; Precipitation; Atmospheric sciences; Climate change; Physical geography; Climatology; Global change; Meteorology; Ecosystem; Ecology; Geography; Photosynthesis","score_opus":0.01890598617339918,"score_gpt":0.24296495587654238,"score_spread":0.2240589697031432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1614912833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99653447,0.000528066,0.00022471322,0.00028086794,0.000008571705,0.000008757463,0.00047147414,0.000003955837,0.001939259],"genre_scores_gemma":[0.9968426,0.0007760496,0.00048268188,0.00015044509,0.00002161575,0.000024785697,0.0008285512,0.000004611784,0.0008686985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999368,0.000025652958,0.0000024286355,0.000010590801,0.000009060529,0.000015485983],"domain_scores_gemma":[0.99981135,0.00006240473,0.000038436432,0.000008555047,0.0000327971,0.00004652858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024520297,0.00021169959,0.00013108779,0.0005683708,0.00041178017,0.00055387116,0.0002500792,0.00018504234,0.0012864028],"category_scores_gemma":[0.0011471234,0.00015605868,0.00018892206,0.00095111865,0.00012321222,0.00036434684,0.00037555044,0.00029317738,0.00020429546],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035603018,0.0002023467,0.96115476,0.000056841207,0.00022171382,0.0005082115,0.0010223375,0.0018060697,0.0034172216,0.00094223703,0.002234697,0.02807739],"study_design_scores_gemma":[0.000012603351,0.00009253928,0.98756,0.000027312513,0.00011736648,0.00010741176,0.0011406906,0.00445047,0.00070495316,0.00059986196,0.005174229,0.000012681624],"about_ca_topic_score_codex":0.107534885,"about_ca_topic_score_gemma":0.18220958,"teacher_disagreement_score":0.107534885,"about_ca_system_score_codex":0.0008431813,"about_ca_system_score_gemma":0.0005189572,"threshold_uncertainty_score":0.21381795},"labels":[],"label_agreement":null},{"id":"W1615909119","doi":"10.1029/2011gb004226","title":"Potential role of inorganic polyphosphate in the cycling of phosphorus within the hypoxic water column of Effingham Inlet, British Columbia","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Aquatic Ecosystems and Phytoplankton Dynamics","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Water column; Redox; Environmental chemistry; Chemistry; Polyphosphate; Phosphorus; Saturation (graph theory); Particulates; Remineralisation; Anoxic waters; Phosphate; Inorganic chemistry; Geology; Oceanography; Fluoride","score_opus":0.0037437925092595604,"score_gpt":0.18916491799807883,"score_spread":0.18542112548881928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1615909119","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99408215,0.00040859144,0.00015580065,0.00015840937,0.0000065260756,0.000016952037,0.0003867015,0.00001380776,0.004771061],"genre_scores_gemma":[0.99714226,0.000296664,0.00034058996,0.00008548168,0.0000021635558,0.0000122201,0.0002132316,0.000010257454,0.0018971418],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996568,0.000024789528,0.000018439452,0.000096235286,0.00008306062,0.00012070322],"domain_scores_gemma":[0.9995653,0.00004389193,0.000047191712,0.000013580419,0.00021570663,0.000114411785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025844097,0.00035707225,0.00037583985,0.0009414496,0.002698792,0.0020472207,0.00089727866,0.00044719692,0.0014841033],"category_scores_gemma":[0.00059154426,0.0003125598,0.00012071281,0.0011079884,0.00088997703,0.0004381761,0.00088565215,0.00044017177,0.00019469263],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050944724,0.00011258521,0.7950377,0.00033928573,0.00011081637,0.0013718401,0.002216873,0.0011046907,0.16009709,0.00072809664,0.0009636148,0.037408024],"study_design_scores_gemma":[0.0000051840443,0.000026354657,0.991879,0.00002556989,0.000017445434,0.00007403114,0.0016114298,0.00089359126,0.0035040407,0.00006839008,0.0018807129,0.000014279751],"about_ca_topic_score_codex":0.9294202,"about_ca_topic_score_gemma":0.9633834,"teacher_disagreement_score":0.07057983,"about_ca_system_score_codex":0.008354791,"about_ca_system_score_gemma":0.006505342,"threshold_uncertainty_score":0.1419909},"labels":[],"label_agreement":null},{"id":"W1619186350","doi":"10.1029/2003gb002209","title":"Effect of water table drawdown on northern peatland methane dynamics: Implications for climate change","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":201,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Peat; Water table; Environmental science; Evapotranspiration; Hydrology (agriculture); Drawdown (hydrology); Climate change; Methane; Atmospheric sciences; Groundwater; Ecology; Geology; Oceanography","score_opus":0.008158479174335376,"score_gpt":0.2521502376224401,"score_spread":0.24399175844810472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1619186350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986526,0.00010252296,0.000050028066,0.00011961472,0.0000043657087,0.00000480457,0.0005904522,0.000012222571,0.00046338458],"genre_scores_gemma":[0.9989598,0.00008766281,0.00009040784,0.00004449913,0.0000022750887,0.000004705052,0.0003673511,0.0000035760336,0.00043973152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992394,0.000012395245,0.0000027047781,0.000015911666,0.000011323194,0.0000337237],"domain_scores_gemma":[0.9995617,0.00005619773,0.00007650861,0.000020926367,0.00012341348,0.00016118871],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022670742,0.0001955324,0.00028095624,0.00023408492,0.00055658043,0.0005677295,0.00032133635,0.00033307896,0.0016065745],"category_scores_gemma":[0.0005098228,0.00009113759,0.0002330132,0.0004302705,0.00045539447,0.00028020726,0.00017151692,0.00023169395,0.00010724766],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018921996,0.00034457326,0.8977241,0.000105162355,0.00016741008,0.00065219344,0.00049254304,0.007991821,0.068389416,0.00026026892,0.0018466101,0.020133756],"study_design_scores_gemma":[0.000008086397,0.000026615944,0.99755436,0.0000023696869,0.000007932845,0.000013532744,0.00012432641,0.001091425,0.00074343476,0.000024053805,0.00039885938,0.0000051898355],"about_ca_topic_score_codex":0.83798856,"about_ca_topic_score_gemma":0.89196783,"teacher_disagreement_score":0.83798856,"about_ca_system_score_codex":0.007887815,"about_ca_system_score_gemma":0.002769506,"threshold_uncertainty_score":0.32593107},"labels":[],"label_agreement":null},{"id":"W1620524097","doi":"10.1002/gbc.20025","title":"Evidence for elevated emissions from high‐latitude wetlands contributing to high atmospheric CH<sub>4</sub>concentration in the early Holocene","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Holocene; Deglaciation; Peat; Wetland; Ice core; Physical geography; Climate change; Marsh; Atmospheric methane; Glacier; Environmental science; Geology; Glacial period; Greenhouse gas; Climatology; Oceanography; Ecology; Geography; Geomorphology","score_opus":0.013099188102686257,"score_gpt":0.24288551726122598,"score_spread":0.22978632915853972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1620524097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99688894,0.0006349595,0.00021636131,0.00006444542,0.000005800978,0.000002836004,0.00015954318,0.000013105198,0.0020140174],"genre_scores_gemma":[0.9990715,0.0004214784,0.00020982625,0.00001858882,0.000008428414,0.0000020197851,0.000100978046,0.0000027237745,0.00016430873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992585,0.000017375041,0.000007997456,0.000016543938,0.000014528859,0.000017742252],"domain_scores_gemma":[0.9995957,0.00016295811,0.00011267279,0.000024420193,0.000068086185,0.000036141544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030883588,0.00015409852,0.000111054534,0.0005740966,0.0004954094,0.0004574051,0.00012198228,0.00023172065,0.0013924722],"category_scores_gemma":[0.0004699588,0.00012986269,0.00018743533,0.00059399544,0.0004904568,0.00026096628,0.00025665382,0.00015302828,0.000117791074],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027360252,0.000046741046,0.94051516,0.00028407213,0.000120402736,0.0010350739,0.0009301319,0.0006899705,0.03369205,0.00054280914,0.00026913243,0.0216009],"study_design_scores_gemma":[0.000001984024,0.000018156741,0.9971802,0.0000105174595,0.000029314495,0.000082177525,0.00039487745,0.00012238136,0.0014213413,0.000109902154,0.00062560284,0.0000034804534],"about_ca_topic_score_codex":0.018801326,"about_ca_topic_score_gemma":0.031301368,"teacher_disagreement_score":0.018801326,"about_ca_system_score_codex":0.00033943963,"about_ca_system_score_gemma":0.00029183572,"threshold_uncertainty_score":0.037383795},"labels":[],"label_agreement":null},{"id":"W1622911508","doi":"10.1029/2007gb003136","title":"The accumulation of silver in marine sediments: A link to biogenic Ba and marine productivity","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Heavy metals in environment","field":"Environmental Science","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Sediment; Sulfate; Environmental chemistry; Sedimentary rock; Scavenging; Continental shelf; Redox; Trace metal; Geology; Oceanography; Mineralogy; Chemistry; Metal; Geochemistry; Paleontology; Inorganic chemistry","score_opus":0.02216085767864107,"score_gpt":0.27037839018870136,"score_spread":0.2482175325100603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1622911508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956673,0.0001061317,0.00008161165,0.000014692403,4.1253318e-7,5.9221395e-7,0.000042205964,0.0000031530221,0.0001845907],"genre_scores_gemma":[0.9996024,0.00008895022,0.00011262176,0.0000033734,0.0000014839768,9.947228e-7,0.000046548765,0.0000010975393,0.00014262504],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999465,0.000007882931,0.0000043579785,0.000016507965,0.000011695033,0.000013074964],"domain_scores_gemma":[0.9997181,0.000058469675,0.000110989495,0.000016198628,0.00006111001,0.000035083696],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014887069,0.00018821169,0.00011917441,0.0008140862,0.00015715175,0.0005316561,0.00014596734,0.0002127232,0.0002968648],"category_scores_gemma":[0.0006615155,0.00019120766,0.00006800564,0.000630854,0.00037492515,0.00025331523,0.0003208747,0.00014148324,0.00008112105],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012421346,0.000010619502,0.9365796,0.000040747665,0.00005167766,0.0001420436,0.00023204384,0.00032281742,0.057311296,0.00008911005,0.00002274035,0.0050731804],"study_design_scores_gemma":[0.0000024431636,0.000032220603,0.9971323,0.0000027888555,0.000009323229,0.00006916655,0.00008414683,0.0003455738,0.0020977198,0.000099464756,0.00012238913,0.0000023479367],"about_ca_topic_score_codex":0.009306631,"about_ca_topic_score_gemma":0.015040771,"teacher_disagreement_score":0.009306631,"about_ca_system_score_codex":0.0003868332,"about_ca_system_score_gemma":0.0001635442,"threshold_uncertainty_score":0.018504918},"labels":[],"label_agreement":null},{"id":"W1629767359","doi":"10.1029/2005gb002489","title":"A factorial analysis of the marine carbon cycle and ocean circulation controls on atmospheric CO<sub>2</sub>","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Environment Research Council","keywords":"Carbonate; Carbon cycle; Environmental science; Solubility; Atmospheric circulation; Ocean current; Circulation (fluid dynamics); Factorial experiment; Total organic carbon; Oceanography; Carbon dioxide; Atmospheric sciences; Climatology; Chemistry; Environmental chemistry; Geology; Thermodynamics; Ecology","score_opus":0.003627663393595826,"score_gpt":0.195727797807964,"score_spread":0.19210013441436818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1629767359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98421603,0.00006786961,0.013674347,0.00007445366,0.00014429902,0.00037745977,0.00044739855,0.00020042343,0.0007976814],"genre_scores_gemma":[0.97759205,0.00008531653,0.01768788,0.00014270631,0.000085275205,0.001743898,0.0006353276,0.00007414521,0.0019534673],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99774784,0.0009728681,0.00010926599,0.00054887665,0.00029614713,0.000324926],"domain_scores_gemma":[0.99146324,0.005230454,0.0010430135,0.0011982349,0.00060271495,0.00046233577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030340392,0.0011915971,0.0013888256,0.00036995273,0.00059683487,0.0009436665,0.0008599513,0.0006723942,0.0023889202],"category_scores_gemma":[0.0050217216,0.00045878958,0.0021342207,0.0003448989,0.0011034643,0.00066160446,0.00063161476,0.001206615,0.0002570101],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.11435646,0.015528533,0.04228811,0.0009000399,0.0025503417,0.0004995996,0.0004920966,0.066713415,0.6928431,0.010820811,0.0020629142,0.050944682],"study_design_scores_gemma":[0.01107045,0.11679365,0.1671765,0.00004026213,0.003342642,0.00026575464,0.00024178158,0.43197522,0.24971947,0.01138819,0.007324525,0.00066156767],"about_ca_topic_score_codex":0.0026082117,"about_ca_topic_score_gemma":0.0019953155,"teacher_disagreement_score":0.0030340392,"about_ca_system_score_codex":0.001373522,"about_ca_system_score_gemma":0.0010968461,"threshold_uncertainty_score":0.01604575},"labels":[],"label_agreement":null},{"id":"W1629799863","doi":"10.1029/2009gb003723","title":"Importance of CO<sub>2</sub> evasion from small boreal streams","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; Trent University","funders":"","keywords":"STREAMS; Boreal; Environmental science; Atmosphere (unit); Taiga; Hydrology (agriculture); Drainage basin; Ecology; Geology; Meteorology; Geography; Biology","score_opus":0.0056433676364317405,"score_gpt":0.20455461895299548,"score_spread":0.19891125131656373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1629799863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984139,0.00022555458,0.00007797463,0.00003316489,0.000004546019,0.0000030952974,0.00005223001,0.0000073978854,0.0011820695],"genre_scores_gemma":[0.99956554,0.00009859209,0.00006382982,0.000007955609,0.000006088706,9.0500544e-7,0.000056795136,0.0000023026766,0.00019806631],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998584,0.000023599341,0.000014249452,0.00003494312,0.00003451159,0.00003420232],"domain_scores_gemma":[0.9996536,0.00005921056,0.000115931965,0.000011528626,0.00009542972,0.00006428066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015168116,0.00021330264,0.00022602282,0.00034279472,0.00055532565,0.00091757486,0.0001761662,0.00016971002,0.001098674],"category_scores_gemma":[0.0004546887,0.00011852073,0.0001443895,0.0003114675,0.0003145699,0.00040159968,0.000301597,0.00014109389,0.00008272751],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015683289,0.00006675948,0.8022822,0.00021068972,0.0001074912,0.0015182939,0.00056535465,0.0022632978,0.1476732,0.00044526003,0.00056535733,0.042733897],"study_design_scores_gemma":[0.000008820828,0.00009676561,0.990409,0.000008742541,0.000033648084,0.0004977617,0.0004886481,0.0012030558,0.00558298,0.00013471536,0.0015270973,0.000008704455],"about_ca_topic_score_codex":0.018098326,"about_ca_topic_score_gemma":0.028660255,"teacher_disagreement_score":0.018098326,"about_ca_system_score_codex":0.0004503055,"about_ca_system_score_gemma":0.00043608097,"threshold_uncertainty_score":0.035985947},"labels":[],"label_agreement":null},{"id":"W1630877035","doi":"10.1002/2014gb005000","title":"The stoichiometry of carbon and nutrients in peat formation","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":121,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Nature Conservancy of Canada; Université de Montréal; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Peat; Bog; Nutrient; Litter; Biogeochemical cycle; Plant litter; Vegetation (pathology); Phosphorus; Environmental chemistry; Chemistry; Carbon fibers; Environmental science; Ecology; Biology","score_opus":0.00506711594313705,"score_gpt":0.21414532640923933,"score_spread":0.20907821046610228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1630877035","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987954,0.00017754038,0.000100498946,0.00000524732,8.395624e-7,0.0000031928782,0.00018317385,0.000003492863,0.000730668],"genre_scores_gemma":[0.99929273,0.00009281171,0.00019223292,0.000004557464,6.5333944e-7,0.0000030745637,0.00018377138,0.0000020234697,0.00022828487],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999846,0.000010292941,0.000010407341,0.00004336814,0.000048561305,0.000041462754],"domain_scores_gemma":[0.9997633,0.000025067528,0.00005519426,0.000010422272,0.000098996425,0.000047026188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020011456,0.00015729161,0.00019451522,0.0011161366,0.0007202585,0.0007740094,0.00025983542,0.00017298193,0.0005038365],"category_scores_gemma":[0.0003933207,0.00018885724,0.00010709702,0.0007424279,0.00057449675,0.00030260853,0.00028059407,0.000087572276,0.00009247694],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013931401,0.0000103023085,0.9318433,0.00009015657,0.000066539826,0.00017150695,0.00056559715,0.0010990533,0.058910266,0.00020032062,0.00010973284,0.006793823],"study_design_scores_gemma":[0.0000013027319,0.0000077740615,0.99711394,0.000006217025,0.000006144724,0.00005288878,0.00025325074,0.0004456724,0.0016118597,0.00006841204,0.00042921497,0.0000032903763],"about_ca_topic_score_codex":0.414605,"about_ca_topic_score_gemma":0.5795099,"teacher_disagreement_score":0.414605,"about_ca_system_score_codex":0.0027174267,"about_ca_system_score_gemma":0.0013308731,"threshold_uncertainty_score":0.82438344},"labels":[],"label_agreement":null},{"id":"W1633181716","doi":"10.1029/2008gb003273","title":"Temperature sensitivity of N<sub>2</sub>O emissions from fertilized agricultural soils: Mathematical modeling in ecosys","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Agriculture and Agri-Food Canada; University of Alberta","funders":"Western Canada Research Grid","keywords":"Environmental science; Climate change; Greenhouse gas; Soil water; Atmospheric sciences; Precipitation; Global warming; Climate sensitivity; Climate model; Soil science; Ecology; Meteorology; Geography","score_opus":0.01884526915226712,"score_gpt":0.2166162462954073,"score_spread":0.19777097714314018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1633181716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5587652,0.00081126386,0.40306675,0.0009387368,0.00007688312,0.00010497748,0.0007761144,0.00047282124,0.034987222],"genre_scores_gemma":[0.9653707,0.00078157923,0.023915406,0.00011890634,0.00002863116,0.00020493982,0.00018880212,0.00012285798,0.009268216],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999255,0.000022414208,0.000005291961,0.00001356275,0.000019602685,0.000013770803],"domain_scores_gemma":[0.99964964,0.00022263764,0.000057843903,0.000014899669,0.000039813658,0.0000152105595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032286748,0.0004194269,0.0003599416,0.00031615858,0.00033668178,0.00053277443,0.00055433327,0.00068645144,0.0018771868],"category_scores_gemma":[0.00084578356,0.0003309317,0.0008409354,0.00027850267,0.00056293973,0.0006954223,0.0005813144,0.00054611196,0.00018848538],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000066776156,0.000010416336,0.00048365392,0.000016889044,0.00001346743,0.000024230074,0.000020546311,0.99045426,0.0011999918,0.0068514426,0.00009706311,0.0008214466],"study_design_scores_gemma":[0.0000023539753,0.0000024613166,0.00016248682,0.0000017335108,0.0000035134995,0.0000041308276,0.0000051194734,0.9980526,0.0002165804,0.0012923366,0.00025459583,0.0000021600015],"about_ca_topic_score_codex":0.018453786,"about_ca_topic_score_gemma":0.008987127,"teacher_disagreement_score":0.018453786,"about_ca_system_score_codex":0.0009759408,"about_ca_system_score_gemma":0.0006899734,"threshold_uncertainty_score":0.03669274},"labels":[],"label_agreement":null},{"id":"W1634020409","doi":"10.1029/2009gb003765","title":"Simulating the effects of climate and agricultural management practices on global crop yield","year":2011,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change impacts on agriculture","field":"Agricultural and Biological Sciences","cited_by":384,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Environmental science; Crop yield; Sowing; Agriculture; Yield (engineering); Irrigation; Crop simulation model; Crop; Agronomy; DSSAT; Climate change; Precipitation; Agricultural engineering; Geography; Meteorology; Biology; Ecology","score_opus":0.035360263131140206,"score_gpt":0.2652247790480992,"score_spread":0.229864515916959,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1634020409","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9792336,0.00012276144,0.013240571,0.00016943147,0.00003347975,0.000036814945,0.0023499408,0.00017586391,0.004637482],"genre_scores_gemma":[0.99510163,0.000089374706,0.0035665652,0.000025385505,0.0000051222037,0.0000283816,0.0007622413,0.000023316452,0.00039804968],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990606,0.000034648183,0.0000051824563,0.000026728709,0.0000109226,0.000016420723],"domain_scores_gemma":[0.9997676,0.00010844974,0.000039390958,0.000033582295,0.00003281525,0.000018115183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038954127,0.00054179906,0.00019141505,0.00021010054,0.0001870631,0.0003251533,0.0004998068,0.00046247547,0.001182169],"category_scores_gemma":[0.0009233574,0.00019578163,0.0004650517,0.00050684944,0.00017797799,0.00058762275,0.00034166878,0.00034254644,0.00011242894],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030027883,0.00002557717,0.011007407,0.00001993022,0.00003367935,0.000021191525,0.0000143410625,0.98430806,0.0010243449,0.00049372454,0.00026211038,0.0027596292],"study_design_scores_gemma":[0.000026615522,0.00007612574,0.012589411,0.0000047932317,0.000036778278,0.00001187526,0.000030664734,0.98422205,0.0011557755,0.0010029556,0.000831062,0.000011991465],"about_ca_topic_score_codex":0.027931197,"about_ca_topic_score_gemma":0.021752473,"teacher_disagreement_score":0.027931197,"about_ca_system_score_codex":0.0009097951,"about_ca_system_score_gemma":0.0004948442,"threshold_uncertainty_score":0.055537224},"labels":[],"label_agreement":null},{"id":"W1634036610","doi":"10.1029/2001gb001457","title":"Modeling seasonal to annual carbon balance of Mer Bleue Bog, Ontario, Canada","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":202,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Trent University; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Peat; Environmental science; Eddy covariance; Ecosystem respiration; Carbon cycle; Primary production; Bog; Hydrology (agriculture); Soil respiration; Atmospheric sciences; Soil carbon; Ecosystem; Ecology; Soil water; Soil science; Geology","score_opus":0.007115553374584659,"score_gpt":0.19521660841859884,"score_spread":0.18810105504401417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1634036610","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97752964,0.00025211403,0.0024384458,0.00027873207,0.00002528693,0.000068457004,0.0053732754,0.00023804708,0.01379591],"genre_scores_gemma":[0.99127346,0.00015393208,0.0018011346,0.000033937806,0.0000037823565,0.000031449512,0.0019406404,0.00003496312,0.0047265952],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999049,0.000009251342,0.0000037477746,0.000026199601,0.000022229162,0.000033789176],"domain_scores_gemma":[0.9997669,0.000037177717,0.000020174426,0.00000968517,0.00011255096,0.00005360457],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016300942,0.00052118977,0.00032952632,0.00038835328,0.0011657826,0.00073669176,0.0011526077,0.0006082475,0.0032221093],"category_scores_gemma":[0.00053359265,0.00037873338,0.0003823196,0.00058648695,0.00047953095,0.0003404946,0.00033297992,0.00034383291,0.0001975126],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014149373,0.000049684935,0.03867577,0.0000530933,0.000052001276,0.00013086041,0.00012555259,0.95118695,0.0021036332,0.0006877369,0.002453275,0.0043399725],"study_design_scores_gemma":[0.000075289325,0.000028859598,0.027512077,0.000015321386,0.000026393272,0.000016975182,0.00016940002,0.96791327,0.00046112254,0.0002399591,0.0035159534,0.000025360581],"about_ca_topic_score_codex":0.9872766,"about_ca_topic_score_gemma":0.99075377,"teacher_disagreement_score":0.016919434,"about_ca_system_score_codex":0.016919434,"about_ca_system_score_gemma":0.012012527,"threshold_uncertainty_score":0.12275964},"labels":[],"label_agreement":null},{"id":"W1634450063","doi":"10.1029/2007gb003038","title":"Age‐dependent variation in the biophysical properties of boreal forests","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Environmental science; Ecological succession; Evergreen; Deciduous; Taiga; Vegetation (pathology); Boreal; Normalized Difference Vegetation Index; Transect; Atmospheric sciences; Physical geography; Climate change; Leaf area index; Ecology; Geology; Geography; Biology","score_opus":0.010990307829449947,"score_gpt":0.20126079749257972,"score_spread":0.19027048966312976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1634450063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990638,0.00013245657,0.00016953333,0.00000941055,0.0000044713174,0.0000029976752,0.00020674286,0.000007963524,0.00040272842],"genre_scores_gemma":[0.999463,0.000037766757,0.0001352589,0.0000114041195,0.0000031103893,0.000002227294,0.00022632883,0.0000020345435,0.00011891029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984574,0.000022330898,0.0000122163265,0.000056864123,0.000033798657,0.000029078938],"domain_scores_gemma":[0.9993343,0.00008563684,0.00020785288,0.00009036035,0.00016523976,0.000116562216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005160863,0.00016845908,0.0001231205,0.00050877273,0.00023698523,0.00031901983,0.00016003792,0.00012271413,0.0003227262],"category_scores_gemma":[0.0008457313,0.00010709458,0.00011820042,0.0003352015,0.00020983866,0.00028492187,0.00013481372,0.00013730618,0.00005901469],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005746422,0.000022389793,0.9793779,0.000006793426,0.000032625117,0.00004924461,0.00017126191,0.000106692336,0.015735883,0.000028525012,0.000097816424,0.0043133744],"study_design_scores_gemma":[2.5691816e-7,0.000004313114,0.99974734,2.5211816e-7,0.0000019355518,0.000026099768,0.0000150926,0.000044564673,0.00008561025,0.0000035259459,0.000069825226,0.0000010653208],"about_ca_topic_score_codex":0.033714604,"about_ca_topic_score_gemma":0.11164551,"teacher_disagreement_score":0.033714604,"about_ca_system_score_codex":0.00042042427,"about_ca_system_score_gemma":0.00020083424,"threshold_uncertainty_score":0.06703669},"labels":[],"label_agreement":null},{"id":"W1639141565","doi":"10.1029/2008gb003294","title":"Predicting export of dissolved organic carbon from forested catchments in glaciated landscapes with shallow soils","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":143,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University; Ontario Forest Research Institute; Fisheries and Oceans Canada; Environment and Climate Change Canada; Natural Resources Canada; Western University","funders":"","keywords":"Wetland; Hydrology (agriculture); Transect; Environmental science; Surface runoff; Drainage basin; Soil water; Total organic carbon; STREAMS; Dissolved organic carbon; Physical geography; Geology; Soil science; Ecology; Geography","score_opus":0.0076985452092164525,"score_gpt":0.20747497988596922,"score_spread":0.19977643467675277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1639141565","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995435,0.000005652902,0.00038119758,0.000003991848,3.3090413e-7,0.0000016471495,0.000027890099,0.000008681984,0.000027094497],"genre_scores_gemma":[0.99921465,0.000010430727,0.0005211551,0.0000023561095,9.3163135e-7,0.000002792724,0.00018826849,0.0000025527638,0.00005684026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999448,0.000014336822,0.00000338651,0.000016948834,0.000006534869,0.000014014288],"domain_scores_gemma":[0.9998122,0.00009054256,0.000032770866,0.000013323251,0.00001900409,0.00003220783],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002550176,0.00031601515,0.0003138375,0.00026398883,0.0001913563,0.00048152482,0.00019280793,0.00022236313,0.0002515578],"category_scores_gemma":[0.00073832757,0.00018446804,0.00028841884,0.00023919147,0.00020550872,0.000332557,0.0002541346,0.00016075079,0.000049961247],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026360748,0.00020570574,0.75305176,0.00002288747,0.0000935543,0.00017009409,0.000120546356,0.22645402,0.008800582,0.00012779383,0.00012351394,0.010565882],"study_design_scores_gemma":[0.00005200908,0.00007780076,0.43184885,0.000002699795,0.000023956332,0.000036079546,0.000093239454,0.5661476,0.0014022419,0.00019586155,0.0001089107,0.000010782921],"about_ca_topic_score_codex":0.031517927,"about_ca_topic_score_gemma":0.041419685,"teacher_disagreement_score":0.031517927,"about_ca_system_score_codex":0.00068968185,"about_ca_system_score_gemma":0.0003581055,"threshold_uncertainty_score":0.06266892},"labels":[],"label_agreement":null},{"id":"W1641115601","doi":"10.1029/2012gb004342","title":"Biodegradability of dissolved organic carbon in the Yukon River and its tributaries: Seasonality and importance of inorganic nitrogen","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":284,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dissolved organic carbon; Seasonality; Environmental science; Tributary; Arctic; Total organic carbon; Hydrology (agriculture); Oceanography; Environmental chemistry; Ecology; Chemistry; Geology; Geography","score_opus":0.010627596095550583,"score_gpt":0.20871668851033928,"score_spread":0.1980890924147887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1641115601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997372,0.000029526167,0.00003119593,0.0000037896352,3.8400825e-7,0.0000012012871,0.00008893108,0.0000015695645,0.000106238826],"genre_scores_gemma":[0.9995369,0.000029247063,0.00006701203,0.000004195283,3.3136646e-7,0.0000032020116,0.00021250792,0.0000014870075,0.00014512609],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992275,0.000007684565,0.000011241417,0.000029700519,0.000012400657,0.000016290225],"domain_scores_gemma":[0.9997645,0.000032151733,0.000056365872,0.000013307999,0.000088528264,0.000045131463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012541033,0.00016034754,0.00022104893,0.00047626384,0.00046474944,0.000535175,0.00017418638,0.00022518176,0.00027924075],"category_scores_gemma":[0.00026538485,0.00014069729,0.0001972341,0.00094434194,0.00026741272,0.00028730626,0.00032435608,0.00012883992,0.000052517033],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006774987,0.000020078534,0.9844022,0.000022664599,0.000045951758,0.00010161056,0.0004993011,0.00026081532,0.0115553355,0.00003099198,0.000045940982,0.0029474408],"study_design_scores_gemma":[0.000001089041,0.0000127217,0.99858034,0.0000016572669,0.000009491076,0.000033460492,0.00035836693,0.00042174154,0.00045187806,0.00001259736,0.000113731236,0.000003006162],"about_ca_topic_score_codex":0.09432738,"about_ca_topic_score_gemma":0.21243604,"teacher_disagreement_score":0.9056726,"about_ca_system_score_codex":0.00079316547,"about_ca_system_score_gemma":0.00061790546,"threshold_uncertainty_score":0.18755668},"labels":[],"label_agreement":null},{"id":"W1644402576","doi":"10.1029/2002gb002019","title":"Pyrogenic carbon in native grassland soils along a climosequence in North America","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":166,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Soil water; Topsoil; Soil carbon; Environmental science; Silt; Environmental chemistry; Total organic carbon; Biomass (ecology); Transect; Soil pH; Chemistry; Soil science; Agronomy; Ecology; Geology; Biology","score_opus":0.011445885275200561,"score_gpt":0.22427215255366284,"score_spread":0.21282626727846227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1644402576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99982184,0.000036087305,0.000019418023,0.0000044557564,2.3147628e-7,0.0000014544529,0.000032413733,0.0000012181604,0.000082805556],"genre_scores_gemma":[0.9996469,0.000063985746,0.00010690761,0.000007756314,0.0000010716678,0.000004095198,0.0000973962,7.059904e-7,0.00007125421],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999119,0.000014622789,0.0000058868477,0.000037126913,0.000016415102,0.000014049356],"domain_scores_gemma":[0.9997594,0.0000380005,0.00008146469,0.000015011862,0.000055889832,0.00005018712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019096679,0.00017903566,0.00015318202,0.00059065636,0.0004093085,0.00036323463,0.00017480316,0.00015174468,0.00031391706],"category_scores_gemma":[0.00027697874,0.00018222356,0.00010138098,0.0005325845,0.00042603118,0.00022652399,0.00032101973,0.00010280005,0.00004555955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015794055,0.000039133054,0.95353293,0.00006036921,0.00009375516,0.00025613068,0.0013296435,0.00042079663,0.037294634,0.000050593277,0.00006847601,0.0066956207],"study_design_scores_gemma":[0.0000010132709,0.000007061225,0.9997019,9.0123393e-7,0.0000028047114,0.000017046003,0.00009397806,0.00007679722,0.000057149224,0.0000040916175,0.000036375037,7.096096e-7],"about_ca_topic_score_codex":0.07107926,"about_ca_topic_score_gemma":0.1904209,"teacher_disagreement_score":0.07107926,"about_ca_system_score_codex":0.00045915335,"about_ca_system_score_gemma":0.00034459078,"threshold_uncertainty_score":0.14133108},"labels":[],"label_agreement":null},{"id":"W1647882225","doi":"10.1029/2002gb001915","title":"Environmental control of leaf area production: Implications for vegetation and land‐surface modeling","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":153,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Division of Environmental Biology; National Center For Environmental Assessment; University of California, Santa Barbara","keywords":"Leaf area index; Environmental science; Vegetation (pathology); Canopy; Land cover; Atmospheric sciences; Evapotranspiration; Plant cover; Water content; Land use; Agronomy; Ecology","score_opus":0.009177157407932542,"score_gpt":0.208613209885092,"score_spread":0.19943605247715945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1647882225","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.59208244,0.010165824,0.348991,0.01075134,0.00035164814,0.00013114027,0.0025062026,0.00075325096,0.03426714],"genre_scores_gemma":[0.97943044,0.002381405,0.01343955,0.00020953518,0.00012756867,0.00009513999,0.00031189935,0.00012337453,0.0038810712],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998286,0.00008008176,0.000010386456,0.000033498774,0.000026427078,0.000020963158],"domain_scores_gemma":[0.99947876,0.00032027724,0.00006302748,0.000034589182,0.000057533656,0.00004577605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085462077,0.000526389,0.00063371524,0.00038104955,0.0003485358,0.001238733,0.0009744351,0.0011028743,0.002121809],"category_scores_gemma":[0.0024313303,0.00031758143,0.0005955691,0.00082642725,0.00081139605,0.0016919111,0.0006051222,0.000534646,0.00021989593],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002052315,0.000024239534,0.0024153234,0.00004346185,0.000026205238,0.00004271742,0.00003459639,0.96964353,0.0015330864,0.021398325,0.00045839307,0.0043596164],"study_design_scores_gemma":[0.000007991468,0.0000067392652,0.0013697221,0.0000056828835,0.000006270649,0.00000647638,0.0000185663,0.9798289,0.00019310124,0.01771446,0.0008320974,0.000009976282],"about_ca_topic_score_codex":0.020402635,"about_ca_topic_score_gemma":0.011767148,"teacher_disagreement_score":0.020402635,"about_ca_system_score_codex":0.0013080444,"about_ca_system_score_gemma":0.0007266243,"threshold_uncertainty_score":0.040567756},"labels":[],"label_agreement":null},{"id":"W1648603950","doi":"10.1029/2004gb002438","title":"Dissolved organic carbon and dissolved organic nitrogen export from forested watersheds in Nova Scotia: Identifying controlling factors","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Dissolved organic carbon; Environmental science; Nutrient; Watershed; Total organic carbon; Soil carbon; Hydrology (agriculture); Estuary; Biogeochemistry; Nitrate; Soil water; Environmental chemistry; Ecology; Soil science; Oceanography; Chemistry; Geology; Biology","score_opus":0.01119811273810542,"score_gpt":0.22248119985044426,"score_spread":0.21128308711233884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1648603950","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99951506,0.00002461082,0.00006900662,0.000019997675,0.0000012714089,0.0000037181308,0.00015073796,0.0000034738057,0.0002120959],"genre_scores_gemma":[0.99933773,0.000030056246,0.000102758786,0.000008996748,0.0000010305849,0.0000034691311,0.0003119306,0.00000238613,0.00020154816],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998233,0.000028424496,0.000013013236,0.00006234058,0.000023679693,0.000049315648],"domain_scores_gemma":[0.9992374,0.00021067684,0.00015560268,0.000055424887,0.00019033573,0.00015053636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004246479,0.00032955522,0.00023539424,0.00039262147,0.000521038,0.0009081734,0.0003686397,0.0002043962,0.0004497602],"category_scores_gemma":[0.0014390094,0.0002529713,0.00033589377,0.00037325438,0.0005683816,0.00020216354,0.00045229087,0.00026365477,0.00010049699],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005028053,0.000018512386,0.99411076,0.000009180137,0.000042652067,0.00014660454,0.00019013444,0.0029264074,0.0009844408,0.00005577561,0.00009216388,0.001373148],"study_design_scores_gemma":[0.000005747828,0.000011044764,0.9901772,0.000009206885,0.000014127653,0.000034356413,0.00028019145,0.009136129,0.000119661156,0.000037482798,0.00017024901,0.0000045711804],"about_ca_topic_score_codex":0.84692395,"about_ca_topic_score_gemma":0.8839574,"teacher_disagreement_score":0.15307605,"about_ca_system_score_codex":0.004009242,"about_ca_system_score_gemma":0.0025925238,"threshold_uncertainty_score":0.3079551},"labels":[],"label_agreement":null},{"id":"W1656341315","doi":"10.1029/2008gb003416","title":"Groundfish overfishing, diatom decline, and the marine silica cycle: Lessons from Saanich Inlet, Canada, and the Baltic Sea cod crash","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and fisheries research","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Ocean Networks Canada Society; University of Victoria","funders":"","keywords":"Groundfish; Oceanography; Overfishing; Population; Diatom; Environmental science; Gadus; Water column; Fishery; Geology; Biology; Fisheries management; Fishing","score_opus":0.006127424872317376,"score_gpt":0.22917614782445553,"score_spread":0.22304872295213815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1656341315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897878,0.0032489747,0.000036320624,0.0028572876,0.000020883213,0.000008177204,0.00031483057,0.0000038189073,0.0037218856],"genre_scores_gemma":[0.9953962,0.002961822,0.000059443024,0.0004717436,0.00002222105,0.000002422953,0.00023201903,0.0000023875552,0.00085180363],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999,0.000015799873,0.0000049677315,0.000015208668,0.000022456963,0.00004159121],"domain_scores_gemma":[0.99921525,0.00016226163,0.00011081207,0.000029331546,0.00023272316,0.00024957123],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043481763,0.00023763254,0.00024061142,0.0005991431,0.0010226249,0.0010050854,0.00058243325,0.0005490719,0.0014199242],"category_scores_gemma":[0.0015123391,0.00014483806,0.0002102781,0.0010139148,0.0011233178,0.00043146266,0.0005195274,0.0006284689,0.000077746525],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000116309544,0.000044662673,0.9815623,0.00004373879,0.00007337188,0.0008839352,0.001639888,0.00036383755,0.00029118662,0.00037870012,0.0014283314,0.013173591],"study_design_scores_gemma":[0.000010573606,0.000024727924,0.9935455,0.000050099246,0.000039401017,0.000088771834,0.0036025923,0.00034678157,0.000054922286,0.0002766341,0.0019499282,0.000010053829],"about_ca_topic_score_codex":0.9560258,"about_ca_topic_score_gemma":0.97722137,"teacher_disagreement_score":0.04397422,"about_ca_system_score_codex":0.0064577935,"about_ca_system_score_gemma":0.010015864,"threshold_uncertainty_score":0.088466346},"labels":[],"label_agreement":null},{"id":"W1657665316","doi":"10.1029/2002gb001984","title":"Water and carbon cycles in the Mississippi River basin: Potential implications for the Northern Hemisphere residual terrestrial sink","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Johns Hopkins University","keywords":"Environmental science; Eddy covariance; Transpiration; Sink (geography); Evapotranspiration; Interception; Primary production; Hydrology (agriculture); Ecosystem; Carbon sink; Atmospheric sciences; Carbon cycle; Flux (metallurgy); Ecology; Photosynthesis; Chemistry; Geology; Biology","score_opus":0.008011656306265911,"score_gpt":0.21576919554408602,"score_spread":0.20775753923782012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1657665316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96247834,0.007473703,0.0011130619,0.015394145,0.00004693885,0.000010658677,0.0021391094,0.000093446855,0.011250563],"genre_scores_gemma":[0.99579155,0.0023517075,0.00036677704,0.00020705322,0.00003207002,0.00000632021,0.00026654988,0.000011991363,0.0009660197],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999591,0.00000891552,0.0000019409274,0.000010952857,0.0000070752376,0.000012076625],"domain_scores_gemma":[0.9998388,0.000029977113,0.00003581357,0.0000058525075,0.0000405053,0.00004905159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018503016,0.00026250823,0.00020783673,0.0007795057,0.0007753555,0.0013639857,0.00032204387,0.00064319535,0.0032888646],"category_scores_gemma":[0.0005940673,0.0001445628,0.00015408368,0.0011515828,0.0008160896,0.0013951734,0.00068804785,0.00026227432,0.00013755425],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006149798,0.00012416579,0.69230586,0.0007978774,0.00031552193,0.0018592447,0.0024024083,0.047305908,0.024692893,0.0835348,0.015089433,0.13095695],"study_design_scores_gemma":[0.00006283459,0.000099970915,0.80374503,0.00025490712,0.00020148339,0.0002985349,0.0039734147,0.06437046,0.0026980697,0.07914544,0.04504558,0.0001043961],"about_ca_topic_score_codex":0.15192384,"about_ca_topic_score_gemma":0.22662324,"teacher_disagreement_score":0.15192384,"about_ca_system_score_codex":0.0026729552,"about_ca_system_score_gemma":0.0014713171,"threshold_uncertainty_score":0.30207908},"labels":[],"label_agreement":null},{"id":"W1659367893","doi":"10.1029/2006gb002795","title":"Satellite boreal measurements over Alaska and Canada during June–July 2004: Simultaneous measurements of upper tropospheric CO, C<sub>2</sub>H<sub>6</sub>, HCN, CH<sub>3</sub>Cl, CH<sub>4</sub>, C<sub>2</sub>H<sub>2</sub>, CH<sub>3</sub>OH, HCOOH, OCS, and SF<sub>6</sub> mixing ratios","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds De La Recherche Scientifique - FNRS; European Space Agency; Canadian Space Agency; National Oceanic and Atmospheric Administration; National Center for Atmospheric Research","keywords":"Mixing ratio; Troposphere; Boreal; Atmospheric sciences; Environmental science; Atmosphere (unit); Taiga; Latitude; Atmospheric chemistry; Ozone; Climatology; Analytical Chemistry (journal); Chemistry; Environmental chemistry; Meteorology; Geology; Geography","score_opus":0.0074152398573201815,"score_gpt":0.19876298209058144,"score_spread":0.19134774223326126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1659367893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99566805,0.00012268538,0.0001870256,0.000035970468,0.000012885458,0.0000098404025,0.0012221081,0.00003595133,0.002705484],"genre_scores_gemma":[0.99550545,0.00014605402,0.0006313034,0.000041918945,0.000006277947,0.000009894604,0.0022172143,0.000007419973,0.0014344555],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998597,0.000005611493,0.0000054310817,0.000048633527,0.000054495387,0.000026034979],"domain_scores_gemma":[0.9997137,0.000011728203,0.000034341763,0.000012658472,0.00016965235,0.000057807905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015095122,0.0003070573,0.0001751106,0.00035085945,0.0011192407,0.0005313544,0.00023463932,0.00028905694,0.0006148521],"category_scores_gemma":[0.0002468619,0.00019706247,0.00016576322,0.00052499626,0.00031800955,0.00024362278,0.00031159105,0.00025894484,0.00010814718],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008642598,0.00009241463,0.9191365,0.000060001006,0.00017413804,0.00030868076,0.0015209507,0.0017547145,0.061302923,0.00013956682,0.0018370092,0.012808806],"study_design_scores_gemma":[0.000009612346,0.000028084844,0.9928403,0.0000055177484,0.000040040293,0.00007331559,0.0004895651,0.00052667374,0.004052986,0.000015362595,0.0019091803,0.000009291389],"about_ca_topic_score_codex":0.8155034,"about_ca_topic_score_gemma":0.93090475,"teacher_disagreement_score":0.18449658,"about_ca_system_score_codex":0.0032959636,"about_ca_system_score_gemma":0.0020300266,"threshold_uncertainty_score":0.37116623},"labels":[],"label_agreement":null},{"id":"W1662180232","doi":"10.1029/2002gb001866","title":"In situ calcium carbonate dissolution in the Pacific Ocean","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":234,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization; Fisheries and Oceans Canada","funders":"","keywords":"Aragonite; Water column; Alkalinity; Oceanography; Dissolution; Calcium carbonate; Carbonate; Geology; Dissolved organic carbon; Hydrography; Total inorganic carbon; Marine snow; Sediment trap; Ocean acidification; Biogeochemistry; Seawater; Environmental science; Mineralogy; Carbon dioxide; Calcite; Chemistry","score_opus":0.01657827432356887,"score_gpt":0.23257856987354025,"score_spread":0.21600029554997138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1662180232","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99759966,0.00021514636,0.00040610007,0.00002393976,0.0000031363581,0.0000065256013,0.0004955429,0.000010938419,0.0012390835],"genre_scores_gemma":[0.9972466,0.0003243307,0.0010022601,0.00002078534,0.0000044641383,0.000009583197,0.00072878087,0.000010744347,0.0006524363],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998914,0.000009181167,0.000007612428,0.00003674187,0.000034704328,0.000020361811],"domain_scores_gemma":[0.9998628,0.00002985498,0.000038001606,0.000015583442,0.000035690628,0.0000181385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014870528,0.00024334095,0.00023715677,0.0003058311,0.0002491686,0.0004006439,0.0002428607,0.0001942891,0.0004348265],"category_scores_gemma":[0.000361956,0.00021195266,0.00020785337,0.00041511253,0.00018369926,0.00020415407,0.00026948197,0.00030529886,0.00007503861],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006395747,0.00007316882,0.14644301,0.0002096015,0.00013044622,0.00016776516,0.00036329578,0.0026837704,0.8352526,0.00010282043,0.0001596329,0.013774413],"study_design_scores_gemma":[0.000082993494,0.00039018295,0.54434913,0.000029769551,0.00014115515,0.0002765252,0.0004349996,0.019031303,0.43051714,0.00023257353,0.004477326,0.00003693288],"about_ca_topic_score_codex":0.03717001,"about_ca_topic_score_gemma":0.02725612,"teacher_disagreement_score":0.03717001,"about_ca_system_score_codex":0.00047148255,"about_ca_system_score_gemma":0.00031190133,"threshold_uncertainty_score":0.073907316},"labels":[],"label_agreement":null},{"id":"W1662375993","doi":"10.1029/2002gb001983","title":"Interannual variability in the peatland‐atmosphere carbon dioxide exchange at an ombrotrophic bog","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":415,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; Trent University","funders":"","keywords":"Ombrotrophic; Eddy covariance; Peat; Bog; Ecosystem respiration; Carbon dioxide; Environmental science; Atmospheric sciences; Atmosphere (unit); Carbon sink; Carbon cycle; Respiration; Sink (geography); Animal science; Ecosystem; Hydrology (agriculture); Climatology; Chemistry; Ecology; Botany; Meteorology; Geology; Geography; Biology","score_opus":0.008145369816264056,"score_gpt":0.22803424605860134,"score_spread":0.21988887624233727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1662375993","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996649,0.000016792776,0.000031567124,0.000004598646,0.0000014814013,0.0000011900124,0.00011503392,0.0000070040305,0.00015755005],"genre_scores_gemma":[0.9995203,0.000010697805,0.00005232795,0.0000031746297,0.0000012612892,0.0000023339173,0.00024676224,0.0000020447399,0.00016104575],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999255,0.0000070055557,0.000004354696,0.000021918697,0.000015617568,0.00002557194],"domain_scores_gemma":[0.99973685,0.000040971474,0.0000547601,0.000025058785,0.000076599856,0.00006573876],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022928294,0.00015769408,0.000154409,0.00033335347,0.00023618895,0.00028411378,0.00017078548,0.00016777076,0.00030195402],"category_scores_gemma":[0.00039567135,0.00010097498,0.00010475284,0.00018667964,0.0001349018,0.00013559796,0.0001581894,0.0001235507,0.00008223051],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002679982,0.00010052482,0.95142245,0.000018954566,0.00007976876,0.00020784461,0.00060132315,0.0010935718,0.03812601,0.000055526514,0.00049617136,0.0075297435],"study_design_scores_gemma":[0.0000013696151,0.000007626456,0.99908173,0.000001066634,0.000004122967,0.000015214334,0.000028798337,0.0004952387,0.00025500593,0.0000037532234,0.00010412807,0.0000019433378],"about_ca_topic_score_codex":0.085686624,"about_ca_topic_score_gemma":0.18905056,"teacher_disagreement_score":0.085686624,"about_ca_system_score_codex":0.00064550433,"about_ca_system_score_gemma":0.0003044629,"threshold_uncertainty_score":0.17037576},"labels":[],"label_agreement":null},{"id":"W1668805092","doi":"10.1029/2007gb002951","title":"Subglacial methanogenesis: A potential climatic amplifier?","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Carbon cycle; Methane; Methanogenesis; Environmental science; Organic matter; Total organic carbon; Anaerobic oxidation of methane; Blue carbon; Carbon dioxide in Earth's atmosphere; Carbon dioxide; Earth science; Geology; Environmental chemistry; Oceanography; Ecosystem; Carbon sequestration; Climate change; Ecology; Chemistry","score_opus":0.02451161676922147,"score_gpt":0.2558561908836451,"score_spread":0.2313445741144236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1668805092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7938466,0.15187193,0.0139508145,0.018696688,0.0005384512,0.000011244071,0.0008402769,0.000510936,0.019733014],"genre_scores_gemma":[0.9854049,0.012716842,0.0006271674,0.00045140873,0.0002805361,0.0000028769978,0.00013439811,0.000020265394,0.00036167775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984694,0.000032800457,0.000008875346,0.00003849888,0.000027283138,0.00004557629],"domain_scores_gemma":[0.99961436,0.00009274494,0.00012089359,0.00003775547,0.000057977722,0.00007613328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051278016,0.00028785132,0.0004300177,0.00043383572,0.00025376488,0.0011796036,0.00040821315,0.00045844683,0.0015786227],"category_scores_gemma":[0.000925899,0.00014156583,0.0002567833,0.0006624407,0.00068739604,0.0018540139,0.0011625682,0.00060048315,0.00031771502],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012939558,0.00005798804,0.47493678,0.0030809978,0.0008789481,0.0032934914,0.0031410505,0.010096352,0.099697985,0.058898143,0.005104977,0.3395193],"study_design_scores_gemma":[0.000036929534,0.0004744802,0.7616297,0.0005050358,0.0005304,0.0027816934,0.0037516423,0.008413295,0.0103000775,0.09935606,0.112093166,0.00012746613],"about_ca_topic_score_codex":0.001985385,"about_ca_topic_score_gemma":0.0026475994,"teacher_disagreement_score":0.001985385,"about_ca_system_score_codex":0.00045174945,"about_ca_system_score_gemma":0.00043558012,"threshold_uncertainty_score":0.005281031},"labels":[],"label_agreement":null},{"id":"W1669508192","doi":"10.1029/2002gb001949","title":"Biological degradation of methyl chloride in coastal seawater","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Aeronautics and Space Administration","keywords":"Seawater; Sink (geography); Environmental chemistry; Chloride; Halogen; Water column; Environmental science; Degradation (telecommunications); Atmosphere (unit); Chemistry; Oceanography; Geology; Meteorology","score_opus":0.01826297704299787,"score_gpt":0.22970245438979403,"score_spread":0.21143947734679616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1669508192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968568,0.0007189219,0.00045252155,0.00004321066,0.00000993883,0.000014085247,0.000582983,0.000016332364,0.0013052154],"genre_scores_gemma":[0.994055,0.00096651335,0.0013263408,0.000066254834,0.0000055628498,0.000025927462,0.0008471812,0.000012137155,0.002695054],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99980277,0.00001660731,0.000016442202,0.00005590047,0.00007217251,0.000036081317],"domain_scores_gemma":[0.99973303,0.00002568349,0.000059765585,0.000024456507,0.00012592055,0.000031106916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022433978,0.00039503723,0.00024668002,0.0002946932,0.00026149928,0.0005500839,0.000247414,0.00032547585,0.0004165324],"category_scores_gemma":[0.0003052965,0.00017544237,0.00031315096,0.00026778647,0.00022715163,0.00016542376,0.00029912544,0.00027285403,0.00030788628],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001237521,0.000014726728,0.011870293,0.00007275733,0.000010207505,0.00006655145,0.000063115076,0.0002602992,0.9838118,0.000023543482,0.00006332072,0.0036195999],"study_design_scores_gemma":[0.00002531454,0.00092668884,0.1820705,0.000034154153,0.000037049103,0.00023938922,0.0004326589,0.002688752,0.81078583,0.000064709566,0.0026652063,0.000029914765],"about_ca_topic_score_codex":0.042996343,"about_ca_topic_score_gemma":0.035482112,"teacher_disagreement_score":0.042996343,"about_ca_system_score_codex":0.0010631715,"about_ca_system_score_gemma":0.00052191754,"threshold_uncertainty_score":0.085492134},"labels":[],"label_agreement":null},{"id":"W1670370105","doi":"10.1002/2014gb004845","title":"Climate change reduces the capacity of northern peatlands to absorb the atmospheric carbon dioxide: The different responses of bogs and fens","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; Memorial University of Newfoundland","funders":"","keywords":"Peat; Bog; Carbon dioxide; Environmental science; Carbon dioxide in Earth's atmosphere; Climate change; Physical geography; Hydrology (agriculture); Atmospheric sciences; Ecology; Geology; Oceanography; Geography","score_opus":0.013268013233153304,"score_gpt":0.22517054881456058,"score_spread":0.2119025355814073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1670370105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995214,0.000018599692,0.000056425088,0.000010974468,0.0000010236466,0.0000012676686,0.000041830357,0.000007592938,0.0003408248],"genre_scores_gemma":[0.9997123,0.000019034258,0.000066231,0.00000749318,5.611128e-7,0.0000020584425,0.000060762144,0.0000022371898,0.00012924052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990606,0.000016075392,0.0000035823816,0.00001823181,0.000008865532,0.0000471655],"domain_scores_gemma":[0.999788,0.00004423882,0.000032033982,0.00001815322,0.00003561275,0.00008192999],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024732767,0.0002119882,0.00027484298,0.00021393201,0.0003168801,0.00049405877,0.00024558668,0.0002577001,0.0009222641],"category_scores_gemma":[0.00057817466,0.00013573184,0.00039028673,0.00020391964,0.00038094458,0.0002389118,0.00032958697,0.00017132975,0.00006377389],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012896345,0.00020954145,0.57376057,0.00016035486,0.00030704288,0.0006797546,0.0005523592,0.236838,0.16868742,0.0013024543,0.0008245695,0.01538824],"study_design_scores_gemma":[0.000030950847,0.00015138923,0.9084868,0.000015961528,0.000058257363,0.00012641193,0.0009710988,0.082229935,0.0060380534,0.0006181908,0.0012443323,0.000028500235],"about_ca_topic_score_codex":0.092476845,"about_ca_topic_score_gemma":0.1062604,"teacher_disagreement_score":0.092476845,"about_ca_system_score_codex":0.0010440089,"about_ca_system_score_gemma":0.0006651379,"threshold_uncertainty_score":0.18387711},"labels":[],"label_agreement":null},{"id":"W1670565333","doi":"10.1029/2002gb001956","title":"How surface fire in Siberian Scots pine forests affects soil organic carbon in the forest floor: Stocks, molecular structure, and conversion to black carbon (charcoal)","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":191,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Sport Centre Pacific; Natural Resources Canada","funders":"","keywords":"Scots pine; Forest floor; Environmental chemistry; Environmental science; Taiga; Soil carbon; Total organic carbon; Carbon fibers; Charcoal; Chemistry; Forestry; Soil water; Soil science; Botany; Organic chemistry; Materials science","score_opus":0.0035761071436303587,"score_gpt":0.19083200649447313,"score_spread":0.18725589935084277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1670565333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99982697,0.00004774105,0.000018323131,0.00000513943,0.000001405121,7.4611177e-7,0.000041124284,0.0000013302746,0.000057258832],"genre_scores_gemma":[0.99967253,0.000051544674,0.000029944586,0.000013538116,0.0000013388068,0.0000022301099,0.00011253775,0.00000100741,0.00011541215],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99994504,0.000008873584,0.0000051721263,0.000018603725,0.0000072073653,0.000015236587],"domain_scores_gemma":[0.99991095,0.000012557338,0.00002433438,0.0000065810527,0.000009612486,0.000035958976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015335783,0.00024604183,0.00022253962,0.00017470251,0.00026176145,0.00025723982,0.00012431294,0.00020707714,0.0005152318],"category_scores_gemma":[0.00013837648,0.00011190101,0.00024736466,0.00017899672,0.000253028,0.00014942179,0.00017186825,0.00019384851,0.000078075806],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015997216,0.00024064288,0.65861285,0.00010850717,0.0002876916,0.00048713275,0.0004269783,0.0015604096,0.32359686,0.00006047431,0.00012863199,0.012890172],"study_design_scores_gemma":[0.0000022928816,0.00004147861,0.998271,8.9417273e-7,0.000009659608,0.000023209837,0.00005869046,0.00029281017,0.0012581563,0.000011314776,0.000028742905,0.0000017599189],"about_ca_topic_score_codex":0.016873382,"about_ca_topic_score_gemma":0.018149506,"teacher_disagreement_score":0.016873382,"about_ca_system_score_codex":0.000402919,"about_ca_system_score_gemma":0.00019205235,"threshold_uncertainty_score":0.033550322},"labels":[],"label_agreement":null},{"id":"W1670975376","doi":"10.1029/2007gb002935","title":"Simulating the effects of past changes in climate, atmospheric composition, and fire disturbance on soil carbon in Canada's forests and wetlands","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Canadian Foundation for Climate and Atmospheric Sciences; BIOCAP Canada","keywords":"Environmental science; Wetland; Taiga; Soil water; Boreal; Ecosystem; Soil carbon; Deposition (geology); Climate change; Carbon cycle; Peat; Terrestrial ecosystem; Hydrology (agriculture); Ecology; Forestry; Soil science; Geology; Geography; Oceanography","score_opus":0.005134139320864758,"score_gpt":0.1863947045845698,"score_spread":0.18126056526370504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1670975376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957675,0.0000815743,0.00036205075,0.00011168935,0.000011099643,0.000021620335,0.0014853772,0.000063471925,0.0020955987],"genre_scores_gemma":[0.9970962,0.00009114976,0.00079158996,0.000031818323,0.0000023408338,0.00001695809,0.0011976671,0.000009787839,0.0007623672],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998555,0.000017254864,0.0000047134763,0.000025769914,0.000020784819,0.00007592011],"domain_scores_gemma":[0.9996024,0.00010002944,0.0000342241,0.00001646839,0.0001181587,0.0001287446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002933566,0.0008508879,0.00045343416,0.0005218489,0.0012351702,0.000821074,0.0013064564,0.0008259432,0.0014846001],"category_scores_gemma":[0.0007003983,0.0005234393,0.00076539983,0.0008408068,0.0008304034,0.00034550182,0.00040693022,0.000702795,0.00009204435],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024987332,0.000101061785,0.038811937,0.00004150634,0.0000944338,0.00013028373,0.000061518906,0.9552439,0.0014716813,0.0004656796,0.0008394969,0.0024886033],"study_design_scores_gemma":[0.0002081077,0.00008893041,0.045918137,0.000011908665,0.000091100905,0.000026941781,0.0002093065,0.95127493,0.0009705139,0.00022668322,0.00093501626,0.000038313727],"about_ca_topic_score_codex":0.9597331,"about_ca_topic_score_gemma":0.95360774,"teacher_disagreement_score":0.04026687,"about_ca_system_score_codex":0.014158608,"about_ca_system_score_gemma":0.010179392,"threshold_uncertainty_score":0.10272837},"labels":[],"label_agreement":null},{"id":"W1671783768","doi":"10.1029/2008gb003398","title":"Characterizing uncertainty in modeling primary terrestrial ecosystem processes","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University; University of Victoria","funders":"","keywords":"Environmental science; Terrestrial ecosystem; Carbon cycle; Forcing (mathematics); Ecosystem; Atmospheric sciences; Climate model; Climate change; Range (aeronautics); Radiative forcing; Primary production; Climatology; Global warming; Atmospheric model; Ecology; Meteorology; Geology; Geography; Biology","score_opus":0.008913049495962168,"score_gpt":0.2144371796802685,"score_spread":0.20552413018430635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1671783768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7080344,0.0006510726,0.28431222,0.0004910031,0.000029157265,0.000047926773,0.00042055454,0.00022790872,0.0057858573],"genre_scores_gemma":[0.99075705,0.00016150424,0.008728698,0.000022963304,0.000009553068,0.00002574291,0.00009142604,0.000016251586,0.0001868511],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989281,0.00057034864,0.000052837866,0.00012159972,0.00021871757,0.00010824311],"domain_scores_gemma":[0.9926481,0.0060368474,0.00056577363,0.0004318193,0.0002222884,0.00009518348],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026759836,0.0005819313,0.00046494353,0.0005107954,0.0003434406,0.0012018438,0.00076638185,0.00085658353,0.00053120375],"category_scores_gemma":[0.016831163,0.0004016931,0.00055032986,0.0006968819,0.0007763156,0.0018188598,0.0010724942,0.0006797418,0.000055889137],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026681031,0.000011979838,0.004004757,0.000029195708,0.000032953023,0.000041522584,0.000061054794,0.9825881,0.00057755155,0.009868751,0.00008139518,0.0026759622],"study_design_scores_gemma":[0.0000047779176,0.000015131528,0.00077538984,0.000008626398,0.00001073807,0.000015450585,0.00002361622,0.9783959,0.00040552524,0.02004127,0.00029682022,0.000006743324],"about_ca_topic_score_codex":0.0049263895,"about_ca_topic_score_gemma":0.0024415802,"teacher_disagreement_score":0.0049263895,"about_ca_system_score_codex":0.0009048864,"about_ca_system_score_gemma":0.00062079204,"threshold_uncertainty_score":0.01415211},"labels":[],"label_agreement":null},{"id":"W1674831397","doi":"10.1029/2005gb002514","title":"Estimating changes in global vegetation cover (1850–2100) for use in climate models","year":2006,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Alberta Ministry of Agriculture and Forestry; Natural Resources Canada; Pacific Institute for Climate Solutions; University of Victoria; University of Alberta","funders":"Canadian Forest Service; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Biosphere; Environmental science; Vegetation (pathology); Land cover; Biosphere model; Climatology; Physical geography; Grassland; Climate change; Land use; Geography; Ecology; Geology","score_opus":0.01183034882074371,"score_gpt":0.23075927274864103,"score_spread":0.2189289239278973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1674831397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9614348,0.00026501314,0.020784121,0.00006888686,0.000041877498,0.00006591951,0.014253042,0.00035931822,0.0027270266],"genre_scores_gemma":[0.96265715,0.00019440865,0.021879474,0.000020115518,0.0000150865035,0.000113169604,0.014762881,0.00005272601,0.00030504752],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998416,0.00004088848,0.000013713597,0.000046006582,0.000031722917,0.000026121153],"domain_scores_gemma":[0.9997266,0.000087727676,0.000049955845,0.00005985441,0.000052038828,0.000023755865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00084053125,0.0005449127,0.0003803921,0.0015716681,0.00033925864,0.00043842703,0.00050511,0.00038024562,0.0010778122],"category_scores_gemma":[0.0019665398,0.00045517055,0.000759949,0.0018456894,0.00018905343,0.0006682494,0.00050988747,0.0003194624,0.00031497562],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002537926,0.00024206436,0.36839482,0.00025659095,0.00071583304,0.00019263095,0.00024704117,0.5552806,0.006901002,0.0027068588,0.0038332632,0.060975444],"study_design_scores_gemma":[0.00007935716,0.00017100132,0.45916653,0.00004877578,0.00016607021,0.0002482576,0.0001626095,0.5220412,0.0067627435,0.0028069848,0.008266375,0.00008001764],"about_ca_topic_score_codex":0.02988796,"about_ca_topic_score_gemma":0.05078292,"teacher_disagreement_score":0.02988796,"about_ca_system_score_codex":0.0011386285,"about_ca_system_score_gemma":0.0007432236,"threshold_uncertainty_score":0.059428036},"labels":[],"label_agreement":null},{"id":"W1675752274","doi":"10.1029/2011gb004047","title":"Nitrogen enrichment and the emission of nitrous oxide from streams","year":2011,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":162,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo; Université de Montréal; Trent University; University of Saskatchewan","funders":"","keywords":"STREAMS; Nitrous oxide; Environmental science; Nitrate; Greenhouse gas; Hydrology (agriculture); Nitrogen; Nitrogen cycle; Aquatic ecosystem; Ecosystem; Environmental chemistry; Atmospheric sciences; Ecology; Chemistry; Oceanography; Geology","score_opus":0.008223260155157031,"score_gpt":0.19920104541377623,"score_spread":0.1909777852586192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1675752274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986492,0.00028693597,0.0001612321,0.000017214863,0.0000021968422,0.0000048648935,0.0003684078,0.000004846348,0.00050520047],"genre_scores_gemma":[0.99842787,0.00032478236,0.00027734076,0.000015002524,0.000004857567,0.000006770582,0.00060313405,0.000002866495,0.00033728636],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998524,0.000016345974,0.000009312535,0.000046652993,0.000050597755,0.000024580486],"domain_scores_gemma":[0.9995473,0.00006338463,0.00019107542,0.00000801452,0.00013062636,0.000059558086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021771272,0.0002520019,0.00016157568,0.0004899262,0.00051447947,0.0007293035,0.00022652722,0.00020118056,0.00043434493],"category_scores_gemma":[0.000552332,0.00016270678,0.00011942957,0.0007877155,0.00034974056,0.00025703094,0.00022876414,0.00020010083,0.00008260501],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015228125,0.00002272593,0.9858064,0.000023897224,0.000046747016,0.000081122074,0.00015647699,0.0005119062,0.010615586,0.000039962273,0.000105036444,0.0024377506],"study_design_scores_gemma":[0.0000022497038,0.000020708814,0.99696356,0.0000064633696,0.000012013197,0.000039042727,0.000089214365,0.00083218457,0.0016253412,0.000058800088,0.00034724112,0.0000031301138],"about_ca_topic_score_codex":0.15687628,"about_ca_topic_score_gemma":0.3016087,"teacher_disagreement_score":0.15687628,"about_ca_system_score_codex":0.0020752747,"about_ca_system_score_gemma":0.001012492,"threshold_uncertainty_score":0.3119263},"labels":[],"label_agreement":null},{"id":"W1678752961","doi":"10.1029/2008gb003297","title":"The<i>p</i>CO<sub>2</sub>dynamics in lakes in the boreal region of northern Québec, Canada","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Boreal; Environmental science; Trophic level; Dissolved organic carbon; Lake ecosystem; Co-occurrence; Precipitation; Drainage basin; Ecology; Water quality; Phytoplankton; Chlorophyll a; Taiga; Physical geography; Hydrology (agriculture); Ecosystem; Nutrient; Geology; Geography; Chemistry; Biology","score_opus":0.004966513049100617,"score_gpt":0.18066429675062254,"score_spread":0.17569778370152192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1678752961","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99850684,0.00012615266,0.00012297652,0.000063673855,0.0000014579387,0.000006145748,0.00059176993,0.000010812602,0.00057013746],"genre_scores_gemma":[0.9992224,0.000051268453,0.00011389101,0.000019651548,9.616474e-7,0.000003494463,0.00032182774,0.0000036012516,0.000262832],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998878,0.00001197689,0.0000046915284,0.000027364906,0.000021869846,0.000046402034],"domain_scores_gemma":[0.9995864,0.00004694623,0.000096694544,0.000015583993,0.000183202,0.000071330796],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020096738,0.00020860128,0.00019746723,0.0005998671,0.0010126893,0.00080017815,0.00038197736,0.00019943075,0.0008798523],"category_scores_gemma":[0.0005310172,0.00012819532,0.00019982913,0.0011347083,0.00047764095,0.00025114368,0.00028229234,0.00017498192,0.00007391338],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096700714,0.000025125724,0.98322713,0.000033703058,0.00010083401,0.00013131407,0.0007220877,0.0029068596,0.0034658588,0.00015609853,0.0010239306,0.008110254],"study_design_scores_gemma":[0.0000034716772,0.0000061728833,0.99607927,0.0000039189927,0.000013226412,0.000021492164,0.00033226234,0.002904442,0.0001403367,0.000021828202,0.00046758537,0.0000060497086],"about_ca_topic_score_codex":0.9873374,"about_ca_topic_score_gemma":0.9936219,"teacher_disagreement_score":0.01266259,"about_ca_system_score_codex":0.010746532,"about_ca_system_score_gemma":0.004549015,"threshold_uncertainty_score":0.077971935},"labels":[],"label_agreement":null},{"id":"W1680801808","doi":"10.1029/2006gb002866","title":"Variation in methane production pathways associated with permafrost decomposition in collapse scar bogs of Alberta, Canada","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Permafrost; Methanogenesis; Sphagnum; Organic matter; Environmental chemistry; Environmental science; Peat; Vegetation (pathology); Bog; Ecology; Methane; Chemistry; Biology","score_opus":0.005276921240847056,"score_gpt":0.21097824750279165,"score_spread":0.2057013262619446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1680801808","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989644,0.00008862385,0.000063947,0.000015767428,0.0000013513575,0.0000042237593,0.0003439098,0.0000067553437,0.00051097356],"genre_scores_gemma":[0.9986644,0.000060458005,0.0001402441,0.000010154047,7.327205e-7,0.0000030518142,0.00049403554,0.0000032885575,0.000623646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980956,0.00001566507,0.000006368058,0.00003661434,0.000058077152,0.00007383079],"domain_scores_gemma":[0.9996026,0.000028148117,0.000059927745,0.000012689286,0.00018273697,0.00011387362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017861126,0.00021577325,0.00019011163,0.0011640242,0.00087035587,0.00052459113,0.0003265301,0.0001945822,0.00071592425],"category_scores_gemma":[0.00039625113,0.00017717642,0.00014549127,0.0010153658,0.0005266969,0.00010336319,0.00031086055,0.00015239573,0.00010606707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024870355,0.000027077984,0.97819316,0.00001724237,0.00005025069,0.00018873082,0.0012381608,0.00041349384,0.012263873,0.00011728043,0.00032881825,0.006913194],"study_design_scores_gemma":[0.0000011989465,0.0000042774327,0.9992567,0.0000025747931,0.0000029402709,0.000020184409,0.0002775911,0.0001385512,0.00012109664,0.000007413542,0.00016550512,0.0000020506734],"about_ca_topic_score_codex":0.95462817,"about_ca_topic_score_gemma":0.9892335,"teacher_disagreement_score":0.04537183,"about_ca_system_score_codex":0.006920879,"about_ca_system_score_gemma":0.00352734,"threshold_uncertainty_score":0.09127802},"labels":[],"label_agreement":null},{"id":"W1689144894","doi":"10.1029/2011gb004249","title":"Predictability of biomass burning in response to climate changes","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":429,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; University of Calgary; Canadian Forest Service","funders":"Natural Environment Research Council; Sight Research UK; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Environmental science; Biomass (ecology); Predictability; Biomass burning; Climatology; Climate change; Charcoal; Moisture; Atmospheric sciences; Global warming; Meteorology; Aerosol; Geology; Geography; Oceanography","score_opus":0.008819101219117711,"score_gpt":0.24523485681450705,"score_spread":0.23641575559538933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1689144894","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979722,0.000087273824,0.00059576886,0.00015708808,0.0000101530195,0.0000031895381,0.0002450348,0.0000322526,0.0008969734],"genre_scores_gemma":[0.999703,0.0000293495,0.000052806387,0.000011309932,0.000008407483,0.0000012561163,0.00013091424,0.0000042461543,0.000058665675],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99979025,0.00004668686,0.00001710462,0.00006187186,0.00003683203,0.000047265214],"domain_scores_gemma":[0.99837863,0.00067672535,0.00048553664,0.00017650035,0.00012584317,0.00015670668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077463506,0.00017244555,0.0002831862,0.0004550228,0.000277086,0.0010111613,0.00020057934,0.00032534433,0.00075184857],"category_scores_gemma":[0.0032529132,0.00021980831,0.00028535927,0.00036691103,0.00039640206,0.00040849225,0.00042129788,0.0005195856,0.00017388436],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019040566,0.000055198914,0.94739354,0.000018356252,0.00016644104,0.0001666545,0.00010614128,0.040722292,0.0038391836,0.0010217669,0.0005336198,0.005786444],"study_design_scores_gemma":[0.000006749365,0.000023796292,0.94075173,0.0000050306535,0.000017357534,0.0000582925,0.00007291582,0.056678273,0.00043663126,0.0015879597,0.00034606518,0.000015209278],"about_ca_topic_score_codex":0.005598031,"about_ca_topic_score_gemma":0.006163074,"teacher_disagreement_score":0.005598031,"about_ca_system_score_codex":0.00042166273,"about_ca_system_score_gemma":0.00025603376,"threshold_uncertainty_score":0.011130929},"labels":[],"label_agreement":null},{"id":"W1696369099","doi":"10.1029/2001gb001415","title":"Can CFCs be used to determine anthropogenic CO<sub>2</sub>?","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization; Fisheries and Oceans Canada","funders":"","keywords":"Ocean gyre; Environmental science; Upwelling; Subtropics; Water column; Oceanography; Pacific ocean; Atmospheric sciences; Climatology; Geology; Ecology; Biology","score_opus":0.010928599707111035,"score_gpt":0.2302758421344827,"score_spread":0.21934724242737166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1696369099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8911893,0.0007357262,0.080481336,0.0014097648,0.00029888653,0.00010368998,0.005601652,0.0030698106,0.017109836],"genre_scores_gemma":[0.9823477,0.00016657867,0.015754974,0.0001079682,0.000028090668,0.00003918338,0.0007788556,0.0001610155,0.00061563036],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99970764,0.00007022139,0.000014712001,0.00006168095,0.00009634808,0.000049428356],"domain_scores_gemma":[0.9972652,0.0008454304,0.00055889454,0.0002522223,0.0009630028,0.000115326984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012417773,0.0007840983,0.00044708783,0.0008230814,0.00028917988,0.00082617224,0.00077950646,0.0008977776,0.0010535918],"category_scores_gemma":[0.008010648,0.00047717587,0.00037398667,0.0007985952,0.00048849254,0.0011607341,0.0003132671,0.00044721333,0.0004561326],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002188822,0.000067819936,0.15934534,0.00009796779,0.00013510107,0.000057184607,0.000052698164,0.7834054,0.0052792714,0.0025049683,0.0026679658,0.046167377],"study_design_scores_gemma":[0.000031043928,0.00001761413,0.021440279,0.00002001365,0.000027634855,0.000013385728,0.000021327614,0.9695463,0.004901159,0.0014227153,0.0025111747,0.000047293557],"about_ca_topic_score_codex":0.13971767,"about_ca_topic_score_gemma":0.11310272,"teacher_disagreement_score":0.13971767,"about_ca_system_score_codex":0.0018215853,"about_ca_system_score_gemma":0.0017250552,"threshold_uncertainty_score":0.27780885},"labels":[],"label_agreement":null},{"id":"W1724974053","doi":"10.1029/2007gb003029","title":"Seasonal cycle of O<sub>2</sub> and <i>p</i>CO<sub>2</sub> in the central Labrador Sea: Atmospheric, biological, and physical implications","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sink (geography); Mixed layer; Environmental science; Oceanography; Bloom; Atmospheric sciences; Spring bloom; Carbon cycle; Phytoplankton; Geology; Chemistry; Ecosystem; Nutrient; Ecology; Geography","score_opus":0.010397318723574307,"score_gpt":0.20703699910472426,"score_spread":0.19663968038114996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1724974053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990024,0.000067161614,0.000042488213,0.000024061856,0.0000024338678,0.0000016028018,0.00046215867,0.000024134342,0.00037354237],"genre_scores_gemma":[0.9989858,0.000044683795,0.00008123137,0.000017985316,0.0000036072868,0.000003117238,0.0006573259,0.0000056208514,0.0002005002],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995005,0.0000043283217,0.0000053823182,0.000015329317,0.00000790381,0.000017003533],"domain_scores_gemma":[0.99982494,0.000011021943,0.00007949267,0.000011310299,0.000037972415,0.000035267192],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000108875836,0.00021069434,0.00018673485,0.00057787413,0.0002620159,0.00057005347,0.0002365811,0.00019815094,0.00074523455],"category_scores_gemma":[0.00019608223,0.00014080358,0.00021283762,0.0006336585,0.00021908186,0.00024269658,0.00026891657,0.00012541367,0.00012567261],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003690856,0.000049531536,0.96295166,0.000081971135,0.00017432409,0.00019945264,0.00034529355,0.0028155325,0.016267374,0.0001291194,0.0012383871,0.015378188],"study_design_scores_gemma":[0.0000034893421,0.000017279386,0.9977324,0.0000034412028,0.000017458611,0.000030064968,0.000106230116,0.00071990513,0.0008495177,0.00001214372,0.00050332956,0.0000046773266],"about_ca_topic_score_codex":0.09541441,"about_ca_topic_score_gemma":0.1294792,"teacher_disagreement_score":0.9045856,"about_ca_system_score_codex":0.0009486073,"about_ca_system_score_gemma":0.00043059775,"threshold_uncertainty_score":0.18971807},"labels":[],"label_agreement":null},{"id":"W1728787300","doi":"10.1029/2012gb004349","title":"Biological productivity along Line P in the subarctic northeast Pacific: In situ versus incubation‐based methods","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Subarctic climate; Productivity; Incubation; Primary production; Environmental science; In situ; Mixed layer; Primary productivity; New production; Oceanography; Chemistry; Animal science; Atmospheric sciences; Nutrient; Biology; Phytoplankton; Ecology; Geology; Ecosystem","score_opus":0.037326726556312625,"score_gpt":0.2842729646621794,"score_spread":0.24694623810586674,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1728787300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966987,0.00022734901,0.0016554305,0.000006629222,0.000005193396,0.000013727266,0.00041697352,0.000021363196,0.00095456565],"genre_scores_gemma":[0.99437886,0.00034505408,0.0038438379,0.00002007489,0.00001163209,0.000054653785,0.00069139083,0.000018622271,0.00063601247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981385,0.000022739274,0.000009587255,0.00010444495,0.00003365968,0.00001580002],"domain_scores_gemma":[0.99964786,0.00005973098,0.00014557429,0.000027263872,0.00007213051,0.000047418205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024346742,0.000523567,0.00020564828,0.00065320585,0.0003581325,0.00046713784,0.00034075844,0.0002196432,0.00038159246],"category_scores_gemma":[0.00038911094,0.00031042667,0.0001684175,0.0008324764,0.00029290194,0.000276979,0.00032470725,0.0002371794,0.00012403408],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003093857,0.00007989457,0.7333406,0.00011654395,0.00015767674,0.00019152663,0.0007234425,0.0012565351,0.24936877,0.000051908282,0.000062812134,0.014340915],"study_design_scores_gemma":[0.0000036469648,0.00004789237,0.9902147,0.0000032453859,0.000037624974,0.0000493781,0.00011489559,0.001056178,0.008142153,0.000017941918,0.00030717818,0.000005162578],"about_ca_topic_score_codex":0.029283773,"about_ca_topic_score_gemma":0.060121655,"teacher_disagreement_score":0.029283773,"about_ca_system_score_codex":0.0005679035,"about_ca_system_score_gemma":0.00031491645,"threshold_uncertainty_score":0.058226645},"labels":[],"label_agreement":null},{"id":"W1773228276","doi":"10.1002/2012gb004536","title":"National‐scale estimates of forest root biomass carbon stocks and associated carbon fluxes in Canada","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Canadian Forest Service","funders":"Australian Government","keywords":"Primary production; Environmental science; Biomass (ecology); Carbon cycle; Carbon sequestration; Carbon fibers; Ecosystem; Atmosphere (unit); Forestry; Atmospheric sciences; Agronomy; Carbon dioxide; Ecology; Biology; Geography; Mathematics; Geology","score_opus":0.003987288057634833,"score_gpt":0.18694409607524634,"score_spread":0.1829568080176115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1773228276","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96355903,0.0013264586,0.0012645966,0.00018264499,0.000008617921,0.000027028584,0.02674343,0.00011627328,0.006771878],"genre_scores_gemma":[0.98772275,0.0006431961,0.0015253518,0.0000440416,0.0000033441986,0.00001371655,0.0079906555,0.000013725305,0.0020432272],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997998,0.000008382826,0.000009356643,0.000043326698,0.000091602335,0.000047511745],"domain_scores_gemma":[0.99886084,0.000056393605,0.00009636237,0.000025557385,0.0008770092,0.00008396711],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028910823,0.0003651433,0.00019917836,0.0018015862,0.0008748644,0.00079019275,0.00046359218,0.00019079552,0.0011729314],"category_scores_gemma":[0.00089756504,0.00019112218,0.00036812612,0.0029395628,0.00018282747,0.00030238734,0.0003806643,0.00026170205,0.00017162996],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009042193,0.00003462016,0.94378084,0.00014774811,0.00027257574,0.00011143321,0.00042967618,0.013379563,0.0020410814,0.0009898932,0.0062563205,0.032465894],"study_design_scores_gemma":[0.000005987857,0.0000045359006,0.9854292,0.000039116996,0.000038568134,0.000022695514,0.0002366012,0.008861168,0.00038778232,0.00011396149,0.0048430976,0.000017323846],"about_ca_topic_score_codex":0.995717,"about_ca_topic_score_gemma":0.99687,"teacher_disagreement_score":0.019623289,"about_ca_system_score_codex":0.019623289,"about_ca_system_score_gemma":0.013796799,"threshold_uncertainty_score":0.14237756},"labels":[],"label_agreement":null},{"id":"W1776313780","doi":"10.1029/2005gb002593","title":"Source and transport of terrigenous organic matter in the upper Yukon River: Evidence from isotope (δ<sup>13</sup>C, Δ<sup>14</sup>C, and δ<sup>15</sup>N) composition of dissolved, colloidal, and particulate phases","year":2006,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":308,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"Cold Regions Research and Engineering Laboratory","keywords":"Terrigenous sediment; Dissolved organic carbon; Organic matter; Total organic carbon; Environmental chemistry; Particulates; Chemistry; Isotopes of nitrogen; Isotopes of carbon; Stable isotope ratio; Nitrogen; Mineralogy; Geology; Sediment","score_opus":0.0066994146393838105,"score_gpt":0.1927016062961711,"score_spread":0.1860021916567873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1776313780","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996754,0.00006276209,0.000027998574,0.000007870864,4.6189717e-7,0.0000015404695,0.00009291713,0.0000021368603,0.00012878557],"genre_scores_gemma":[0.99923193,0.00011660264,0.00012666661,0.000014142039,7.7992536e-7,0.0000058297205,0.00027435235,0.0000024034941,0.00022711231],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999182,0.0000045714946,0.000009290793,0.000029733117,0.00001493885,0.000023277042],"domain_scores_gemma":[0.99985695,0.0000149593325,0.000029831497,0.0000055569344,0.00005447118,0.00003825293],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008552174,0.00019059442,0.0002572798,0.0005146418,0.0006714406,0.00061573327,0.00023195673,0.00037138208,0.00035570693],"category_scores_gemma":[0.00014984526,0.00028222235,0.00018349216,0.00073791924,0.00029943016,0.00031521084,0.00046897185,0.0001997535,0.000085541804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015171761,0.00003616489,0.8375552,0.00010902004,0.00007556684,0.00046151364,0.0009979886,0.00041153352,0.15207545,0.00011113869,0.00009915395,0.007915563],"study_design_scores_gemma":[0.0000027629972,0.000019585736,0.997414,0.000004390039,0.000013067398,0.000058286587,0.0005185014,0.0003191097,0.0013945439,0.000015238993,0.00023469076,0.0000057490274],"about_ca_topic_score_codex":0.14125173,"about_ca_topic_score_gemma":0.22353226,"teacher_disagreement_score":0.85874826,"about_ca_system_score_codex":0.0011215354,"about_ca_system_score_gemma":0.001058501,"threshold_uncertainty_score":0.2808591},"labels":[],"label_agreement":null},{"id":"W1776877885","doi":"10.1029/2005gb002457","title":"Carbon dioxide and methane emissions and the carbon budget of a 10‐year old tropical reservoir (Petit Saut, French Guiana)","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":489,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hydro-Québec","funders":"","keywords":"Carbon dioxide; Environmental science; Hydrology (agriculture); Methane; Flux (metallurgy); Estuary; Total inorganic carbon; Discharge; Environmental chemistry; Chemistry; Oceanography; Drainage basin; Geology","score_opus":0.004993542802437694,"score_gpt":0.2082273329580143,"score_spread":0.2032337901555766,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1776877885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997403,0.000015342084,0.000017887041,0.000012315925,2.5876426e-7,0.0000014768888,0.000076004806,0.0000037766874,0.00013262099],"genre_scores_gemma":[0.9995952,0.00002007447,0.00006870686,0.0000054457523,7.2874474e-7,0.000002864957,0.0001337773,0.0000015378506,0.00017171007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999318,0.00001429554,0.0000029957994,0.000018260294,0.000009217808,0.00002350839],"domain_scores_gemma":[0.9998549,0.00002887837,0.000034543773,0.000010974843,0.000027942777,0.000042735268],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017515905,0.0003259752,0.00013320034,0.0005409484,0.0005846215,0.00044814148,0.0004393244,0.00036531183,0.00085717876],"category_scores_gemma":[0.00022227579,0.00020427832,0.00024390839,0.00044755387,0.0003740152,0.00027548522,0.00030496402,0.00019361298,0.00016022788],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003411875,0.00018849621,0.9539107,0.000020277723,0.00009721024,0.0022480313,0.0013591221,0.0022826355,0.032673012,0.000114619565,0.00024541555,0.0065192217],"study_design_scores_gemma":[0.000008546914,0.00009755777,0.9959453,0.0000024761296,0.000017799814,0.00023140918,0.00024193124,0.002474934,0.0006442271,0.00001049294,0.00031450047,0.000010859732],"about_ca_topic_score_codex":0.29813388,"about_ca_topic_score_gemma":0.31328574,"teacher_disagreement_score":0.29813388,"about_ca_system_score_codex":0.0023311137,"about_ca_system_score_gemma":0.0005160474,"threshold_uncertainty_score":0.5927971},"labels":[],"label_agreement":null},{"id":"W1793083427","doi":"10.1029/2005gb002484","title":"Holocene climate and carbon cycle dynamics: Experiments with the “green” McGill Paleoclimate Model","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Paleoclimatology; Carbon cycle; Climatology; Orbital forcing; Holocene; Geology; Ice sheet; Atmospheric sciences; Environmental science; Precipitation; Vegetation (pathology); Climate change; Oceanography; Ecosystem; Insolation; Meteorology; Geography","score_opus":0.01281672879723041,"score_gpt":0.24426206075478424,"score_spread":0.23144533195755382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1793083427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997081,0.00004092058,0.0007766836,0.00016071662,0.000019872985,0.000014614231,0.0005121987,0.000099579214,0.0012944029],"genre_scores_gemma":[0.9974214,0.000033120137,0.0015055117,0.00007268867,0.00000850825,0.000022326241,0.00058095006,0.000033613902,0.00032191654],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998479,0.00005312147,0.00000586737,0.00002768402,0.000021788203,0.00004358021],"domain_scores_gemma":[0.9991486,0.00038066835,0.00009524162,0.000090027905,0.000108876244,0.00017654216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061204686,0.00064816873,0.0004264924,0.0002813208,0.00058486836,0.00047908074,0.0018289629,0.00067600486,0.0014773281],"category_scores_gemma":[0.0017183308,0.00033171728,0.0005848118,0.00035280705,0.0007387784,0.0005843945,0.000515124,0.0011307315,0.000100725905],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011295017,0.00047241044,0.022788651,0.00007709794,0.0002528718,0.00038097388,0.00018691049,0.95754695,0.007984197,0.0031419096,0.0019907812,0.004047757],"study_design_scores_gemma":[0.00020675242,0.00016756963,0.0059518693,0.000006121964,0.00006479512,0.000011526325,0.000044373803,0.99026614,0.0022429517,0.0005390012,0.00047622694,0.000022675964],"about_ca_topic_score_codex":0.19762196,"about_ca_topic_score_gemma":0.14703645,"teacher_disagreement_score":0.19762196,"about_ca_system_score_codex":0.0017871914,"about_ca_system_score_gemma":0.0012135897,"threshold_uncertainty_score":0.39294332},"labels":[],"label_agreement":null},{"id":"W1809582875","doi":"10.1029/2008gb003231","title":"Seasonal and spatial variability in dissolved organic matter quantity and composition from the Yukon River basin, Alaska","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":346,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dissolved organic carbon; Colored dissolved organic matter; Environmental science; Organic matter; Hydrology (agriculture); Drainage basin; Environmental chemistry; Vegetation (pathology); Lignin; Biogeochemistry; Humus; Nutrient; Soil water; Geology; Ecology; Chemistry; Soil science","score_opus":0.007350501273176097,"score_gpt":0.1879356617350085,"score_spread":0.1805851604618324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1809582875","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99951315,0.00009507559,0.000046072113,0.0000075964385,0.0000014486695,0.0000014130061,0.00015453911,0.0000026384107,0.00017804332],"genre_scores_gemma":[0.9991204,0.00012434252,0.0001227607,0.00000679727,9.674251e-7,0.0000039931733,0.0003712573,0.0000013027716,0.00024808967],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989545,0.0000078260955,0.000016493372,0.000038064834,0.000025895974,0.000016384445],"domain_scores_gemma":[0.99971944,0.000044938006,0.000052051015,0.000012732545,0.00012262257,0.000048099897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024575205,0.0001528992,0.00020467173,0.0009770906,0.00074114243,0.0006881561,0.00018482404,0.00021524701,0.00028117117],"category_scores_gemma":[0.0003775778,0.00015960254,0.0001397421,0.0012308875,0.0003542521,0.00028666353,0.00052100373,0.00012340023,0.000047205507],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050167466,0.000011909252,0.9884071,0.00003477648,0.00006240019,0.00013552634,0.0011401045,0.00034641442,0.0047889957,0.00003249584,0.00006662019,0.004923528],"study_design_scores_gemma":[0.0000013221777,0.000006452244,0.9981989,0.0000047547696,0.000016548016,0.000039804363,0.0010625791,0.00017222507,0.00026069747,0.000013347423,0.00021967525,0.0000036556976],"about_ca_topic_score_codex":0.27357417,"about_ca_topic_score_gemma":0.47699252,"teacher_disagreement_score":0.27357417,"about_ca_system_score_codex":0.0011249412,"about_ca_system_score_gemma":0.00094121776,"threshold_uncertainty_score":0.54396355},"labels":[],"label_agreement":null},{"id":"W1811130305","doi":"10.1029/2002gb001898","title":"Methyl bromide cycling in a warm‐core eddy of the North Atlantic Ocean","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Bromide; Thermocline; Seawater; Oceanography; Cycling; Biogeochemical cycle; Environmental science; Chemistry; Atmospheric sciences; Environmental chemistry; Geology; Geography","score_opus":0.01687732824481485,"score_gpt":0.20740835574850064,"score_spread":0.19053102750368578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1811130305","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998764,0.000023032859,0.00002978196,0.0000047790895,7.2606696e-7,6.324545e-7,0.000025707099,0.0000013741337,0.00003749257],"genre_scores_gemma":[0.9995415,0.000029759667,0.00014536528,0.00001138057,0.0000029589173,0.0000025795562,0.00018817247,0.0000018460679,0.00007652954],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994946,0.000007714031,0.000004212879,0.00001649401,0.000010703807,0.000011492294],"domain_scores_gemma":[0.9998641,0.00002791339,0.00003839384,0.000010110071,0.000028824625,0.00003059019],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018484237,0.00018142501,0.00023627115,0.00021951739,0.00040648397,0.00031904568,0.00023106388,0.0002793161,0.00019097097],"category_scores_gemma":[0.00034447797,0.00022885423,0.00024245512,0.00013962596,0.00018525172,0.00026694348,0.00027505847,0.00017973573,0.000053657728],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000785794,0.00014829265,0.7324551,0.00004958676,0.00014653815,0.0003550421,0.00056017813,0.0018369856,0.25680643,0.000081440674,0.0001319074,0.0066425963],"study_design_scores_gemma":[0.000023237873,0.00015341929,0.99166393,0.0000039292713,0.000026836156,0.00007424605,0.000082917155,0.0029299886,0.004771783,0.000027542814,0.0002339686,0.000008228361],"about_ca_topic_score_codex":0.012537651,"about_ca_topic_score_gemma":0.02484379,"teacher_disagreement_score":0.012537651,"about_ca_system_score_codex":0.0004568168,"about_ca_system_score_gemma":0.00024822963,"threshold_uncertainty_score":0.024929345},"labels":[],"label_agreement":null},{"id":"W1811729449","doi":"10.1029/2010gb004008","title":"The effect of vertical and horizontal dilution on fertilized patch experiments","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Fisheries and Oceans Canada","funders":"","keywords":"Phytoplankton; Iron fertilization; Total organic carbon; Environmental science; Carbon fibers; Nitrogen; Nutrient; Subarctic climate; Chemistry; Environmental chemistry; Geology; Oceanography; Ecology; Biology; Mathematics","score_opus":0.0078015487996139525,"score_gpt":0.22790513864335968,"score_spread":0.22010358984374573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1811729449","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98856914,0.00063863065,0.0063090003,0.00018241112,0.00011400506,0.00022552905,0.0006384078,0.000086562315,0.0032364305],"genre_scores_gemma":[0.9882228,0.00032678014,0.0071191904,0.00025122528,0.0000406106,0.00036460266,0.00039679356,0.00007851689,0.0031994758],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989279,0.0004329005,0.00010326874,0.00026989006,0.00016917886,0.00009682531],"domain_scores_gemma":[0.9936341,0.004265179,0.0008086515,0.0006254587,0.00046029326,0.00020630911],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00094265456,0.00039395358,0.00064276025,0.0002018927,0.00032366198,0.00046482365,0.0010341938,0.00071766245,0.003205887],"category_scores_gemma":[0.003429801,0.00029168636,0.0003814575,0.00021777478,0.0005577647,0.00041886256,0.0008264793,0.00081522804,0.00025346648],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.013922192,0.0022635586,0.03772697,0.0011678512,0.00059001223,0.00076636707,0.00029750442,0.07855814,0.8223144,0.0037396299,0.0011203771,0.0375331],"study_design_scores_gemma":[0.0025225137,0.021589104,0.057023987,0.00010073253,0.00077743735,0.00039613547,0.00017594003,0.20183654,0.7006119,0.004551965,0.010215305,0.00019854291],"about_ca_topic_score_codex":0.0051877387,"about_ca_topic_score_gemma":0.0032252362,"teacher_disagreement_score":0.0051877387,"about_ca_system_score_codex":0.00087843195,"about_ca_system_score_gemma":0.0003058655,"threshold_uncertainty_score":0.010724783},"labels":[],"label_agreement":null},{"id":"W1820071717","doi":"10.1002/2015gb005137","title":"Is atmospheric phosphorus pollution altering global alpine Lake stoichiometry?","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Aquatic Ecosystems and Phytoplankton Dynamics","field":"Environmental Science","cited_by":188,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Environmental Biology; Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Deposition (geology); Environmental science; Phosphorus; Environmental chemistry; Precipitation; Nutrient; Biomass (ecology); Flux (metallurgy); Pollution; Biogeochemical cycle; Atmospheric sciences; Chemistry; Ecology; Biology; Geology; Meteorology; Sediment; Geography","score_opus":0.01336384734676624,"score_gpt":0.24526460726022928,"score_spread":0.23190075991346304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1820071717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99713564,0.00062216306,0.00028416392,0.00026579556,0.000009503084,0.0000034221805,0.00026547606,0.000021828711,0.0013919175],"genre_scores_gemma":[0.9994204,0.00024385672,0.000090910034,0.000041876738,0.000010030883,0.0000013616997,0.00008828621,0.0000023586742,0.000100935016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986553,0.00003374206,0.00001301458,0.000040061892,0.000031830292,0.000015838494],"domain_scores_gemma":[0.99975103,0.000048395763,0.000110913265,0.000015043511,0.000052719202,0.000021846367],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039266882,0.00016409515,0.000231949,0.00041293292,0.00032226226,0.0008395679,0.0001487569,0.0002918797,0.0009100751],"category_scores_gemma":[0.0005577158,0.00012316604,0.00015631945,0.0004668238,0.00041973733,0.00055384764,0.00035811015,0.00013668908,0.00010649485],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019638518,0.000026703607,0.93586516,0.00012809483,0.00020907926,0.00026125662,0.000120976474,0.002036505,0.05009339,0.00038995006,0.00030025435,0.010372303],"study_design_scores_gemma":[0.0000087790895,0.000047872567,0.99342346,0.0000057861344,0.00003662485,0.000064912136,0.00012893275,0.0030153848,0.0020716302,0.000550445,0.00064100325,0.0000050431145],"about_ca_topic_score_codex":0.00978505,"about_ca_topic_score_gemma":0.0104895765,"teacher_disagreement_score":0.00978505,"about_ca_system_score_codex":0.00041871844,"about_ca_system_score_gemma":0.00026264216,"threshold_uncertainty_score":0.019456208},"labels":[],"label_agreement":null},{"id":"W1825708147","doi":"10.1029/2002gb001976","title":"Numerical modeling: A complementary tool for studying CO<sub>2</sub> emissions from hydroelectric reservoirs","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Université Laval","funders":"","keywords":"Hydroelectricity; Environmental science; Sampling (signal processing); Surface water; Hydrology (agriculture); Geology; Environmental engineering; Ecology; Geotechnical engineering","score_opus":0.020802333379810776,"score_gpt":0.23877772917398443,"score_spread":0.21797539579417366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1825708147","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.20769602,0.0017531463,0.75469774,0.001337671,0.00021476054,0.00020793283,0.0011361454,0.0013045721,0.031651974],"genre_scores_gemma":[0.83391213,0.0012537397,0.16046253,0.000102534,0.00009011322,0.00028765423,0.00031717072,0.000077764584,0.0034964911],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985576,0.00005723422,0.000009206328,0.00001754449,0.000048236005,0.000011959967],"domain_scores_gemma":[0.9994091,0.0003174334,0.000079747326,0.00006501578,0.000106891865,0.000021871347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028790097,0.00035560504,0.00034766717,0.00046694512,0.0003399834,0.00078890123,0.00047494232,0.00057545083,0.0015067597],"category_scores_gemma":[0.00166864,0.00018144543,0.00022708949,0.0006066273,0.0005013668,0.00052763755,0.00037906534,0.00029204867,0.00018605485],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040196475,0.000051508414,0.0045992737,0.0001205305,0.0000308883,0.00009090306,0.00009923982,0.93715423,0.010146014,0.021041874,0.000677187,0.025948165],"study_design_scores_gemma":[0.0000069829944,0.000007737206,0.0004323921,0.000007906327,0.0000037840339,0.000011166724,0.0000180292,0.9954437,0.00091095356,0.0016109454,0.0015419825,0.0000044236763],"about_ca_topic_score_codex":0.0354536,"about_ca_topic_score_gemma":0.017287575,"teacher_disagreement_score":0.0354536,"about_ca_system_score_codex":0.00093442015,"about_ca_system_score_gemma":0.0010891285,"threshold_uncertainty_score":0.07049447},"labels":[],"label_agreement":null},{"id":"W1826173682","doi":"10.1029/2003gb002063","title":"Geochemical indices allow estimation of heavy metal background concentrations in soils","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Heavy metals in environment","field":"Environmental Science","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Barrick Gold (Canada)","funders":"","keywords":"Soil water; Environmental science; Environmental chemistry; Heavy metals; Metal; Pollution; Soil science; Earth science; Geology; Chemistry; Ecology","score_opus":0.014454307254323387,"score_gpt":0.26467840531012493,"score_spread":0.25022409805580154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1826173682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5072545,0.0016274618,0.4698197,0.00017022951,0.000054809418,0.00008535776,0.002393105,0.0023403221,0.016254587],"genre_scores_gemma":[0.886097,0.0005561542,0.11043104,0.000021853555,0.000021570257,0.000033300195,0.0007644415,0.000060100225,0.0020144922],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9998635,0.000028732888,0.0000082316465,0.000038767113,0.00004940981,0.000011338803],"domain_scores_gemma":[0.9996592,0.000073921554,0.0001078923,0.00004728751,0.000094454015,0.00001731137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000296667,0.0003635327,0.0003086201,0.001177699,0.00011929891,0.0007688565,0.0003100667,0.00034267234,0.00092391716],"category_scores_gemma":[0.001175536,0.00017512581,0.00015003541,0.0012744095,0.00018093112,0.0006094809,0.00030339282,0.00043802118,0.0005932231],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018441674,0.00010408016,0.32313958,0.0002645311,0.0001835218,0.00020196101,0.00018463918,0.03507365,0.22603549,0.010899917,0.003609016,0.40011922],"study_design_scores_gemma":[0.00002335613,0.00023882998,0.43165895,0.000052891577,0.00017370257,0.0008852834,0.00034307034,0.32838106,0.18468475,0.021750387,0.03170231,0.00010541765],"about_ca_topic_score_codex":0.0013552546,"about_ca_topic_score_gemma":0.0028624225,"teacher_disagreement_score":0.0013552546,"about_ca_system_score_codex":0.00020707911,"about_ca_system_score_gemma":0.00015999048,"threshold_uncertainty_score":0.0030908585},"labels":[],"label_agreement":null},{"id":"W1826238075","doi":"10.1029/2006gb002854","title":"Sediment organic carbon burial in agriculturally eutrophic impoundments over the last century","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":524,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Sediment; Total organic carbon; Watershed; Eutrophication; Environmental science; Deposition (geology); Hydrology (agriculture); Geology; Nutrient; Ecology; Geomorphology","score_opus":0.00486961538088466,"score_gpt":0.19096231028627425,"score_spread":0.1860926949053896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1826238075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995403,0.000112003414,0.00009511536,0.00000770978,6.778698e-7,4.9716095e-7,0.00012726993,0.0000033048443,0.00011306546],"genre_scores_gemma":[0.99920505,0.00017207769,0.0001420701,0.000003556896,0.0000027586166,0.0000015646873,0.00030931484,0.0000015193756,0.00016215573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989784,0.000011341226,0.000013956134,0.000031406216,0.000025772946,0.00001971871],"domain_scores_gemma":[0.9991486,0.00010283962,0.0005088326,0.00003938621,0.00015466512,0.000045584176],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025850773,0.0003099148,0.00012835544,0.001143462,0.00030455957,0.0004456507,0.00019779362,0.0001911856,0.00036637363],"category_scores_gemma":[0.0014207737,0.0001886713,0.00021765397,0.0014893139,0.00030453288,0.0005065314,0.00047857568,0.00019296737,0.00009119731],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004066419,0.0000072885105,0.988311,0.000016802203,0.00006615863,0.00012675804,0.00021294747,0.0016109869,0.0013717633,0.00003443369,0.000047775728,0.008153359],"study_design_scores_gemma":[0.0000011099812,0.000013315069,0.998281,0.0000027627075,0.000015370486,0.00010244738,0.00007070754,0.00078202056,0.00040978877,0.000019793415,0.00029843775,0.0000032392945],"about_ca_topic_score_codex":0.020703675,"about_ca_topic_score_gemma":0.042876124,"teacher_disagreement_score":0.020703675,"about_ca_system_score_codex":0.00058197876,"about_ca_system_score_gemma":0.00014847136,"threshold_uncertainty_score":0.041166306},"labels":[],"label_agreement":null},{"id":"W1827294658","doi":"10.1029/2009gb003654","title":"Ongoing transients in carbonate compensation","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Ocean acidification; Carbonate; Carbonate compensation depth; Dissolution; Calcite; Saturation (graph theory); Aragonite; Snow; Geology; Biogeochemical cycle; Sedimentary rock; Mineralogy; Environmental science; Oceanography; Geomorphology; Climate change; Chemistry; Geochemistry; Environmental chemistry","score_opus":0.008885057383285325,"score_gpt":0.22744283927148645,"score_spread":0.21855778188820113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1827294658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.982806,0.0001728982,0.007927095,0.00072544446,0.000046346162,0.000010888348,0.00032049834,0.0002518631,0.0077389632],"genre_scores_gemma":[0.999008,0.00005278593,0.00030264273,0.000029175717,0.0000042451775,0.0000035094115,0.0000749412,0.000010118827,0.00051451987],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999306,0.000011147346,0.0000034572047,0.00001951374,0.000014282126,0.000020970057],"domain_scores_gemma":[0.9998362,0.000044719483,0.000035475452,0.000019225943,0.000030386096,0.000033915832],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017905852,0.0002637395,0.00018439032,0.00012822417,0.00025804652,0.00064583943,0.0003188128,0.00071344513,0.0027596585],"category_scores_gemma":[0.001052933,0.00026410108,0.00041237296,0.0001581971,0.000307339,0.00071250065,0.00069852354,0.0005243079,0.00019575476],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008222972,0.00017632735,0.16234349,0.0002920546,0.00023002358,0.0011883116,0.0005865752,0.6421889,0.12265478,0.03155462,0.005689963,0.03227258],"study_design_scores_gemma":[0.0001756357,0.00032127197,0.13831039,0.00003603888,0.00011660751,0.00027990618,0.0006001201,0.8110675,0.021553338,0.018008085,0.009435566,0.00009544558],"about_ca_topic_score_codex":0.009535542,"about_ca_topic_score_gemma":0.006632493,"teacher_disagreement_score":0.009535542,"about_ca_system_score_codex":0.0009904819,"about_ca_system_score_gemma":0.00048568123,"threshold_uncertainty_score":0.018960118},"labels":[],"label_agreement":null},{"id":"W1831866922","doi":"10.1029/2001gb001639","title":"Distribution of anthropogenic CO<sub>2</sub> in the Pacific Ocean","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":157,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization; Fisheries and Oceans Canada","funders":"","keywords":"Equator; Oceanography; Latitude; Longitude; Pacific ocean; Geology; Southern Hemisphere; Pacific decadal oscillation; Environmental science; Climatology","score_opus":0.010642899720311285,"score_gpt":0.20565482983813024,"score_spread":0.19501193011781895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1831866922","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99540496,0.00047263646,0.00036075246,0.00004468825,0.000004245681,0.0000047163458,0.0008184093,0.000025606174,0.0028639673],"genre_scores_gemma":[0.9982539,0.0004770043,0.00025285833,0.000013829059,0.000008301072,0.0000062676636,0.0006706255,0.0000076028896,0.00030958408],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999037,0.000008612636,0.000008982788,0.000024188483,0.000035254565,0.000019314446],"domain_scores_gemma":[0.99949455,0.000036344365,0.00017221442,0.000034445384,0.00018700278,0.00007547875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001245924,0.00017395118,0.00013411006,0.001042748,0.00019964516,0.0004767585,0.00015556127,0.00008980248,0.0007053649],"category_scores_gemma":[0.0003808242,0.00012137558,0.0001362191,0.0015187372,0.00033358362,0.00023502644,0.00037295345,0.00013591847,0.00013584203],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009152779,0.00000931688,0.97416353,0.00003668817,0.000078459474,0.0001536414,0.00020665031,0.0008389092,0.0066577885,0.00016836046,0.00032604675,0.017268982],"study_design_scores_gemma":[0.0000013003269,0.000009903602,0.99797815,0.000006298242,0.00000957977,0.00008581589,0.00013870769,0.00041789218,0.00039733693,0.000040840077,0.00091131486,0.0000028796567],"about_ca_topic_score_codex":0.03132422,"about_ca_topic_score_gemma":0.027295342,"teacher_disagreement_score":0.03132422,"about_ca_system_score_codex":0.00044191486,"about_ca_system_score_gemma":0.0003089242,"threshold_uncertainty_score":0.062283754},"labels":[],"label_agreement":null},{"id":"W1832456282","doi":"10.1029/2001gb001813","title":"Volatile organic compound emissions in relation to plant carbon fixation and the terrestrial carbon budget","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":198,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"California Institute of Technology","keywords":"Environmental science; Primary production; Biosphere; Carbon cycle; Carbon fibers; Total organic carbon; Biome; Terrestrial ecosystem; Eddy covariance; Productivity; Ecosystem; Atmospheric sciences; Environmental chemistry; Chemistry; Ecology; Geology","score_opus":0.011031112454362984,"score_gpt":0.20293884226579478,"score_spread":0.1919077298114318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1832456282","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9824776,0.011812238,0.0007536893,0.0004877986,0.000014447054,0.000005704433,0.00045504398,0.000015466383,0.0039781346],"genre_scores_gemma":[0.99605197,0.0029793826,0.00021279603,0.000027792279,0.000020819723,0.0000038871053,0.00019471641,0.0000069400962,0.00050174794],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996734,0.000007369453,0.0000020373993,0.000006979494,0.0000072958737,0.000009053628],"domain_scores_gemma":[0.99980253,0.00009515084,0.000049061917,0.000005850738,0.000026721911,0.000020723035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001377359,0.00018922566,0.00014879221,0.00049816276,0.00018413345,0.0005224997,0.0001314583,0.0002949712,0.0012627911],"category_scores_gemma":[0.0005269643,0.00011750478,0.00009865702,0.00083310215,0.00022821774,0.00035724827,0.00023105858,0.00017585655,0.00016658193],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001107964,0.00012813638,0.7770073,0.0004615024,0.00041697084,0.0008553851,0.0003669851,0.039961796,0.08810752,0.0091255,0.001645034,0.080815926],"study_design_scores_gemma":[0.000020752737,0.000067411514,0.97322977,0.00003634322,0.00006298299,0.00020508506,0.00020847289,0.011192973,0.004391627,0.0065576327,0.00401254,0.000014402006],"about_ca_topic_score_codex":0.0095823975,"about_ca_topic_score_gemma":0.009743431,"teacher_disagreement_score":0.0095823975,"about_ca_system_score_codex":0.00071618054,"about_ca_system_score_gemma":0.0001779824,"threshold_uncertainty_score":0.01905322},"labels":[],"label_agreement":null},{"id":"W1833483487","doi":"10.1002/2014gb005063","title":"A new look at ocean carbon remineralization for estimating deepwater sequestration","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":196,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Fisheries and Oceans Canada","funders":"Natural Environment Research Council; Région Bretagne; Università degli Studi di Milano; Fondation Veolia Environnement; Universität Bremen; Université Pierre et Marie Curie; Centre National de la Recherche Scientifique; University College Dublin; Sight Research UK; Agence Nationale de la Recherche; Muséum National d'Histoire Naturelle; University of Alberta","keywords":"Remineralisation; Carbon sequestration; Oceanography; Environmental science; Geology; Carbon dioxide; Chemistry","score_opus":0.017698726302121985,"score_gpt":0.25037249473004297,"score_spread":0.23267376842792098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1833483487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8097937,0.0021476073,0.18342113,0.00027307257,0.000022603235,0.000027241396,0.0006561527,0.0005446778,0.0031137543],"genre_scores_gemma":[0.9691594,0.00025899586,0.030223805,0.000022781282,0.0000060907723,0.000010677678,0.000102236496,0.000026586866,0.00018937216],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999299,0.000025865791,0.0000047213807,0.00002248558,0.000011569751,0.000005392423],"domain_scores_gemma":[0.9998405,0.000056137218,0.000035917714,0.000026048536,0.000032109132,0.000009398575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030527092,0.0004736071,0.00030951557,0.00075115816,0.000105076484,0.0003040171,0.00021744012,0.00024744676,0.0004147261],"category_scores_gemma":[0.0006382828,0.00017087065,0.0003397318,0.0005842814,0.00021224245,0.0004483096,0.00028396564,0.00022385092,0.0000825184],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017839379,0.00005497917,0.26121226,0.0002754892,0.0007201684,0.0002817263,0.00013818164,0.3615298,0.2879392,0.004429086,0.0005228555,0.082717784],"study_design_scores_gemma":[0.000019494242,0.00009309022,0.2525371,0.000055714452,0.00014679223,0.0002542979,0.00011999632,0.6745039,0.06579647,0.003874428,0.0025401828,0.000058523492],"about_ca_topic_score_codex":0.007181334,"about_ca_topic_score_gemma":0.0068722405,"teacher_disagreement_score":0.007181334,"about_ca_system_score_codex":0.00035193464,"about_ca_system_score_gemma":0.00021554253,"threshold_uncertainty_score":0.0142790675},"labels":[],"label_agreement":null},{"id":"W1838764073","doi":"10.1029/2007gb002952","title":"Farming the planet: 1. Geographic distribution of global agricultural lands in the year 2000","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Remote Sensing in Agriculture","field":"Environmental Science","cited_by":1983,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Wageningen University and Research; National Aeronautics and Space Administration","keywords":"Longitude; Land cover; Agricultural land; Data set; Range (aeronautics); Environmental science; Geographic coordinate system; Satellite; Agriculture; Spatial distribution; Land use; Geography; Physical geography; Remote sensing; Latitude; Cartography; Statistics; Mathematics; Geodesy; Ecology","score_opus":0.005893881323986145,"score_gpt":0.19857388597381853,"score_spread":0.1926800046498324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1838764073","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.77571446,0.004489563,0.002540513,0.0022054622,0.0001190514,0.00007039692,0.16702293,0.00037177248,0.047465928],"genre_scores_gemma":[0.9278518,0.0025168413,0.0026706192,0.00024511793,0.00006839794,0.00005810324,0.060298868,0.000041523326,0.0062488085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998859,0.000010712848,0.000010193358,0.00003672394,0.00003954208,0.000016803346],"domain_scores_gemma":[0.9997223,0.000022977012,0.00011031271,0.000016599719,0.00008852301,0.00003916301],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018671436,0.00028662581,0.000093483,0.001710322,0.00015270164,0.00068278395,0.00023131716,0.0002518004,0.003513932],"category_scores_gemma":[0.00066236843,0.00008497773,0.000116859825,0.0034462004,0.00020109426,0.0007420428,0.00045626893,0.0001806665,0.0013816436],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011502222,0.000051131567,0.7952419,0.000271188,0.00005825358,0.00020654657,0.0009348463,0.0019166296,0.002456575,0.002116202,0.064204276,0.13242751],"study_design_scores_gemma":[0.0000048512034,0.000020845246,0.95541644,0.000030453617,0.000010176897,0.00019327272,0.00039855583,0.0004896499,0.00021654996,0.00029669213,0.042917583,0.0000049488663],"about_ca_topic_score_codex":0.010651154,"about_ca_topic_score_gemma":0.012041951,"teacher_disagreement_score":0.010651154,"about_ca_system_score_codex":0.00037338125,"about_ca_system_score_gemma":0.0001785045,"threshold_uncertainty_score":0.021178305},"labels":[],"label_agreement":null},{"id":"W1839952345","doi":"10.1029/2009gb003655","title":"Challenges of modeling depth‐integrated marine primary productivity over multiple decades: A case study at BATS and HOT","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":191,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Government of Canada; Fisheries and Oceans Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"SeaWiFS; Environmental science; Ocean gyre; Primary production; Ocean color; Biogeochemical cycle; Climatology; Productivity; Primary productivity; Oceanography; Physical geography; Atmospheric sciences; Ecology; Phytoplankton; Geology; Ecosystem; Geography; Satellite; Biology; Subtropics","score_opus":0.0205365306476707,"score_gpt":0.23557926053808093,"score_spread":0.21504272989041023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1839952345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99350375,0.00041358967,0.003796565,0.0008720523,0.000016009688,0.000014720739,0.00040905373,0.000090626,0.0008836214],"genre_scores_gemma":[0.9953661,0.00013092975,0.004039695,0.00007368107,0.0000137946045,0.00001375139,0.00019230787,0.000025482543,0.00014431035],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99915946,0.00046627264,0.000075543016,0.00017392458,0.00006280967,0.00006201295],"domain_scores_gemma":[0.99466175,0.0035462894,0.000533113,0.0005253241,0.00047469666,0.00025893693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0059953635,0.00056887564,0.0007425893,0.0005186539,0.0005479123,0.001438473,0.0013236551,0.0016273833,0.0003674797],"category_scores_gemma":[0.010977025,0.0005829345,0.0011676875,0.0010068829,0.00036473275,0.001669565,0.00082211645,0.00084159477,0.000068626614],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016901355,0.00015709581,0.3470767,0.00007740019,0.00067628827,0.00050115184,0.0003621075,0.6348699,0.0011053857,0.0010626117,0.00061788014,0.013324491],"study_design_scores_gemma":[0.00004792192,0.00015495757,0.05824765,0.000052162424,0.00020176402,0.00016247253,0.00061785144,0.9356335,0.0014389333,0.002040175,0.0013539126,0.000048689115],"about_ca_topic_score_codex":0.09627859,"about_ca_topic_score_gemma":0.0732066,"teacher_disagreement_score":0.09627859,"about_ca_system_score_codex":0.0018039974,"about_ca_system_score_gemma":0.0016515566,"threshold_uncertainty_score":0.19143641},"labels":[],"label_agreement":null},{"id":"W1842683167","doi":"10.1029/2010gb003821","title":"Sedimentary opal records in the eastern equatorial Pacific: It is not all about leakage","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Earth Institute, Columbia University; National Science Foundation; International Association of Sedimentologists; Canadian Foundation for Climate and Atmospheric Sciences; Lamont-Doherty Earth Observatory, Columbia University; Oregon State University; Canadian Institute for Advanced Research","keywords":"Deglaciation; Geology; Oceanography; Upwelling; Sedimentary rock; Diatom; Glacial period; Productivity; Biogenic silica; Deep sea; Silicic acid; Last Glacial Maximum; Tephra; Holocene; Geochemistry; Paleontology; Volcano","score_opus":0.024208696512912842,"score_gpt":0.2766502226094265,"score_spread":0.25244152609651366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1842683167","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99759406,0.00082119374,0.00016613577,0.00007697972,0.000008443678,0.000003069153,0.00043375924,0.000014858343,0.0008815594],"genre_scores_gemma":[0.9984806,0.0006213939,0.00021096325,0.00007243513,0.000024059362,0.000002996897,0.00041784628,0.0000062577615,0.00016348013],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999386,0.0000064743963,0.000010246988,0.000020934676,0.000012503766,0.000011186594],"domain_scores_gemma":[0.9995455,0.00004302473,0.00022302625,0.00004941143,0.00009387388,0.000045090517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000245556,0.00023545572,0.00021856232,0.00080637285,0.0003310491,0.0007936928,0.00018805098,0.0002402071,0.00043308825],"category_scores_gemma":[0.000698074,0.0001346571,0.00014463671,0.0015253796,0.0003754685,0.0007066746,0.000617813,0.00021174965,0.00008575146],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010957939,0.000010000919,0.9759942,0.00007545523,0.00012489036,0.00016531184,0.0006776166,0.00014706785,0.009176708,0.00009054783,0.00018318152,0.013245471],"study_design_scores_gemma":[0.0000018223981,0.000009253788,0.99883586,0.000007933315,0.000020645504,0.000046492496,0.00015619853,0.000098645636,0.0002764536,0.000029247043,0.0005144397,0.0000031410084],"about_ca_topic_score_codex":0.013277204,"about_ca_topic_score_gemma":0.019464986,"teacher_disagreement_score":0.013277204,"about_ca_system_score_codex":0.00030193417,"about_ca_system_score_gemma":0.00018030543,"threshold_uncertainty_score":0.02639985},"labels":[],"label_agreement":null},{"id":"W1842986359","doi":"10.1029/2007gb003024","title":"Comparison of regional carbon flux estimates from CO<sub>2</sub> concentration measurements and remote sensing based footprint integration","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of Toronto","funders":"","keywords":"Eddy covariance; Environmental science; Flux (metallurgy); Atmospheric sciences; Carbon cycle; Diurnal cycle; Carbon sink; Primary production; Planetary boundary layer; Climatology; Boundary layer; Ecosystem; Climate change; Geology; Physics; Chemistry","score_opus":0.025310841481210527,"score_gpt":0.25037740092531646,"score_spread":0.22506655944410595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1842986359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97756517,0.0004406174,0.015626205,0.000051409126,0.000011587905,0.000030471914,0.0011115225,0.0004108424,0.004752142],"genre_scores_gemma":[0.96752053,0.00022709956,0.028836146,0.00006476276,0.00001498484,0.00006606982,0.0024878187,0.00011827126,0.0006643822],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995981,0.00010139691,0.000028128641,0.00011280079,0.00011989365,0.000039705934],"domain_scores_gemma":[0.9990017,0.0002568621,0.0001359732,0.0001075692,0.00047801877,0.000019856747],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001211599,0.0005531309,0.00043821224,0.0016456806,0.00013920282,0.0008038101,0.0005751185,0.00049838435,0.0007836064],"category_scores_gemma":[0.002402365,0.00038881061,0.00053335796,0.0013899654,0.00015833262,0.0008668739,0.0004138888,0.0001964563,0.00034844925],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015494236,0.0002015028,0.49771675,0.00040639637,0.00120381,0.0003144042,0.000753527,0.1526306,0.083008565,0.0011053786,0.0023122986,0.25879738],"study_design_scores_gemma":[0.00013350481,0.00014839125,0.78536534,0.00006152245,0.0003917169,0.00019748276,0.00031869503,0.18111159,0.028544063,0.00041331112,0.003198797,0.000115588715],"about_ca_topic_score_codex":0.015127317,"about_ca_topic_score_gemma":0.025667673,"teacher_disagreement_score":0.015127317,"about_ca_system_score_codex":0.00060700445,"about_ca_system_score_gemma":0.00025909278,"threshold_uncertainty_score":0.03007859},"labels":[],"label_agreement":null},{"id":"W1844537331","doi":"10.1029/2011gb004150","title":"Redefinition and global estimation of basal ecosystem respiration rate","year":2011,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Respiration; Ecosystem; Environmental science; Basal (medicine); Estimation; Ecology; Biology; Economics","score_opus":0.014013882363362708,"score_gpt":0.2133412817223719,"score_spread":0.1993273993590092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1844537331","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.70595586,0.00438771,0.27905288,0.00023309728,0.00009169124,0.00005232437,0.0033387656,0.00082591316,0.006061695],"genre_scores_gemma":[0.9306847,0.0010461328,0.0656092,0.000051093008,0.000021215617,0.000036684294,0.0018202049,0.0001089343,0.00062191486],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996562,0.00006883415,0.000021379763,0.00017947072,0.00004825297,0.000025863768],"domain_scores_gemma":[0.9997029,0.00007714826,0.000081380575,0.00007016756,0.000056807163,0.0000115300745],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007300434,0.0007119468,0.00037661023,0.0006101679,0.00013425067,0.00060525286,0.00052929553,0.0004271566,0.00065301376],"category_scores_gemma":[0.0012694587,0.0002801482,0.00044663667,0.0009842654,0.0002190622,0.0011690758,0.00043449024,0.00043083113,0.0002756886],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001826106,0.00010237901,0.4128156,0.000640502,0.0005154088,0.00019497087,0.00033196024,0.30149814,0.05855598,0.005365799,0.002195066,0.21760158],"study_design_scores_gemma":[0.000020279102,0.00010716835,0.39000317,0.00012422941,0.00023063394,0.00028072554,0.00012216189,0.57263947,0.022040218,0.0027551183,0.0115801785,0.000096652104],"about_ca_topic_score_codex":0.0065879305,"about_ca_topic_score_gemma":0.010127653,"teacher_disagreement_score":0.0065879305,"about_ca_system_score_codex":0.00043910393,"about_ca_system_score_gemma":0.0002937686,"threshold_uncertainty_score":0.013099134},"labels":[],"label_agreement":null},{"id":"W1852280710","doi":"10.1029/2009gb003699","title":"Tree ring evidence for limited direct CO<sub>2</sub> fertilization of forests over the 20th century","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":149,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Human fertilization; Productivity; Environmental science; Dendrochronology; Climate change; Latitude; Carbon sequestration; Ecology; Pinus <genus>; Global warming; Atmospheric sciences; Agronomy; Biology; Geography; Botany; Carbon dioxide; Geology","score_opus":0.0124817787139838,"score_gpt":0.2435446185676738,"score_spread":0.23106283985369,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1852280710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98989236,0.0017582582,0.00037446705,0.00027983557,0.000028012058,0.0000030177728,0.0010641232,0.000020836436,0.0065792385],"genre_scores_gemma":[0.9984376,0.00033725088,0.00011833218,0.00008104808,0.000031070664,0.0000020527928,0.00043985873,0.0000037843804,0.0005490335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998148,0.000021960373,0.000019251898,0.000084683554,0.00002835013,0.000030948453],"domain_scores_gemma":[0.9971595,0.0003800632,0.0014485045,0.00027473643,0.00050165266,0.0002355995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005808649,0.00009629469,0.00013968896,0.00044201384,0.000253679,0.0004507459,0.00021238434,0.00026112134,0.0028908644],"category_scores_gemma":[0.0016046085,0.000120943594,0.000113910915,0.0004559285,0.00041661618,0.00030246776,0.00031852175,0.00022329966,0.00041490464],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002469106,0.000019063827,0.97338593,0.00009621023,0.000093769886,0.00014203283,0.0002617531,0.00022372577,0.010795437,0.0005351876,0.00059037586,0.013609456],"study_design_scores_gemma":[0.0000024058443,0.00001884786,0.9975522,0.0000084119465,0.000022881593,0.00011746427,0.000046523037,0.000094573945,0.0005281619,0.000054263226,0.00155211,0.0000021351607],"about_ca_topic_score_codex":0.0056933714,"about_ca_topic_score_gemma":0.0124412365,"teacher_disagreement_score":0.0056933714,"about_ca_system_score_codex":0.0002488723,"about_ca_system_score_gemma":0.00016928368,"threshold_uncertainty_score":0.011320472},"labels":[],"label_agreement":null},{"id":"W1855007063","doi":"10.1002/gbc.20055","title":"Future Arctic Ocean primary productivity from CMIP5 simulations: Uncertain outcome, but consistent mechanisms","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":236,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"European Organization for the Exploitation of Meteorological Satellites; Natural Environment Research Council; Sight Research UK; U.S. Department of Energy","keywords":"Arctic; Environmental science; Sea ice; Coupled model intercomparison project; Climatology; Arctic geoengineering; Climate change; Oceanography; Primary production; Arctic ice pack; Climate model; Shoaling and schooling; Atmospheric sciences; Geology; Sea ice thickness; Ecosystem","score_opus":0.012235891051987564,"score_gpt":0.21777476749117816,"score_spread":0.2055388764391906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1855007063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9810097,0.00057668897,0.0052134753,0.0019690297,0.00013384076,0.00007883647,0.004572088,0.0005955037,0.005850872],"genre_scores_gemma":[0.9964233,0.00013462306,0.0016964322,0.00013817352,0.000022683414,0.000047058536,0.0012555378,0.000060343275,0.00022176253],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991456,0.0003567692,0.00008211311,0.00018957682,0.000112247515,0.00011377001],"domain_scores_gemma":[0.99712497,0.0013813223,0.00048800957,0.00037977018,0.0004551231,0.0001707358],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0046312916,0.0016124616,0.0007683735,0.0006766188,0.00072038,0.0016462863,0.0025940877,0.0025344952,0.0016075539],"category_scores_gemma":[0.007998151,0.0008693827,0.0015900409,0.0008503951,0.0006708343,0.0016108326,0.00091013283,0.0007991597,0.00024074956],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043588202,0.00016749899,0.090293296,0.00027524785,0.0008651123,0.00035356614,0.00014277709,0.8913589,0.002707692,0.004568865,0.002566779,0.006264418],"study_design_scores_gemma":[0.0002425215,0.00009550312,0.027056495,0.0000653102,0.00021662335,0.0000351399,0.00009722352,0.96684486,0.0018232341,0.0026597942,0.0007909227,0.00007229457],"about_ca_topic_score_codex":0.02465161,"about_ca_topic_score_gemma":0.010397784,"teacher_disagreement_score":0.02465161,"about_ca_system_score_codex":0.001677974,"about_ca_system_score_gemma":0.0010787196,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W1856821798","doi":"10.1029/2008gb003404","title":"Patterns in<i>p</i>CO<sub>2</sub>in boreal streams and rivers of northern Quebec, Canada","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":189,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"STREAMS; Boreal; Environmental science; Hydrology (agriculture); Tributary; Wetland; Surface water; Range (aeronautics); Ecology; Geology; Geography","score_opus":0.0028255946563416436,"score_gpt":0.1803737260534254,"score_spread":0.17754813139708375,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1856821798","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973949,0.00025075814,0.00010639987,0.00008490343,0.0000032727803,0.000010921395,0.0008366903,0.000013238124,0.001298818],"genre_scores_gemma":[0.9983967,0.00011526332,0.00012533236,0.000041803894,0.000001940112,0.000008212816,0.0006137647,0.0000049884175,0.0006920028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977106,0.000018557399,0.000010403068,0.00007216341,0.000048115773,0.00007971674],"domain_scores_gemma":[0.9991899,0.00005356526,0.00014933443,0.000017953102,0.00044301097,0.00014626961],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018913925,0.00018723868,0.000221813,0.0012546177,0.0011808611,0.0010268907,0.0004043822,0.0002734457,0.0012001399],"category_scores_gemma":[0.00061387575,0.00015453775,0.00018517772,0.0017406836,0.00068044604,0.00021833282,0.00034939527,0.00022930415,0.000089711415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001464386,0.000021915144,0.97968227,0.00003700391,0.00007432146,0.00015160826,0.0019408799,0.00039311836,0.0053547956,0.00015416149,0.00094897597,0.011094442],"study_design_scores_gemma":[0.0000015674335,0.0000048139527,0.99880564,0.000004662627,0.0000051475986,0.00001736104,0.00041651956,0.00015821893,0.00008751807,0.0000063112234,0.00048763663,0.000004693159],"about_ca_topic_score_codex":0.9796668,"about_ca_topic_score_gemma":0.9936947,"teacher_disagreement_score":0.02033317,"about_ca_system_score_codex":0.00971498,"about_ca_system_score_gemma":0.00420218,"threshold_uncertainty_score":0.07048744},"labels":[],"label_agreement":null},{"id":"W1859777507","doi":"10.1002/gbc.20031","title":"Diel vertical migration: Ecological controls and impacts on the biological pump in a one‐dimensional ocean model","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":181,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Canadian Institute for Advanced Research; Princeton University; U.S. Department of Energy","keywords":"Diel vertical migration; Zooplankton; Environmental science; Oceanography; Plankton; Ecosystem; Ecology; Biological pump; Mesopelagic zone; Pelagic zone; Primary producers; Biomass (ecology); Nutrient cycle; Carbon cycle; Nutrient; Phytoplankton; Biology; Geology","score_opus":0.02010722826794381,"score_gpt":0.2077725743703658,"score_spread":0.187665346102422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1859777507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93486863,0.00043701538,0.042400178,0.0017256441,0.00007815,0.000059102433,0.0022875005,0.0002960857,0.017847674],"genre_scores_gemma":[0.9886707,0.00021529713,0.004792201,0.00018453332,0.000026429028,0.00011422867,0.00071854464,0.00007079374,0.0052073547],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987674,0.00004227325,0.000007740766,0.000027114465,0.000013762661,0.00003238335],"domain_scores_gemma":[0.9994491,0.00021936654,0.0001159643,0.000034502165,0.00006771056,0.00011349156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033414285,0.0005952317,0.0006822909,0.000445093,0.0006223257,0.00139417,0.0016489131,0.0019428901,0.002474042],"category_scores_gemma":[0.0013157079,0.0005918615,0.00080286735,0.00057223585,0.0012308764,0.00087800977,0.0014489369,0.0010111699,0.00024136507],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036110425,0.000017816525,0.002228588,0.000010354476,0.000014888876,0.00003612427,0.000017065868,0.9940503,0.00029781813,0.0026661658,0.00019912813,0.0004255818],"study_design_scores_gemma":[0.000026137068,0.000011248276,0.0005483808,0.000002891434,0.0000062698637,0.000005081516,0.0000122508045,0.9986082,0.000031279706,0.0005799293,0.00016226376,0.0000060652073],"about_ca_topic_score_codex":0.05721623,"about_ca_topic_score_gemma":0.02242118,"teacher_disagreement_score":0.05721623,"about_ca_system_score_codex":0.0015484293,"about_ca_system_score_gemma":0.001277371,"threshold_uncertainty_score":0.11376637},"labels":[],"label_agreement":null},{"id":"W1867174815","doi":"10.1002/2014gb004989","title":"Temperature, oxygen, and vegetation controls on decomposition in a James Bay peatland","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Tanzania Commission for Science and Technology; National Science Foundation","keywords":"Peat; Sphagnum; Bay; Holocene; Vegetation (pathology); Environmental chemistry; Decomposition; Chemistry; Oxygen; Bog; Nitrogen; Environmental science; Ecology; Botany; Geology; Biology; Oceanography","score_opus":0.008673178993351863,"score_gpt":0.24675364577248463,"score_spread":0.23808046677913275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1867174815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998374,0.000020954549,0.000018140514,0.0000014207394,3.8529257e-7,0.0000015402843,0.00004203292,0.0000011680833,0.00007699185],"genre_scores_gemma":[0.9995307,0.000022266982,0.000091263544,0.000004237393,4.804286e-7,0.0000022304869,0.0001174043,0.0000012210991,0.0002303666],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991345,0.0000075783264,0.000005187964,0.000021193808,0.00002412633,0.000028408034],"domain_scores_gemma":[0.9997309,0.000023778202,0.00004799789,0.0000073503056,0.00008270782,0.00010726721],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001867977,0.00020590136,0.00018951474,0.00068283797,0.0005554452,0.00041786334,0.00020759134,0.00011271888,0.0004166736],"category_scores_gemma":[0.000180986,0.00015251101,0.00012305628,0.0003894505,0.00027041908,0.00011566439,0.00022089768,0.00014252464,0.000071830465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007513507,0.00015599186,0.7932434,0.000033347693,0.000058450714,0.0002947422,0.00065379165,0.00031109212,0.19947286,0.00004734337,0.00007679035,0.004900819],"study_design_scores_gemma":[0.0000012935014,0.000028940198,0.9981414,0.0000011675285,0.000004481903,0.000014270706,0.00014657293,0.00018881173,0.0013952388,0.000003846142,0.00007224221,0.0000017911215],"about_ca_topic_score_codex":0.28315422,"about_ca_topic_score_gemma":0.5127336,"teacher_disagreement_score":0.28315422,"about_ca_system_score_codex":0.0014731222,"about_ca_system_score_gemma":0.00090136175,"threshold_uncertainty_score":0.5630121},"labels":[],"label_agreement":null},{"id":"W1867297214","doi":"10.1029/2001gb001831","title":"Soil CO<sub>2</sub> production and surface flux at four climate observatories in eastern Canada","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Environmental science; Water content; Soil water; Context (archaeology); Flux (metallurgy); Soil science; Soil horizon; Subsurface flow; Thermal diffusivity; Carbon dioxide; Moisture; Atmosphere (unit); Atmospheric sciences; Hydrology (agriculture); Groundwater; Geology; Chemistry; Geography; Meteorology","score_opus":0.009965943683674948,"score_gpt":0.18766267196718736,"score_spread":0.1776967282835124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1867297214","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99872583,0.000058748516,0.00007461599,0.000037389225,8.530422e-7,0.0000041701087,0.0005668738,0.000008908347,0.0005226691],"genre_scores_gemma":[0.998481,0.00007990246,0.00018488691,0.0000126979885,8.0244183e-7,0.0000029540365,0.00044607703,0.0000037190548,0.00078793423],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998497,0.000008460138,0.0000058639903,0.000036663052,0.00003990119,0.00005944903],"domain_scores_gemma":[0.9995524,0.000044097662,0.00006229308,0.000014451671,0.00023018912,0.000096413176],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014862901,0.00022870392,0.0001853383,0.0006589231,0.001339179,0.00082781684,0.00039071278,0.00020203348,0.0008203443],"category_scores_gemma":[0.0005672078,0.00019299095,0.00014311624,0.0013562732,0.00067168614,0.00022886558,0.0005387076,0.00020562121,0.00007813763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010961328,0.000020028403,0.9821326,0.000028979939,0.000046844572,0.00017658097,0.0012475873,0.0012382221,0.0038261842,0.0001879872,0.00048906216,0.010496255],"study_design_scores_gemma":[0.000003319527,0.0000056779827,0.99740666,0.0000045331335,0.000009764795,0.000019865793,0.00078575115,0.00085501414,0.0004245145,0.000025994968,0.00045343812,0.0000055457695],"about_ca_topic_score_codex":0.9914206,"about_ca_topic_score_gemma":0.9974625,"teacher_disagreement_score":0.011958866,"about_ca_system_score_codex":0.011958866,"about_ca_system_score_gemma":0.007973068,"threshold_uncertainty_score":0.08676809},"labels":[],"label_agreement":null},{"id":"W1875023735","doi":"10.1029/2004gb002334","title":"Maximum reservoir capacity of vegetation for persistent organic pollutants: Implications for global cycling","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Toxic Organic Pollutants Impact","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Department for Environment, Food and Rural Affairs, UK Government","keywords":"Cycling; Vegetation (pathology); Environmental science; Pollutant; Atmosphere (unit); Atmospheric sciences; Range (aeronautics); Physical geography; Hydrology (agriculture); Ecology; Geology; Meteorology; Geography; Forestry","score_opus":0.02322202608258384,"score_gpt":0.27110082841938193,"score_spread":0.2478788023367981,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1875023735","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96881044,0.0035501944,0.01810178,0.0004253117,0.00002450321,0.000011570225,0.0007368194,0.0001213738,0.008217989],"genre_scores_gemma":[0.9986505,0.00038225774,0.00074997626,0.0000066254765,0.000004409139,0.0000028475092,0.00006478769,0.000007933537,0.0001307354],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999348,0.000015092033,0.0000028120076,0.000019157791,0.000011426403,0.00001670241],"domain_scores_gemma":[0.9996697,0.00015653583,0.00006804851,0.000031649084,0.000049076876,0.000025019996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032870303,0.000195371,0.00017675762,0.0005877855,0.00017718437,0.0005455051,0.00032138661,0.0001687916,0.0013489183],"category_scores_gemma":[0.0007323613,0.000109562905,0.00021368962,0.000611625,0.0004833332,0.001069161,0.00056223193,0.0001710557,0.000104020524],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003436514,0.00007247659,0.39575073,0.0006823096,0.00023774542,0.0006613613,0.0005926358,0.20171148,0.20478894,0.03945763,0.0016284157,0.15407254],"study_design_scores_gemma":[0.000018435261,0.00020383908,0.52065575,0.00009967843,0.00012185586,0.00069488643,0.0015841317,0.39337826,0.036701173,0.037121024,0.009308457,0.000112446825],"about_ca_topic_score_codex":0.0047762287,"about_ca_topic_score_gemma":0.002991907,"teacher_disagreement_score":0.0047762287,"about_ca_system_score_codex":0.0006240062,"about_ca_system_score_gemma":0.00021981627,"threshold_uncertainty_score":0.009496868},"labels":[],"label_agreement":null},{"id":"W1876373815","doi":"10.1029/2003gb002152","title":"Speciation and fluxes of nutrients (N, P, Si) from the upper Yukon River","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Cold Regions Research and Engineering Laboratory","keywords":"Nutrient; Particulates; Environmental chemistry; Flux (metallurgy); Genetic algorithm; Dissolved organic carbon; Chemistry; Environmental science; Hydrology (agriculture); Geology; Ecology; Biology","score_opus":0.005619435491930932,"score_gpt":0.20139279163000778,"score_spread":0.19577335613807686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1876373815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990695,0.000055482204,0.00013122603,0.000017835262,8.662202e-7,0.0000054794336,0.0002586744,0.000009533108,0.00045132512],"genre_scores_gemma":[0.99818665,0.00009045831,0.00033923824,0.000031467374,6.2569546e-7,0.0000114511795,0.0006818036,0.0000066762045,0.00065162475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990034,0.000006984746,0.000010781818,0.00003435171,0.000025780113,0.000021858132],"domain_scores_gemma":[0.9999014,0.000010880495,0.000017423168,0.0000045248557,0.00004866516,0.000017151115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009274488,0.00021328028,0.00030930023,0.00055989606,0.00081887643,0.00080755475,0.00023921723,0.00031236885,0.0006119807],"category_scores_gemma":[0.00021227563,0.0002871222,0.00022974226,0.00087879365,0.000254353,0.0003487151,0.00047220607,0.00021793162,0.000091817295],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032034903,0.000044756885,0.6756949,0.00016577612,0.00015555829,0.0005794952,0.002189136,0.0014965802,0.30093357,0.00035013538,0.0004484385,0.017621309],"study_design_scores_gemma":[0.000007747281,0.000046399808,0.9886901,0.000008850493,0.000038203714,0.00013736697,0.0011717359,0.0017262828,0.006661452,0.00006447673,0.0014315522,0.000015871155],"about_ca_topic_score_codex":0.2199291,"about_ca_topic_score_gemma":0.34542874,"teacher_disagreement_score":0.2199291,"about_ca_system_score_codex":0.0020321463,"about_ca_system_score_gemma":0.0011754122,"threshold_uncertainty_score":0.43729794},"labels":[],"label_agreement":null},{"id":"W1877005220","doi":"10.1029/2007gb003118","title":"Carbon‐cycle feedbacks of changes in the Atlantic meridional overturning circulation under future atmospheric CO<sub>2</sub>","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Environmental science; Carbon cycle; Northern Hemisphere; Atmospheric sciences; Climatology; Biosphere; Thermohaline circulation; Shutdown of thermohaline circulation; Latitude; Atmosphere (unit); Zonal and meridional; Oceanography; North Atlantic Deep Water; Ecosystem; Geology; Ecology; Meteorology","score_opus":0.006489094040237502,"score_gpt":0.20106105850027167,"score_spread":0.19457196446003416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1877005220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99507684,0.00004365806,0.0016783978,0.0002510245,0.00002150002,0.000008860897,0.0003402435,0.00007313378,0.0025065131],"genre_scores_gemma":[0.9993374,0.00002968814,0.00023401403,0.0000143897205,0.0000040137556,0.0000047834465,0.00008570671,0.0000079362835,0.0002819853],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994063,0.000021852113,0.0000033308147,0.000008947065,0.00000799855,0.000017264221],"domain_scores_gemma":[0.9996681,0.00016236553,0.00004637516,0.000015366733,0.000043807908,0.00006400083],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002537293,0.0003285827,0.00018303747,0.00018663178,0.0002893597,0.0005318401,0.00029069305,0.00051344873,0.0014893954],"category_scores_gemma":[0.0011474895,0.00020942293,0.00038013453,0.00020807226,0.000341095,0.0005044903,0.0003027805,0.0003907348,0.000078299934],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035128923,0.00007839297,0.041743215,0.000035825982,0.00009564187,0.00022639002,0.00006920848,0.93467164,0.011204559,0.0064172656,0.00091489515,0.0041915644],"study_design_scores_gemma":[0.000075458156,0.0000763917,0.029659303,0.0000033587353,0.000035282374,0.000025968691,0.000037473026,0.9673547,0.00063453155,0.0017285439,0.00035488734,0.0000139970925],"about_ca_topic_score_codex":0.032477573,"about_ca_topic_score_gemma":0.024648495,"teacher_disagreement_score":0.032477573,"about_ca_system_score_codex":0.00086874055,"about_ca_system_score_gemma":0.00053806946,"threshold_uncertainty_score":0.06457704},"labels":[],"label_agreement":null},{"id":"W1877806058","doi":"10.1029/2008gb003311","title":"Inventory changes in anthropogenic carbon from 1997–2003 in the Atlantic Ocean between 20°S and 65°N","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Sink (geography); North Atlantic Deep Water; Carbon cycle; Oceanography; Carbon sink; Water column; Climate change; Water mass; Carbon fibers; Thermohaline circulation; Geology; Ecosystem; Geography; Ecology","score_opus":0.011809454307115913,"score_gpt":0.2147579652404998,"score_spread":0.2029485109333839,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1877806058","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98667866,0.0003236592,0.0002641075,0.000079403515,0.000015091544,0.0000068453464,0.010766347,0.00003591905,0.0018300423],"genre_scores_gemma":[0.9814538,0.00050357904,0.00052753295,0.000061027018,0.000018059656,0.000019702478,0.016217422,0.000010600022,0.0011883213],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982196,0.000012601807,0.000028589042,0.000042433177,0.00006603315,0.000028426872],"domain_scores_gemma":[0.99922,0.00004970443,0.00041743333,0.000042036376,0.00022247,0.000048383667],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022344342,0.000246676,0.00015418172,0.0010055462,0.0002046536,0.00070600683,0.00027146397,0.0001811899,0.0005981988],"category_scores_gemma":[0.0005668954,0.00016990367,0.00044422114,0.0020772931,0.00016156351,0.0002734517,0.00030674422,0.00020901758,0.00022776713],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007751015,0.000018150677,0.9858115,0.000039017617,0.00017469282,0.00010882837,0.000084279025,0.002205833,0.0019410055,0.00007875562,0.0008850321,0.0085754655],"study_design_scores_gemma":[0.000002408831,0.000007738333,0.997398,0.000005936066,0.000024544688,0.00005341089,0.00006279265,0.00087444,0.00035726363,0.000017832492,0.0011924688,0.0000032747637],"about_ca_topic_score_codex":0.13351583,"about_ca_topic_score_gemma":0.1882931,"teacher_disagreement_score":0.13351583,"about_ca_system_score_codex":0.001366354,"about_ca_system_score_gemma":0.00078809843,"threshold_uncertainty_score":0.26547736},"labels":[],"label_agreement":null},{"id":"W1879333998","doi":"10.1002/2014gb004871","title":"Nitrous oxide emissions from cultivated black soil: A case study in Northeast China and global estimates using empirical model","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Nanjing Agricultural University; Dalhousie University; Chinese Academy of Sciences; National Natural Science Foundation of China; Agricultural Research Service; Montana State University; Universidad de Buenos Aires; U.S. Department of Agriculture","keywords":"Fertilizer; Denitrification; Manure; Nitrous oxide; Nitrification; Animal science; Nitrogen; Chemistry; Nitrate; Soil water; Agronomy; Environmental science; Environmental chemistry; Soil science; Biology","score_opus":0.02613010633849343,"score_gpt":0.2818418833459391,"score_spread":0.2557117770074457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1879333998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99914086,0.00004799217,0.00040081356,0.000018369166,9.4093144e-7,0.0000039450993,0.00016764083,0.000015742758,0.00020369547],"genre_scores_gemma":[0.9990482,0.00008573014,0.00036103875,0.0000036579775,0.0000014907135,0.000005434934,0.00036010446,0.0000026462835,0.00013177124],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998678,0.000024527124,0.000009795335,0.000036617417,0.00002253276,0.000038701415],"domain_scores_gemma":[0.99963045,0.00011147715,0.000092418064,0.000044557084,0.000088174835,0.000032821234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005643769,0.0008773228,0.0003286438,0.000848774,0.0003526601,0.00042622472,0.00078302564,0.0004778643,0.0003603143],"category_scores_gemma":[0.0005537012,0.00030387132,0.00073059875,0.0012505286,0.00038145098,0.00064791273,0.00037691317,0.00019487462,0.000051581283],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021604159,0.00021850526,0.4354954,0.00015417446,0.00022255135,0.0016844089,0.00022033037,0.5439043,0.00558787,0.0006578753,0.00041693018,0.01122159],"study_design_scores_gemma":[0.000038515678,0.00009080863,0.25017476,0.000015335989,0.000094410716,0.00008544669,0.00038128122,0.7467465,0.0015973931,0.0002885174,0.00045431385,0.000032769607],"about_ca_topic_score_codex":0.26709092,"about_ca_topic_score_gemma":0.18452077,"teacher_disagreement_score":0.26709092,"about_ca_system_score_codex":0.002174419,"about_ca_system_score_gemma":0.0010717716,"threshold_uncertainty_score":0.53107256},"labels":[],"label_agreement":null},{"id":"W1885078460","doi":"10.1029/2007gb002947","title":"Farming the planet: 2. Geographic distribution of crop areas, yields, physiological types, and net primary production in the year 2000","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Land Use and Ecosystem Services","field":"Environmental Science","cited_by":1945,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Land cover; Land use; Longitude; Geography; Agriculture; Agricultural land; Crop; Food security; Environmental science; Agroforestry; Latitude; Ecology; Forestry; Biology","score_opus":0.009531080575781527,"score_gpt":0.19576073583253314,"score_spread":0.18622965525675161,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1885078460","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5003154,0.00080562814,0.0046529593,0.0005023274,0.00005086305,0.0000923773,0.45323333,0.0008598305,0.03948724],"genre_scores_gemma":[0.7457801,0.001227255,0.012316578,0.00008363705,0.000045960765,0.00015032462,0.2309083,0.00011786922,0.009369917],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995434,0.0000055476053,0.000003093856,0.000014237113,0.000013585187,0.000009204935],"domain_scores_gemma":[0.99988353,0.00001578073,0.00003980555,0.00001147962,0.00003373932,0.000015645266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000082475446,0.00028784582,0.0001242987,0.001513465,0.000087019296,0.00058829697,0.00018287246,0.00014179577,0.006750934],"category_scores_gemma":[0.00031173573,0.0001074487,0.00014136794,0.0026747177,0.00013040533,0.00035166432,0.00040116636,0.00012971208,0.0019394977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032864048,0.00007859536,0.5895961,0.0005058527,0.00017478217,0.00037641358,0.0016879084,0.006669638,0.006044667,0.0031523518,0.15935361,0.23203155],"study_design_scores_gemma":[0.000017917575,0.000022052764,0.9170638,0.000032449952,0.000025544963,0.0002971989,0.0004922674,0.0016608577,0.0006216467,0.0005188651,0.079238534,0.000008871949],"about_ca_topic_score_codex":0.010251263,"about_ca_topic_score_gemma":0.013436919,"teacher_disagreement_score":0.010251263,"about_ca_system_score_codex":0.00023472703,"about_ca_system_score_gemma":0.00014622702,"threshold_uncertainty_score":0.02258414},"labels":[],"label_agreement":null},{"id":"W1895288913","doi":"10.1029/2001gb001462","title":"Carbon isotope discrimination in forest and pasture ecosystems of the Amazon Basin, Brazil","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Lethbridge","funders":"","keywords":"Environmental science; Pasture; Seasonality; Carbon cycle; δ13C; Isotopes of carbon; Ecosystem; Tree canopy; Vegetation (pathology); Ecology; Canopy; Atmospheric sciences; Stable isotope ratio; Total organic carbon; Biology; Geology","score_opus":0.005783445052169141,"score_gpt":0.19348413965212632,"score_spread":0.1877006945999572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1895288913","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998481,0.00038199555,0.00015423312,0.000017006343,0.000001416292,0.0000113244,0.00015774301,0.0000058028277,0.00078953756],"genre_scores_gemma":[0.99916446,0.00019824608,0.000349065,0.000014290918,0.0000013904457,0.000007197324,0.00015518603,0.0000032277787,0.00010683971],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998642,0.00002305845,0.000015209995,0.000041023537,0.00003279183,0.000023662762],"domain_scores_gemma":[0.99973994,0.000042558324,0.00009751941,0.000015447391,0.000070297894,0.00003422209],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002673617,0.00027264157,0.0003004155,0.0007360907,0.000421058,0.00047034127,0.00023957422,0.00016296093,0.00044599],"category_scores_gemma":[0.00065105816,0.00025413095,0.0001632426,0.00080035045,0.00040282318,0.00037575458,0.00034121258,0.0001122614,0.00006697731],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013089074,0.00005886556,0.93443185,0.0001309544,0.000102954946,0.00024235692,0.0028990717,0.00025031,0.045419957,0.000305333,0.00009432778,0.015932962],"study_design_scores_gemma":[0.0000061640108,0.00003539793,0.9979102,0.000009825648,0.000017507009,0.000119488424,0.0004671756,0.00039350562,0.0004634494,0.000082186416,0.0004896528,0.0000054579646],"about_ca_topic_score_codex":0.062076684,"about_ca_topic_score_gemma":0.1422436,"teacher_disagreement_score":0.062076684,"about_ca_system_score_codex":0.00063120766,"about_ca_system_score_gemma":0.00036228844,"threshold_uncertainty_score":0.12343073},"labels":[],"label_agreement":null},{"id":"W1896846014","doi":"10.1002/gbc.20041","title":"<sup>210</sup>Pb and <sup>137</sup>Cs in margin sediments of the Arctic Ocean: Controls on boundary scavenging","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba; Fisheries and Oceans Canada; Institut National de la Recherche Scientifique","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Oceanography; Geology; Arctic; Sediment; Bay; Scavenging; Transect; Water column; Canada Basin; Deposition (geology); Canyon; Sedimentation; Sediment trap; Phytodetritus; Nepheloid layer; Benthic zone; Geomorphology","score_opus":0.0056396960002960675,"score_gpt":0.20420731182196572,"score_spread":0.19856761582166965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1896846014","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99958307,0.000104265615,0.000034051805,0.0000060705147,0.000001197056,6.4734553e-7,0.000059291986,0.0000016878283,0.00020976557],"genre_scores_gemma":[0.9992532,0.00016075815,0.00010441029,0.000010144765,0.0000035312041,0.0000024261283,0.00019047986,0.0000029022362,0.0002720259],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988246,0.000017575856,0.000010026471,0.00003720216,0.000023835919,0.000028857281],"domain_scores_gemma":[0.99969447,0.00004727944,0.00010697797,0.0000126220875,0.000085784784,0.000052868523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023486896,0.00036632546,0.00025276782,0.0005953032,0.00048735907,0.0007769357,0.00017608675,0.00020228137,0.00042625197],"category_scores_gemma":[0.0003486722,0.00034237208,0.00013494669,0.00043094676,0.00049597473,0.0002793904,0.00038387248,0.0001483986,0.00014736726],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012902644,0.000027255215,0.7763639,0.000071307106,0.00009133487,0.0003151385,0.00075264944,0.0006858417,0.21171318,0.00012937118,0.00008101735,0.00847883],"study_design_scores_gemma":[0.0000034619839,0.000038447306,0.99505013,0.0000038096098,0.000014182834,0.00004790191,0.00018698085,0.00020443753,0.0042248038,0.00002446457,0.00019834295,0.0000030928195],"about_ca_topic_score_codex":0.040707048,"about_ca_topic_score_gemma":0.07224671,"teacher_disagreement_score":0.040707048,"about_ca_system_score_codex":0.000740355,"about_ca_system_score_gemma":0.00056059373,"threshold_uncertainty_score":0.08094025},"labels":[],"label_agreement":null},{"id":"W1898979306","doi":"10.1029/2012gb004477","title":"Correction to “Contribution of winter soil respiration to annual soil CO<sub>2</sub> emission in a Mollisol under different tillage practices in northeast China”","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Agriculture and Agri-Food Canada","funders":"","keywords":"Mollisol; Tillage; China; Agriculture; Beijing; Environmental science; Geography; Agronomy; Forestry; Soil water; Soil science; Archaeology; Biology","score_opus":0.012329900214078504,"score_gpt":0.2549008653478723,"score_spread":0.2425709651337938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1898979306","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0006114544,0.00094819546,0.0023888608,0.025871262,0.9652682,0.000020591528,0.002397322,0.00083961245,0.0016545112],"genre_scores_gemma":[0.073479936,0.009939771,0.017717203,0.08576795,0.5611921,0.00035224846,0.015923787,0.006089256,0.22953776],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99666154,0.0003875457,0.0005313725,0.0005776472,0.0015300551,0.0003119179],"domain_scores_gemma":[0.9741377,0.003147568,0.0013115249,0.0014757605,0.018704629,0.0012228127],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0029108452,0.0032490846,0.002685139,0.0028818264,0.0033326596,0.0029566388,0.0048236153,0.004871401,0.040506087],"category_scores_gemma":[0.030100713,0.0011956288,0.0022808902,0.003225624,0.0019457261,0.0026592466,0.002512786,0.007428679,0.018333705],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010355393,0.000010534734,0.00022382628,0.00024701844,0.00003516786,0.00030027342,0.000077140576,0.00023113884,0.00043221642,0.0006744233,0.98985505,0.0078096003],"study_design_scores_gemma":[0.0000947291,0.00004081057,0.0029551282,0.00023490078,0.00008605192,0.00047452215,0.00013185224,0.0014337413,0.0015391741,0.0014815107,0.9914403,0.00008726096],"about_ca_topic_score_codex":0.036586918,"about_ca_topic_score_gemma":0.033161547,"teacher_disagreement_score":0.040506087,"about_ca_system_score_codex":0.0041364757,"about_ca_system_score_gemma":0.005587818,"threshold_uncertainty_score":0.13550639},"labels":[],"label_agreement":null},{"id":"W1900254199","doi":"10.1029/2006gb002708","title":"Photomineralization of terrigenous dissolved organic matter in Arctic coastal waters from 1979 to 2003: Interannual variability and implications of climate change","year":2006,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":157,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Fisheries and Oceans Canada; Université du Québec à Rimouski","funders":"","keywords":"Dissolved organic carbon; Colored dissolved organic matter; Terrigenous sediment; Environmental science; Arctic; Oceanography; Water column; Sea ice; Organic matter; Geology; Phytoplankton; Chemistry; Nutrient; Geomorphology","score_opus":0.006193713093962137,"score_gpt":0.20750951207598928,"score_spread":0.20131579898202714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1900254199","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99941194,0.00010159928,0.00007756047,0.000015112896,0.0000025571642,0.0000012096862,0.00024107781,0.0000044099347,0.0001445698],"genre_scores_gemma":[0.9992525,0.000058049558,0.00010388429,0.000008959302,0.0000031972593,0.000002887043,0.00047394392,0.0000016883212,0.000094797506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991643,0.000010167398,0.000008056001,0.000035948095,0.000013742222,0.000015646512],"domain_scores_gemma":[0.9996933,0.00004309191,0.000091748625,0.000022248953,0.00010856462,0.000041047595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036480962,0.0002675494,0.00019128041,0.00054524856,0.0003218637,0.00047030137,0.00021118771,0.00030478468,0.00021515365],"category_scores_gemma":[0.00047663218,0.00014860605,0.00036118424,0.0005309122,0.00015512668,0.0002704237,0.0002439226,0.0001653263,0.00008321315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018786157,0.000038837177,0.9836971,0.000019580946,0.00010943874,0.00009811738,0.00018609749,0.0014481191,0.00923814,0.000031481944,0.0001308115,0.004814274],"study_design_scores_gemma":[0.0000016423523,0.000014925813,0.9977869,0.000002467222,0.000012288896,0.000028421518,0.00005480356,0.0013020885,0.0006161024,0.000008551732,0.00016853852,0.0000031543193],"about_ca_topic_score_codex":0.069795124,"about_ca_topic_score_gemma":0.08619079,"teacher_disagreement_score":0.069795124,"about_ca_system_score_codex":0.0010707332,"about_ca_system_score_gemma":0.0003099319,"threshold_uncertainty_score":0.13877773},"labels":[],"label_agreement":null},{"id":"W1909479374","doi":"10.1029/2009gb003503","title":"Glacial to postglacial transformation of organic input pathways in Arctic Ocean basins","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Glacial period; Geology; Oceanography; Terrigenous sediment; Deglaciation; Arctic; Sea ice; Last Glacial Maximum; Holocene; Glacial landform; Physical geography; Sediment; Geomorphology; Moraine; Geography","score_opus":0.012977082066405904,"score_gpt":0.2374239986035894,"score_spread":0.2244469165371835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1909479374","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995789,0.000095041236,0.000023810304,0.000008919281,0.00000123492,6.125126e-7,0.00008162721,0.0000018023087,0.00020807832],"genre_scores_gemma":[0.99941957,0.000094605886,0.000044653258,0.00001486465,0.0000025301238,0.0000029136577,0.00030321008,0.0000023414152,0.000115374365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999193,0.000012909585,0.0000063760735,0.000023292345,0.000013750651,0.000024524363],"domain_scores_gemma":[0.99980086,0.000028897335,0.000058587437,0.000014695172,0.00006429222,0.000032730233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025913256,0.00014695498,0.00019299425,0.0008715364,0.00051518757,0.0006937638,0.00014502712,0.00016000618,0.00047421854],"category_scores_gemma":[0.00048375013,0.00019044073,0.00015989089,0.000673635,0.00042447733,0.0002633912,0.00042951727,0.00013751033,0.00008388669],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024177242,0.000026531041,0.96715957,0.000030378042,0.000108004475,0.00010652967,0.00082064176,0.0005191324,0.023284236,0.00025288362,0.00010717185,0.0073431944],"study_design_scores_gemma":[0.0000013032277,0.00001097957,0.9992053,0.0000020250109,0.0000074904083,0.000017547694,0.00016437603,0.00011954791,0.00030730903,0.000025546067,0.00013719288,0.0000013370725],"about_ca_topic_score_codex":0.023010386,"about_ca_topic_score_gemma":0.051185474,"teacher_disagreement_score":0.023010386,"about_ca_system_score_codex":0.0006946864,"about_ca_system_score_gemma":0.0005103518,"threshold_uncertainty_score":0.045752883},"labels":[],"label_agreement":null},{"id":"W1912984227","doi":"10.1029/2006gb002856","title":"Mackenzie River nutrient delivery to the Arctic Ocean and effects of the Mackenzie Delta during open water conditions","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Environmental science; Delta; Dissolved organic carbon; Nutrient; Biogeochemical cycle; Floodplain; Hydrology (agriculture); River delta; Water quality; Total organic carbon; Oceanography; Environmental chemistry; Chemistry; Ecology; Geology","score_opus":0.017351323644711442,"score_gpt":0.22938865403576317,"score_spread":0.21203733039105171,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1912984227","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99951375,0.00004047418,0.000040358394,0.00002584901,0.0000016284889,0.0000012917938,0.000051918603,0.000003133981,0.00032156412],"genre_scores_gemma":[0.9993272,0.00008692676,0.00011090251,0.00002069922,0.0000023027992,0.0000038165495,0.00010226156,0.0000039563665,0.00034200927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998815,0.000023488832,0.000009461807,0.00003663975,0.00002098007,0.000027976665],"domain_scores_gemma":[0.9997341,0.000043612625,0.00010245904,0.000018717563,0.0000467442,0.000054362677],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022295522,0.00032423116,0.00023784066,0.00033123474,0.0005457404,0.00062652613,0.00023612614,0.00023824215,0.0005111634],"category_scores_gemma":[0.00066390925,0.00021290946,0.000418421,0.00022657258,0.0003343181,0.00033379262,0.0006992219,0.00025930456,0.000074575924],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009410065,0.00011572408,0.9531859,0.00005041941,0.00019210493,0.0003208233,0.0006554124,0.005597551,0.029804278,0.00024544596,0.00026987965,0.008621357],"study_design_scores_gemma":[0.00000747112,0.000096199656,0.9947541,0.000007923411,0.00004127261,0.000026782376,0.0003321695,0.002845356,0.001340991,0.0000377273,0.0005027046,0.000007416543],"about_ca_topic_score_codex":0.15765779,"about_ca_topic_score_gemma":0.19751829,"teacher_disagreement_score":0.8423422,"about_ca_system_score_codex":0.0017159334,"about_ca_system_score_gemma":0.0008295461,"threshold_uncertainty_score":0.31348026},"labels":[],"label_agreement":null},{"id":"W1926205133","doi":"10.1029/2003gb002098","title":"Response of the water balance to climate change in the United States over the 20th and 21st centuries: Results from the VEMAP Phase 2 model intercomparisons","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Oak Ridge Institute for Science and Education; U.S. Forest Service; U.S. Geological Survey; University of Texas at Austin; U.S. Department of Energy; Electric Power Research Institute; U.S. Department of Agriculture; National Aeronautics and Space Administration","keywords":"Environmental science; Surface runoff; Water balance; Precipitation; Evapotranspiration; Climate change; Climate model; Forcing (mathematics); Hydrology (agriculture); Radiative forcing; Water cycle; Atmospheric sciences; Climatology; Meteorology; Geography; Ecology; Geology","score_opus":0.01389310875171433,"score_gpt":0.2512022027306373,"score_spread":0.237309093978923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1926205133","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99822634,0.00017954333,0.0002346956,0.000085937,0.0000067699125,0.0000036513347,0.00085315004,0.000014069292,0.00039575397],"genre_scores_gemma":[0.9975318,0.00015518205,0.00046650993,0.000034138877,0.0000070617316,0.000010617084,0.001671241,0.000006463422,0.000116968105],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997515,0.0001230317,0.000013869262,0.00004347294,0.000037261587,0.00003079772],"domain_scores_gemma":[0.99950945,0.00017589862,0.000102853606,0.00006184776,0.0001173125,0.000032568118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010294497,0.00018692616,0.00016842953,0.0003607243,0.00019693119,0.0003828842,0.00023598455,0.00032512666,0.0004176278],"category_scores_gemma":[0.0022139833,0.00012978482,0.00036219365,0.0008230124,0.00020264913,0.00044450344,0.00042682304,0.0002633342,0.000050851555],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031606556,0.00012706601,0.90598595,0.0000507744,0.0004276206,0.00010964352,0.00029551677,0.06925178,0.0011038103,0.00074617914,0.0018650448,0.019720586],"study_design_scores_gemma":[0.000073463874,0.000110348825,0.92112553,0.000014928877,0.0001253695,0.00006479023,0.00021707358,0.07184213,0.0019614182,0.00066003395,0.0037742392,0.000030719682],"about_ca_topic_score_codex":0.037235823,"about_ca_topic_score_gemma":0.04275906,"teacher_disagreement_score":0.037235823,"about_ca_system_score_codex":0.000802628,"about_ca_system_score_gemma":0.00033804064,"threshold_uncertainty_score":0.07403821},"labels":[],"label_agreement":null},{"id":"W1928512854","doi":"10.1002/2015gb005153","title":"Sea‐air CO<sub>2</sub> exchange in the western Arctic coastal ocean","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; University of Manitoba; University of Calgary","funders":"","keywords":"Sea ice; Oceanography; Seawater; Environmental science; Sea ice concentration; Arctic; Arctic ice pack; Biogeochemical cycle; Carbon dioxide; Climatology; Arctic sea ice decline; Flux (metallurgy); Sea ice thickness; Atmospheric sciences; Geology; Chemistry; Environmental chemistry","score_opus":0.016415330475407337,"score_gpt":0.22958501431758957,"score_spread":0.21316968384218224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1928512854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987238,0.00007810267,0.00007343556,0.00001644441,0.0000025664938,0.0000015017657,0.0005994431,0.000005509322,0.0004990817],"genre_scores_gemma":[0.99878126,0.00009332313,0.00019833149,0.000010038933,0.000004242336,0.000004321737,0.0007585272,0.0000031337636,0.00014669822],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999018,0.000015677948,0.0000119433735,0.000031416825,0.00002165497,0.000017456603],"domain_scores_gemma":[0.99977833,0.000020574764,0.00007559528,0.000018207487,0.000083489984,0.000023740924],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002915415,0.00025641976,0.00020673212,0.0007808625,0.00038923466,0.00069140777,0.00013661831,0.00015806819,0.00030989794],"category_scores_gemma":[0.0003519536,0.00015922131,0.00022885119,0.0013706837,0.00021300593,0.00031319755,0.0003283854,0.00010718958,0.00009847646],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011402544,0.000029751554,0.982781,0.00003159049,0.00008649139,0.00014363586,0.00023523493,0.0023601379,0.007731357,0.00008054699,0.00031959653,0.006086567],"study_design_scores_gemma":[0.000001177629,0.0000061626833,0.99790573,0.000004616958,0.000010154445,0.000018219422,0.00013369431,0.0012625065,0.00032229224,0.000017423452,0.0003151589,0.00000284128],"about_ca_topic_score_codex":0.20016918,"about_ca_topic_score_gemma":0.24902736,"teacher_disagreement_score":0.20016918,"about_ca_system_score_codex":0.00062073197,"about_ca_system_score_gemma":0.000620937,"threshold_uncertainty_score":0.3980081},"labels":[],"label_agreement":null},{"id":"W1931423081","doi":"10.1029/2001gb001702","title":"Methane efflux from boreal wetlands: Theory and testing of the ecosystem model Ecosys with chamber and tower flux measurements","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Alberta","funders":"","keywords":"Environmental science; Flux (metallurgy); Ecosystem; Wetland; Boreal; Hydrology (agriculture); Volatilisation; Atmospheric sciences; Methane; Ecology; Chemistry; Geology","score_opus":0.018979139299402502,"score_gpt":0.21410183623344847,"score_spread":0.19512269693404596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1931423081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931297,0.000045626108,0.005395706,0.000067089895,0.0000072793628,0.000018498384,0.00019960925,0.00012556608,0.0010109508],"genre_scores_gemma":[0.9974354,0.000022544347,0.0022864759,0.000011607646,0.0000034142854,0.000019865549,0.00011948875,0.000014870694,0.000086355816],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996062,0.00017582288,0.000028934806,0.00007887936,0.00006977816,0.00004029348],"domain_scores_gemma":[0.998409,0.0009535186,0.00019923235,0.00015692935,0.00019924395,0.00008212217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016960858,0.0008688627,0.0004451435,0.00026406583,0.0004208923,0.0006492977,0.0010904133,0.00055215176,0.00041295477],"category_scores_gemma":[0.0032732813,0.0004013574,0.00059759954,0.00024265583,0.00038847976,0.0011153957,0.0005919732,0.00034495577,0.00005872753],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006928898,0.00027262335,0.09467916,0.00007866737,0.00015332988,0.00017887894,0.00015311099,0.88098925,0.010111085,0.0025096145,0.00029361513,0.009887832],"study_design_scores_gemma":[0.000060929364,0.00016119544,0.021041552,0.000005108559,0.000027023785,0.000022481176,0.000026872618,0.975662,0.0024421676,0.00036345498,0.00016439904,0.000022779672],"about_ca_topic_score_codex":0.0638568,"about_ca_topic_score_gemma":0.024571123,"teacher_disagreement_score":0.0638568,"about_ca_system_score_codex":0.0011692407,"about_ca_system_score_gemma":0.000864878,"threshold_uncertainty_score":0.12697023},"labels":[],"label_agreement":null},{"id":"W1942752920","doi":"10.1002/2013gb004726","title":"Linking variability in soil solution dissolved organic carbon to climate, soil type, and vegetation type","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":149,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; McMaster University","funders":"Centre for Ecology and Hydrology; Vlaamse regering","keywords":"Dissolved organic carbon; Environmental science; Soil water; Vegetation (pathology); Terrestrial ecosystem; Ecosystem; Temperate climate; Carbon cycle; Soil carbon; Taiga; Vegetation type; Temperate rainforest; Forest ecology; Temperate forest; Soil science; Hydrology (agriculture); Environmental chemistry; Ecology; Chemistry; Geology; Biology","score_opus":0.006140743880010292,"score_gpt":0.2142804449475999,"score_spread":0.2081397010675896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1942752920","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994462,0.00004450403,0.00014225434,0.0000042027837,9.883609e-7,0.0000013028024,0.00024040786,0.0000037429843,0.000116387426],"genre_scores_gemma":[0.99960643,0.000015180934,0.00006231511,0.0000026550292,9.976928e-7,0.000001248781,0.00027186135,0.0000014349278,0.000037992402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979836,0.00005261787,0.000013920652,0.00007551668,0.000023157882,0.00003651358],"domain_scores_gemma":[0.99910873,0.0003872919,0.00020976884,0.000073957555,0.0001020259,0.00011818271],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051821506,0.00017293659,0.00023319076,0.00077043485,0.00015362023,0.0004988161,0.00017437167,0.00022622138,0.00070146343],"category_scores_gemma":[0.00084130047,0.00012332047,0.00019632673,0.00088818104,0.00023720948,0.0002515415,0.0003035861,0.0001385522,0.00011307598],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004071668,0.00001066531,0.99616015,0.000005330481,0.00008871664,0.00001930091,0.000027745824,0.00041332783,0.0020413315,0.000020232292,0.000025872585,0.0011464818],"study_design_scores_gemma":[0.0000011338993,0.000006982743,0.9992848,9.170851e-7,0.0000070094443,0.000015491183,0.000030173034,0.00048821518,0.00010671327,0.000017489561,0.000040032934,0.0000011482207],"about_ca_topic_score_codex":0.006762355,"about_ca_topic_score_gemma":0.008962888,"teacher_disagreement_score":0.006762355,"about_ca_system_score_codex":0.00018106315,"about_ca_system_score_gemma":0.00012704497,"threshold_uncertainty_score":0.013445973},"labels":[],"label_agreement":null},{"id":"W1943566327","doi":"10.1029/2003gb002154","title":"Nitrogen deposition and increased carbon accumulation in ombrotrophic peatlands in eastern Canada","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":179,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal; McGill University","funders":"Cure Cancer Australia Foundation","keywords":"Ombrotrophic; Peat; Deposition (geology); Nitrogen; Animal science; Environmental chemistry; Environmental science; Chemistry; Geology; Ecology; Bog; Biology; Geomorphology; Sediment","score_opus":0.008116647111348543,"score_gpt":0.22297196676950998,"score_spread":0.21485531965816143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1943566327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943036,0.00016408646,0.000018802317,0.000014242931,7.9470465e-7,0.0000014164129,0.00013518821,0.0000022147033,0.00023284032],"genre_scores_gemma":[0.999134,0.0001560023,0.00007975412,0.00001147723,7.6902916e-7,0.0000016938087,0.00018612912,0.000001910622,0.00042838612],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998368,0.0000070836068,0.000009439682,0.000034998233,0.000039503953,0.00007220416],"domain_scores_gemma":[0.9995334,0.000030036485,0.00010043874,0.000013758237,0.00017524528,0.00014703035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020221772,0.00024653165,0.00021023439,0.0009713021,0.001302529,0.00083295803,0.00035264177,0.00022775213,0.0006586036],"category_scores_gemma":[0.00043425593,0.00023487881,0.00017155797,0.0010183244,0.0005947313,0.00019408728,0.00039252496,0.00016981816,0.00007566678],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013674097,0.000021141172,0.9846202,0.000038794922,0.000060624534,0.00032134977,0.0010487745,0.00035531353,0.0073236655,0.00008125195,0.0001661086,0.0058261],"study_design_scores_gemma":[0.0000016128942,0.00000398142,0.99920326,0.0000042496854,0.0000045204847,0.000031019943,0.00029682164,0.000104227984,0.00012418088,0.0000075327657,0.00021603976,0.0000024892997],"about_ca_topic_score_codex":0.973571,"about_ca_topic_score_gemma":0.9938699,"teacher_disagreement_score":0.026428998,"about_ca_system_score_codex":0.009449358,"about_ca_system_score_gemma":0.006114401,"threshold_uncertainty_score":0.06856024},"labels":[],"label_agreement":null},{"id":"W1948649959","doi":"10.1002/2014gb004932","title":"Inherited hypoxia: A new challenge for reoligotrophicated lakes under global warming","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Aquatic Ecosystems and Phytoplankton Dynamics","field":"Environmental Science","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Hypoxia (environmental); Eutrophication; Climate change; Environmental science; Ecosystem; Anthropocene; Nutrient; Aquatic ecosystem; Ecology; Biodiversity; Regime shift; Global warming; Environmental change; Biology; Oxygen; Chemistry","score_opus":0.014723346809014553,"score_gpt":0.243310090962567,"score_spread":0.22858674415355246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1948649959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9850529,0.0013496199,0.006957715,0.004267921,0.00005279017,0.000008775702,0.00018120553,0.00008382595,0.0020451986],"genre_scores_gemma":[0.9981785,0.00040664952,0.00077981787,0.00018816243,0.000046515852,0.0000056977497,0.000048930964,0.00001573172,0.00032991523],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999813,0.00006724715,0.000009013208,0.000046726494,0.000021220516,0.00004273535],"domain_scores_gemma":[0.9996069,0.00007785576,0.00011663115,0.00003909935,0.00006698528,0.00009249331],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007506132,0.0002889936,0.0004726194,0.0002457361,0.0005759222,0.0012712708,0.00040018855,0.0006111093,0.00081156817],"category_scores_gemma":[0.0010792676,0.0001251561,0.00028213978,0.0003612739,0.0011487806,0.0012083396,0.0010065204,0.0003845917,0.000086426764],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000407769,0.0000992505,0.7576563,0.00034499943,0.0004363997,0.0022225184,0.0044598687,0.060607042,0.04341024,0.026953116,0.0044515594,0.09895095],"study_design_scores_gemma":[0.00002301309,0.00058409455,0.81578547,0.00014377477,0.000187601,0.00094819523,0.011487216,0.08692125,0.0035381257,0.05492613,0.025290428,0.00016472969],"about_ca_topic_score_codex":0.0050172373,"about_ca_topic_score_gemma":0.0072864247,"teacher_disagreement_score":0.0050172373,"about_ca_system_score_codex":0.00066654984,"about_ca_system_score_gemma":0.0005759589,"threshold_uncertainty_score":0.009976089},"labels":[],"label_agreement":null},{"id":"W1948862158","doi":"10.1029/2011gb004187","title":"The net carbon footprint of a newly created boreal hydroelectric reservoir","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":164,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Hydro-Québec; McGill University; GDG Environnement; Université du Québec à Montréal","funders":"","keywords":"Environmental science; Hydroelectricity; Flood myth; Hydrology (agriculture); Carbon footprint; Boreal; Greenhouse gas; Carbon cycle; Extrapolation; Physical geography; Ecosystem; Ecology; Geography; Geology; Oceanography","score_opus":0.006104116501467364,"score_gpt":0.21094759055465756,"score_spread":0.2048434740531902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1948862158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996416,0.00014143554,0.00050525134,0.000039681465,0.000005137791,0.0000147908195,0.0006476233,0.00002146712,0.0022086757],"genre_scores_gemma":[0.9979134,0.0001469722,0.0005448159,0.000014176018,0.0000028087354,0.000006766532,0.00047417465,0.000005674213,0.00089115946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998286,0.000016522084,0.000004609164,0.000026162897,0.000078879675,0.000045191897],"domain_scores_gemma":[0.99947983,0.000040346942,0.000104762046,0.000042980442,0.00021949614,0.000112630085],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030124266,0.00030614587,0.00022152852,0.0004904813,0.0006303209,0.0010401615,0.0004834703,0.00030826344,0.000768054],"category_scores_gemma":[0.0005150467,0.00012427809,0.00022736985,0.0006468901,0.0004981865,0.0006439025,0.00048245778,0.00026602627,0.00009197416],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006992624,0.00025227317,0.78061587,0.00022429766,0.0005225891,0.0024623536,0.00059543055,0.052236315,0.08178244,0.0011900091,0.0017726502,0.077646464],"study_design_scores_gemma":[0.000012189822,0.00017817403,0.96889853,0.000024976516,0.000081095975,0.00039673375,0.0006761208,0.016390314,0.006510757,0.00018541892,0.006586476,0.000059239934],"about_ca_topic_score_codex":0.33159444,"about_ca_topic_score_gemma":0.66331846,"teacher_disagreement_score":0.33159444,"about_ca_system_score_codex":0.0060971514,"about_ca_system_score_gemma":0.002592547,"threshold_uncertainty_score":0.6593287},"labels":[],"label_agreement":null},{"id":"W1948938282","doi":"10.1002/2015gb005211","title":"The imbalance of new and export production in the western Antarctic Peninsula, a potentially “leaky” ecosystem","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"New production; Upwelling; Nitrate; Environmental science; Oceanography; Phytoplankton; Sediment trap; Ecosystem; Nitrogen; Drawdown (hydrology); Nutrient; Hydrology (agriculture); Geology; Ecology; Water column; Chemistry; Biology","score_opus":0.014609104825304612,"score_gpt":0.21726013623703944,"score_spread":0.20265103141173482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1948938282","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996569,0.000029607116,0.000058615322,0.000017713473,8.2020006e-7,0.0000010424646,0.000065114196,0.000004502187,0.00016561816],"genre_scores_gemma":[0.9995722,0.000045266523,0.0001631642,0.0000145217955,0.0000020368664,0.0000024345013,0.0000786038,0.0000028820896,0.000118953234],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993575,0.000010859162,0.0000057262905,0.00002003135,0.000015917076,0.000011682669],"domain_scores_gemma":[0.99983096,0.000020573689,0.000059373073,0.000023283268,0.000033152657,0.00003268128],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023818036,0.00026329455,0.00016818735,0.00038381832,0.00052785635,0.0007287029,0.00020168166,0.00020622929,0.00056172337],"category_scores_gemma":[0.0002684695,0.0002566749,0.00015699223,0.0005222771,0.00044658175,0.00069921924,0.00044827777,0.00018525435,0.00011974659],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019907615,0.000029856768,0.9429323,0.00004005207,0.000115460076,0.0005458985,0.00057397445,0.0021423267,0.044534996,0.00014528348,0.00027144494,0.008469318],"study_design_scores_gemma":[0.000004397032,0.000028789853,0.9960033,0.0000035527826,0.000015228474,0.00007928071,0.00042766333,0.0020910755,0.0009769963,0.00008288683,0.0002817847,0.0000050367535],"about_ca_topic_score_codex":0.024433045,"about_ca_topic_score_gemma":0.054220524,"teacher_disagreement_score":0.024433045,"about_ca_system_score_codex":0.00083493436,"about_ca_system_score_gemma":0.0004227601,"threshold_uncertainty_score":0.04858166},"labels":[],"label_agreement":null},{"id":"W1950010039","doi":"10.1002/2014gb005001","title":"N‐loss isotope effects in the Peru oxygen minimum zone studied using a mesoscale eddy as a natural tracer experiment","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Oxygen minimum zone; Isotope fractionation; TRACER; Mesoscale meteorology; Biogeochemical cycle; Photic zone; Isotopologue; Isotope; Chemistry; Isotopes of nitrogen; Water column; Isotopes of oxygen; Fractionation; Environmental chemistry; Nitrogen; Geology; Oxygen; Oceanography; Phytoplankton","score_opus":0.016844754415313856,"score_gpt":0.25226395684423053,"score_spread":0.23541920242891667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1950010039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996469,0.000022981874,0.00010524022,0.000010237347,7.204161e-7,0.0000048268603,0.00006127588,0.0000059108243,0.00014187087],"genre_scores_gemma":[0.99928266,0.00003677203,0.00032824447,0.0000162427,0.0000022388936,0.00002255194,0.00021258114,0.0000037475359,0.00009497475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999926,0.000016870881,0.0000042559723,0.000025354326,0.000012421742,0.000015145608],"domain_scores_gemma":[0.9998042,0.000045379176,0.00006302872,0.000016107175,0.000032183012,0.000039093156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025910808,0.00026774334,0.00022660888,0.00044580342,0.00039541497,0.00033513474,0.00035741265,0.0004049319,0.00035834438],"category_scores_gemma":[0.00040621535,0.00021494369,0.00023420727,0.00035681567,0.0003115441,0.0002650157,0.00046584453,0.00028604787,0.000050337952],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009905112,0.00042075466,0.61790377,0.000089268884,0.00023361933,0.00045561837,0.00091468374,0.0018606158,0.3702836,0.00019175335,0.00018346262,0.006472235],"study_design_scores_gemma":[0.000030409265,0.00022157429,0.98922986,0.0000051808893,0.000026639687,0.00004569571,0.00020151437,0.0032562092,0.0065267934,0.000033930395,0.00041004736,0.0000120471805],"about_ca_topic_score_codex":0.015604077,"about_ca_topic_score_gemma":0.028911756,"teacher_disagreement_score":0.015604077,"about_ca_system_score_codex":0.0005780942,"about_ca_system_score_gemma":0.0002672947,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W1952580789","doi":"10.1002/2015gb005188","title":"Explicitly representing soil microbial processes in Earth system models","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":424,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Canadian Forest Service","funders":"U.S. Department of Agriculture; U.S. Department of Energy; National Institute of Food and Agriculture; National Science Foundation","keywords":"Biogeochemical cycle; Earth system science; Biogeochemistry; Earth science; Computer science; Carbon cycle; Scale (ratio); Environmental science; Process (computing); Benchmarking; Soil carbon; Biochemical engineering; Soil water; Ecology; Soil science; Ecosystem; Biology; Geology; Engineering; Geography","score_opus":0.029218283339460804,"score_gpt":0.2300970440144956,"score_spread":0.2008787606750348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1952580789","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1556243,0.0016530873,0.8120936,0.0027224978,0.0002241242,0.000107582026,0.0022691,0.0013340819,0.023971582],"genre_scores_gemma":[0.8767147,0.0014664218,0.11589271,0.00037663375,0.00013053618,0.00027152058,0.0008524937,0.00024869223,0.0040463028],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99949884,0.00028527915,0.000032777843,0.000058834874,0.00008536439,0.00003894738],"domain_scores_gemma":[0.9989164,0.0006060715,0.000118135846,0.00013582966,0.00015756006,0.00006608669],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012625909,0.00065292884,0.00053981395,0.0005823375,0.00050706277,0.0016381221,0.0011016116,0.0014378574,0.001816676],"category_scores_gemma":[0.0033763205,0.00042989702,0.0009587886,0.00096545735,0.000841337,0.0022196115,0.0013985517,0.0012366205,0.00037713855],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005360066,0.000012241684,0.00072090165,0.000022003092,0.00002240249,0.00001874862,0.000032581414,0.97764915,0.00042018795,0.018880008,0.00026465562,0.001951655],"study_design_scores_gemma":[0.000006295675,0.0000066861735,0.00015686531,0.0000135705195,0.000007629538,0.000004799662,0.000015247417,0.98037624,0.00019740124,0.01688377,0.0023246636,0.000006766762],"about_ca_topic_score_codex":0.01905224,"about_ca_topic_score_gemma":0.015293897,"teacher_disagreement_score":0.01905224,"about_ca_system_score_codex":0.0013780035,"about_ca_system_score_gemma":0.0014059304,"threshold_uncertainty_score":0.037882686},"labels":[],"label_agreement":null},{"id":"W1953314333","doi":"10.1029/2009gb003671","title":"Production of methyl halides by <i>Prochlorococcus</i> and <i>Synechococcus</i>","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Prochlorococcus; Synechococcus; Cyanobacteria; Environmental chemistry; Iodide; Phytoplankton; Chemistry; Biology; Ecology; Nutrient; Bacteria","score_opus":0.005725811401465998,"score_gpt":0.20442415509776607,"score_spread":0.19869834369630007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1953314333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980094,0.00032900574,0.000881852,0.000054052576,0.0000073113565,0.000007608642,0.00015785928,0.000029121631,0.0005239185],"genre_scores_gemma":[0.9969273,0.0001677106,0.0018921421,0.000027322914,0.0000046670675,0.000012573319,0.00034228805,0.000013470856,0.0006125745],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997739,0.000047990394,0.000015784812,0.000065358494,0.000062331856,0.00003467223],"domain_scores_gemma":[0.9997892,0.00004078555,0.000055712055,0.000032171545,0.000049196577,0.000032957687],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025468133,0.0003828488,0.00024509733,0.00019425947,0.00020688493,0.00042920007,0.0002565572,0.00027081618,0.00025037647],"category_scores_gemma":[0.00037472812,0.00021767242,0.00026425824,0.00016171225,0.00025326668,0.00033553335,0.00056395185,0.00028778653,0.0001504543],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006936115,0.000007110504,0.0029206914,0.000029350489,0.000005997726,0.00002776888,0.000029980682,0.00010221452,0.99539465,0.000036264933,0.000029475059,0.0013470069],"study_design_scores_gemma":[0.000014562347,0.00018991441,0.032271,0.0000058979444,0.000021238768,0.00013605722,0.0001267929,0.0022764087,0.96391666,0.000108712884,0.0009205429,0.00001213132],"about_ca_topic_score_codex":0.004382091,"about_ca_topic_score_gemma":0.004542205,"teacher_disagreement_score":0.004382091,"about_ca_system_score_codex":0.00046802394,"about_ca_system_score_gemma":0.00033211662,"threshold_uncertainty_score":0.008713186},"labels":[],"label_agreement":null},{"id":"W1956280464","doi":"10.1029/2008gb003327","title":"Soil organic carbon pools in the northern circumpolar permafrost region","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":2657,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Agriculture and Agri-Food Canada","funders":"","keywords":"Permafrost; Soil water; Total organic carbon; Soil carbon; Peat; Geology; Carbon fibers; Dissolved organic carbon; Soil science; Environmental science; Hydrology (agriculture); Environmental chemistry; Oceanography; Ecology; Chemistry","score_opus":0.02057857765593021,"score_gpt":0.2296279766223913,"score_spread":0.20904939896646108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1956280464","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941194,0.0009746922,0.00023593436,0.000024118885,0.0000015139176,0.000008356028,0.0031907035,0.000016581898,0.001428637],"genre_scores_gemma":[0.9947515,0.0007645481,0.0005930329,0.000015264304,0.000003885001,0.000015287513,0.0035999892,0.000004146493,0.00025228714],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991596,0.000012120294,0.000006542082,0.00003071836,0.000019147183,0.000015459264],"domain_scores_gemma":[0.9997516,0.000029000072,0.00010296039,0.000013571855,0.00005580365,0.000046995243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002167988,0.0003102225,0.00021875852,0.0017284456,0.00042691318,0.0006195782,0.00014899227,0.00015376284,0.0007691713],"category_scores_gemma":[0.0002770337,0.000121445264,0.00012925289,0.0020601922,0.00016683641,0.00036540395,0.0003553461,0.00010464961,0.00020164915],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013098601,0.000025525338,0.96818674,0.00009037047,0.00012725296,0.00026714598,0.0004815355,0.00312255,0.0068639587,0.00014420271,0.0003514482,0.02020836],"study_design_scores_gemma":[0.000002772115,0.000007918166,0.99775034,0.000011877725,0.000013819789,0.000041095263,0.00014460954,0.0007506599,0.0003658733,0.00006014768,0.0008466088,0.0000042197526],"about_ca_topic_score_codex":0.058845434,"about_ca_topic_score_gemma":0.08583172,"teacher_disagreement_score":0.058845434,"about_ca_system_score_codex":0.00055951864,"about_ca_system_score_gemma":0.00040900346,"threshold_uncertainty_score":0.117005825},"labels":[],"label_agreement":null},{"id":"W1964268554","doi":"10.1002/2014gb004842","title":"Contribution of anthropogenic phosphorus to agricultural soil fertility and food production","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Phosphorus and nutrient management","field":"Environmental Science","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Institut National de la Recherche Agronomique; Ministère de l'Écologie, du Développement Durable et de l'Énergie; Agence de l'Environnement et de la Maîtrise de l'Energie; Ministère de l'Agriculture, de l'Agroalimentaire et de la Forêt","keywords":"Biogeochemical cycle; Agriculture; Environmental science; Fertilizer; Phosphorus; Soil fertility; Ecology; Soil water; Soil science; Chemistry; Biology","score_opus":0.005688001011325689,"score_gpt":0.2113792370397231,"score_spread":0.20569123602839742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964268554","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965743,0.00004883658,0.0025379544,0.000029897592,0.0000019799988,0.000006058895,0.00024413799,0.000019183792,0.00053772086],"genre_scores_gemma":[0.99915934,0.000027715869,0.00060752087,0.0000035715975,0.000001042245,0.000006149852,0.00011647136,0.0000025236993,0.000075718846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998772,0.000043910946,0.000008250795,0.000033072778,0.00001607183,0.000021470296],"domain_scores_gemma":[0.99970716,0.00011565581,0.000073729374,0.000033246888,0.000051685667,0.000018414159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048707417,0.0002588545,0.00018369943,0.00047415975,0.00016418687,0.00051607104,0.00032934887,0.00027157634,0.0005636724],"category_scores_gemma":[0.0007484294,0.0001697105,0.00062891014,0.0006573128,0.00022948,0.00034589565,0.00035583563,0.0001696508,0.00006840904],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010691954,0.000036616,0.5071059,0.00004625541,0.0002331569,0.00030951845,0.00004620149,0.47778,0.0049241562,0.00069874135,0.00017578159,0.008536825],"study_design_scores_gemma":[0.00003394764,0.00015977578,0.37277368,0.00001221833,0.0000805304,0.00023758528,0.00014450186,0.6207272,0.0033529478,0.0011751638,0.0012742901,0.000028095903],"about_ca_topic_score_codex":0.014240146,"about_ca_topic_score_gemma":0.008232324,"teacher_disagreement_score":0.014240146,"about_ca_system_score_codex":0.0006535847,"about_ca_system_score_gemma":0.00050023856,"threshold_uncertainty_score":0.02831453},"labels":[],"label_agreement":null},{"id":"W1979173583","doi":"10.1029/1999gb900078","title":"Isotopic constraints on the transpiration, evaporation, energy, and gross primary production Budgets of a large boreal watershed: Ottawa River Basin, Canada","year":2000,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Evapotranspiration; Environmental science; Hydrology (agriculture); Eddy covariance; Transpiration; Primary production; Drainage basin; Permafrost; Atmospheric sciences; Geology; Ecosystem; Ecology; Photosynthesis; Chemistry","score_opus":0.004671606637676154,"score_gpt":0.1908699054744841,"score_spread":0.18619829883680794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979173583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969415,0.00014674744,0.00011275912,0.00005425111,0.000001787331,0.0000120957,0.0014376245,0.000017813556,0.0012754034],"genre_scores_gemma":[0.9967464,0.00020569933,0.0005554918,0.000023890034,0.0000012344037,0.0000114848535,0.0013546036,0.000011545131,0.0010896672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998584,0.0000065350773,0.000008959624,0.00003770492,0.000041726464,0.00004675728],"domain_scores_gemma":[0.99968445,0.000031502874,0.000032646996,0.000010744554,0.0001780156,0.00006265094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018998333,0.00028072705,0.00025013095,0.0007658814,0.0018131565,0.0011885059,0.00067777955,0.0002316915,0.00096916547],"category_scores_gemma":[0.00046333706,0.00024780942,0.0002700414,0.0016352462,0.00061483163,0.00032127384,0.00040821976,0.00020379758,0.00010305258],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035850957,0.00008065484,0.9346897,0.00014483188,0.00025484274,0.0003271277,0.001552539,0.016598172,0.021767067,0.0016325038,0.0024911542,0.020102961],"study_design_scores_gemma":[0.000016732018,0.0000126662,0.9857099,0.00001912324,0.000071607144,0.000045890934,0.00096329564,0.009430147,0.001169637,0.000120272154,0.0024068234,0.00003382572],"about_ca_topic_score_codex":0.9957457,"about_ca_topic_score_gemma":0.99810326,"teacher_disagreement_score":0.029776854,"about_ca_system_score_codex":0.029776854,"about_ca_system_score_gemma":0.018890949,"threshold_uncertainty_score":0.21604723},"labels":[],"label_agreement":null},{"id":"W1986869158","doi":"10.1002/2014gb004875","title":"Worldwide retention of nutrient silicon by river damming: From sparse data set to global estimate","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arsenic contamination and mitigation","field":"Environmental Science","cited_by":119,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Biogeochemical cycle; Environmental science; Hydrology (agriculture); Drainage basin; Nutrient; STREAMS; Soil science; Environmental chemistry; Geology; Ecology; Chemistry","score_opus":0.017562756396985527,"score_gpt":0.2660803633130244,"score_spread":0.2485176069160389,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986869158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97926784,0.00034699152,0.004103923,0.00005713679,0.0000048192915,0.000011817444,0.014617334,0.00018124384,0.0014088564],"genre_scores_gemma":[0.97895736,0.00021135072,0.0021184843,0.000017287532,0.000007906563,0.000020626949,0.018494124,0.000019770792,0.00015316409],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996432,0.00009383346,0.000043801803,0.00013003072,0.0000652304,0.000023858729],"domain_scores_gemma":[0.9975274,0.00068166666,0.00079399045,0.00053814583,0.00036202886,0.00009675246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012176346,0.0004865032,0.0003814673,0.001991121,0.00009064468,0.0004371162,0.00031837236,0.00027542142,0.00069540576],"category_scores_gemma":[0.002492947,0.0002037904,0.00053778285,0.0024742996,0.00022201973,0.00074348605,0.00081136014,0.00022422131,0.00028318298],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006872662,0.00002584206,0.9535517,0.00010526245,0.00057763304,0.00010038821,0.000071682596,0.023036381,0.0016201519,0.00021354722,0.0011870271,0.019441556],"study_design_scores_gemma":[0.000013244658,0.000059641585,0.95823944,0.0000398083,0.00018494057,0.00012768416,0.00012551164,0.03612921,0.0016188079,0.0003671002,0.0030662953,0.00002831907],"about_ca_topic_score_codex":0.010678724,"about_ca_topic_score_gemma":0.012714703,"teacher_disagreement_score":0.010678724,"about_ca_system_score_codex":0.0002998564,"about_ca_system_score_gemma":0.00022279246,"threshold_uncertainty_score":0.021233141},"labels":[],"label_agreement":null},{"id":"W1992709528","doi":"10.1029/1999gb001206","title":"Approaches for reducing uncertainties in regional forest carbon balance","year":2000,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Harvard University","keywords":"Environmental science; Terrestrial ecosystem; Cycling; Carbon cycle; Ecosystem; Deposition (geology); Climate change; Atmospheric sciences; Physical geography; Ecology; Geography; Forestry; Geology; Biology","score_opus":0.014252142385587929,"score_gpt":0.21112232780231327,"score_spread":0.19687018541672535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992709528","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.016376536,0.0005390534,0.9789781,0.00046054766,0.000041898224,0.000044342654,0.000117600204,0.0002574162,0.003184491],"genre_scores_gemma":[0.41347215,0.00070751546,0.5833949,0.00028097193,0.0000960845,0.00022266773,0.0002480058,0.00019945632,0.0013782902],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987602,0.0005716031,0.000059558428,0.00023442217,0.00029855195,0.00007557666],"domain_scores_gemma":[0.9975872,0.0012483223,0.0002664317,0.00041236245,0.00043604942,0.0000496626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0045632017,0.0012998199,0.0008639317,0.0011482567,0.00056772464,0.001458261,0.002203695,0.0010437916,0.0016695632],"category_scores_gemma":[0.007825138,0.00066893274,0.0011552953,0.0008813131,0.0007966609,0.002121946,0.0026508537,0.0017075879,0.00016976747],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003024385,0.00004018997,0.0014444628,0.00009009225,0.00022311063,0.000033726326,0.00010827558,0.8968576,0.0028749802,0.043006565,0.000672722,0.05461799],"study_design_scores_gemma":[0.000025523424,0.000030913845,0.0005760634,0.000032830194,0.00008982404,0.000014918836,0.00005553402,0.9227218,0.0017489176,0.07061442,0.004051841,0.000037418456],"about_ca_topic_score_codex":0.010404768,"about_ca_topic_score_gemma":0.009846248,"teacher_disagreement_score":0.010404768,"about_ca_system_score_codex":0.0013894506,"about_ca_system_score_gemma":0.0018047076,"threshold_uncertainty_score":0.024132788},"labels":[],"label_agreement":null},{"id":"W1999245469","doi":"10.1029/2000gb001286","title":"<i>Sphagnum</i> peatland distribution in North America and Eurasia during the past 21,000 years","year":2001,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":127,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration","keywords":"Peat; Sphagnum; Boreal; Physical geography; Geology; Deglaciation; Taiga; Abundance (ecology); Spore; Ecology; Geography; Oceanography; Holocene; Forestry; Paleontology; Biology","score_opus":0.004163259381751535,"score_gpt":0.20052439872650732,"score_spread":0.1963611393447558,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999245469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988017,0.00022230903,0.0000391074,0.000020701875,0.0000014739566,0.0000011928738,0.00029458886,0.000007947363,0.0006108816],"genre_scores_gemma":[0.99842834,0.00029086982,0.00014972495,0.00001294943,0.0000031018876,0.0000032121582,0.0005261194,0.0000020339476,0.00058365404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999651,0.0000037181983,0.0000048050247,0.000011110752,0.00000682433,0.000008525867],"domain_scores_gemma":[0.9998265,0.000012346435,0.000093021794,0.00000559215,0.00003730669,0.000025360314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009877826,0.000077662204,0.00007073242,0.0006202281,0.00013210584,0.0002222811,0.00008051506,0.00008149702,0.0004968562],"category_scores_gemma":[0.00016737722,0.00005122418,0.00008154234,0.00044876218,0.00012762524,0.00019672004,0.00016606807,0.00007065476,0.00008019645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000083138024,0.000017646093,0.94779795,0.00009251324,0.00009861978,0.00037949096,0.0011921414,0.00052407477,0.009679337,0.00016291953,0.0009022331,0.039070014],"study_design_scores_gemma":[8.9252006e-7,0.00000788253,0.99833494,0.0000045092443,0.0000058126784,0.000096511336,0.00009156273,0.00006760678,0.0001334958,0.000010659856,0.0012451285,0.0000010672281],"about_ca_topic_score_codex":0.017571284,"about_ca_topic_score_gemma":0.045422774,"teacher_disagreement_score":0.017571284,"about_ca_system_score_codex":0.00023759811,"about_ca_system_score_gemma":0.00016514416,"threshold_uncertainty_score":0.034937978},"labels":[],"label_agreement":null},{"id":"W2007537037","doi":"10.1029/1999gb900101","title":"Winter fluxes of greenhouse gases from snow‐covered agricultural soil:intra‐annual and interannual variations","year":2000,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Soil water; Snow; Environmental science; Temperate climate; Greenhouse gas; Hydrology (agriculture); Atmospheric sciences; Temperate forest; Growing season; Denitrification; Nitrous oxide; Nitrogen; Agronomy; Soil science; Chemistry; Ecology; Geology","score_opus":0.007127485076771408,"score_gpt":0.20614275482543742,"score_spread":0.199015269748666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007537037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986625,0.0001631896,0.00014198346,0.000016373982,0.0000021928693,0.0000036162094,0.0005073317,0.000014123334,0.00048877957],"genre_scores_gemma":[0.9982255,0.000121645215,0.00014999777,0.00001744914,0.0000025619936,0.000006400646,0.0010347541,0.000005563444,0.0004361333],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999305,0.0000049027017,0.0000027448787,0.000018041665,0.000021522117,0.000022263464],"domain_scores_gemma":[0.99976224,0.000032017393,0.000059886348,0.000008374377,0.00010330198,0.00003418762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015905137,0.00023486694,0.00019762886,0.0005546565,0.00044470452,0.0004697843,0.0001619732,0.00017637493,0.00055247446],"category_scores_gemma":[0.00021581564,0.000108126245,0.00011861547,0.00064752845,0.00017959646,0.0002082406,0.0001352929,0.00012410944,0.000096058524],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000235125,0.000031642317,0.96093535,0.000033533648,0.00011535742,0.00011498146,0.00056027446,0.0006955039,0.025908707,0.000043493957,0.00049519364,0.010830866],"study_design_scores_gemma":[0.0000011195485,0.0000054309435,0.9991385,0.0000014319243,0.000004379988,0.000009303117,0.000067389825,0.00022722408,0.00031514282,0.000005435109,0.00022282661,0.0000018006008],"about_ca_topic_score_codex":0.57131976,"about_ca_topic_score_gemma":0.764157,"teacher_disagreement_score":0.57131976,"about_ca_system_score_codex":0.0023923055,"about_ca_system_score_gemma":0.0009788945,"threshold_uncertainty_score":0.86240965},"labels":[],"label_agreement":null},{"id":"W2014163476","doi":"10.1029/1999gb001207","title":"Annual carbon balance of Canada's forests during 1895–1996","year":2000,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":200,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Carbon sink; Atmospheric sciences; Carbon cycle; Forest ecology; Precipitation; Climate change; Ecosystem; Terrestrial ecosystem; Deposition (geology); Physical geography; Ecology; Geography; Meteorology; Biology; Geology","score_opus":0.002467786012036233,"score_gpt":0.17714570868509727,"score_spread":0.17467792267306104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014163476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8109474,0.0042569833,0.0011410681,0.0006659124,0.000072946044,0.00007941117,0.15115644,0.00023823408,0.031441532],"genre_scores_gemma":[0.9345265,0.0025134105,0.0015597513,0.00015196891,0.000015375637,0.00003441975,0.05049042,0.000033359018,0.0106748],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998017,0.000005580759,0.000008120995,0.000032268188,0.000093367256,0.00005910102],"domain_scores_gemma":[0.9996087,0.000009198446,0.000034073597,0.000012526419,0.0002906244,0.000044912766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018964687,0.00043659945,0.00023803256,0.0014315819,0.0015776835,0.0009692518,0.0005152731,0.00024551433,0.0028713879],"category_scores_gemma":[0.00048440674,0.00020788133,0.00033562857,0.0023823346,0.00022689966,0.00041735318,0.0002850928,0.0003192931,0.0004239478],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006609879,0.000103602084,0.71261483,0.0004979222,0.00075495755,0.0007193664,0.0011079656,0.05378796,0.005720109,0.004703291,0.068500094,0.15082882],"study_design_scores_gemma":[0.000032555152,0.000019529169,0.89634454,0.000093736526,0.000100524136,0.000118152835,0.00035636305,0.011992567,0.0015539645,0.00026189812,0.08907481,0.00005134364],"about_ca_topic_score_codex":0.9942021,"about_ca_topic_score_gemma":0.9949479,"teacher_disagreement_score":0.033571325,"about_ca_system_score_codex":0.033571325,"about_ca_system_score_gemma":0.014908709,"threshold_uncertainty_score":0.24357814},"labels":[],"label_agreement":null},{"id":"W2014634808","doi":"10.1029/1999gb001232","title":"Estimating global land use change over the past 300 years: The HYDE Database","year":2001,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":1026,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Rijksinstituut voor Volksgezondheid en Milieu","keywords":"Land use; Global change; Geography; Temperate climate; Population; Land use, land-use change and forestry; Pace; Database; Climate change; Land cover; Agricultural land; Agriculture; Physical geography; Archaeology; Ecology; Demography; Computer science","score_opus":0.017537403650443886,"score_gpt":0.23838830180296555,"score_spread":0.22085089815252168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014634808","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06822628,0.00071998243,0.005216667,0.00021295146,0.00003801685,0.00012564354,0.9164374,0.0015205428,0.007502468],"genre_scores_gemma":[0.114782825,0.0010901948,0.014561946,0.000059768197,0.00003115171,0.00039478272,0.8673166,0.00033882505,0.0014239284],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999624,0.000044907203,0.00009310652,0.000085685206,0.00011538454,0.00003699204],"domain_scores_gemma":[0.99832183,0.000405389,0.00043101507,0.00036969958,0.00032383832,0.00014815373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006472502,0.00063590356,0.0006036823,0.0060677193,0.00019049595,0.0009828887,0.00076848734,0.00058429973,0.004841204],"category_scores_gemma":[0.0027316215,0.0003808832,0.00055577257,0.011073147,0.00023430376,0.0017708678,0.0009729975,0.00040568787,0.002847738],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004482048,0.00023177618,0.41272324,0.0029565669,0.00088279916,0.0012854879,0.0009475751,0.07308746,0.0037519282,0.0070750937,0.28847605,0.20813388],"study_design_scores_gemma":[0.00013373184,0.000096970645,0.48778424,0.0003285083,0.00020919458,0.0008221512,0.0011969842,0.030712893,0.007501219,0.0037685274,0.4672503,0.00019527896],"about_ca_topic_score_codex":0.01936348,"about_ca_topic_score_gemma":0.012217008,"teacher_disagreement_score":0.01936348,"about_ca_system_score_codex":0.00059509836,"about_ca_system_score_gemma":0.00063927367,"threshold_uncertainty_score":0.03850156},"labels":[],"label_agreement":null},{"id":"W2018041230","doi":"10.1002/2014gb004805","title":"Global dry deposition of nitrogen dioxide and sulfur dioxide inferred from space‐based measurements","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Environment Canada; Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Ozone Monitoring Instrument; Flux (metallurgy); Environmental science; Deposition (geology); Satellite; Atmospheric sciences; Nitrogen dioxide; Sulfur dioxide; Atmosphere (unit); Nitrogen; Climatology; Meteorology; Chemistry; Geography; Geology; Troposphere; Physics","score_opus":0.014415104981113046,"score_gpt":0.2203077648055336,"score_spread":0.20589265982442057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018041230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98670363,0.00028847213,0.0071660434,0.000026562133,0.000012753088,0.00001597233,0.003389475,0.00022180151,0.0021753649],"genre_scores_gemma":[0.98963696,0.00020028443,0.0058212853,0.000015169222,0.0000107675605,0.000028536077,0.0038841723,0.000027511112,0.00037544503],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999262,0.000010696333,0.0000048581574,0.000032499396,0.000019742076,0.0000059273348],"domain_scores_gemma":[0.99992573,0.000016777274,0.000022950499,0.0000095241685,0.000019836882,0.000005130295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026252074,0.00056069525,0.00026698114,0.0010503348,0.00012665971,0.0002874301,0.00017458279,0.00018512334,0.00045049956],"category_scores_gemma":[0.00023556373,0.00019276401,0.0003829596,0.00081187254,0.00013213065,0.00026283305,0.00023961307,0.000083352286,0.00013831645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023612457,0.000049659022,0.801595,0.0002012837,0.00056565093,0.0001701001,0.0001690773,0.07992714,0.0744851,0.0007127751,0.0010468261,0.040841375],"study_design_scores_gemma":[0.000031280284,0.000044046985,0.8929249,0.00001693781,0.00011194275,0.000054551547,0.00006280784,0.08949779,0.014196464,0.00041423304,0.0026164385,0.000028547918],"about_ca_topic_score_codex":0.012099257,"about_ca_topic_score_gemma":0.015337051,"teacher_disagreement_score":0.012099257,"about_ca_system_score_codex":0.00042417416,"about_ca_system_score_gemma":0.0002531559,"threshold_uncertainty_score":0.024057686},"labels":[],"label_agreement":null},{"id":"W2032782847","doi":"10.1029/2000gb001346","title":"Carbon accumulation in bay of fundy salt marshes: Implications for restoration of reclaimed marshes","year":2001,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Natural Sciences and Engineering Research Council of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Salt marsh; Bay; Marsh; Environmental science; Hydrology (agriculture); Sediment; Blue carbon; Soil carbon; Vegetation (pathology); Carbon sequestration; Wetland; Total organic carbon; Oceanography; Soil water; Geology; Ecology; Soil science; Carbon dioxide; Geomorphology; Biology","score_opus":0.024864481004754933,"score_gpt":0.28205135711892626,"score_spread":0.25718687611417135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032782847","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99933225,0.0001226394,0.00006485647,0.00013696255,0.000002355297,0.000003766253,0.00006590608,0.0000040063196,0.00026718044],"genre_scores_gemma":[0.9994986,0.00013640901,0.00018154398,0.000015004354,0.0000029743478,0.0000028119955,0.000044565913,9.225064e-7,0.00011710041],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990714,0.00001543613,0.000009406178,0.00001999726,0.000016452608,0.000031582153],"domain_scores_gemma":[0.9990852,0.000090138,0.0003640632,0.000035799345,0.00017148814,0.00025330894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038144572,0.0001856094,0.00018881095,0.0005574835,0.00042151622,0.0006938487,0.0003574573,0.0003001693,0.0007423105],"category_scores_gemma":[0.0012717946,0.000088527275,0.00014551125,0.00059006247,0.0005008171,0.00048606796,0.00047694464,0.00018748452,0.000065555716],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019731185,0.000056844292,0.9720097,0.00006190087,0.000029159146,0.0003222344,0.0006023002,0.00092350016,0.007906358,0.00009272821,0.00013850923,0.017659465],"study_design_scores_gemma":[0.0000010568957,0.000027697113,0.998868,0.00000627597,0.0000030927001,0.000031918273,0.00031063243,0.0003701361,0.00018513964,0.000017667202,0.00017610133,0.0000022503627],"about_ca_topic_score_codex":0.056430124,"about_ca_topic_score_gemma":0.14550538,"teacher_disagreement_score":0.9435699,"about_ca_system_score_codex":0.0010814654,"about_ca_system_score_gemma":0.0010300624,"threshold_uncertainty_score":0.11220336},"labels":[],"label_agreement":null},{"id":"W2049664370","doi":"10.1029/2000gb001306","title":"Controls on carbon and energy exchange by a black spruce–moss ecosystem: Testing the mathematical model <i>Ecosys</i> with data from the BOREAS Experiment","year":2001,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Black spruce; Moss; Taiga; Boreal; Environmental science; Transpiration; Mineralization (soil science); Soil water; Ecosystem; Canopy; Environmental chemistry; Plant litter; Forest floor; Chemistry; Ecology; Atmospheric sciences; Photosynthesis; Soil science; Geology; Biology","score_opus":0.022377997339194183,"score_gpt":0.23301399139912943,"score_spread":0.21063599405993524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049664370","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99869424,0.000022238804,0.00080860587,0.000036198664,0.0000028927589,0.00000633253,0.00011097463,0.000023054125,0.00029548255],"genre_scores_gemma":[0.9989039,0.000019521014,0.00076311623,0.000010600747,0.0000019496447,0.000012055002,0.00009782014,0.000008354526,0.00018272786],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998073,0.000068613386,0.000017222666,0.00004965175,0.000018318455,0.000038792896],"domain_scores_gemma":[0.9982843,0.00119435,0.00022481364,0.000073823976,0.00009839766,0.00012430649],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012314117,0.0006059327,0.00045455268,0.00020764876,0.00038409964,0.00075037155,0.00076150685,0.00042679516,0.0012728997],"category_scores_gemma":[0.0014523427,0.00026644536,0.000855915,0.0001353782,0.00055126805,0.0007318517,0.0004544801,0.00042782046,0.00008504688],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016970643,0.00036840755,0.042357963,0.000115125775,0.00022943843,0.00020063725,0.00013135669,0.9267006,0.021230599,0.0035687778,0.00042673163,0.002973328],"study_design_scores_gemma":[0.00015988016,0.00032539992,0.015980067,0.000004141857,0.00006776832,0.000021112946,0.000047771908,0.97930783,0.0031158892,0.00072332646,0.00022534892,0.000021471255],"about_ca_topic_score_codex":0.054778136,"about_ca_topic_score_gemma":0.029161628,"teacher_disagreement_score":0.054778136,"about_ca_system_score_codex":0.0016819775,"about_ca_system_score_gemma":0.00077843125,"threshold_uncertainty_score":0.10891855},"labels":[],"label_agreement":null},{"id":"W2050834159","doi":"10.1029/2000gb001312","title":"Carbon accumulation in West Siberian Mires, Russia <i>Sphagnum</i> peatland distribution in North America and Eurasia during the past 21,000 years","year":2001,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":158,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Academy of Finland","keywords":"Bog; Peat; Boreal; Mire; Holocene; Carbon sink; Sphagnum; Physical geography; Charcoal; Shrub; Wetland; Carbon cycle; Geology; Environmental science; Ecology; Geography; Chemistry; Paleontology; Oceanography; Climate change; Ecosystem; Biology","score_opus":0.006513227761343674,"score_gpt":0.2207447322441679,"score_spread":0.21423150448282424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050834159","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99962986,0.00010717079,0.000013989874,0.000005857565,9.401538e-7,4.4034715e-7,0.000116996795,0.0000021172998,0.00012267988],"genre_scores_gemma":[0.99941576,0.00012474481,0.00003804095,0.0000040360655,0.0000017613221,0.0000015498645,0.00028741654,9.41404e-7,0.00012565881],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993587,0.000009262329,0.000012116156,0.0000179526,0.000012271738,0.000012509887],"domain_scores_gemma":[0.9998423,0.000018259445,0.00007584689,0.000010149071,0.000028504004,0.000025035057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025445584,0.00016451236,0.00015192853,0.00087237044,0.00025376584,0.00038383697,0.00011242787,0.00012285181,0.0003513487],"category_scores_gemma":[0.00026394226,0.000093646275,0.00015664144,0.0005714878,0.00020351817,0.00021205998,0.0002836764,0.000096371485,0.00009499703],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006339274,0.000011746087,0.9892553,0.000029324428,0.00006657348,0.00021168753,0.00047793795,0.00024906636,0.0034685263,0.000039566145,0.00007797848,0.006048891],"study_design_scores_gemma":[3.927848e-7,0.000005756462,0.9996511,0.0000017996255,0.000004544409,0.000029624396,0.00005564516,0.000065350025,0.00007060425,0.0000033540468,0.00011109716,8.016143e-7],"about_ca_topic_score_codex":0.0188558,"about_ca_topic_score_gemma":0.035279624,"teacher_disagreement_score":0.0188558,"about_ca_system_score_codex":0.00043939747,"about_ca_system_score_gemma":0.00023428367,"threshold_uncertainty_score":0.037492096},"labels":[],"label_agreement":null},{"id":"W2053150180","doi":"10.1002/2013gb004580","title":"Observational constraints on the distribution, seasonality, and environmental predictors of North American boreal methane emissions","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"U.S. Department of Energy","keywords":"Atmospheric methane; Methane; Environmental science; Biogeochemical cycle; Wetland; Flux (metallurgy); Atmospheric sciences; Bay; Climatology; Oceanography; Geology; Ecology; Environmental chemistry; Chemistry","score_opus":0.009029017221516524,"score_gpt":0.21458758238776873,"score_spread":0.2055585651662522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053150180","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960892,0.00014868131,0.0005144487,0.00011103489,0.0000039017204,0.000003210778,0.0011260203,0.000018091201,0.0019854004],"genre_scores_gemma":[0.99806553,0.00011978189,0.00034275776,0.000034469685,0.000004225839,0.0000037421792,0.0012522454,0.000005849459,0.00017134596],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99960154,0.00008137699,0.000027989403,0.00011908578,0.000092487426,0.000077512625],"domain_scores_gemma":[0.9980545,0.00063724734,0.00042396176,0.00020132007,0.00055815524,0.00012491716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010043307,0.00021144217,0.0001654127,0.0005693229,0.00065678894,0.00054287014,0.00032309224,0.00017280951,0.00070928165],"category_scores_gemma":[0.0030349393,0.00019946917,0.0002123473,0.0009644562,0.0005103963,0.0004737441,0.00038461975,0.00025663548,0.000066520035],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038036804,0.00001758575,0.98923033,0.000015940306,0.00005131804,0.000025711477,0.00032883236,0.0016816816,0.0012645847,0.00023300078,0.0005972681,0.0065158196],"study_design_scores_gemma":[0.0000011645756,0.000001767052,0.9977308,0.000004718443,0.0000104229375,0.000010649383,0.00018967775,0.0013451648,0.00006873166,0.00005170351,0.0005801784,0.000005030671],"about_ca_topic_score_codex":0.73479706,"about_ca_topic_score_gemma":0.9041325,"teacher_disagreement_score":0.26520294,"about_ca_system_score_codex":0.001378799,"about_ca_system_score_gemma":0.0020756854,"threshold_uncertainty_score":0.5335295},"labels":[],"label_agreement":null},{"id":"W2080284689","doi":"10.1029/2010gb004003","title":"Primary production and carbon export rates across the subpolar N. Atlantic Ocean basin based on triple oxygen isotope and dissolved O<sub>2</sub> and Ar gas measurements","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Dissolved organic carbon; Primary production; Animal science; Oceanography; Chemistry; Geology; Ecosystem; Biology; Ecology","score_opus":0.013457510048899776,"score_gpt":0.209720813805937,"score_spread":0.1962633037570372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080284689","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99817884,0.00007857039,0.00015338157,0.000015147879,0.0000024517037,0.0000033371991,0.0008498102,0.0000077818595,0.0007106385],"genre_scores_gemma":[0.9970283,0.00016870488,0.00031652808,0.000018404511,0.0000047021836,0.000008699788,0.0018504574,0.0000051689653,0.0005990492],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995816,0.0000043107743,0.0000034064628,0.00001775017,0.000008891651,0.0000073851943],"domain_scores_gemma":[0.9997998,0.000036358444,0.000054478092,0.000011162886,0.00005535009,0.00004292111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015213541,0.00028058095,0.00012402049,0.0003515274,0.00018325665,0.0003683599,0.00010657135,0.000109272114,0.0007459714],"category_scores_gemma":[0.00023430175,0.00013255795,0.00017574221,0.00033439047,0.00013166982,0.00020294497,0.00018611534,0.00014088323,0.00015726913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015785442,0.000014888246,0.9784614,0.000017842023,0.000062848085,0.00009214216,0.00012849958,0.00071229966,0.014857419,0.00005515578,0.00022389383,0.0052156067],"study_design_scores_gemma":[0.0000018057337,0.0000060489033,0.9992079,7.114647e-7,0.0000060543166,0.000011424665,0.000022122445,0.00043911464,0.00017907027,0.00000974841,0.00011520481,8.872571e-7],"about_ca_topic_score_codex":0.06158256,"about_ca_topic_score_gemma":0.14489913,"teacher_disagreement_score":0.06158256,"about_ca_system_score_codex":0.00049699337,"about_ca_system_score_gemma":0.00019679546,"threshold_uncertainty_score":0.122448206},"labels":[],"label_agreement":null},{"id":"W2081128107","doi":"10.1029/2003gb002050","title":"Dissolved organic carbon in a northern boreal landscape","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":121,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Dissolved organic carbon; Throughfall; Environmental science; Hydrology (agriculture); Stemflow; Peat; Wetland; Surface runoff; Bog; Total organic carbon; Boreal; Soil water; Environmental chemistry; Soil science; Chemistry; Geology; Ecology","score_opus":0.005228622752040195,"score_gpt":0.2080346346437194,"score_spread":0.2028060118916792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081128107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997124,0.000045041612,0.000014713727,0.000009687505,7.338014e-7,0.0000015928119,0.00006285402,0.0000014365176,0.00015147998],"genre_scores_gemma":[0.9993825,0.00006373426,0.00013422585,0.000024128241,0.0000023184427,0.0000029334565,0.00022799683,9.842832e-7,0.00016133451],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992144,0.0000097237635,0.000003774113,0.00002531314,0.000020396592,0.000019286921],"domain_scores_gemma":[0.9998605,0.000008918586,0.00004748804,0.0000049915316,0.000038075596,0.000040028848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001097889,0.00015146768,0.00013252838,0.0003194307,0.0007564379,0.0005485516,0.00014629368,0.00013456815,0.00020204466],"category_scores_gemma":[0.00024115828,0.00013789767,0.000107158616,0.0004914864,0.000265752,0.0002022723,0.00021255737,0.00012679446,0.00003543936],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007354156,0.00004514207,0.9863012,0.000012207792,0.000028928005,0.0002142384,0.00071839895,0.00014991307,0.007692485,0.000025929807,0.000087562614,0.0046504354],"study_design_scores_gemma":[0.000001701955,0.000018019884,0.99917775,0.0000012134532,0.000005415413,0.00006225692,0.0002807902,0.00010662331,0.00009577743,0.0000072815246,0.00024131617,0.0000017974633],"about_ca_topic_score_codex":0.47612482,"about_ca_topic_score_gemma":0.7758721,"teacher_disagreement_score":0.47612482,"about_ca_system_score_codex":0.0015708862,"about_ca_system_score_gemma":0.0006523224,"threshold_uncertainty_score":0.94670695},"labels":[],"label_agreement":null},{"id":"W2093267972","doi":"10.1029/2002gb001917","title":"Global carbon sequestration in tidal, saline wetland soils","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":1778,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Wetland; Mangrove; Salt marsh; Blue carbon; Marsh; Environmental science; Carbon sequestration; Swamp; Brackish marsh; Soil carbon; Peat; Carbon sink; Ecosystem; Hydrology (agriculture); Spartina; Oceanography; Carbon cycle; Ecology; Soil water; Geology; Climate change; Carbon dioxide; Soil science; Biology","score_opus":0.007242845141338563,"score_gpt":0.22730396863222427,"score_spread":0.22006112349088572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093267972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957241,0.00050804,0.00015670493,0.00009034958,0.0000043171785,0.0000023600348,0.0019780835,0.000033420267,0.0015026031],"genre_scores_gemma":[0.9981997,0.00037424234,0.00016570353,0.000017734068,0.000005566697,0.0000038077021,0.0010559425,0.0000034565069,0.00017385365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995625,0.0000072020107,0.000004035422,0.000013766144,0.000007725208,0.000011034792],"domain_scores_gemma":[0.9999057,0.000007524781,0.000039946608,0.000010937471,0.000018879917,0.000017077482],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001311902,0.0002439226,0.0001599978,0.00073880475,0.00011543841,0.0003033315,0.00011527615,0.00019699823,0.0008004523],"category_scores_gemma":[0.00018276351,0.00007920766,0.00016151901,0.0011425568,0.00015979153,0.00030872517,0.00030392752,0.000072575305,0.00019939005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010507097,0.000022058039,0.95075023,0.00010187741,0.00021628727,0.00015576078,0.00017206355,0.0044949786,0.01574222,0.0007163051,0.0009865883,0.026536597],"study_design_scores_gemma":[0.0000034106597,0.000014470574,0.99659663,0.0000067701303,0.000033940614,0.00005151856,0.0000686697,0.0010113975,0.0004549505,0.00022790748,0.0015261164,0.0000042135393],"about_ca_topic_score_codex":0.008800247,"about_ca_topic_score_gemma":0.012886927,"teacher_disagreement_score":0.008800247,"about_ca_system_score_codex":0.00028572898,"about_ca_system_score_gemma":0.00021038076,"threshold_uncertainty_score":0.017498016},"labels":[],"label_agreement":null},{"id":"W2094785557","doi":"10.1029/1999gb900059","title":"Iron supply and demand in the upper ocean","year":2000,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":553,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration; U.S. Department of Energy; University of Victoria; National Science Foundation","keywords":"Upwelling; Phytoplankton; Photic zone; New production; Nitrate; Environmental science; Iron fertilization; Flux (metallurgy); Oceanography; Nutrient; Environmental chemistry; Chemistry; Geology","score_opus":0.005355613089244463,"score_gpt":0.19220593755947005,"score_spread":0.1868503244702256,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094785557","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98720205,0.0006361436,0.00052677514,0.00017782737,0.0000038663784,0.0000035608284,0.00082568295,0.00001633409,0.010607825],"genre_scores_gemma":[0.99666214,0.00036128095,0.0003978977,0.000044032677,0.00000713658,0.0000049054092,0.0005678738,0.0000074180953,0.0019472991],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993384,0.0000052621613,0.0000043596947,0.000016812615,0.000024589406,0.000015104934],"domain_scores_gemma":[0.9999132,0.000018618328,0.000019746318,0.0000059015324,0.000021864147,0.000020692229],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000072926625,0.00017120663,0.00025050994,0.00033624747,0.00020121415,0.00071506377,0.00016015072,0.00025350854,0.0017325445],"category_scores_gemma":[0.00034657182,0.000159429,0.00014775108,0.00044753597,0.00016991905,0.00029500748,0.00040840855,0.00013393459,0.00043179613],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045973185,0.00005257109,0.75502014,0.00032648153,0.00011714885,0.00080236135,0.0007061437,0.02373044,0.12459506,0.007886168,0.0018678078,0.08443595],"study_design_scores_gemma":[0.000014369235,0.00004107484,0.9685884,0.000030076108,0.000027481672,0.0001671331,0.0004525048,0.01678924,0.0031976937,0.003306324,0.007366418,0.000019271156],"about_ca_topic_score_codex":0.03239787,"about_ca_topic_score_gemma":0.020905292,"teacher_disagreement_score":0.03239787,"about_ca_system_score_codex":0.00071634026,"about_ca_system_score_gemma":0.0004769619,"threshold_uncertainty_score":0.064418554},"labels":[],"label_agreement":null},{"id":"W2095102607","doi":"10.1029/1999gb001243","title":"Interannual variability of net ecosystem CO<sub>2</sub> exchange at a subarctic fen","year":2000,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":142,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Subarctic climate; Environmental science; Ecosystem respiration; Ecosystem; Carbon sink; Wetland; Phenology; Growing season; Sink (geography); Snowmelt; Carbon cycle; Atmospheric sciences; Climatology; Primary production; Hydrology (agriculture); Ecology; Oceanography; Geography; Surface runoff; Geology","score_opus":0.006218277583068053,"score_gpt":0.21755153655111445,"score_spread":0.2113332589680464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095102607","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99958104,0.000019098141,0.00006155074,0.000008319595,0.0000016437543,9.2896477e-7,0.0001379882,0.0000036233832,0.00018577128],"genre_scores_gemma":[0.9995359,0.000014048305,0.000044238757,0.0000053665913,0.0000024657859,0.0000026124662,0.00026252965,0.000001931481,0.00013083073],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999411,0.0000101338155,0.000004003931,0.000015482685,0.000013998062,0.000015212702],"domain_scores_gemma":[0.9996377,0.00008517798,0.000087755936,0.000028401717,0.000100914134,0.000060025828],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026432553,0.00011045308,0.00013061389,0.00046262163,0.00023271746,0.0002694866,0.00012423815,0.00015236303,0.0004780049],"category_scores_gemma":[0.00050518854,0.000082100836,0.00008042061,0.0003180017,0.00016858024,0.0001685415,0.00016815384,0.00016032584,0.000112278314],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011102244,0.000048922815,0.9866955,0.000009153746,0.000063114116,0.000089328394,0.00034626471,0.0006658562,0.0067374264,0.000050133018,0.00028715114,0.0048961863],"study_design_scores_gemma":[6.552427e-7,0.0000065742,0.9993272,7.0268857e-7,0.0000037944696,0.000017020333,0.000040347437,0.00037968936,0.00012045071,0.000008320639,0.000093950264,0.0000013593334],"about_ca_topic_score_codex":0.020904668,"about_ca_topic_score_gemma":0.05352023,"teacher_disagreement_score":0.020904668,"about_ca_system_score_codex":0.00034513226,"about_ca_system_score_gemma":0.00013815485,"threshold_uncertainty_score":0.041565955},"labels":[],"label_agreement":null},{"id":"W2096467657","doi":"10.1029/2011gb004246","title":"A meta‐analysis of water vapor deuterium‐excess in the midlatitude atmospheric surface layer","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ministry of Science and Technology of the People's Republic of China; Chinese Academy of Sciences; Ministry of Education of the People's Republic of China; National Natural Science Foundation of China; CERN","keywords":"Atmospheric sciences; Environmental science; Water vapor; Planetary boundary layer; Relative humidity; Diurnal cycle; Atmosphere (unit); Surface layer; Flux (metallurgy); Climatology; Geology; Turbulence; Chemistry; Layer (electronics); Geography; Meteorology","score_opus":0.0334830753289103,"score_gpt":0.25024597444788443,"score_spread":0.21676289911897412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096467657","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.78791887,0.17175154,0.0065777847,0.0014098954,0.000759738,0.000066789486,0.029513976,0.00042921538,0.0015721943],"genre_scores_gemma":[0.9843592,0.006072887,0.0021710086,0.00026726766,0.0000965805,0.000054352655,0.006678851,0.000072550654,0.00022722875],"study_design_codex":"observational","study_design_gemma":"meta_analysis","domain_scores_codex":[0.9974899,0.00093923934,0.0002793365,0.00090745685,0.00020308116,0.00018094275],"domain_scores_gemma":[0.9963032,0.0017981518,0.00043936947,0.00086282106,0.0003801204,0.00021626904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0044288365,0.0011390878,0.00230361,0.0033520544,0.00057634746,0.0017418507,0.0013791018,0.0009507155,0.0015738808],"category_scores_gemma":[0.0047523957,0.00068961387,0.009839723,0.005268454,0.0002998838,0.0009861238,0.0010384455,0.0009326493,0.0002913867],"study_design_candidate":"meta_analysis","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015441164,0.00006465976,0.6325881,0.0057755383,0.3324635,0.00040971473,0.00027070448,0.0018109229,0.0047874567,0.00035626235,0.0030487138,0.016880374],"study_design_scores_gemma":[0.00019137924,0.0002291707,0.80944175,0.0008415255,0.17349201,0.00032907477,0.0005536688,0.004581856,0.0021538564,0.00057209167,0.007528377,0.00008529406],"about_ca_topic_score_codex":0.012559838,"about_ca_topic_score_gemma":0.021026218,"teacher_disagreement_score":0.012559838,"about_ca_system_score_codex":0.00046879862,"about_ca_system_score_gemma":0.0008346675,"threshold_uncertainty_score":0.024973452},"labels":[],"label_agreement":null},{"id":"W2096896799","doi":"10.1029/2011gb004096","title":"Nitrogen fixation and identification of potential diazotrophs in the Canadian Arctic","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":150,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Université du Québec à Rimouski","funders":"","keywords":"Diazotroph; Nitrogen fixation; Arctic; Bay; Biology; Fjord; Oceanography; Ecology; Geology; Bacteria; Paleontology","score_opus":0.007764890809288589,"score_gpt":0.19925937179697337,"score_spread":0.1914944809876848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096896799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967141,0.00049195474,0.00020774096,0.000037523954,0.0000022441957,0.000013367131,0.0007337342,0.00000751914,0.0017917443],"genre_scores_gemma":[0.9958116,0.0006240511,0.0012823497,0.00003486032,0.0000017068547,0.000012340936,0.0010417434,0.0000051422553,0.0011862393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996383,0.00001952326,0.000011801141,0.00007158454,0.0001270956,0.00013157951],"domain_scores_gemma":[0.999516,0.000025816895,0.00005293485,0.000014099726,0.00029800896,0.00009314415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043058724,0.00042362057,0.000283572,0.0019145391,0.0034090574,0.00079998374,0.0004593731,0.00026512158,0.00049334724],"category_scores_gemma":[0.00067077426,0.00029768219,0.00029273526,0.0021619154,0.00042064456,0.0001713229,0.00063877914,0.00020881837,0.00011315353],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034858767,0.000041196,0.9179523,0.00014664428,0.00008177284,0.0003551461,0.0021065003,0.0016021283,0.053115115,0.0003542092,0.00073273206,0.023163665],"study_design_scores_gemma":[0.000006119899,0.000037020516,0.991248,0.00002372474,0.00003423159,0.00011665438,0.0014331135,0.0011257618,0.002990021,0.000043447868,0.0029195945,0.000022263454],"about_ca_topic_score_codex":0.9843413,"about_ca_topic_score_gemma":0.9940268,"teacher_disagreement_score":0.015658677,"about_ca_system_score_codex":0.008384274,"about_ca_system_score_gemma":0.011744657,"threshold_uncertainty_score":0.06083244},"labels":[],"label_agreement":null},{"id":"W2098142712","doi":"10.1029/2005gb002508","title":"Origin of the deep Bering Sea nitrate deficit: Constraints from the nitrogen and oxygen isotopic composition of water column nitrate and benthic nitrate fluxes","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Denitrification; Nitrate; Benthic zone; Water column; Environmental science; Nitrogen; Environmental chemistry; Hydrology (agriculture); Oceanography; Geology; Chemistry","score_opus":0.00845112448772732,"score_gpt":0.19496592367794785,"score_spread":0.18651479919022054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098142712","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975872,0.00070855574,0.00057237706,0.000034717992,0.00000698062,0.0000026086911,0.00018556186,0.000011498762,0.00089044595],"genre_scores_gemma":[0.9986092,0.00030714268,0.00058166025,0.000024889081,0.0000056675326,0.0000050270155,0.00022067892,0.000010038907,0.00023559397],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999013,0.000008886094,0.000007755143,0.000049977298,0.000015446349,0.00001655169],"domain_scores_gemma":[0.9998043,0.00003609724,0.00006890164,0.000012825838,0.00003764252,0.000040262126],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002885616,0.0004990729,0.00039739587,0.00033545468,0.00022114844,0.00051754643,0.00026204687,0.0002958341,0.0003234744],"category_scores_gemma":[0.00038941877,0.00026722281,0.00016375877,0.00026550988,0.0004190021,0.000530553,0.00047326006,0.00027103574,0.00014672423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005528188,0.000034311866,0.659303,0.00018250226,0.00008404256,0.00045346317,0.0002435122,0.0037534414,0.31744862,0.0006811539,0.00016199611,0.017101197],"study_design_scores_gemma":[0.000010861549,0.00005047682,0.98653316,0.000014150359,0.0000259273,0.00008119736,0.00008916255,0.0042892965,0.007867186,0.00034132056,0.000683859,0.000013450521],"about_ca_topic_score_codex":0.017578999,"about_ca_topic_score_gemma":0.021670254,"teacher_disagreement_score":0.017578999,"about_ca_system_score_codex":0.00095573236,"about_ca_system_score_gemma":0.0004894121,"threshold_uncertainty_score":0.034953356},"labels":[],"label_agreement":null},{"id":"W2098226271","doi":"10.1002/gbc.20016","title":"Annual cycle of air‐sea CO<sub>2</sub> exchange in an Arctic Polynya Region","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; Fisheries and Oceans Canada; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Excellence Research Chairs, Government of Canada","keywords":"Environmental science; Atmospheric sciences; Climatology; Sea ice; Sink (geography); Outgassing; Arctic; Annual cycle; Wind speed; Oceanography; Geology; Chemistry; Geography","score_opus":0.008878709728561727,"score_gpt":0.2166535550828561,"score_spread":0.20777484535429439,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098226271","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99900466,0.000034053624,0.000092479815,0.000018290088,0.0000025045008,0.0000030011274,0.00037598266,0.000010495934,0.0004585461],"genre_scores_gemma":[0.99875903,0.00005064051,0.00022162807,0.000014094141,0.000002899833,0.0000054992906,0.0006938422,0.0000036424847,0.00024887393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999467,0.0000069472753,0.0000034388752,0.000014780724,0.000017117676,0.000010887341],"domain_scores_gemma":[0.99978334,0.000021387174,0.00003915838,0.000013251537,0.00008510122,0.00005770705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018737673,0.00015247567,0.00012384841,0.00036659112,0.00044057664,0.00030998926,0.00014548392,0.0001191001,0.00032388637],"category_scores_gemma":[0.00031776467,0.0000912589,0.00009228947,0.00033537313,0.00020160148,0.00012743809,0.00020009052,0.00014137858,0.00007940883],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000112690046,0.000035020454,0.97849977,0.00002270388,0.00011127449,0.00011188465,0.0004709242,0.0015264399,0.0098557845,0.000092301896,0.0007292669,0.008431921],"study_design_scores_gemma":[0.0000012371787,0.000007347969,0.99842715,0.0000015993495,0.000005810339,0.000018034652,0.000061367566,0.0008099635,0.00026449235,0.0000075010817,0.00039299674,0.0000025330362],"about_ca_topic_score_codex":0.30891597,"about_ca_topic_score_gemma":0.46757314,"teacher_disagreement_score":0.30891597,"about_ca_system_score_codex":0.0011871029,"about_ca_system_score_gemma":0.0006685513,"threshold_uncertainty_score":0.61423576},"labels":[],"label_agreement":null},{"id":"W2099008009","doi":"10.1029/2004gb002351","title":"A comparison of methane flux in a boreal landscape between a dry and a wet year","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":146,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University; York University; National Aeronautics and Space Administration","keywords":"Environmental science; Permafrost; Flux (metallurgy); Wetland; Boreal; Soil water; Taiga; Atmospheric sciences; Atmosphere (unit); Spatial variability; Land cover; Precipitation; Hydrology (agriculture); Physical geography; Geology; Soil science; Oceanography; Geography; Ecology; Land use; Forestry; Chemistry; Meteorology","score_opus":0.012685848624363,"score_gpt":0.2749690229708365,"score_spread":0.26228317434647347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099008009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99966085,0.000020406178,0.000040837527,0.0000047642366,0.0000012698712,0.0000012663531,0.00012228431,0.0000034508869,0.00014482539],"genre_scores_gemma":[0.99930954,0.000020148627,0.00010913102,0.000008952828,0.0000033445338,0.000003294227,0.00045867116,0.0000021538917,0.00008483722],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990666,0.000020603266,0.000006462937,0.000027854427,0.000018472576,0.000019970455],"domain_scores_gemma":[0.9997336,0.00005347871,0.00009244665,0.000022235765,0.000040493625,0.000057664023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002766106,0.00019989927,0.00015586788,0.0005801392,0.0002852306,0.00039226288,0.00017556956,0.00019512099,0.00038556082],"category_scores_gemma":[0.00054121815,0.00013222391,0.00018988608,0.00038398596,0.00023440385,0.00030024114,0.00017322505,0.000115036884,0.00005468452],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007852421,0.00013348012,0.9715919,0.00001994827,0.00012596314,0.00018338615,0.00029312234,0.000911602,0.020400211,0.00007342412,0.00014852946,0.0053332592],"study_design_scores_gemma":[0.0000029032747,0.000023595161,0.99949825,4.679681e-7,0.0000045648835,0.000023523422,0.000032428223,0.00022248251,0.00013498352,0.000005788599,0.000049393027,0.0000015075109],"about_ca_topic_score_codex":0.025598383,"about_ca_topic_score_gemma":0.049846582,"teacher_disagreement_score":0.025598383,"about_ca_system_score_codex":0.0003819615,"about_ca_system_score_gemma":0.00011223314,"threshold_uncertainty_score":0.05089873},"labels":[],"label_agreement":null},{"id":"W2099063502","doi":"10.1029/2001gb001850","title":"The application and interpretation of Keeling plots in terrestrial carbon cycle research","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":789,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Lethbridge","funders":"","keywords":"Ecosystem; Environmental science; Carbon cycle; Terrestrial ecosystem; Carbon sink; Isotopes of carbon; Eddy covariance; Atmospheric sciences; δ13C; Carbon flux; Ecosystem respiration; Stable isotope ratio; Ecology; Physical geography; Total organic carbon; Biology; Geography; Physics","score_opus":0.00994069893351847,"score_gpt":0.2652137609550973,"score_spread":0.25527306202157884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099063502","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3830431,0.0028502708,0.6008391,0.00016234894,0.00020757025,0.00031502583,0.0022427915,0.0017905274,0.008549296],"genre_scores_gemma":[0.687199,0.0006213208,0.30994296,0.000042816875,0.0000690575,0.00025557505,0.0007564373,0.00047111837,0.0006416807],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99521834,0.0032649052,0.0003589211,0.0005853993,0.0004966253,0.00007585211],"domain_scores_gemma":[0.965721,0.026226742,0.0030450826,0.0030066296,0.0017549394,0.000245548],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.011310304,0.0005810715,0.0005183993,0.0039075543,0.00074367493,0.0021873564,0.00069886446,0.00039663096,0.001830534],"category_scores_gemma":[0.03743416,0.00039616993,0.00043787985,0.0054956246,0.0013614589,0.0015947782,0.0010667711,0.00069899706,0.00028244389],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00071992446,0.00011874943,0.3170042,0.0012872316,0.0008096297,0.00072264916,0.00592457,0.048345674,0.02695313,0.03884338,0.004192922,0.55507797],"study_design_scores_gemma":[0.000095895935,0.0003677145,0.6747818,0.00042672147,0.00020480306,0.0013741653,0.0030501469,0.14043619,0.019796787,0.103458956,0.055724468,0.0002823615],"about_ca_topic_score_codex":0.0023862568,"about_ca_topic_score_gemma":0.0063225944,"teacher_disagreement_score":0.011310304,"about_ca_system_score_codex":0.00048713776,"about_ca_system_score_gemma":0.0004883761,"threshold_uncertainty_score":0.059815347},"labels":[],"label_agreement":null},{"id":"W2102622779","doi":"10.1029/2007gb002953","title":"Future changes in climate, ocean circulation, ecosystems, and biogeochemical cycling simulated for a business‐as‐usual CO<sub>2</sub> emission scenario until year 4000 AD","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":449,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"","keywords":"Biogeochemical cycle; Environmental science; Ocean gyre; Carbon cycle; Oceanography; Climatology; Atmospheric sciences; Ocean current; Subtropics; Ecosystem; Geology; Chemistry; Environmental chemistry","score_opus":0.015065650644833607,"score_gpt":0.25003873640261204,"score_spread":0.23497308575777842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102622779","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98941654,0.000087158274,0.0031540217,0.00031564306,0.000056792967,0.000016140999,0.0020493462,0.00009710957,0.0048072184],"genre_scores_gemma":[0.99561995,0.00009424271,0.0014205032,0.00004672022,0.0000102518015,0.000035027886,0.001339284,0.000021517357,0.0014125457],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992955,0.000025382868,0.000003534993,0.000015035969,0.00000943845,0.000017059072],"domain_scores_gemma":[0.99966145,0.00013608481,0.000051828418,0.000020481488,0.00006555826,0.00006455159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034341376,0.0006147136,0.0003694526,0.0003101397,0.00041215503,0.00062164787,0.0005202425,0.00094330823,0.002084081],"category_scores_gemma":[0.0009065131,0.0003145147,0.0005860997,0.00047690966,0.00039260968,0.0007116077,0.00028225087,0.00065541704,0.00018188506],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008182023,0.00002908168,0.008761512,0.000014102883,0.000030875293,0.00006914645,0.000011073112,0.9888032,0.0005449127,0.00061357627,0.00039015122,0.0006504868],"study_design_scores_gemma":[0.000064408174,0.000059225687,0.0062248907,0.000006521262,0.000032726562,0.00003317979,0.000046086407,0.991736,0.0003958712,0.0006282263,0.0007555388,0.000017340515],"about_ca_topic_score_codex":0.060158063,"about_ca_topic_score_gemma":0.035926603,"teacher_disagreement_score":0.060158063,"about_ca_system_score_codex":0.0014367972,"about_ca_system_score_gemma":0.0008073709,"threshold_uncertainty_score":0.11961585},"labels":[],"label_agreement":null},{"id":"W2102761435","doi":"10.1029/2005gb002557","title":"Wintertime phytoplankton bloom in the subarctic Pacific supported by continental margin iron","year":2006,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":219,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; Argonne National Laboratory; Basic Energy Sciences; Biological and Environmental Research; Natural Sciences and Engineering Research Council of Canada; U.S. Department of Energy; Office of Science; National Science Foundation","keywords":"Subarctic climate; Continental margin; Oceanography; Continental shelf; Geology; Phytoplankton; Bloom; Iron fertilization; Oxygen minimum zone; Southern Hemisphere; Upwelling; Paleontology; Climatology; Ecology; Nutrient; Biology","score_opus":0.0044763594804910975,"score_gpt":0.18582387505275236,"score_spread":0.18134751557226125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102761435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998136,0.000012861515,0.00001194059,0.000007556418,3.833727e-7,3.909952e-7,0.000014720411,0.0000018550604,0.00013674746],"genre_scores_gemma":[0.99982315,0.000021764841,0.000032874337,0.0000050922854,8.7567037e-7,9.918615e-7,0.00003669685,5.6095513e-7,0.00007808976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996936,0.0000054942475,0.0000017421186,0.000007903451,0.000004853125,0.00001053625],"domain_scores_gemma":[0.99986947,0.000017007804,0.000052827017,0.000011914457,0.00001766787,0.00003112849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001134725,0.00011861525,0.00013234904,0.00022014808,0.0002637332,0.00025117362,0.00012391729,0.000114430004,0.00045075148],"category_scores_gemma":[0.0003084942,0.00014937078,0.0000886043,0.0001647043,0.00026446595,0.00010708558,0.00032613406,0.000117719,0.00006419068],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025762545,0.000027128623,0.96786994,0.000018902309,0.000039998104,0.0004979898,0.00030037342,0.0006472785,0.025638234,0.000081972146,0.00012116904,0.0044994634],"study_design_scores_gemma":[0.0000035628925,0.000016141013,0.9989033,0.000001445501,0.000007953608,0.0000445037,0.00012360419,0.00036366188,0.00043767403,0.000021365575,0.000075760545,0.0000010467186],"about_ca_topic_score_codex":0.02150169,"about_ca_topic_score_gemma":0.035746854,"teacher_disagreement_score":0.02150169,"about_ca_system_score_codex":0.00045959518,"about_ca_system_score_gemma":0.0002878203,"threshold_uncertainty_score":0.0427531},"labels":[],"label_agreement":null},{"id":"W2105570658","doi":"10.1029/2002gb001966","title":"Atmospheric sulfur deposition alters pathways of gaseous carbon production in peatlands","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Česká geologická služba; Society of Wetland Scientists; University of Alberta; National Science Foundation","keywords":"Methanogenesis; Peat; Sulfate; Mineralization (soil science); Environmental chemistry; Environmental science; Sulfur; Sink (geography); Deposition (geology); Chemistry; Methane; Ecology; Geology; Soil science; Soil water; Sediment; Biology","score_opus":0.006875851992150162,"score_gpt":0.20464739140083268,"score_spread":0.19777153940868253,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105570658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956876,0.000065583125,0.000044742665,0.000009121173,0.0000014649584,0.0000012453077,0.000054371103,0.0000072990397,0.0002473715],"genre_scores_gemma":[0.9994869,0.00009068314,0.00009577985,0.000010802221,0.0000013588779,0.0000021642015,0.00011299625,0.000004736012,0.0001945178],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999925,0.00001148934,0.000006490481,0.000020531403,0.0000119766155,0.000024615278],"domain_scores_gemma":[0.9999223,0.000013210097,0.00002281621,0.000006949438,0.0000136900835,0.000021040734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010080922,0.00020570436,0.00020321508,0.0003269659,0.00030752984,0.0003895361,0.00010585862,0.0002104191,0.00065210945],"category_scores_gemma":[0.00015400157,0.00018074333,0.00019424612,0.00018476765,0.00024395634,0.00019367298,0.00029324784,0.0001491792,0.000096804186],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008435897,0.0000694692,0.11642784,0.00006315418,0.00007545904,0.00020949673,0.00026762046,0.0007196116,0.87623733,0.00020234947,0.00007822634,0.0048058964],"study_design_scores_gemma":[0.000022024617,0.00018480932,0.94620854,0.000008324399,0.000032151147,0.00013255452,0.00033413575,0.0010325767,0.051101003,0.0002826605,0.00065025064,0.000011023388],"about_ca_topic_score_codex":0.009070509,"about_ca_topic_score_gemma":0.013257785,"teacher_disagreement_score":0.009070509,"about_ca_system_score_codex":0.00036825123,"about_ca_system_score_gemma":0.00034012378,"threshold_uncertainty_score":0.018035412},"labels":[],"label_agreement":null},{"id":"W2111414931","doi":"10.1029/2008gb003413","title":"Integrating peatlands and permafrost into a dynamic global vegetation model: 2. Evaluation and sensitivity of vegetation and carbon cycle processes","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":245,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Environment Research Council; Sight Research UK; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Peat; Permafrost; Soil carbon; Environmental science; Primary production; Carbon cycle; Vegetation (pathology); Carbon fibers; Ecosystem; Atmospheric sciences; Soil science; Soil water; Hydrology (agriculture); Ecology; Geology; Oceanography","score_opus":0.006427262617456306,"score_gpt":0.25637405242968536,"score_spread":0.24994678981222906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111414931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99475116,0.00009611712,0.0031205628,0.00006593771,0.000017952718,0.000050638664,0.0003854799,0.00009710017,0.0014152318],"genre_scores_gemma":[0.9958955,0.000058643116,0.0034194195,0.000023370887,0.000006183557,0.00004286929,0.00027711818,0.000030043348,0.00024682964],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99976057,0.00009776483,0.000016153926,0.000049928723,0.000028379674,0.000047225425],"domain_scores_gemma":[0.99908376,0.0005898706,0.00006805268,0.00007265736,0.00010006836,0.00008566496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009987607,0.00091608457,0.0006062877,0.00041373336,0.0003966879,0.0009700171,0.0009123342,0.0012277786,0.0008405184],"category_scores_gemma":[0.0019518695,0.0005717823,0.000773766,0.0004176861,0.00044282633,0.00088173256,0.00080425525,0.00078812806,0.00011272093],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013342433,0.00008982613,0.011864833,0.000025719128,0.00006120938,0.00005346175,0.000025734487,0.98349047,0.0016465753,0.00019870876,0.000057554218,0.0023525392],"study_design_scores_gemma":[0.00003659096,0.00006137594,0.0028616353,0.0000034013121,0.00002020084,0.000007719421,0.0000146873845,0.9960343,0.000731502,0.00010663297,0.00011050314,0.000011499602],"about_ca_topic_score_codex":0.041394074,"about_ca_topic_score_gemma":0.021809682,"teacher_disagreement_score":0.041394074,"about_ca_system_score_codex":0.0010292997,"about_ca_system_score_gemma":0.0007652737,"threshold_uncertainty_score":0.082306266},"labels":[],"label_agreement":null},{"id":"W2112931328","doi":"10.1029/2006gb002914","title":"Comparison of quantification methods to measure fire‐derived (black/elemental) carbon in soils and sediments using reference materials from soil, water, sediment and the atmosphere","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":876,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Air Canada; Environment and Climate Change Canada","funders":"","keywords":"Carbon black; Soil water; Soot; Environmental science; Sediment; Environmental chemistry; Carbon fibers; Soil carbon; Total organic carbon; Combustion; Sedimentary rock; Atmosphere (unit); Carbon cycle; Soil science; Geology; Chemistry; Geochemistry; Ecology; Meteorology; Materials science; Geomorphology; Ecosystem; Geography","score_opus":0.04077555922069852,"score_gpt":0.31230273777521844,"score_spread":0.2715271785545199,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112931328","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7548749,0.007139973,0.23154847,0.00019340334,0.00022743216,0.0007152189,0.0010467598,0.00061116496,0.0036427893],"genre_scores_gemma":[0.6269554,0.003977455,0.362287,0.000463428,0.00008948975,0.0012193894,0.0023492535,0.00033465127,0.002323942],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9857545,0.003916508,0.00084982073,0.003829018,0.0051909843,0.0004592208],"domain_scores_gemma":[0.9921072,0.0028406186,0.00072199246,0.00110743,0.0030491059,0.00017354742],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.012550285,0.0016191909,0.0004788182,0.004006914,0.0008241707,0.0011340318,0.0014574717,0.0016625117,0.0004707874],"category_scores_gemma":[0.009990368,0.0008672973,0.0010637768,0.001323122,0.0013322656,0.00067533355,0.001459503,0.0008022709,0.00049161544],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006158827,0.00041101,0.06321958,0.00091983384,0.0012835804,0.000089805,0.0008728508,0.0030617455,0.856981,0.0007346098,0.0003486188,0.07146155],"study_design_scores_gemma":[0.00006496481,0.0013154147,0.09916465,0.0001708296,0.00058646203,0.00066984975,0.00036446462,0.00992831,0.881147,0.0006051516,0.0058501638,0.00013283809],"about_ca_topic_score_codex":0.0032774175,"about_ca_topic_score_gemma":0.006663311,"teacher_disagreement_score":0.012550285,"about_ca_system_score_codex":0.0010154427,"about_ca_system_score_gemma":0.0010915659,"threshold_uncertainty_score":0.06637299},"labels":[],"label_agreement":null},{"id":"W2118188303","doi":"10.1029/2011gb004098","title":"The importance of the terrestrial weathering feedback for multimillennial coral reef habitat recovery","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Coral and Marine Ecosystems Studies","field":"Environmental Science","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Reef; Coral reef; Coral; Resilience of coral reefs; Environmental science; Oceanography; Weathering; Ocean acidification; Coral bleaching; Aragonite; Sea surface temperature; Climate change; Effects of global warming on oceans; Carbon cycle; Habitat; Environmental issues with coral reefs; Geology; Global warming; Ecology; Ecosystem; Geomorphology; Biology; Calcite","score_opus":0.014542184972048441,"score_gpt":0.23689604678793133,"score_spread":0.2223538618158829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118188303","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99653107,0.000038421957,0.0014499224,0.00021691882,0.000009710461,0.0000056376934,0.00014059049,0.000051827345,0.0015558379],"genre_scores_gemma":[0.9996333,0.00001983706,0.00018448525,0.00001858252,0.0000017176296,0.0000033664917,0.000039536648,0.000008671601,0.000090530855],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999268,0.000018696264,0.000005402011,0.000017414939,0.0000070659935,0.000024697621],"domain_scores_gemma":[0.9996822,0.00012936389,0.00006868552,0.000033369146,0.0000216717,0.00006473024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034112766,0.00029979835,0.00023973211,0.00023563764,0.00039511482,0.0005625423,0.0003211609,0.00060416036,0.0025810343],"category_scores_gemma":[0.0020209586,0.00023647175,0.0007038615,0.0001801391,0.0004540453,0.0006605715,0.000632822,0.0005226653,0.00009389003],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018377932,0.000117701675,0.12457201,0.00006497917,0.00017832457,0.0003020669,0.000106633575,0.843004,0.019307163,0.0034852927,0.0007598711,0.0079182],"study_design_scores_gemma":[0.000071058676,0.000111153364,0.12960352,0.000013084499,0.00005962168,0.00011345456,0.000187858,0.8648506,0.0016742763,0.0027084735,0.000561323,0.000045584933],"about_ca_topic_score_codex":0.010553407,"about_ca_topic_score_gemma":0.01033993,"teacher_disagreement_score":0.010553407,"about_ca_system_score_codex":0.0006229034,"about_ca_system_score_gemma":0.00058838807,"threshold_uncertainty_score":0.020983994},"labels":[],"label_agreement":null},{"id":"W2118490152","doi":"10.1029/2011gb004060","title":"Characteristics and drivers of global NDVI‐based FPAR from 1982 to 2006","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Remote Sensing in Agriculture","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"National Key Research and Development Program of China","keywords":"Environmental science; Normalized Difference Vegetation Index; Vegetation (pathology); Photosynthetically active radiation; Advanced very-high-resolution radiometer; Deforestation (computer science); Climatology; Precipitation; Arid; Land cover; Leaf area index; Physical geography; Atmospheric sciences; Geography; Land use; Meteorology; Geology; Satellite; Ecology","score_opus":0.006159137959843174,"score_gpt":0.21546707407238178,"score_spread":0.2093079361125386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118490152","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99568367,0.00027827386,0.0005012542,0.00006965842,0.000007876395,0.0000051472666,0.0019050174,0.000031653602,0.0015175651],"genre_scores_gemma":[0.99719137,0.00011449624,0.000276417,0.000011682559,0.0000055963096,0.000004753591,0.002147548,0.0000074339923,0.00024075076],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998727,0.000011256517,0.000011871803,0.000053840915,0.000026770136,0.000023430366],"domain_scores_gemma":[0.99955124,0.000056352026,0.00019053176,0.00003300589,0.00013870961,0.00003019596],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027042165,0.000213275,0.000103064966,0.00064075686,0.00012236592,0.00043136868,0.00018650333,0.0001488883,0.00033835147],"category_scores_gemma":[0.0006588308,0.00010274115,0.00018715837,0.0012921601,0.00011339419,0.00029967577,0.00020331239,0.00020558768,0.00009959925],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025287938,0.000019647274,0.98243606,0.000023524688,0.00004966403,0.0001052189,0.00015223055,0.0018002568,0.0014199502,0.00021812263,0.0007612559,0.012988849],"study_design_scores_gemma":[6.4079114e-7,0.00000495034,0.9970601,0.0000038953544,0.000008869586,0.000044880107,0.0000468748,0.0017753872,0.0001671713,0.000032777887,0.0008514291,0.0000030705457],"about_ca_topic_score_codex":0.015917825,"about_ca_topic_score_gemma":0.018365446,"teacher_disagreement_score":0.015917825,"about_ca_system_score_codex":0.00043614,"about_ca_system_score_gemma":0.00022629,"threshold_uncertainty_score":0.031650364},"labels":[],"label_agreement":null},{"id":"W2118813439","doi":"10.1002/2015gb005204","title":"Multimolecular tracers of terrestrial carbon transfer across the pan‐Arctic: <sup>14</sup>C characteristics of sedimentary carbon components and their environmental controls","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Natural Environment Research Council; Fisheries and Oceans Canada; University of California, Davis; Eidgenössische Technische Hochschule Zürich; Nordisk Ministerråd; Knut och Alice Wallenbergs Stiftelse; Russian Academy of Sciences; Russian Foundation for Basic Research; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; National Oceanic and Atmospheric Administration; Sight Research UK; Polarforskningssekretariatet; Woods Hole Oceanographic Institution; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Vetenskapsrådet; National Science Foundation","keywords":"Cutin; Suberin; Permafrost; Terrestrial ecosystem; Arctic; Tundra; Carbon fibers; Terrestrial plant; Environmental chemistry; Total organic carbon; Soil carbon; Wax; Geology; Chemistry; Environmental science; Ecology; Lignin; Oceanography; Soil water; Soil science; Paleontology; Ecosystem; Biology","score_opus":0.022455625980663918,"score_gpt":0.22703359347830057,"score_spread":0.20457796749763665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118813439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99481684,0.0005460579,0.0024787,0.000026456422,0.00001048247,0.000007514797,0.00071218115,0.00004747659,0.0013543079],"genre_scores_gemma":[0.99535733,0.000373663,0.0029444161,0.000036862228,0.00001276364,0.000017115624,0.00065366045,0.00002934961,0.00057474297],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998994,0.000009985874,0.0000034629734,0.000048539263,0.000025179726,0.00001341201],"domain_scores_gemma":[0.9998543,0.00002662937,0.00004087559,0.000008770521,0.00005224619,0.00001721359],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027657344,0.00033518966,0.0001608446,0.0007978935,0.00052199466,0.0005761198,0.00024356517,0.00027932596,0.00086386304],"category_scores_gemma":[0.00022757675,0.00015596363,0.000118915814,0.0008804124,0.00027027834,0.0002858178,0.0002313895,0.00031403682,0.00021078074],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043025144,0.000041624022,0.21954082,0.00012905501,0.00019963054,0.00010147279,0.00030681226,0.0022925166,0.75325394,0.00051607337,0.00021519623,0.022972688],"study_design_scores_gemma":[0.000009883509,0.00008727804,0.9173673,0.000015314521,0.00009715347,0.00012541648,0.0003310332,0.006578038,0.07183415,0.00026013804,0.0032717453,0.000022597487],"about_ca_topic_score_codex":0.024856614,"about_ca_topic_score_gemma":0.035139453,"teacher_disagreement_score":0.024856614,"about_ca_system_score_codex":0.00065622205,"about_ca_system_score_gemma":0.000366083,"threshold_uncertainty_score":0.049423873},"labels":[],"label_agreement":null},{"id":"W2119953010","doi":"10.1029/2001gb001851","title":"Stable carbon isotopic evidence for methane oxidation in plumes above Hydrate Ridge, Cascadia Oregon Margin","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Methane; Clathrate hydrate; Anaerobic oxidation of methane; Water column; Fractionation; Hydrate; Isotopes of carbon; Geology; Carbon fibers; Chemistry; Stable isotope ratio; Environmental chemistry; Mineralogy; Total organic carbon; Oceanography; Chromatography; Materials science; Organic chemistry","score_opus":0.026927488460223113,"score_gpt":0.26019408362875224,"score_spread":0.23326659516852913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119953010","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99941564,0.000026994137,0.00006455185,0.000012055671,5.6617193e-7,0.0000013623348,0.00011751512,0.0000058547575,0.0003555482],"genre_scores_gemma":[0.9993794,0.0000511405,0.00011808684,0.0000053772974,8.037952e-7,0.0000033299614,0.00025254738,0.0000033403653,0.00018592324],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999194,0.0000039544743,0.0000059410468,0.000025762936,0.00003039532,0.000014533504],"domain_scores_gemma":[0.99985397,0.000021076852,0.00003630712,0.000013980459,0.000045291377,0.000029289897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011028626,0.00024621244,0.00018775696,0.00058789534,0.00049699337,0.0003357892,0.0002671464,0.00021958878,0.00076007465],"category_scores_gemma":[0.00036146687,0.0002854023,0.0001646098,0.00045057343,0.00048678432,0.00018340434,0.00041983539,0.00020348401,0.00010793609],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040060183,0.000035998884,0.50931937,0.00005244444,0.00005500661,0.0002862063,0.0007634359,0.00049352297,0.48365912,0.00016198763,0.00005788436,0.0047143856],"study_design_scores_gemma":[0.000009585808,0.000043851906,0.98410827,0.000004266425,0.000016453941,0.000081414044,0.0003051558,0.0005430549,0.0145344,0.000051524716,0.0002947779,0.000007263506],"about_ca_topic_score_codex":0.047597308,"about_ca_topic_score_gemma":0.06548998,"teacher_disagreement_score":0.047597308,"about_ca_system_score_codex":0.000640104,"about_ca_system_score_gemma":0.00034890915,"threshold_uncertainty_score":0.09464055},"labels":[],"label_agreement":null},{"id":"W2124085139","doi":"10.1029/2004gb002398","title":"Terrigenous dissolved organic matter in the Arctic Ocean and its transport to surface and deep waters of the North Atlantic","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":205,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Bundesministerium für Bildung und Forschung","keywords":"Terrigenous sediment; Dissolved organic carbon; Oceanography; Arctic; Geology; Surface water; Environmental science; Geochemistry; Sedimentary rock","score_opus":0.005335043121927189,"score_gpt":0.18528540929016865,"score_spread":0.17995036616824145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124085139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963159,0.0016534255,0.00007517272,0.00008640718,0.000018882109,0.0000025279405,0.00044028,0.0000043045534,0.0014031784],"genre_scores_gemma":[0.99697554,0.0015081238,0.00022524295,0.000042929867,0.000021368784,0.0000031069949,0.00043372018,0.000003359059,0.0007865475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998919,0.000009332801,0.0000075942307,0.000031928117,0.0000336021,0.000025654472],"domain_scores_gemma":[0.99981636,0.000015488282,0.00005410661,0.0000049003374,0.00006341614,0.000045740882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017656256,0.0002365908,0.00020833116,0.0006410088,0.00077439635,0.0009107943,0.00017499577,0.00023349911,0.000520619],"category_scores_gemma":[0.00025513628,0.00017261568,0.00025483314,0.0010796157,0.00016607647,0.0003219033,0.0004702297,0.00019931326,0.00014731499],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019688277,0.000031016854,0.9596996,0.000086283006,0.00010653197,0.00036843878,0.0006424964,0.0004851626,0.021160671,0.0001928688,0.00026297983,0.01676701],"study_design_scores_gemma":[0.0000017760568,0.000013448273,0.9984113,0.000010613643,0.000015245431,0.00003412974,0.00030565803,0.0002387761,0.00027435092,0.000033051954,0.00065865164,0.0000030510876],"about_ca_topic_score_codex":0.26250565,"about_ca_topic_score_gemma":0.28856233,"teacher_disagreement_score":0.26250565,"about_ca_system_score_codex":0.0014178286,"about_ca_system_score_gemma":0.0010106339,"threshold_uncertainty_score":0.5219554},"labels":[],"label_agreement":null},{"id":"W2125017195","doi":"10.1002/2013gb004685","title":"Regional contribution of CO<sub>2</sub> and CH<sub>4</sub> fluxes from the fluvial network in a lowland boreal landscape of Québec","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":137,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Hydro-Québec","keywords":"Fluvial; STREAMS; Boreal; Greenhouse gas; Environmental science; Hydrology (agriculture); Atmospheric sciences; Physical geography; Geology; Oceanography; Geography; Geomorphology","score_opus":0.0037559542890650663,"score_gpt":0.18630656621959224,"score_spread":0.18255061193052718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125017195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971752,0.0001569628,0.00010504351,0.000063067266,0.0000022230965,0.000006586284,0.0014662389,0.00001781194,0.001006896],"genre_scores_gemma":[0.9986903,0.000067580804,0.00010395653,0.0000152172515,0.0000015500206,0.0000036302565,0.00063220965,0.0000033425697,0.00048218534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989617,0.000011012495,0.000004109343,0.000032929107,0.000019910742,0.00003595371],"domain_scores_gemma":[0.99963784,0.00004263953,0.00006158119,0.000010507334,0.0001728374,0.000074615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014762365,0.00023561741,0.00019123519,0.0009065165,0.0007368157,0.0010402997,0.00030778738,0.00027481705,0.0017428445],"category_scores_gemma":[0.00035206098,0.000107249194,0.00024447558,0.0010964313,0.00042435923,0.00020053325,0.00028665914,0.000171565,0.000106521366],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011964345,0.000021946938,0.9784873,0.000041557832,0.00012418714,0.00023468545,0.0005615671,0.0026082029,0.007346749,0.00015731638,0.0009688751,0.009328041],"study_design_scores_gemma":[0.0000024486403,0.0000035080504,0.99795794,0.0000057536877,0.000010879696,0.000016761736,0.0001986723,0.0012850051,0.0000962614,0.000009170338,0.00040815596,0.0000054075126],"about_ca_topic_score_codex":0.97092754,"about_ca_topic_score_gemma":0.9830358,"teacher_disagreement_score":0.029072464,"about_ca_system_score_codex":0.00832299,"about_ca_system_score_gemma":0.0025683395,"threshold_uncertainty_score":0.06038773},"labels":[],"label_agreement":null},{"id":"W2126770601","doi":"10.1029/2009gb003688","title":"Biogeochemical weathering under ice: Size matters","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":248,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Biogeochemical cycle; Weathering; Earth science; Geology; Ice sheet; Antarctic ice sheet; Meltwater; Biogeochemistry; Glacier; Cryosphere; Oceanography; Environmental science; Sea ice; Geomorphology; Environmental chemistry; Chemistry","score_opus":0.011903593161872847,"score_gpt":0.2271366139702117,"score_spread":0.21523302080833887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126770601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9654328,0.004779516,0.0011972595,0.0014105887,0.00006909236,0.00000911491,0.0005295619,0.00005027171,0.026521772],"genre_scores_gemma":[0.99554354,0.0020023407,0.00015089405,0.00018062584,0.0001195224,0.0000046359514,0.00020771573,0.000046796275,0.0017439959],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999224,0.000012925173,0.000004279621,0.000027030914,0.000017921446,0.000015438734],"domain_scores_gemma":[0.9991974,0.0003077521,0.00023034317,0.00007698632,0.00005321667,0.000134244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027306663,0.00018543073,0.00025552433,0.00026939594,0.00021286786,0.0010740745,0.00024531124,0.00019946459,0.0058510336],"category_scores_gemma":[0.0013541017,0.00010198359,0.00014832702,0.00034778018,0.00047713902,0.0012565827,0.00034650738,0.00016518762,0.0006421822],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038469193,0.00009845479,0.60114294,0.000562533,0.00036465694,0.0006306989,0.0007304509,0.009664539,0.17239407,0.012278815,0.0086396495,0.19310856],"study_design_scores_gemma":[0.000014992807,0.00014901556,0.95499396,0.00005289773,0.00009563936,0.00055329624,0.0008496163,0.002347155,0.011107701,0.012050059,0.017767819,0.00001792355],"about_ca_topic_score_codex":0.0012729343,"about_ca_topic_score_gemma":0.0020984735,"teacher_disagreement_score":0.0058510336,"about_ca_system_score_codex":0.0003003591,"about_ca_system_score_gemma":0.00015106858,"threshold_uncertainty_score":0.019573629},"labels":[],"label_agreement":null},{"id":"W2127376629","doi":"10.1029/2007gb003176","title":"Carbon cycling under 300 years of land use change: Importance of the secondary vegetation sink","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":456,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Ford Motor Company; National Oceanic and Atmospheric Administration; U.S. Department of Commerce; National Aeronautics and Space Administration","keywords":"Environmental science; Sink (geography); Carbon sink; Primary production; Carbon cycle; Vegetation (pathology); Land use, land-use change and forestry; Land use; Atmospheric sciences; Deforestation (computer science); Ecosystem; Hydrology (agriculture); Precipitation; Pasture; Ecology; Forestry; Geography; Meteorology; Geology","score_opus":0.011648614854049506,"score_gpt":0.22023227962347217,"score_spread":0.20858366476942267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127376629","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99429435,0.000049775645,0.002666516,0.00014394148,0.000009363955,0.000008778209,0.00094993185,0.0001341796,0.0017431886],"genre_scores_gemma":[0.9984611,0.000025477475,0.00066581107,0.000022057035,0.000003634952,0.000012981188,0.00058821816,0.000026551137,0.00019415368],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998977,0.000026924557,0.000005514646,0.00003390673,0.000012251765,0.000023679491],"domain_scores_gemma":[0.99972814,0.000114457485,0.00004247486,0.000031926604,0.000033475644,0.000049517363],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034389534,0.0004483075,0.0005404866,0.00026353615,0.00038276796,0.0006515262,0.00082072633,0.00076688634,0.001182508],"category_scores_gemma":[0.0011052765,0.00028519772,0.0007176395,0.00045156796,0.00036340885,0.00081667426,0.00042428155,0.00046779469,0.0001542286],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015378582,0.000060263897,0.052703995,0.00002813562,0.000082159,0.00013622578,0.00004344406,0.9382997,0.003740934,0.0009400237,0.0005072598,0.003303958],"study_design_scores_gemma":[0.000041618187,0.000032996468,0.014925568,0.00000307718,0.000015878693,0.000025937463,0.000022080856,0.98287636,0.0009066457,0.0006733733,0.0004622189,0.000014208641],"about_ca_topic_score_codex":0.03156998,"about_ca_topic_score_gemma":0.016898602,"teacher_disagreement_score":0.03156998,"about_ca_system_score_codex":0.0010719856,"about_ca_system_score_gemma":0.00067202735,"threshold_uncertainty_score":0.06277245},"labels":[],"label_agreement":null},{"id":"W2128379409","doi":"10.1029/2007gb002997","title":"Global prediction of <i>δ</i><sub>A</sub> and <i>δ</i><sup>2</sup>H‐<i>δ</i><sup>18</sup>O evaporation slopes for lakes and soil water accounting for seasonality","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":275,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; BC Innovation Council; University of Victoria","funders":"","keywords":"Environmental science; Soil water; Precipitation; Seasonality; Humidity; Atmospheric sciences; Latitude; Surface water; Stable isotope ratio; Evaporation; Potential evaporation; Hydrology (agriculture); Water cycle; Relative humidity; Climatology; Geology; Soil science; Ecology; Geography; Meteorology","score_opus":0.014146269505646271,"score_gpt":0.21016226424145715,"score_spread":0.19601599473581088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128379409","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99172133,0.000057558886,0.0039893403,0.00013977029,0.00001395088,0.0000059539875,0.000548595,0.00017423482,0.0033492495],"genre_scores_gemma":[0.9980235,0.000035512014,0.0012045528,0.00001776169,0.0000025839447,0.0000072092903,0.00036507967,0.000030178435,0.0003135968],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996674,0.000010198228,0.000001466663,0.000011353199,0.000003043904,0.0000071197005],"domain_scores_gemma":[0.99986446,0.000054390504,0.000021031174,0.000015678395,0.000022391965,0.000022120666],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025182008,0.00057793193,0.00020453245,0.00022585415,0.00016928706,0.00038629424,0.0002913281,0.0007113266,0.0010857417],"category_scores_gemma":[0.00048736352,0.00024812904,0.00051650166,0.00029702362,0.0003464803,0.0004062432,0.0003088008,0.00031201524,0.00018846111],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053453463,0.000020470305,0.022223625,0.000015066619,0.00004792191,0.000058345293,0.000023062097,0.9711822,0.0025518043,0.00042805207,0.00037545615,0.0030204924],"study_design_scores_gemma":[0.000030301846,0.000045646033,0.022289343,0.0000053129966,0.000029832916,0.000019311938,0.000049608443,0.9754562,0.00095625606,0.0007500255,0.0003567362,0.000011386755],"about_ca_topic_score_codex":0.011714361,"about_ca_topic_score_gemma":0.008943523,"teacher_disagreement_score":0.011714361,"about_ca_system_score_codex":0.0004630421,"about_ca_system_score_gemma":0.0003852494,"threshold_uncertainty_score":0.023292363},"labels":[],"label_agreement":null},{"id":"W2130347201","doi":"10.1029/2012gb004299","title":"Landscape‐level controls on dissolved carbon flux from diverse catchments of the circumboreal","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Permafrost; Weathering; Dissolved organic carbon; Biogeochemistry; Surface runoff; Mineralization (soil science); Environmental chemistry; Carbonate; Hydrology (agriculture); Environmental science; Boreal; Arctic; Geology; Soil water; Soil science; Chemistry; Oceanography; Geochemistry; Ecology","score_opus":0.03567341441564383,"score_gpt":0.2475722590309286,"score_spread":0.21189884461528477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130347201","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99980193,0.000018262625,0.000032006516,0.0000066236585,4.113706e-7,0.0000020212772,0.00007469147,0.0000020547786,0.00006214159],"genre_scores_gemma":[0.99964726,0.00001539522,0.000075306714,0.000009848047,9.162933e-7,0.0000044793337,0.00020065419,0.0000022086765,0.000043794797],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998061,0.00004000835,0.0000118104645,0.000081830585,0.000018927863,0.000041345567],"domain_scores_gemma":[0.9996573,0.000071849354,0.00007366926,0.000034658235,0.00005570635,0.00010698215],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036590258,0.0002624119,0.00042237277,0.0007048952,0.00061497965,0.00082146213,0.00028920663,0.00024018924,0.0005487611],"category_scores_gemma":[0.00060555054,0.00019738705,0.0002704526,0.0008087199,0.0006247137,0.0003190092,0.00074804615,0.00021062803,0.000047723224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002394168,0.00006997391,0.96996236,0.000021057658,0.00012942358,0.00015205098,0.0013244984,0.00061344844,0.02393554,0.00011344484,0.000096010364,0.0033427237],"study_design_scores_gemma":[0.0000034870802,0.000010327878,0.99916744,0.0000012838458,0.0000111992,0.000014063888,0.0002526653,0.0003569912,0.00011068774,0.000014566183,0.000055011642,0.000002239795],"about_ca_topic_score_codex":0.07115668,"about_ca_topic_score_gemma":0.127429,"teacher_disagreement_score":0.07115668,"about_ca_system_score_codex":0.00082659896,"about_ca_system_score_gemma":0.00034308818,"threshold_uncertainty_score":0.14148498},"labels":[],"label_agreement":null},{"id":"W2130997100","doi":"10.1029/2004gb002316","title":"Effect of thinning on surface fluxes in a boreal forest","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":220,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Academy of Finland","keywords":"Environmental science; Atmospheric sciences; Thinning; Transpiration; Leaf area index; Taiga; Boreal; Sink (geography); Hydrology (agriculture); Canopy; Soil science; Ecology; Photosynthesis; Botany; Geology; Biology","score_opus":0.003984279988692368,"score_gpt":0.2203808940416679,"score_spread":0.21639661405297556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130997100","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947923,0.000081283724,0.000062515566,0.000010871359,0.0000047125386,0.0000018460514,0.00006419368,0.000013841057,0.0002815999],"genre_scores_gemma":[0.9995989,0.000046991063,0.00010638633,0.000017850447,0.0000042037987,0.000002222744,0.00012973437,0.00000488877,0.00008877144],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999126,0.000016830354,0.000007142382,0.000017521974,0.00001731533,0.000028538921],"domain_scores_gemma":[0.9996593,0.00009840895,0.00008480195,0.00003003849,0.000041608255,0.000085807456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027582134,0.00035741623,0.0003153828,0.0002021256,0.00041460313,0.0003971618,0.00015477341,0.00027131833,0.0006835929],"category_scores_gemma":[0.00041054864,0.00014170061,0.00025885698,0.00014368602,0.00026277243,0.00029553164,0.00017147178,0.00030200614,0.00007348657],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004248182,0.00082552247,0.28075647,0.00013300045,0.0002180732,0.0008974137,0.00021917863,0.01437997,0.6758635,0.00032610868,0.0006951596,0.021437414],"study_design_scores_gemma":[0.00006086282,0.00075471116,0.97231084,0.0000063678513,0.00007537354,0.0002083412,0.0001208298,0.008279026,0.017552389,0.00016135126,0.000449495,0.000020414664],"about_ca_topic_score_codex":0.008559897,"about_ca_topic_score_gemma":0.006856261,"teacher_disagreement_score":0.008559897,"about_ca_system_score_codex":0.0003021346,"about_ca_system_score_gemma":0.00015126822,"threshold_uncertainty_score":0.017020106},"labels":[],"label_agreement":null},{"id":"W2133011208","doi":"10.1029/2009gb003757","title":"Relative role of decreasing precipitation sulfate and climate on recent lake recovery","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Precipitation; Temperate climate; Boreal; Alkalinity; Sulfate; Climate change; Acid rain; Northern Hemisphere; Acid neutralizing capacity; Aquatic ecosystem; Ecosystem; Environmental chemistry; Deposition (geology); Physical geography; Acid deposition; Hydrology (agriculture); Atmospheric sciences; Oceanography; Ecology; Chemistry; Geology; Structural basin; Geography; Soil science; Meteorology","score_opus":0.0052465189301991915,"score_gpt":0.21620073484289967,"score_spread":0.21095421591270047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133011208","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982924,0.0007022081,0.00007395071,0.00023844594,0.0000059763383,0.0000024641797,0.00013812294,0.000008060009,0.0005383228],"genre_scores_gemma":[0.99951184,0.00019705582,0.00003982575,0.000031978045,0.00001783416,0.0000010388677,0.00011359191,0.0000017494077,0.00008494361],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997347,0.00005790645,0.00003596344,0.00006538111,0.000035365043,0.00007057144],"domain_scores_gemma":[0.9985454,0.00020549126,0.0008025606,0.000083232575,0.00019484934,0.00016851487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009005827,0.00018773315,0.000308473,0.00061007956,0.0003408403,0.0005248337,0.00025784853,0.00042112765,0.0012651357],"category_scores_gemma":[0.0023385154,0.00017635575,0.0003287817,0.0005198858,0.0006486612,0.0005271942,0.0005647724,0.00024457675,0.000112880974],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004305501,0.000023271412,0.98703057,0.000039328923,0.00014377515,0.00009914011,0.00015289846,0.00043314803,0.0029984855,0.00012681664,0.00014584302,0.008376287],"study_design_scores_gemma":[0.000002188375,0.000027253094,0.9993814,0.0000020789914,0.000015895012,0.00003343928,0.0000507723,0.00017063832,0.00013960658,0.000014886468,0.00015983034,0.0000018599791],"about_ca_topic_score_codex":0.009056363,"about_ca_topic_score_gemma":0.015377055,"teacher_disagreement_score":0.009056363,"about_ca_system_score_codex":0.0005715219,"about_ca_system_score_gemma":0.0004151776,"threshold_uncertainty_score":0.018007278},"labels":[],"label_agreement":null},{"id":"W2141766893","doi":"10.1029/2008gb003237","title":"Fluxes of CH<sub>4</sub> and CO<sub>2</sub> from soil and termite mounds in south Sudanian savanna of Burkina Faso (West Africa)","year":2009,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Insect and Arachnid Ecology and Behavior","field":"Biochemistry, Genetics and Molecular Biology","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Soil respiration; Dry season; Sorghum; Environmental science; Soil water; Wet season; Sink (geography); Tropics; Crop; Agronomy; Seasonality; Ecosystem; Hydrology (agriculture); Geography; Forestry; Ecology; Biology; Soil science; Geology","score_opus":0.007754682781335523,"score_gpt":0.22805680253826194,"score_spread":0.22030211975692643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141766893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99981266,0.00003724266,0.000037594942,0.0000041616995,2.8613653e-7,9.2245745e-7,0.00003355634,0.0000014181214,0.00007226758],"genre_scores_gemma":[0.9996057,0.000067572226,0.00016967626,0.0000036180652,7.7925637e-7,0.0000029349064,0.000054247717,8.738917e-7,0.00009455955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999961,0.0000070706164,0.0000028123789,0.00001046674,0.0000068888344,0.0000116622905],"domain_scores_gemma":[0.9999161,0.000012490779,0.000038450395,0.0000047277813,0.000015133055,0.000013035138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013749223,0.00020048373,0.000100969395,0.0003748467,0.0004034479,0.00057991204,0.00012798452,0.00018444307,0.0003099015],"category_scores_gemma":[0.00016875361,0.00013513792,0.00010313005,0.00036437757,0.0001895189,0.0003789674,0.00023594272,0.00011035876,0.00003850256],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027364082,0.000040732735,0.88626033,0.000058295005,0.00006867776,0.00042619265,0.0013168379,0.0020097846,0.09828365,0.000120442084,0.00006535265,0.011076018],"study_design_scores_gemma":[0.000005642309,0.000044712626,0.99323326,0.000010136253,0.000017701323,0.000096154865,0.0006423283,0.0016988375,0.0036336016,0.000048256145,0.00056129525,0.000007926584],"about_ca_topic_score_codex":0.024523493,"about_ca_topic_score_gemma":0.050103743,"teacher_disagreement_score":0.024523493,"about_ca_system_score_codex":0.0005703665,"about_ca_system_score_gemma":0.0002339892,"threshold_uncertainty_score":0.048761487},"labels":[],"label_agreement":null},{"id":"W2141808005","doi":"10.1029/2010gb003914","title":"Spectral model of depth‐integrated water column photosynthesis and its inhibition by ultraviolet radiation","year":2011,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke; Dalhousie University","funders":"","keywords":"Photosynthesis; Irradiance; Water column; Photosynthetically active radiation; Environmental science; Atmospheric sciences; Solar irradiance; Physics; Botany; Biology; Optics; Ecology","score_opus":0.012598705854252025,"score_gpt":0.1851035882374395,"score_spread":0.17250488238318748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141808005","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.44307345,0.00039755343,0.5394945,0.0002951367,0.00005282605,0.000057902653,0.00070393836,0.0006415853,0.015283135],"genre_scores_gemma":[0.9804294,0.0002619437,0.013982679,0.000053267817,0.000019123287,0.00009099792,0.00020280141,0.000055201923,0.0049044257],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999069,0.00001821674,0.0000044547246,0.00002711306,0.000029374249,0.000014035987],"domain_scores_gemma":[0.9998423,0.00005136767,0.000030479303,0.000020797985,0.000039635073,0.000015270965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020690662,0.00046394073,0.0002638796,0.00026175773,0.00022334055,0.00037563065,0.0010606243,0.0005033999,0.0009516158],"category_scores_gemma":[0.0005435844,0.00033721808,0.0005827511,0.00034873272,0.0003846386,0.0007758345,0.00046596685,0.00037168936,0.00023167381],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021324176,0.000029862882,0.001091614,0.000028002552,0.000023400691,0.00003263154,0.000044258017,0.9708073,0.016676268,0.0073222145,0.00017997876,0.0037432057],"study_design_scores_gemma":[0.0000044688313,0.000008557329,0.0006726503,0.0000014030898,0.0000040717086,0.000009143572,0.0000041085377,0.9972474,0.0005739725,0.0012663536,0.00020321175,0.0000046419113],"about_ca_topic_score_codex":0.0103587285,"about_ca_topic_score_gemma":0.0050268797,"teacher_disagreement_score":0.0103587285,"about_ca_system_score_codex":0.00084749673,"about_ca_system_score_gemma":0.0006909236,"threshold_uncertainty_score":0.020596862},"labels":[],"label_agreement":null},{"id":"W2142213607","doi":"10.1029/2012gb004306","title":"Carbon dioxide and methane emissions from the Yukon River system","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":288,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Tributary; Methane; Carbon dioxide; Environmental science; Flux (metallurgy); Hydrology (agriculture); Greenhouse gas; Radiative forcing; Drainage basin; Surface water; Total organic carbon; Atmospheric sciences; Environmental chemistry; Climate change; Chemistry; Geology; Oceanography; Environmental engineering","score_opus":0.0066316292971425675,"score_gpt":0.2039992134966655,"score_spread":0.19736758419952294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142213607","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970162,0.00016397478,0.00009955461,0.000053661708,0.0000032828764,0.0000051441175,0.0016561032,0.000014379961,0.0009876428],"genre_scores_gemma":[0.99754614,0.00012637298,0.00013821555,0.00002400397,0.0000014256258,0.00000818784,0.0016802136,0.000004411157,0.0004709517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998859,0.000012984893,0.000013637658,0.00003209785,0.000031374646,0.00002408401],"domain_scores_gemma":[0.9998914,0.000018201072,0.0000192616,0.000009588904,0.00004708135,0.000014443865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009926464,0.00026197243,0.00019299405,0.0005808425,0.0004893575,0.00063554547,0.00019553202,0.00031833566,0.00073690736],"category_scores_gemma":[0.00025718563,0.00016050924,0.00042154736,0.001375631,0.00017554661,0.00029394595,0.00043903486,0.00015957393,0.00008765081],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013643611,0.000028251257,0.964564,0.00015826171,0.00048377167,0.00066717266,0.0003962413,0.008735997,0.0076498077,0.00042758422,0.0014464622,0.015305832],"study_design_scores_gemma":[0.000007364963,0.000009687545,0.9925706,0.000008602314,0.00005755743,0.00006599118,0.00028345463,0.0049349754,0.00045531787,0.00008551923,0.0015063131,0.000014608991],"about_ca_topic_score_codex":0.30361184,"about_ca_topic_score_gemma":0.40755394,"teacher_disagreement_score":0.6963881,"about_ca_system_score_codex":0.0021378298,"about_ca_system_score_gemma":0.0012977379,"threshold_uncertainty_score":0.60368925},"labels":[],"label_agreement":null},{"id":"W2145740977","doi":"10.1029/2001gb001839","title":"Regional water balance trends and evaporation‐transpiration partitioning from a stable isotope survey of lakes in northern Canada","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":357,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Subarctic climate; Tundra; Environmental science; Evapotranspiration; Arctic; Surface water; Water balance; Hydrology (agriculture); Potential evaporation; Drainage basin; Taiga; Latitude; Transpiration; Boreal; Physical geography; Geology; Oceanography; Ecology; Geography","score_opus":0.03647501419058569,"score_gpt":0.2187551689005207,"score_spread":0.18228015470993503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145740977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99788034,0.00021159378,0.0000666662,0.000039380204,9.923615e-7,0.0000057521756,0.0011041261,0.000008322931,0.0006829452],"genre_scores_gemma":[0.9976484,0.00021255088,0.00020542301,0.000017040653,0.0000011036567,0.0000062381678,0.0011228591,0.0000036624974,0.00078266475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998406,0.0000072826874,0.000007372385,0.000035801546,0.000049568906,0.000059354395],"domain_scores_gemma":[0.9996302,0.000021386957,0.00004813892,0.000008746406,0.00020053236,0.00009097404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019358123,0.00017760503,0.00018952957,0.0011527357,0.00119908,0.0006280985,0.0003345113,0.00015017726,0.00080677675],"category_scores_gemma":[0.00039256047,0.00020278171,0.00017790741,0.0019364542,0.0004470629,0.00018610347,0.00034393618,0.00018525896,0.00010487047],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000113860646,0.000017825616,0.98411036,0.000037376412,0.00006997306,0.00010581871,0.0013554661,0.00035290638,0.0037550677,0.00013777427,0.00059841084,0.009345142],"study_design_scores_gemma":[0.0000018917384,0.00000455704,0.99877673,0.0000043967457,0.0000095980295,0.000021065249,0.00035747275,0.00021330186,0.00016789326,0.000008144235,0.00043161388,0.0000033402648],"about_ca_topic_score_codex":0.9862598,"about_ca_topic_score_gemma":0.99545825,"teacher_disagreement_score":0.013740182,"about_ca_system_score_codex":0.012118279,"about_ca_system_score_gemma":0.0080109285,"threshold_uncertainty_score":0.08792466},"labels":[],"label_agreement":null},{"id":"W2146256391","doi":"10.1029/2001gb001398","title":"Cutover peatlands: A persistent source of atmospheric CO<sub>2</sub>","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":652,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; Johnson and Johnson","keywords":"Peat; Environmental science; Ecosystem respiration; Carbon dioxide; Carbon sink; Sink (geography); Carbon cycle; Ecosystem; Carbon fibers; Atmospheric sciences; Water table; Hydrology (agriculture); Environmental chemistry; Chemistry; Ecology; Primary production; Geology; Geography","score_opus":0.008665238656259018,"score_gpt":0.20454876544341868,"score_spread":0.19588352678715967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146256391","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99937797,0.000052772906,0.00010635562,0.0000042154534,7.654847e-7,0.000003169217,0.00016261231,0.0000057334596,0.00028634194],"genre_scores_gemma":[0.9985123,0.00007250647,0.0003237596,0.000007483743,0.00000140676,0.000003715421,0.00031470662,0.0000022584306,0.0007618578],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999715,0.0000014868243,9.768041e-7,0.0000069375824,0.00000908754,0.000010092024],"domain_scores_gemma":[0.9998795,0.000007466005,0.000034221215,0.000005224867,0.00003537779,0.00003815054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000059653095,0.00014676733,0.000100198835,0.00017693079,0.0002704044,0.0002930743,0.00013097208,0.00010141492,0.0006269861],"category_scores_gemma":[0.00008172302,0.00006116608,0.00004843304,0.00015513896,0.00013176628,0.00014678469,0.00011676881,0.00010872488,0.000118058364],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019343998,0.000075464915,0.84453946,0.000061027265,0.000037131264,0.00057413965,0.000468558,0.00038060758,0.12801144,0.000056956902,0.00032984564,0.025272002],"study_design_scores_gemma":[4.2236667e-7,0.000011505434,0.9986687,0.0000014232286,0.0000019515924,0.000047105696,0.00005875703,0.00011813369,0.00084510044,0.000004875746,0.00024088679,0.0000011673078],"about_ca_topic_score_codex":0.14646867,"about_ca_topic_score_gemma":0.48546454,"teacher_disagreement_score":0.14646867,"about_ca_system_score_codex":0.00061499455,"about_ca_system_score_gemma":0.0003761533,"threshold_uncertainty_score":0.29123223},"labels":[],"label_agreement":null},{"id":"W2146453061","doi":"10.1029/2006gb002735","title":"A satellite‐based biosphere parameterization for net ecosystem CO<sub>2</sub> exchange: Vegetation Photosynthesis and Respiration Model (VPRM)","year":2008,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":497,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"Agricultural Research Service; Office of Science; National Aeronautics and Space Administration; Natural Environment Research Council; U.S. Department of Energy; Harvard University; National Science Foundation","keywords":"Eddy covariance; Environmental science; FluxNet; Enhanced vegetation index; Photosynthetically active radiation; Ecosystem respiration; Leaf area index; Moderate-resolution imaging spectroradiometer; Biome; Biosphere; Vegetation (pathology); Atmospheric sciences; Primary production; Ecosystem; Remote sensing; Normalized Difference Vegetation Index; Satellite; Photosynthesis; Ecology; Geography; Vegetation Index; Chemistry; Geology; Physics","score_opus":0.015089928913771122,"score_gpt":0.21859228135479003,"score_spread":0.2035023524410189,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146453061","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1322199,0.00048342987,0.84659225,0.0005128085,0.00014746068,0.00010952205,0.003960106,0.0037342422,0.012240379],"genre_scores_gemma":[0.804099,0.00043365906,0.18023014,0.00019266053,0.00011011449,0.0005207096,0.004990493,0.0005134247,0.008909761],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992883,0.000016875696,0.0000034902964,0.000022623002,0.000019995368,0.000008237438],"domain_scores_gemma":[0.9999094,0.000025776957,0.000013307212,0.0000147899445,0.000027484684,0.000009162526],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002547838,0.0005834133,0.00033672657,0.00016275456,0.00021309916,0.00043290766,0.0009077451,0.0006996872,0.001236007],"category_scores_gemma":[0.00035480366,0.00026731048,0.0005736743,0.00018750614,0.0001774278,0.0004529108,0.00033017853,0.0005938627,0.00058960094],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020216734,0.000027270204,0.0012552642,0.000023513408,0.000040438732,0.000022911183,0.000013797848,0.9814725,0.0035389573,0.0029402934,0.0016108744,0.00903412],"study_design_scores_gemma":[0.0000061539004,0.000006226559,0.00031530904,0.0000016155725,0.000004619355,0.0000058108244,0.0000015280943,0.9975369,0.00035397228,0.00057659706,0.001187608,0.0000036120787],"about_ca_topic_score_codex":0.010084573,"about_ca_topic_score_gemma":0.008806226,"teacher_disagreement_score":0.010084573,"about_ca_system_score_codex":0.00046990303,"about_ca_system_score_gemma":0.00070646685,"threshold_uncertainty_score":0.020051718},"labels":[],"label_agreement":null},{"id":"W2146464692","doi":"10.1029/2005gb002494","title":"FeCycle: Attempting an iron biogeochemical budget from a mesoscale SF<sub>6</sub> tracer experiment in unperturbed low iron waters","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":323,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Biogeochemical cycle; Biogeochemistry; Mesoscale meteorology; Environmental science; Aerosol; Sink (geography); Iron fertilization; Geotraces; Oceanography; Deposition (geology); TRACER; Particulates; Phytoplankton; Environmental chemistry; Nutrient; Geology; Chemistry; Seawater; Meteorology; Geography; Sediment","score_opus":0.008175658182699124,"score_gpt":0.21214145093061365,"score_spread":0.20396579274791451,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146464692","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961282,0.000025777283,0.002477018,0.000023784904,0.000004253197,0.00006044715,0.00052058464,0.00004154285,0.00071844],"genre_scores_gemma":[0.98421913,0.00006419618,0.013711947,0.00006239726,0.0000034375128,0.00018290494,0.00091793423,0.00004004897,0.0007980659],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998895,0.0000126877485,0.0000071160625,0.000042789026,0.000025532056,0.000022302782],"domain_scores_gemma":[0.99985635,0.000032808086,0.00002595591,0.000030167179,0.00002925853,0.000025424664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040114627,0.0003595614,0.00038739745,0.00021867634,0.00048780104,0.00040371335,0.00052659377,0.00042228625,0.0005828244],"category_scores_gemma":[0.00050343823,0.00033677954,0.000307308,0.00026252476,0.0003128579,0.0003590716,0.00038002056,0.0006956072,0.00009100455],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012223757,0.0002852537,0.10390771,0.00013197542,0.00010575718,0.00028556128,0.0002520815,0.016349291,0.8653312,0.0005906199,0.00028911096,0.011249122],"study_design_scores_gemma":[0.0004473187,0.00250016,0.39593992,0.000024269868,0.00016311806,0.0002165954,0.00030231068,0.15326999,0.4409467,0.0007391879,0.0053726365,0.00007778721],"about_ca_topic_score_codex":0.06877711,"about_ca_topic_score_gemma":0.08062153,"teacher_disagreement_score":0.06877711,"about_ca_system_score_codex":0.0012731634,"about_ca_system_score_gemma":0.00060795073,"threshold_uncertainty_score":0.13675356},"labels":[],"label_agreement":null},{"id":"W2150803389","doi":"10.1029/2006gb002825","title":"Rapid decline of the CO<sub>2</sub> buffering capacity in the North Sea and implications for the North Atlantic Ocean","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":115,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Office of Naval Research; European Commission; National Aeronautics and Space Administration; National Science Foundation","keywords":"Oceanography; Middle latitudes; Water column; North Atlantic oscillation; Environmental science; Carbonate; Surface water; Seawater; Dissolved organic carbon; North Atlantic Deep Water; Sea surface temperature; Climatology; Geology; Thermohaline circulation; Chemistry","score_opus":0.018978622203839387,"score_gpt":0.21802578685660326,"score_spread":0.19904716465276387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150803389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99575585,0.0007409177,0.00019547854,0.0009798099,0.000011871392,0.0000019607617,0.00016077141,0.00003241522,0.0021209],"genre_scores_gemma":[0.9992335,0.00026425396,0.00009846746,0.00012707539,0.000014580433,0.0000013912448,0.00006596786,0.000004048377,0.00019086212],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999954,0.0000055055234,0.000004332373,0.000014428276,0.000009487469,0.000012264929],"domain_scores_gemma":[0.99981385,0.000024388375,0.000058816386,0.000018903078,0.000039433035,0.00004461178],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025126225,0.0001440828,0.00019114111,0.00025792033,0.00029513997,0.0006696331,0.00023832507,0.00040749233,0.001082868],"category_scores_gemma":[0.00043674908,0.00015765558,0.00015504638,0.00025721506,0.00060042104,0.00075163797,0.00034224597,0.00031573538,0.00012166515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00091275206,0.000108992,0.7299521,0.0002599907,0.0001618759,0.0011517016,0.0009926148,0.0096008815,0.17007747,0.0058007673,0.0040845135,0.076896325],"study_design_scores_gemma":[0.00001785545,0.000055401262,0.9878116,0.000010867517,0.000018359226,0.00015271388,0.0002938126,0.0031896068,0.0033119014,0.001997098,0.003126997,0.000013745769],"about_ca_topic_score_codex":0.011351783,"about_ca_topic_score_gemma":0.011345572,"teacher_disagreement_score":0.011351783,"about_ca_system_score_codex":0.0009301002,"about_ca_system_score_gemma":0.0003762051,"threshold_uncertainty_score":0.022571445},"labels":[],"label_agreement":null},{"id":"W2150997164","doi":"10.1029/2001gb001451","title":"A two‐dimensional nitrogen and carbon flux model in a coastal upwelling region","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Fisheries and Oceans Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Upwelling; Photic zone; Oceanography; Environmental science; Sink (geography); Flux (metallurgy); Isopycnal; Total organic carbon; Carbon sink; Dissolved organic carbon; Atmospheric sciences; Geology; Phytoplankton; Climate change; Chemistry; Nutrient; Geography; Environmental chemistry","score_opus":0.015255900548564728,"score_gpt":0.20061838318877423,"score_spread":0.1853624826402095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150997164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91378886,0.00045209448,0.036069054,0.0015027988,0.00014600324,0.00013417703,0.0046167513,0.0004770911,0.042813275],"genre_scores_gemma":[0.9737776,0.0002838326,0.0065695476,0.00014522711,0.000038411832,0.00022048985,0.0012925244,0.00006738999,0.017604949],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998709,0.000030327716,0.000006299081,0.000043607317,0.00001870269,0.000030179619],"domain_scores_gemma":[0.99964654,0.000111155474,0.000048716825,0.000016580218,0.000088076915,0.00008890716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030546426,0.0007557487,0.00082718406,0.00041051264,0.0009684962,0.0016584347,0.0026077083,0.0028031322,0.0043371837],"category_scores_gemma":[0.00078736315,0.00083689933,0.0010670654,0.000716932,0.0010935888,0.0008958606,0.0011551584,0.0010766797,0.00045077148],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005337945,0.00002479498,0.0011890167,0.0000130196895,0.000019426458,0.00012458673,0.00002389486,0.995067,0.0006768706,0.002165517,0.00026025577,0.00038225285],"study_design_scores_gemma":[0.000055297485,0.000012159322,0.00064896344,0.0000032326566,0.0000103297925,0.000009335716,0.000019969273,0.9984315,0.000059098256,0.000439275,0.0003018825,0.000008990835],"about_ca_topic_score_codex":0.22721128,"about_ca_topic_score_gemma":0.0835792,"teacher_disagreement_score":0.22721128,"about_ca_system_score_codex":0.0033272349,"about_ca_system_score_gemma":0.002669053,"threshold_uncertainty_score":0.45177758},"labels":[],"label_agreement":null},{"id":"W2151522428","doi":"10.1029/2010gb003974","title":"What eddy‐covariance measurements tell us about prior land flux errors in CO<sub>2</sub>‐flux inversion schemes","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":115,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Centre de Géomatique du Québec; McMaster University","funders":"Lawrence Berkeley National Laboratory; Natural Resources Canada; Agence Nationale de la Recherche; Natural Sciences and Engineering Research Council of Canada; U.S. Department of Energy; European Commission; University of Virginia; Università degli Studi della Tuscia; Université Laval; Ohio State University; Oak Ridge National Laboratory; Biological and Environmental Research; Canadian Foundation for Climate and Atmospheric Sciences; Microsoft Research; National Science Foundation","keywords":"Eddy covariance; FluxNet; Standard deviation; Environmental science; Inversion (geology); Flux (metallurgy); Covariance; Atmospheric sciences; Spatial ecology; Statistics; Meteorology; Mathematics; Geology; Ecosystem; Physics; Tectonics; Ecology","score_opus":0.012849922036765497,"score_gpt":0.2304356676733735,"score_spread":0.217585745636608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151522428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88733494,0.0006777576,0.10162382,0.0012462774,0.00016453952,0.00003387363,0.002273485,0.0005454237,0.0060998714],"genre_scores_gemma":[0.98229975,0.0002171081,0.01555956,0.00012033205,0.000078402285,0.000016681573,0.0011110603,0.00017998653,0.00041710061],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987602,0.00042965641,0.000111894864,0.00025737574,0.00028023688,0.0001605344],"domain_scores_gemma":[0.98644173,0.005864657,0.0021343818,0.0031529379,0.002143689,0.0002625473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005187456,0.0006471583,0.00059282745,0.00082853844,0.00037381003,0.0020092041,0.00070184935,0.00096183625,0.0013558335],"category_scores_gemma":[0.030555876,0.0008830421,0.00054058066,0.0008655154,0.0006836095,0.0043832688,0.00042844508,0.0012652545,0.0004352578],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051152974,0.00031814666,0.61209375,0.00019405344,0.00071663875,0.00017222902,0.00046669214,0.23678902,0.028020516,0.017671362,0.003927132,0.0991189],"study_design_scores_gemma":[0.00006235463,0.000094308234,0.5171797,0.00017624289,0.00014452866,0.000097276374,0.00019841494,0.44193715,0.022801992,0.0125750555,0.0045601265,0.00017279532],"about_ca_topic_score_codex":0.007615799,"about_ca_topic_score_gemma":0.014919001,"teacher_disagreement_score":0.007615799,"about_ca_system_score_codex":0.0007962893,"about_ca_system_score_gemma":0.0007694616,"threshold_uncertainty_score":0.02743417},"labels":[],"label_agreement":null},{"id":"W2152206558","doi":"10.1029/2002gb001889","title":"Seasonal contribution of CO<sub>2</sub>fluxes in the annual C budget of a northern bog","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Peat; Environmental science; Bog; Growing season; Temperate climate; Primary production; Carbon dioxide; Atmospheric sciences; Ecosystem respiration; Ecosystem; Carbon cycle; Atmosphere (unit); Hydrology (agriculture); Agronomy; Ecology; Biology; Geography; Meteorology; Geology","score_opus":0.0047568279432766035,"score_gpt":0.21894539673618021,"score_spread":0.2141885687929036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152206558","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995555,0.000034969937,0.00011030661,0.000009362773,0.0000015200521,8.218237e-7,0.00006120447,0.00001251262,0.0002138178],"genre_scores_gemma":[0.99964404,0.000023793173,0.00011919163,0.000005109848,0.0000017954642,0.0000022238364,0.00007853675,0.0000061829637,0.00011915844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999776,0.0000042357638,0.0000016144612,0.0000062260033,0.000003986284,0.0000063772],"domain_scores_gemma":[0.9999145,0.000020958701,0.000024818513,0.0000064463557,0.000013397742,0.000019900344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011060706,0.00012807705,0.00012630597,0.00017574994,0.00019973103,0.0003114372,0.000098711316,0.00013271428,0.0005331877],"category_scores_gemma":[0.00017605687,0.0001169141,0.000066804314,0.00009995976,0.00013458123,0.00017171114,0.00012898694,0.00014805628,0.00013476601],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00080402195,0.00016203006,0.61396605,0.00009639954,0.00009829513,0.00028221917,0.0003094925,0.0055606784,0.35297993,0.00028565657,0.00038958687,0.025065582],"study_design_scores_gemma":[0.000003976224,0.000026076226,0.98669297,0.0000030765577,0.000015029644,0.000058855774,0.000056398934,0.0060073244,0.00671662,0.000098591394,0.00031545633,0.000005601543],"about_ca_topic_score_codex":0.0060218205,"about_ca_topic_score_gemma":0.011384302,"teacher_disagreement_score":0.0060218205,"about_ca_system_score_codex":0.000260978,"about_ca_system_score_gemma":0.00015380609,"threshold_uncertainty_score":0.01197356},"labels":[],"label_agreement":null},{"id":"W2155655413","doi":"10.1029/2001gb001849","title":"A circumpolar perspective on fluvial sediment flux to the Arctic ocean","year":2002,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":231,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Arctic; Circumpolar star; Sediment; Physical geography; Environmental science; Oceanography; Flux (metallurgy); The arctic; Geology; Geography; Paleontology","score_opus":0.026161569904170227,"score_gpt":0.24457967418126483,"score_spread":0.2184181042770946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155655413","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.16429469,0.71518755,0.009247215,0.01221976,0.003902248,0.000031072825,0.003280621,0.00011972647,0.09171717],"genre_scores_gemma":[0.42386448,0.5525888,0.008978211,0.0033349814,0.0041208374,0.000053620268,0.0014484233,0.00008181745,0.005528763],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9997633,0.0000927163,0.00003011008,0.000052231117,0.00003623382,0.000025357454],"domain_scores_gemma":[0.99913543,0.0003399534,0.000116986,0.00003141125,0.0003241517,0.000052019066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012423162,0.0007363756,0.0004275324,0.005932548,0.0013454349,0.0025760576,0.00018384574,0.00031786013,0.0020848648],"category_scores_gemma":[0.0010621854,0.00016769208,0.00033833855,0.00699193,0.0011095495,0.0014308583,0.00049076264,0.0006937697,0.00030292053],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041912842,0.00007322432,0.18865569,0.0057603163,0.00059878477,0.001546275,0.010927272,0.013163664,0.008636371,0.19502965,0.028782485,0.54640716],"study_design_scores_gemma":[0.000010305384,0.00014607936,0.37805817,0.0050300984,0.00062455324,0.00057397695,0.0067045116,0.0019364039,0.001962241,0.02480414,0.5800903,0.00005927817],"about_ca_topic_score_codex":0.05173388,"about_ca_topic_score_gemma":0.083348066,"teacher_disagreement_score":0.05173388,"about_ca_system_score_codex":0.0016113542,"about_ca_system_score_gemma":0.0017598597,"threshold_uncertainty_score":0.10286552},"labels":[],"label_agreement":null},{"id":"W2157129937","doi":"10.1029/2004gb002249","title":"Thresholds for warming‐induced growth decline at elevational tree line in the Yukon Territory, Canada","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":302,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Lamont-Doherty Earth Observatory, Columbia University; Office of Science; Parks Canada; U.S. Department of Energy","keywords":"Tree line; Latitude; Environmental science; Precipitation; Dendrochronology; Climatology; Atmospheric sciences; Climate change; Browning; Global warming; Physical geography; Geography; Ecology; Biology; Meteorology; Geology; Horticulture","score_opus":0.020382247798394322,"score_gpt":0.24738662783380364,"score_spread":0.22700438003540932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157129937","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99891853,0.000058210957,0.00006691688,0.00003444937,7.679143e-7,0.0000025625136,0.00026808417,0.0000091246675,0.0006414299],"genre_scores_gemma":[0.9996501,0.000019662173,0.000030982417,0.00000540734,2.244968e-7,8.2112035e-7,0.00018876631,0.0000013480642,0.00010259582],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998857,0.000008933606,0.000006380714,0.000028055896,0.000021475986,0.000049416605],"domain_scores_gemma":[0.99949753,0.000047821904,0.00006230749,0.000021964253,0.00028079972,0.00008956668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019359877,0.00009189123,0.00017138595,0.00044766392,0.0007126932,0.00055427116,0.00027621453,0.00021383412,0.0008623193],"category_scores_gemma":[0.00075094134,0.0000942696,0.00014043899,0.00044490022,0.00037745544,0.00019991567,0.0002703606,0.00017003689,0.00008051744],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006528961,0.000015461346,0.99030465,0.000012638018,0.000024487033,0.00007949795,0.00037021053,0.0022620948,0.0036184005,0.00016390889,0.00035127896,0.0027321],"study_design_scores_gemma":[0.000001140748,0.0000041823246,0.9983918,0.0000024288545,0.0000039005495,0.0000160716,0.00022667434,0.0010391347,0.00014436136,0.000023887133,0.00014358055,0.0000027918377],"about_ca_topic_score_codex":0.9293412,"about_ca_topic_score_gemma":0.9675259,"teacher_disagreement_score":0.0706588,"about_ca_system_score_codex":0.0057913363,"about_ca_system_score_gemma":0.0032059574,"threshold_uncertainty_score":0.1421498},"labels":[],"label_agreement":null},{"id":"W2158410010","doi":"10.1002/2014gb004880","title":"Interactions between reactive nitrogen and the Canadian landscape: A budget approach","year":2014,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"GDG Environnement; Selkirk College; Environment and Climate Change Canada; Agriculture and Agri-Food Canada; Dalhousie University; University of New Brunswick; Cumulative Environmental Management Association","funders":"","keywords":"Reactive nitrogen; Agriculture; Ecosystem; Environmental science; Environmental protection; Geography; Nitrogen; Natural resource economics; Ecology; Economics; Chemistry","score_opus":0.006672623928481602,"score_gpt":0.21059420180918773,"score_spread":0.2039215778807061,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158410010","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.72758114,0.0025435174,0.05579953,0.005380391,0.0000703915,0.00044967778,0.024517499,0.00036122842,0.18329652],"genre_scores_gemma":[0.96116126,0.0018482914,0.02525409,0.00023625638,0.000017149905,0.00017208995,0.0025055506,0.00009489328,0.008710381],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9993475,0.00017574771,0.000027539903,0.00008070017,0.00018988692,0.00017861853],"domain_scores_gemma":[0.99877363,0.00029770643,0.00011263339,0.000055620552,0.0006347322,0.00012564924],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009495197,0.0004906237,0.0004778561,0.004100266,0.002194332,0.0030516856,0.0018165887,0.0005897257,0.0048546935],"category_scores_gemma":[0.003914279,0.00055827666,0.00085282867,0.00700759,0.00080910104,0.0014190456,0.0010754429,0.0005749829,0.00012294287],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009210674,0.00008088699,0.11393711,0.00024935981,0.0004502923,0.00033833113,0.00055521046,0.6664964,0.0013480483,0.16042855,0.009761762,0.046262015],"study_design_scores_gemma":[0.000043824748,0.000044582353,0.10627797,0.00020058015,0.00041521454,0.0000895566,0.0016605105,0.8042516,0.0006871328,0.032958418,0.053227086,0.00014354625],"about_ca_topic_score_codex":0.98802596,"about_ca_topic_score_gemma":0.98907197,"teacher_disagreement_score":0.053217776,"about_ca_system_score_codex":0.053217776,"about_ca_system_score_gemma":0.032642193,"threshold_uncertainty_score":0.38612378},"labels":[],"label_agreement":null},{"id":"W2159815694","doi":"10.1029/2004gb002283","title":"A global model of the marine ecosystem for long‐term simulations: Sensitivity to ocean mixing, buoyancy forcing, particle sinking, and dissolved organic matter cycling","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":176,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Oceanography; Pycnocline; Upwelling; Ocean general circulation model; Environmental science; Thermohaline circulation; Water column; Mixed layer; Dissolved organic carbon; Phytoplankton; Deep ocean water; Geology; Atmospheric sciences; Nutrient; Climate change; Chemistry","score_opus":0.010717334655770003,"score_gpt":0.2225751195959871,"score_spread":0.21185778494021712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159815694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.50664514,0.0009837117,0.4605944,0.0017648203,0.00042612292,0.00018973902,0.005883301,0.002914903,0.020597879],"genre_scores_gemma":[0.86255175,0.0009136528,0.12090534,0.00029493042,0.00018320675,0.0010417906,0.005767064,0.0005548567,0.0077873557],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999099,0.000029077835,0.000005637824,0.000024997955,0.00001745425,0.000012991001],"domain_scores_gemma":[0.99972385,0.00010579305,0.000026339623,0.000043236894,0.00004186637,0.00005887787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041726188,0.0010511916,0.0007060119,0.00026961588,0.0006690778,0.0008541698,0.0014659069,0.0013130147,0.002986592],"category_scores_gemma":[0.0008355925,0.0005185419,0.0011047592,0.00063083536,0.0005214198,0.0011387347,0.0011726102,0.0014468768,0.00043351558],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003291918,0.000027191561,0.00173624,0.0000382842,0.00007215158,0.000057493653,0.000027600754,0.9888003,0.0020999059,0.0028035848,0.0007655614,0.0035386814],"study_design_scores_gemma":[0.000036015754,0.000025142715,0.0009683143,0.0000040271525,0.00002782482,0.000020362357,0.00000813456,0.9941749,0.00022014069,0.0023383382,0.0021667762,0.0000100768875],"about_ca_topic_score_codex":0.012188728,"about_ca_topic_score_gemma":0.011302287,"teacher_disagreement_score":0.012188728,"about_ca_system_score_codex":0.0010023763,"about_ca_system_score_gemma":0.0012731901,"threshold_uncertainty_score":0.024235547},"labels":[],"label_agreement":null},{"id":"W2160526143","doi":"10.1029/2005gb002458","title":"Coupled nitrogen and oxygen isotope measurements of nitrate along the eastern North Pacific margin","year":2005,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":412,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; McGill University; University of British Columbia","funders":"","keywords":"Thermocline; Isotopes of nitrogen; Nitrate; Oceanography; Seawater; Nitrogen; Denitrification; Anomaly (physics); Water column; Geology; Oxygen minimum zone; Oxygen; Redfield ratio; Isotopes of oxygen; Nutrient; Upwelling; Chemistry; Phytoplankton; Geochemistry","score_opus":0.01661376877209762,"score_gpt":0.20428601872784827,"score_spread":0.18767224995575066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160526143","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990169,0.00003775094,0.0001113416,0.00001490672,0.0000023226812,0.0000033583954,0.00014112196,0.000008307813,0.0006639206],"genre_scores_gemma":[0.9987577,0.000061842875,0.00040575827,0.000011610727,0.0000019543888,0.000006825379,0.0002554896,0.0000024831786,0.0004964075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994636,0.0000034686032,0.0000018509204,0.000024521543,0.000016611246,0.000007148375],"domain_scores_gemma":[0.99991035,0.000008936485,0.000022275506,0.0000057752563,0.00003559358,0.00001704151],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008586872,0.00014528885,0.00011621463,0.0002432099,0.00025387522,0.00023231217,0.00020755491,0.00017913365,0.00038691232],"category_scores_gemma":[0.00022120666,0.00022940956,0.0001000661,0.0002331961,0.00015532752,0.00014979312,0.0002975871,0.00015494484,0.000060805392],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005325312,0.00010318705,0.85452294,0.000047544847,0.00018772834,0.00016236791,0.0004937389,0.0062640957,0.11773917,0.00022375614,0.0004980816,0.019224871],"study_design_scores_gemma":[0.000016185453,0.000025287383,0.99400723,0.0000034782806,0.0000287678,0.000013463858,0.00007065108,0.0030597737,0.0023437492,0.000050132472,0.00037623264,0.000005098538],"about_ca_topic_score_codex":0.118621394,"about_ca_topic_score_gemma":0.2568809,"teacher_disagreement_score":0.118621394,"about_ca_system_score_codex":0.0007464365,"about_ca_system_score_gemma":0.0003896046,"threshold_uncertainty_score":0.2358619},"labels":[],"label_agreement":null},{"id":"W2160844592","doi":"10.1029/2011gb004159","title":"Isotopic signals (<sup>18</sup>O, <sup>2</sup>H, <sup>3</sup>H) of six major rivers draining the pan‐Arctic watershed","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Alberta Innovates; University of Victoria","funders":"U.S. Geological Survey; University of Waterloo; National Science Foundation","keywords":"Arctic; Permafrost; Watershed; Drainage basin; Hydrology (agriculture); Wetland; Environmental science; Sampling (signal processing); Structural basin; Geology; Physical geography; Oceanography; Ecology; Geomorphology; Geography","score_opus":0.030456301399453767,"score_gpt":0.24744867164664322,"score_spread":0.21699237024718945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160844592","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99944896,0.00003125262,0.00014373846,0.0000029604723,6.586056e-7,0.000001354403,0.00019243963,0.0000023316973,0.00017624561],"genre_scores_gemma":[0.9980007,0.000071945,0.0010674295,0.000006802044,0.0000017557732,0.000006388101,0.0006474714,0.0000034465363,0.00019398659],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999324,0.000008567744,0.000006329392,0.000026220421,0.000015663916,0.000010856309],"domain_scores_gemma":[0.99985325,0.000013947449,0.00006579453,0.000010073696,0.000037664042,0.000019202267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001540418,0.00014264946,0.00011009198,0.00047046304,0.00032564285,0.00025134897,0.00011962355,0.00011761879,0.0002495759],"category_scores_gemma":[0.00018688409,0.000091464775,0.000103231185,0.00063958624,0.00021060796,0.00013599159,0.00025153765,0.00009728577,0.000043173746],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020524532,0.000017676412,0.92687243,0.00002252119,0.000055324323,0.000054950935,0.00042827698,0.00023323463,0.061222892,0.000038883747,0.00005276004,0.010795718],"study_design_scores_gemma":[0.000002090675,0.00003289556,0.9960163,0.0000013747132,0.000018559089,0.00004576021,0.0001500019,0.00023732583,0.0031460451,0.000012017656,0.00033527214,0.0000023264254],"about_ca_topic_score_codex":0.015825728,"about_ca_topic_score_gemma":0.04921195,"teacher_disagreement_score":0.015825728,"about_ca_system_score_codex":0.00022017094,"about_ca_system_score_gemma":0.0002777104,"threshold_uncertainty_score":0.0314672},"labels":[],"label_agreement":null},{"id":"W2162713835","doi":"10.1029/2007gb002934","title":"Flux and age of dissolved organic carbon exported to the Arctic Ocean: A carbon isotopic study of the five largest arctic rivers","year":2007,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":582,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dissolved organic carbon; Arctic; Environmental science; Spring (device); Total organic carbon; Flux (metallurgy); Oceanography; Hydrology (agriculture); Temperate climate; Period (music); Geology; Environmental chemistry; Ecology; Chemistry","score_opus":0.007387830685851321,"score_gpt":0.2015343302233107,"score_spread":0.19414649953745935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162713835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996594,0.00002566593,0.000042593874,0.0000035242642,5.823907e-7,9.3314446e-7,0.00015456793,0.0000015209206,0.00011122572],"genre_scores_gemma":[0.99871373,0.00006838647,0.0002291618,0.0000093848585,0.0000021689941,0.000004060226,0.0007210081,0.0000034139046,0.00024867637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999052,0.0000112948865,0.000008995996,0.000034357123,0.00001761517,0.0000225065],"domain_scores_gemma":[0.9996873,0.00004821611,0.0000878493,0.000015427468,0.0001175446,0.000043752134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027338028,0.00024931284,0.00021985652,0.0006493803,0.0006807814,0.00069121405,0.00016528579,0.00022099244,0.00018655403],"category_scores_gemma":[0.0003617683,0.00019227662,0.00025299808,0.00071089185,0.00028053363,0.00028996894,0.00026460693,0.00017685235,0.00005771089],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019629959,0.000038094066,0.98060703,0.00002119114,0.00008143546,0.00013708141,0.0006870311,0.000452545,0.01311883,0.00007352619,0.000072618175,0.0045143375],"study_design_scores_gemma":[0.0000031165268,0.000023253513,0.99777067,0.000003547119,0.000020851889,0.00006262518,0.00026303474,0.0005088357,0.0009267272,0.000017195536,0.00039557763,0.000004575527],"about_ca_topic_score_codex":0.089178465,"about_ca_topic_score_gemma":0.12178041,"teacher_disagreement_score":0.089178465,"about_ca_system_score_codex":0.0010686285,"about_ca_system_score_gemma":0.00056981633,"threshold_uncertainty_score":0.17731881},"labels":[],"label_agreement":null},{"id":"W2166055902","doi":"10.1002/2015gb005186","title":"Controls on biogenic silica burial in the Southern Ocean","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"University of Tasmania","keywords":"Biogenic silica; Geology; Oceanography; Biogeochemical cycle; Ocean current; Biogeochemistry; Silicic acid; Diatom","score_opus":0.02594482187011051,"score_gpt":0.2606118992396491,"score_spread":0.2346670773695386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166055902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991392,0.0001304697,0.00015296489,0.000020140658,0.0000010076218,0.0000010173859,0.00012283422,0.000014087935,0.0004182908],"genre_scores_gemma":[0.99960834,0.00006678961,0.00008685955,0.000005068055,0.000002137192,0.0000010463112,0.00013367971,0.0000034201184,0.00009260465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998909,0.000016003652,0.000014193319,0.000035583078,0.000026523894,0.000016671123],"domain_scores_gemma":[0.9994135,0.0001280038,0.00026439587,0.000068042886,0.00006183999,0.0000642368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040105527,0.0002718932,0.00020060975,0.0006147408,0.00016216483,0.00064118265,0.00020776162,0.00015036439,0.00066486065],"category_scores_gemma":[0.00091310986,0.00018789791,0.00024622955,0.0004087069,0.00042171776,0.00027915876,0.00053564215,0.00010118395,0.0001125523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002816927,0.000022374195,0.8634669,0.00008067707,0.00021993532,0.00022695099,0.00028840557,0.008391056,0.11776028,0.0007750799,0.00013032377,0.008356303],"study_design_scores_gemma":[0.00000946855,0.000030887208,0.99188566,0.0000073026195,0.000023115255,0.00005383395,0.00010369444,0.002893101,0.00405284,0.00032620615,0.0006071317,0.000006729914],"about_ca_topic_score_codex":0.008785111,"about_ca_topic_score_gemma":0.009608639,"teacher_disagreement_score":0.008785111,"about_ca_system_score_codex":0.00052540854,"about_ca_system_score_gemma":0.0002521622,"threshold_uncertainty_score":0.017467916},"labels":[],"label_agreement":null},{"id":"W2167005542","doi":"10.1029/2003gb002100","title":"Impacts of atmospheric variability on a coupled upper‐ocean/ecosystem model of the subarctic Northeast Pacific","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization; Pacific Institute for Climate Solutions; University of Victoria; Canadian Institute for Advanced Research","funders":"","keywords":"Thermocline; Environmental science; Subarctic climate; Climatology; Climate change; Ecosystem; Marine ecosystem; Forcing (mathematics); Biological pump; Ecosystem model; Ocean dynamics; Carbon cycle; Pacific decadal oscillation; Atmospheric sciences; Oceanography; Ocean current; Ecology; Sea surface temperature; Geology; Biology","score_opus":0.00709845246953114,"score_gpt":0.18985363189147864,"score_spread":0.1827551794219475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167005542","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943041,0.00009615569,0.0027534068,0.00028140994,0.00001801186,0.000012145987,0.0004049547,0.00007604554,0.0020537965],"genre_scores_gemma":[0.9987639,0.00007036294,0.0005043357,0.00002282497,0.0000065836416,0.00001270476,0.00016057557,0.000010837462,0.00044791118],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990106,0.00003365119,0.000005688785,0.000023728084,0.000013298791,0.00002248581],"domain_scores_gemma":[0.9995223,0.00023712144,0.000087593064,0.000025158184,0.000049299062,0.00007855162],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004309092,0.00058867724,0.00046850042,0.00032594876,0.00075701124,0.0012461394,0.0008541556,0.0009802744,0.0013344078],"category_scores_gemma":[0.0012330032,0.00042825477,0.00061047886,0.0003685914,0.000827,0.00045225507,0.00090847845,0.0009558093,0.00008322696],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006090324,0.000034782195,0.00692589,0.000010324299,0.000033390654,0.00009866019,0.000021365717,0.990866,0.00056753174,0.00074898615,0.00012646151,0.0005056568],"study_design_scores_gemma":[0.000019124851,0.000020898,0.0023604892,0.0000018844863,0.000012654432,0.0000062116537,0.000013334869,0.99723154,0.00008950486,0.00018831267,0.00005120809,0.0000049461883],"about_ca_topic_score_codex":0.12406571,"about_ca_topic_score_gemma":0.0624253,"teacher_disagreement_score":0.12406571,"about_ca_system_score_codex":0.0013895234,"about_ca_system_score_gemma":0.0013782386,"threshold_uncertainty_score":0.24668711},"labels":[],"label_agreement":null},{"id":"W2167388093","doi":"10.1029/2002gb001969","title":"Sensitivity of biogenic carbon export to ocean climate in the Labrador Sea, a deep‐water formation region","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Memorial University of Newfoundland","funders":"","keywords":"Biogeochemical cycle; Mesopelagic zone; Photic zone; Oceanography; Dissolved organic carbon; Convection; Biogeochemistry; Environmental science; Biogenic silica; Deep sea; Mixed layer; Surface water; Biological pump; Carbon cycle; Geology; Atmospheric sciences; Pelagic zone; Nutrient; Phytoplankton; Ecosystem; Chemistry; Environmental chemistry; Ecology; Geography","score_opus":0.009805878564747732,"score_gpt":0.20020486748971003,"score_spread":0.1903989889249623,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167388093","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99932015,0.000017026741,0.0001799306,0.00003984911,0.0000014310679,0.000003294331,0.00013281657,0.000019582543,0.00028606664],"genre_scores_gemma":[0.9992011,0.000036140576,0.000278883,0.000020231233,0.000001540094,0.000007784579,0.0002928525,0.0000070375377,0.00015441634],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99987185,0.0000391281,0.000008561834,0.0000289857,0.000009072953,0.000042381627],"domain_scores_gemma":[0.99970394,0.000119008626,0.000051957413,0.00003549986,0.00003685056,0.00005274845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003634274,0.00071004656,0.00037918027,0.00026269403,0.00041807807,0.0010657954,0.0005420723,0.0005164278,0.00060514064],"category_scores_gemma":[0.0011683033,0.00037393463,0.00077245914,0.00031942126,0.00044430542,0.00056796113,0.0007476299,0.000492674,0.000085298736],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054296904,0.00012321677,0.17898643,0.000041178562,0.00025958478,0.00027584555,0.00011041658,0.805873,0.009817017,0.0008577044,0.00024637964,0.0028663175],"study_design_scores_gemma":[0.00031030527,0.0005118715,0.09628481,0.000013889765,0.00016171177,0.000078925754,0.0001810915,0.8942122,0.006657024,0.0009056708,0.00063408585,0.00004841832],"about_ca_topic_score_codex":0.10277435,"about_ca_topic_score_gemma":0.04498969,"teacher_disagreement_score":0.10277435,"about_ca_system_score_codex":0.002034511,"about_ca_system_score_gemma":0.00069319014,"threshold_uncertainty_score":0.20435226},"labels":[],"label_agreement":null},{"id":"W2167969143","doi":"10.1029/2001gb001508","title":"Simulating past and future dynamics of natural ecosystems in the United States","year":2003,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":162,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Vegetation (pathology); Biogeochemical cycle; Ecosystem; Climate change; Atmospheric sciences; Biomass (ecology); Carbon cycle; Carbon sequestration; Climatology; Physical geography; Ecology; Carbon dioxide; Geography; Geology; Biology","score_opus":0.004130023320440303,"score_gpt":0.20217716124230783,"score_spread":0.19804713792186754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167969143","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922023,0.00013589139,0.0017247973,0.00018214597,0.000021354677,0.00001693236,0.0015203924,0.00011025714,0.004085874],"genre_scores_gemma":[0.9952733,0.00011732608,0.002251019,0.000056249824,0.0000042497854,0.000035727327,0.001306254,0.000014112757,0.000941754],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988675,0.000048663656,0.000005310927,0.000020192649,0.000012525053,0.000026547597],"domain_scores_gemma":[0.9996747,0.00015029291,0.000039614486,0.000023024108,0.000057970272,0.00005456731],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044827713,0.00045068018,0.00029039112,0.0003890718,0.00055437896,0.0006272203,0.0006050622,0.0005904245,0.0020894164],"category_scores_gemma":[0.001108607,0.0003290473,0.00040055742,0.0006882764,0.00034041784,0.00048093792,0.00042023679,0.00044632005,0.00010827379],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000080434664,0.00004618182,0.014972174,0.000015990403,0.000040037183,0.00008026402,0.000029611349,0.98076594,0.0002778734,0.00078467844,0.0010888334,0.0018179814],"study_design_scores_gemma":[0.000053419408,0.000037636863,0.008485687,0.0000082696215,0.000020941636,0.000017033144,0.00007177296,0.98966557,0.00018961902,0.000588359,0.0008517279,0.000010064873],"about_ca_topic_score_codex":0.18873125,"about_ca_topic_score_gemma":0.20587833,"teacher_disagreement_score":0.18873125,"about_ca_system_score_codex":0.0019796065,"about_ca_system_score_gemma":0.0009048837,"threshold_uncertainty_score":0.37526542},"labels":[],"label_agreement":null},{"id":"W2169275263","doi":"10.1029/2004gb002239","title":"Methane fluxes between terrestrial ecosystems and the atmosphere at northern high latitudes during the past century: A retrospective analysis with a process‐based biogeochemistry model","year":2004,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":408,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Northern Hemisphere; Biogeochemistry; Environmental science; Ecosystem; Atmospheric sciences; Latitude; Terrestrial ecosystem; Greenhouse gas; Atmosphere (unit); Climate change; Atmospheric methane; Methane; Soil water; Arctic; Southern Hemisphere; Climatology; Physical geography; Ecology; Oceanography; Meteorology; Geology; Geography; Soil science","score_opus":0.0037271680680117064,"score_gpt":0.1928769978555889,"score_spread":0.1891498297875772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169275263","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966575,0.00007115029,0.0020530336,0.000042546148,0.0000024954584,0.0000042566176,0.00081818027,0.000031849824,0.00031903345],"genre_scores_gemma":[0.99656016,0.0001074303,0.0016412941,0.00000704864,0.0000036137558,0.000008823639,0.0014847375,0.000007790378,0.00017915049],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998797,0.000049839808,0.000009245287,0.000030150884,0.000016526192,0.00001441737],"domain_scores_gemma":[0.9994382,0.00027843198,0.00011495828,0.00006943627,0.00007051715,0.00002843068],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007783504,0.00023573718,0.00017155943,0.0003399424,0.00020980166,0.00048023654,0.00028563448,0.00030274963,0.0004384953],"category_scores_gemma":[0.0017088109,0.00034360564,0.0005621414,0.0005066765,0.00014977527,0.0005213425,0.00029362916,0.00027541065,0.00009480743],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002839602,0.00006974667,0.60419464,0.000038128463,0.0002930319,0.00015790731,0.000103525956,0.3854125,0.0017733277,0.001238965,0.00032334455,0.006110936],"study_design_scores_gemma":[0.00003917475,0.00013055759,0.24668376,0.000011771808,0.00017661307,0.00016423903,0.00008849948,0.74722886,0.0024837544,0.0010274728,0.0019389248,0.000026380463],"about_ca_topic_score_codex":0.028490169,"about_ca_topic_score_gemma":0.02206157,"teacher_disagreement_score":0.028490169,"about_ca_system_score_codex":0.0006221001,"about_ca_system_score_gemma":0.00037418745,"threshold_uncertainty_score":0.05664867},"labels":[],"label_agreement":null},{"id":"W2170817139","doi":"10.1002/gbc.20029","title":"Revisiting “nutrient trapping” in global coupled biogeochemical ocean circulation models","year":2013,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft; University of Victoria","keywords":"Biogeochemical cycle; Ocean current; Biogeochemistry; Oceanography; Environmental science; Nutrient; Ocean general circulation model; Trapping; Climatology; Atmospheric sciences; General Circulation Model; Chemistry; Geology; Ecology; Climate change; Biology; Environmental chemistry","score_opus":0.012563527994143247,"score_gpt":0.21075033813089358,"score_spread":0.19818681013675032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170817139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97829866,0.00016765429,0.018209787,0.00045282202,0.000028987035,0.000024021472,0.0002551661,0.00015171761,0.0024111879],"genre_scores_gemma":[0.99679464,0.00010993837,0.0024488214,0.000070068,0.000016242437,0.00001924679,0.0001397453,0.000035567908,0.00036578107],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99979335,0.00009119721,0.000015689155,0.000038810816,0.000023272138,0.000037629725],"domain_scores_gemma":[0.9990226,0.00054939557,0.00018083163,0.00010115604,0.000074102754,0.00007192697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008697524,0.00074095704,0.0006200549,0.00040786035,0.000577571,0.0012662713,0.0010861399,0.00087193545,0.000601667],"category_scores_gemma":[0.0037666766,0.0004780165,0.0006630417,0.00043589287,0.00096383976,0.0014374864,0.0012574974,0.00070939923,0.00006717816],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034137327,0.00003706837,0.015180895,0.000017915558,0.00008407137,0.00010449459,0.00008989734,0.97809625,0.00083452254,0.0035174608,0.00026796345,0.0017353311],"study_design_scores_gemma":[0.000019179548,0.000020040547,0.001327851,0.0000041304843,0.000015522122,0.000008370698,0.000028304261,0.99611074,0.00014041852,0.0021486727,0.00017148936,0.0000052180762],"about_ca_topic_score_codex":0.043111548,"about_ca_topic_score_gemma":0.029795105,"teacher_disagreement_score":0.043111548,"about_ca_system_score_codex":0.0007932395,"about_ca_system_score_gemma":0.0009967397,"threshold_uncertainty_score":0.085721254},"labels":[],"label_agreement":null},{"id":"W2197392479","doi":"10.1002/2015gb005239","title":"Toward more realistic projections of soil carbon dynamics by Earth system models","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":545,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; Canadian Forest Service","funders":"U.S. Department of Energy; Met Office; Department for Environment, Food and Rural Affairs, UK Government; National Science Foundation","keywords":"Earth system science; Environmental science; Soil carbon; Soil water; Carbon cycle; Climate change; Data assimilation; Soil science; Ecology; Ecosystem; Meteorology; Geography","score_opus":0.027525498730693626,"score_gpt":0.2328700134831373,"score_spread":0.20534451475244367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2197392479","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.40310925,0.0009236512,0.563985,0.004385881,0.0002835171,0.0001371352,0.0048460867,0.0016864421,0.020643074],"genre_scores_gemma":[0.88812876,0.00065205904,0.10620429,0.0003118652,0.00006032289,0.00018571969,0.0024107327,0.00015063827,0.0018955852],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995809,0.00025956592,0.000019328181,0.00005072019,0.00006472744,0.000024833977],"domain_scores_gemma":[0.99911374,0.00036292252,0.00008802955,0.0001395986,0.00022140528,0.00007432163],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013804224,0.0005735671,0.00038693516,0.00053037476,0.0003074249,0.001130787,0.00070883497,0.0010873507,0.0016335999],"category_scores_gemma":[0.0053260857,0.00045761722,0.0006554833,0.0007863258,0.0002530806,0.0019960934,0.0006632465,0.0010070495,0.0004233495],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008758128,0.000012355311,0.001204492,0.000012416462,0.000021698252,0.000011028054,0.000010782908,0.99087286,0.00030569645,0.0047338298,0.0006351133,0.002170976],"study_design_scores_gemma":[0.000008986324,0.0000058432092,0.00046846224,0.00000836674,0.000005438539,0.000003011041,0.00001163203,0.9923369,0.00014685813,0.0058961813,0.0011012349,0.000006990079],"about_ca_topic_score_codex":0.024992807,"about_ca_topic_score_gemma":0.014527255,"teacher_disagreement_score":0.024992807,"about_ca_system_score_codex":0.0010705389,"about_ca_system_score_gemma":0.0013656203,"threshold_uncertainty_score":0.049694657},"labels":[],"label_agreement":null},{"id":"W2227839039","doi":"10.1002/2015gb005286","title":"A century of human‐driven changes in the carbon dioxide concentration of lakes","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"Agence Nationale de la Recherche; Natural Environment Research Council; Sight Research UK","keywords":"Environmental science; Terrigenous sediment; Carbon dioxide; Hypolimnion; Nutrient; Carbon cycle; Climate change; Global warming; Carbon dioxide in Earth's atmosphere; Supersaturation; Environmental chemistry; Sediment; Hydrology (agriculture); Atmospheric sciences; Oceanography; Ecology; Ecosystem; Eutrophication; Geology; Chemistry","score_opus":0.009933626605777776,"score_gpt":0.21004810629411297,"score_spread":0.20011447968833518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2227839039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99614406,0.0006420817,0.0010187995,0.00048167637,0.000015572565,0.0000016493498,0.00035205495,0.00002641052,0.0013176533],"genre_scores_gemma":[0.9991129,0.00024792692,0.00032968188,0.00005492592,0.000010096754,0.000001842874,0.00007939426,0.000004235456,0.00015890099],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999558,0.000008067097,0.0000033333567,0.000015354908,0.000010391494,0.0000070905194],"domain_scores_gemma":[0.9998542,0.00002337802,0.000047289705,0.000021690379,0.000038115606,0.00001525329],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022379948,0.00011217792,0.000108361884,0.0002618461,0.00034799048,0.00079033314,0.00011819771,0.00038525715,0.0007096697],"category_scores_gemma":[0.0005324617,0.00014630819,0.0001178603,0.00055155315,0.00064062036,0.0005832807,0.00040044746,0.00036994304,0.000060838447],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050745846,0.000056536675,0.84550816,0.0001808199,0.00046015286,0.0005334182,0.002210413,0.022837004,0.048104573,0.0067579835,0.002879335,0.06996415],"study_design_scores_gemma":[0.000011531451,0.000044553562,0.96639556,0.000036637193,0.000098406395,0.00020105962,0.00082379935,0.0104237255,0.0069221244,0.0020542433,0.012946008,0.000042394597],"about_ca_topic_score_codex":0.014643275,"about_ca_topic_score_gemma":0.023463149,"teacher_disagreement_score":0.014643275,"about_ca_system_score_codex":0.0007690859,"about_ca_system_score_gemma":0.0003783404,"threshold_uncertainty_score":0.029116094},"labels":[],"label_agreement":null},{"id":"W2274910709","doi":"10.1002/2015gb005332","title":"Toward a quantitative and empirical dissolved organic carbon budget for the Gulf of Maine, a semienclosed shelf sea","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; Dalhousie University; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Colored dissolved organic matter; Dissolved organic carbon; Oceanography; Hydrography; Total organic carbon; Environmental science; Geology; Plume; Submarine groundwater discharge; Hydrology (agriculture); Phytoplankton; Environmental chemistry; Groundwater; Chemistry; Aquifer; Nutrient","score_opus":0.02017809220802831,"score_gpt":0.24848694604185795,"score_spread":0.22830885383382965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2274910709","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978757,0.00011871307,0.0010153414,0.000066540066,0.0000021965814,0.000012646314,0.00047486948,0.000029180334,0.00040489342],"genre_scores_gemma":[0.99760014,0.000081886705,0.0014806683,0.000011621505,0.0000035050775,0.0000080664195,0.00065119687,0.0000063319003,0.00015672852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995065,0.0000107210135,0.000004961028,0.000017798957,0.000009605306,0.000006163416],"domain_scores_gemma":[0.99977654,0.000046556477,0.000063724794,0.000016184564,0.000070430244,0.000026493306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044689266,0.0003598956,0.00012295764,0.00073985494,0.000235206,0.0007804839,0.0002979914,0.00033433596,0.0004329721],"category_scores_gemma":[0.00097564695,0.00017386398,0.0002070574,0.0004429771,0.00022883262,0.00049470295,0.00028887542,0.00014126647,0.00013703074],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048175392,0.000054306773,0.93855727,0.0000408526,0.00007918291,0.00019197063,0.0001621027,0.039988175,0.010605519,0.0005664884,0.0002978402,0.009408158],"study_design_scores_gemma":[0.000018630139,0.00003344811,0.87025636,0.000024637795,0.000013737553,0.000033676897,0.00017608433,0.12668727,0.0013948121,0.0003242924,0.0010258438,0.000011227843],"about_ca_topic_score_codex":0.059543964,"about_ca_topic_score_gemma":0.06256675,"teacher_disagreement_score":0.059543964,"about_ca_system_score_codex":0.001268846,"about_ca_system_score_gemma":0.0006636278,"threshold_uncertainty_score":0.11839479},"labels":[],"label_agreement":null},{"id":"W2281323417","doi":"10.1002/2015gb005200","title":"Low particulate carbon to nitrogen ratios in marine surface waters of the Arctic","year":2015,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; ArcticNet; Division of Ocean Sciences; Universities Space Research Association; University of Victoria; National Science Foundation","keywords":"Photic zone; Phytoplankton; Subarctic climate; Oceanography; Arctic; Chlorophyll a; Bacterioplankton; Environmental science; Redfield ratio; Particulates; Canada Basin; Picoplankton; Environmental chemistry; Nitrogen; Chemistry; Nutrient; Ecology; Geology; Biology","score_opus":0.010204355919823898,"score_gpt":0.19986058194565534,"score_spread":0.18965622602583143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2281323417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990125,0.00010998686,0.00003800939,0.000008529889,0.0000031569955,0.0000019986371,0.00034381027,0.000003550971,0.00047839398],"genre_scores_gemma":[0.99902546,0.000076519216,0.00012560183,0.000016011376,0.0000043619775,0.0000031701725,0.00053258205,0.0000022961995,0.00021394278],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998348,0.000010123591,0.000009019148,0.000038502818,0.00007161398,0.000035825313],"domain_scores_gemma":[0.9996244,0.000027147256,0.00007641511,0.000008393242,0.00018730463,0.00007635028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024706626,0.00035376928,0.00025432292,0.0009800125,0.0009914747,0.00084880955,0.00026398478,0.00022019574,0.0004076454],"category_scores_gemma":[0.00045493216,0.0001957152,0.0001294785,0.0011162811,0.00032978907,0.00019058316,0.00034459602,0.00022602863,0.0000934707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001213429,0.000019587487,0.98738164,0.000019720828,0.000055574594,0.00006439024,0.00034827695,0.00012263493,0.009224963,0.00003674756,0.00010409231,0.002501043],"study_design_scores_gemma":[0.0000010495013,0.000009476704,0.9992281,0.0000021884794,0.0000055361584,0.000015866253,0.00016660654,0.00009342928,0.0003444768,0.0000057525563,0.00012597271,0.0000014751063],"about_ca_topic_score_codex":0.58492947,"about_ca_topic_score_gemma":0.67326,"teacher_disagreement_score":0.58492947,"about_ca_system_score_codex":0.0020805923,"about_ca_system_score_gemma":0.00132295,"threshold_uncertainty_score":0.83502996},"labels":[],"label_agreement":null},{"id":"W2298596790","doi":"10.1002/2015gb005280","title":"A mass budget for mercury and methylmercury in the Arctic Ocean","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":155,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"General Electric (Canada); University of Toronto; University of Alberta","funders":"European Research Council; University of Wollongong; ArcticNet; National Science Foundation","keywords":"Methylmercury; Seawater; Mercury (programming language); Arctic; Permafrost; Bioaccumulation; Sea ice; Environmental science; Environmental chemistry; Oceanography; Chemistry; Geology","score_opus":0.014929170423134592,"score_gpt":0.26772275941101575,"score_spread":0.2527935889878812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2298596790","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9549289,0.001071284,0.025968295,0.0006300564,0.00010537818,0.000087347,0.0036619743,0.00034772,0.013199114],"genre_scores_gemma":[0.98629344,0.00064411253,0.008098151,0.00011343508,0.000033049353,0.00008355743,0.0016823614,0.00007232059,0.0029795824],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998666,0.000027562091,0.0000104854225,0.00002876958,0.000039322455,0.00002721834],"domain_scores_gemma":[0.9997613,0.000034507022,0.000054796496,0.000013319892,0.00010955124,0.000026490072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046378645,0.0009272573,0.00041999127,0.0006868568,0.00071134354,0.0008645893,0.0008248971,0.00075749576,0.0015365749],"category_scores_gemma":[0.0006515699,0.0005156354,0.0010432975,0.000708181,0.00023741016,0.0009607872,0.00048281127,0.00029619056,0.00032684935],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008463775,0.00007448477,0.05485965,0.00008959602,0.00036094768,0.00019409855,0.00004437931,0.9130367,0.01764326,0.004304616,0.0008738621,0.008433794],"study_design_scores_gemma":[0.00008075153,0.00012510095,0.026002688,0.00004992876,0.00020649986,0.000076109616,0.000082254264,0.95979005,0.005427094,0.0027728814,0.005336203,0.000050387778],"about_ca_topic_score_codex":0.102068365,"about_ca_topic_score_gemma":0.053233325,"teacher_disagreement_score":0.102068365,"about_ca_system_score_codex":0.0036425139,"about_ca_system_score_gemma":0.0024183898,"threshold_uncertainty_score":0.20294851},"labels":[],"label_agreement":null},{"id":"W2301898488","doi":"10.1002/2015gb005228","title":"Nitrogen deposition to lakes in national parks of the western Great Lakes region: Isotopic signatures, watershed retention, and algal shifts","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Park Service; Indian Space Research Organisation; University of California, Davis; University of Regina","keywords":"Deposition (geology); Watershed; Environmental science; Sediment; Biogeochemistry; Nitrate; Phytoplankton; Limnology; Hydrology (agriculture); Nutrient; Ecosystem; Diatom; Nitrogen; Oceanography; Environmental chemistry; Ecology; Geology; Chemistry; Geomorphology; Biology","score_opus":0.009551158057931752,"score_gpt":0.19935875802400402,"score_spread":0.18980759996607227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2301898488","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998553,0.00001547641,0.000010951187,0.0000081834105,2.5883722e-7,8.833473e-7,0.000029232617,6.54575e-7,0.00007915262],"genre_scores_gemma":[0.999713,0.000024439765,0.00004855943,0.000009247362,0.000001173676,0.0000034277784,0.0000861951,5.564223e-7,0.00011334887],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999039,0.00002362111,0.000006434366,0.000027962755,0.000020117664,0.000017896027],"domain_scores_gemma":[0.99965453,0.000046180565,0.00016106386,0.000015357266,0.00006223366,0.0000606114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016148773,0.00010697821,0.000119198485,0.0004758677,0.0004699261,0.0002927386,0.00018459544,0.00012059811,0.000480294],"category_scores_gemma":[0.00048211456,0.0001042356,0.000082186685,0.00069926423,0.00036364398,0.0002423153,0.00052539975,0.00011209302,0.000043412707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034628363,0.000015199058,0.9962043,0.000009191419,0.00002380717,0.00006862152,0.0004747738,0.00006315872,0.0016534919,0.000014389479,0.000062631065,0.0013759073],"study_design_scores_gemma":[5.492497e-7,0.0000061824962,0.99956363,7.804819e-7,0.0000019025248,0.000016932454,0.00023634374,0.00006201413,0.00006424191,0.0000055927594,0.0000413592,5.0443145e-7],"about_ca_topic_score_codex":0.046307765,"about_ca_topic_score_gemma":0.17517404,"teacher_disagreement_score":0.046307765,"about_ca_system_score_codex":0.0005406667,"about_ca_system_score_gemma":0.00039688646,"threshold_uncertainty_score":0.09207648},"labels":[],"label_agreement":null},{"id":"W2305783268","doi":"","title":"Source and transport of terrigenous organic matter in the upper Yukon River : Evidence from isotope (δ13C, Δ14C, and δ15N)","year":2006,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Isotope Analysis in Ecology","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrigenous sediment; Organic matter; δ13C; Geology; Isotopes of carbon; Isotope; δ15N; Stable isotope ratio; Isotopes of nitrogen; Oceanography; Geochemistry; Total organic carbon; Environmental chemistry; Chemistry; Sedimentary rock","score_opus":0.0051287823974525745,"score_gpt":0.20251016857975207,"score_spread":0.1973813861822995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2305783268","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948347,0.00008990396,0.00006166311,0.000015345313,0.0000010614825,0.0000017518655,0.00011212293,0.0000030113868,0.0002316734],"genre_scores_gemma":[0.9993642,0.00013660364,0.000119788914,0.000011041877,8.7842847e-7,0.0000027742376,0.00017539719,0.0000037453121,0.00018558577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998896,0.000009038879,0.000014521351,0.00004145373,0.000018009418,0.000027320755],"domain_scores_gemma":[0.9996797,0.00006711274,0.00007014452,0.000021120743,0.00011644737,0.000045496585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001955915,0.00019858862,0.0002636764,0.00079160015,0.0008624705,0.00091828103,0.00042172242,0.00041055432,0.00048436035],"category_scores_gemma":[0.00043491708,0.00033609476,0.00019792549,0.001005253,0.00062595785,0.00054828165,0.00058746483,0.00022795178,0.000093517236],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002813359,0.000044536773,0.9250044,0.00010566167,0.00015141153,0.0003328261,0.0012185831,0.0009043123,0.061137315,0.0005338242,0.00011198104,0.010173699],"study_design_scores_gemma":[0.0000102358445,0.0000266817,0.9949922,0.000011549877,0.000051947267,0.000089989444,0.0007014714,0.0013169503,0.0023214084,0.00012765428,0.00033887153,0.000010989515],"about_ca_topic_score_codex":0.23791821,"about_ca_topic_score_gemma":0.30911118,"teacher_disagreement_score":0.23791821,"about_ca_system_score_codex":0.0013443962,"about_ca_system_score_gemma":0.0016949332,"threshold_uncertainty_score":0.47306675},"labels":[],"label_agreement":null},{"id":"W2318647377","doi":"10.1029/2009gb003601","title":"Biogeochemical fluxes through microzooplankton","year":2010,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":147,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Phytoplankton; Biomass (ecology); Biogeochemical cycle; Environmental science; Biogeochemistry; Oceanography; Plankton; Microbial loop; Environmental chemistry; Nutrient; Ecology; Chemistry; Biology","score_opus":0.008657298531855616,"score_gpt":0.2166615693544857,"score_spread":0.20800427082263007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2318647377","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9726979,0.000242987,0.02137904,0.00014252655,0.000023257902,0.000031796935,0.001256316,0.00022778458,0.003998293],"genre_scores_gemma":[0.99319386,0.00021377498,0.0051895264,0.000019805895,0.000004765288,0.00003576885,0.0004171699,0.000037128866,0.0008881535],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998847,0.000024392151,0.000008353459,0.000050476967,0.000016106796,0.000015948808],"domain_scores_gemma":[0.99984443,0.00004045349,0.00003839136,0.00002064476,0.000036043475,0.000020053756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017807627,0.0006245408,0.0003220875,0.00028004378,0.00027720726,0.0010680091,0.00036931015,0.0004528096,0.0012039664],"category_scores_gemma":[0.0006659676,0.0004557219,0.00072841445,0.0004684026,0.00028966498,0.00095784635,0.0003592743,0.00036272526,0.00018642297],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013110001,0.00006963266,0.15578774,0.00013540006,0.00020854916,0.00009342109,0.00022647904,0.78896713,0.037272062,0.0064849905,0.00053080416,0.010092635],"study_design_scores_gemma":[0.00010356844,0.00014378136,0.08167251,0.000034666675,0.00013332967,0.00007088023,0.00014860701,0.89824426,0.008560889,0.0060335114,0.004805236,0.00004873642],"about_ca_topic_score_codex":0.02340906,"about_ca_topic_score_gemma":0.016220858,"teacher_disagreement_score":0.02340906,"about_ca_system_score_codex":0.0015616682,"about_ca_system_score_gemma":0.0011269888,"threshold_uncertainty_score":0.046545625},"labels":[],"label_agreement":null},{"id":"W2343168782","doi":"10.1002/2015gb005277","title":"Heavy silicon isotopic composition of silicic acid and biogenic silica in Arctic waters over the Beaufort shelf and the Canada Basin","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; University of Victoria","funders":"ArcticNet; University of Victoria","keywords":"Oceanography; Biogenic silica; Water column; Geology; Silicic acid; Pelagic zone; Seawater; Sea ice; Arctic; Canada Basin; Water mass; Diatom","score_opus":0.004409319288645499,"score_gpt":0.1792496009990764,"score_spread":0.17484028171043092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2343168782","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985897,0.0001715079,0.000036206024,0.00002158407,0.000002368552,0.000002054927,0.00041151122,0.0000072000266,0.0007577784],"genre_scores_gemma":[0.9989004,0.00010042099,0.000117581745,0.000014367786,0.0000022592696,0.0000019544016,0.00042199984,0.0000033133792,0.00043770325],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998702,0.0000059551226,0.000005050332,0.00003756943,0.00004736692,0.000033995577],"domain_scores_gemma":[0.99971634,0.000018228178,0.000043066895,0.0000068267586,0.00014428982,0.00007122023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018502382,0.00033063497,0.00025014096,0.0015182766,0.0016094736,0.0008520668,0.00039877318,0.00024313688,0.00061257504],"category_scores_gemma":[0.00026677633,0.00021323108,0.0002555416,0.0012239044,0.00053730863,0.000215515,0.00037971637,0.00014019055,0.00009667412],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017955748,0.000011936851,0.97995627,0.00002894875,0.000107340005,0.00019854418,0.0008981599,0.0007645678,0.011332673,0.00011545691,0.00032380136,0.006082713],"study_design_scores_gemma":[0.0000023413463,0.000005563156,0.9984584,0.0000057454176,0.000009224964,0.00002563568,0.00026581888,0.0005048533,0.00031393036,0.000009034346,0.00039417617,0.0000052917453],"about_ca_topic_score_codex":0.94677734,"about_ca_topic_score_gemma":0.9750972,"teacher_disagreement_score":0.053222656,"about_ca_system_score_codex":0.0060862126,"about_ca_system_score_gemma":0.003976808,"threshold_uncertainty_score":0.107072115},"labels":[],"label_agreement":null},{"id":"W2416562831","doi":"10.1002/2015gb005337","title":"Eroding permafrost coasts release low amounts of dissolved organic carbon (DOC) from ground ice into the nearshore zone of the Arctic Ocean","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Bundesministerium für Bildung und Forschung; Parks Canada; Aurora Research Institute","keywords":"Permafrost; Dissolved organic carbon; Arctic; Environmental science; Oceanography; Total organic carbon; Sea ice; Geology; Hydrology (agriculture); Environmental chemistry; Chemistry","score_opus":0.013629693231525197,"score_gpt":0.21913248074819885,"score_spread":0.20550278751667367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2416562831","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99888486,0.000115748946,0.000076988,0.000004852052,0.000001570961,0.0000021222693,0.0003520706,0.0000052844016,0.0005565912],"genre_scores_gemma":[0.9986325,0.00011325585,0.00017677133,0.000008165712,0.0000011753069,0.0000028473708,0.0006414453,0.0000034505276,0.0004203172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999486,0.0000016873123,0.000003099875,0.00001190226,0.000015348678,0.000019289948],"domain_scores_gemma":[0.99986506,0.000010887843,0.000037643404,0.000005534723,0.000058762376,0.000022034945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000054465258,0.00024644987,0.00017177632,0.00048912945,0.00045816135,0.0005957019,0.00011284374,0.00010784112,0.0006564626],"category_scores_gemma":[0.00012764301,0.000108876775,0.00015279792,0.0005430663,0.00017309959,0.00016757539,0.00014882245,0.00010165746,0.00008532608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018749069,0.00002119522,0.8932846,0.00007859112,0.00008750882,0.00017584657,0.0003144835,0.00080434943,0.08857627,0.00008183772,0.00020718208,0.01618057],"study_design_scores_gemma":[0.0000011290026,0.000012045922,0.99682534,0.0000047023923,0.000008036874,0.000022686529,0.0001835839,0.00027544625,0.0023188065,0.0000072537828,0.00033886783,0.000002089402],"about_ca_topic_score_codex":0.326591,"about_ca_topic_score_gemma":0.4462016,"teacher_disagreement_score":0.326591,"about_ca_system_score_codex":0.0011547754,"about_ca_system_score_gemma":0.00092579547,"threshold_uncertainty_score":0.6493801},"labels":[],"label_agreement":null},{"id":"W2425845278","doi":"10.1002/2016gb005405","title":"Variability in the sensitivity among model simulations of permafrost and carbon dynamics in the permafrost region between 1960 and 2009","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":173,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Office of Science; Lunds Universitet; FP7 Environment; Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; U.S. Department of Energy; European Commission; Met Office; University of Victoria; Ministry of Education, Culture, Sports, Science and Technology; Biological and Environmental Research; Department for Environment, Food and Rural Affairs, UK Government; National Science Foundation","keywords":"Permafrost; Environmental science; Northern Hemisphere; Soil water; Vegetation (pathology); Atmospheric sciences; Soil carbon; Climatology; Climate change; Greenhouse gas; Primary production; Physical geography; Soil science; Geology; Ecosystem; Ecology; Geography; Oceanography","score_opus":0.02417264915322921,"score_gpt":0.24183337177790892,"score_spread":0.21766072262467973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2425845278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99768686,0.00008235968,0.0006032537,0.000074573996,0.000013604772,0.0000074912537,0.0006878702,0.000047409663,0.000796584],"genre_scores_gemma":[0.998616,0.000035943893,0.00038204502,0.00002459527,0.000004111211,0.00000962947,0.0007915855,0.000013834365,0.00012213681],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99964356,0.00010700803,0.000037928436,0.00012277637,0.00003294896,0.000055833716],"domain_scores_gemma":[0.9990716,0.0005024351,0.00011848165,0.00012920858,0.00009984332,0.000078432146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012281821,0.0005969808,0.0005761865,0.00040048696,0.0004593749,0.0008272613,0.00083899533,0.00094718573,0.0012826846],"category_scores_gemma":[0.0027419887,0.0004720069,0.0014865488,0.0004969666,0.00044923383,0.0008231241,0.00051350816,0.0007452289,0.00015763003],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014600506,0.000059111437,0.074966386,0.000025011244,0.0003457444,0.000085354164,0.000044713706,0.92027444,0.0019395946,0.0002878199,0.00029266346,0.001533291],"study_design_scores_gemma":[0.00012816451,0.00015677874,0.061357442,0.000022746188,0.00016971269,0.00007396535,0.00008893941,0.93477446,0.0019803501,0.00047616777,0.0007222298,0.000049012287],"about_ca_topic_score_codex":0.03218769,"about_ca_topic_score_gemma":0.020270666,"teacher_disagreement_score":0.03218769,"about_ca_system_score_codex":0.001247583,"about_ca_system_score_gemma":0.0006200883,"threshold_uncertainty_score":0.064000666},"labels":[],"label_agreement":null},{"id":"W2434927229","doi":"10.1002/2016gb005384","title":"Changes in anthropogenic nitrogen and phosphorus inputs to the St. Lawrence sub‐basin over 110 years and impacts on riverine export","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":134,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Université de Montréal; Université du Québec à Montréal","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Groupe de recherche interuniversitaire en limnologie; Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Environmental science; Eutrophication; Phosphorus; Hydrology (agriculture); Nutrient; Watershed; Nitrogen; Water quality; Deposition (geology); Structural basin; Drainage basin; Fertilizer; Ecology; Chemistry; Geology; Geography","score_opus":0.007332857202834184,"score_gpt":0.22602889593891612,"score_spread":0.21869603873608193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2434927229","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99878424,0.000039821098,0.00008419256,0.000031722757,0.0000010825372,0.000001496835,0.00039756874,0.000010025568,0.00064987753],"genre_scores_gemma":[0.9988533,0.00008351455,0.0001006431,0.0000097791,0.0000017996098,0.0000036194817,0.00040804734,0.0000018098228,0.0005374824],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999261,0.00001063728,0.000005662886,0.000019467034,0.00002281808,0.000015368078],"domain_scores_gemma":[0.9997838,0.000017065453,0.00009290931,0.000010373519,0.00007274433,0.000023122655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013833387,0.00014716841,0.000097992626,0.00042256873,0.00023733436,0.00055235496,0.00018493616,0.0000918744,0.0004986231],"category_scores_gemma":[0.00024259617,0.000098673954,0.0001796427,0.00075358833,0.00024438236,0.00022562341,0.00028992386,0.00012501857,0.00008551905],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033301458,0.000020657675,0.988848,0.00002123563,0.00007176348,0.000073250114,0.00019578646,0.0021917145,0.0014078158,0.00013447598,0.0004006031,0.0066014975],"study_design_scores_gemma":[0.0000018912306,0.000010286527,0.996089,0.0000051262937,0.000012112507,0.00001815054,0.00018256901,0.002207231,0.0003601795,0.00003470743,0.0010754425,0.0000032799362],"about_ca_topic_score_codex":0.25533894,"about_ca_topic_score_gemma":0.4666079,"teacher_disagreement_score":0.7446611,"about_ca_system_score_codex":0.0017114508,"about_ca_system_score_gemma":0.00093956204,"threshold_uncertainty_score":0.5077054},"labels":[],"label_agreement":null},{"id":"W2462471715","doi":"10.1002/2015gb005326","title":"Basin‐wide N<sub>2</sub> fixation in the deep waters of the Mediterranean Sea","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"HORIZON EUROPE Marie Sklodowska-Curie Actions; European Social Fund; Higher Council for Science and Technology; Ministerio de Economía y Competitividad; FPInnovations; European Commission; Institut de Recherche pour le Développement","keywords":"Photic zone; Organic matter; Heterotroph; Oceanography; Water column; Diazotroph; Environmental science; Deep sea; Mediterranean sea; Chlorophyll a; Mediterranean climate; Carbon fixation; Environmental chemistry; Nitrogen fixation; Geology; Photosynthesis; Chemistry; Phytoplankton; Nitrogen; Ecology; Nutrient; Biology; Botany; Paleontology","score_opus":0.008830083686969177,"score_gpt":0.19162824677307214,"score_spread":0.18279816308610297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2462471715","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995908,0.00006332014,0.00003828405,0.0000069524235,7.676789e-7,7.979591e-7,0.00006311642,0.0000029105101,0.00023302388],"genre_scores_gemma":[0.99974746,0.000034053148,0.00005237679,0.000006908664,0.0000013937297,0.0000014836487,0.000085408836,0.0000012488499,0.00006965663],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999404,0.000011471638,0.0000043185078,0.000024461111,0.000008342499,0.000011040291],"domain_scores_gemma":[0.99988985,0.00001846818,0.000034657376,0.000007841486,0.000023588227,0.000025523543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019526709,0.00018859253,0.00017307977,0.0005119211,0.00018030888,0.00031688917,0.00013915318,0.00019180641,0.00034243183],"category_scores_gemma":[0.00024061922,0.000121312514,0.00013258007,0.00029118315,0.00022954828,0.00018293419,0.00032196468,0.000075531534,0.000093455725],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003059805,0.000021698828,0.896823,0.000050365717,0.00018795783,0.00016729884,0.00038265422,0.00076890923,0.08958304,0.000059076137,0.00014411887,0.011505927],"study_design_scores_gemma":[0.0000037947145,0.000020980351,0.9987018,0.0000019909967,0.000009425567,0.00002332737,0.00007594476,0.0003270166,0.0006222521,0.000021088958,0.00019035894,0.0000019524148],"about_ca_topic_score_codex":0.010971658,"about_ca_topic_score_gemma":0.010546662,"teacher_disagreement_score":0.010971658,"about_ca_system_score_codex":0.0003603907,"about_ca_system_score_gemma":0.00015983982,"threshold_uncertainty_score":0.021815598},"labels":[],"label_agreement":null},{"id":"W2494965242","doi":"10.1002/2015gb005354","title":"Oxygen utilization rate (OUR) underestimates ocean respiration: A model study","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; University of Victoria","keywords":"Ocean gyre; Respiration; Advection; Biogeochemical cycle; Oxygen; Ocean current; Apparent oxygen utilisation; Oceanography; Environmental science; Atmospheric sciences; Geology; Chemistry; Biology; Environmental chemistry; Ecology; Subtropics; Physics","score_opus":0.03706284134767012,"score_gpt":0.25967344671763976,"score_spread":0.22261060536996963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2494965242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995182,0.00009543346,0.0031653577,0.00013097645,0.000008661007,0.000012045162,0.00029868595,0.000079275414,0.001027623],"genre_scores_gemma":[0.9984383,0.000061127546,0.001062805,0.000018625058,0.000004529927,0.000025522244,0.00014598964,0.000018647062,0.00022447639],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998209,0.000070267124,0.000010950277,0.000043608507,0.000021207998,0.000033125554],"domain_scores_gemma":[0.99822193,0.0013663352,0.00013410755,0.00008588754,0.00013030444,0.00006147661],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007860478,0.00062487955,0.0006149169,0.0003389405,0.00038196915,0.0007569347,0.0011672188,0.0010288703,0.00063011586],"category_scores_gemma":[0.002236681,0.00026566585,0.00086995406,0.00047911453,0.00044408522,0.0007640156,0.0004960066,0.0005521899,0.000089389476],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000112934584,0.00008155765,0.013903544,0.000030198615,0.000055718192,0.000050034712,0.000030797815,0.9820232,0.0014314981,0.0004826519,0.0002711742,0.0015266684],"study_design_scores_gemma":[0.00003136662,0.000061753904,0.0037042827,0.0000038076967,0.000022881484,0.00000901436,0.000012853405,0.99518615,0.000644942,0.00020860501,0.00010366026,0.000010660645],"about_ca_topic_score_codex":0.047352962,"about_ca_topic_score_gemma":0.020834051,"teacher_disagreement_score":0.047352962,"about_ca_system_score_codex":0.0015392767,"about_ca_system_score_gemma":0.00080010574,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W2508713783","doi":"10.1002/2016gb005411","title":"Historical variations of mercury stable isotope ratios in Arctic glacier firn and ice cores","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Trent University; University of Ottawa; Inuit Circumpolar Council","funders":"National Natural Science Foundation of China; University of Ottawa","keywords":"Ice core; Glacier; Firn; Arctic; Cryosphere; Sea ice; Snow; Mercury (programming language); Arctic ice pack; Oceanography; Geology; Arctic geoengineering; Physical geography; Atmospheric sciences; Environmental science; Antarctic sea ice; Geomorphology","score_opus":0.014362975273503,"score_gpt":0.24504074037341286,"score_spread":0.23067776509990986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2508713783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976548,0.0002077802,0.00008455736,0.000011973093,0.0000066991206,0.0000025478234,0.0010411397,0.000010041074,0.0009804617],"genre_scores_gemma":[0.9979463,0.00013118605,0.00018770149,0.000012660157,0.000005418667,0.0000033435533,0.0013454541,0.0000039464303,0.00036390958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983716,0.000012014433,0.000008252447,0.00004433962,0.00006714739,0.00003117799],"domain_scores_gemma":[0.99946266,0.000034029716,0.000076000295,0.0000144616215,0.00036120682,0.000051561186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004731739,0.00019125489,0.0001512463,0.0017990968,0.00063242856,0.0005425815,0.00021192901,0.00015998849,0.00029805023],"category_scores_gemma":[0.0005643734,0.00009299045,0.00012297923,0.0012692285,0.0002425978,0.00017941622,0.00015883328,0.000112850634,0.00010809491],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000077402794,0.000011069515,0.98757744,0.000013999772,0.00006521644,0.000066447436,0.00021352693,0.00025537994,0.005086284,0.00003439665,0.00026690206,0.0063319416],"study_design_scores_gemma":[3.7725644e-7,0.0000057343464,0.9987589,0.0000019269744,0.0000060848606,0.000018437479,0.00006891964,0.000114345,0.0005245128,0.000003097173,0.00049592665,0.0000017486301],"about_ca_topic_score_codex":0.25579432,"about_ca_topic_score_gemma":0.48320496,"teacher_disagreement_score":0.25579432,"about_ca_system_score_codex":0.0017907711,"about_ca_system_score_gemma":0.0005789417,"threshold_uncertainty_score":0.50861084},"labels":[],"label_agreement":null},{"id":"W2512227809","doi":"10.1002/2015gb005351","title":"Particulate organic carbon and nitrogen export from major Arctic rivers","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":263,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories; Natural Resources Canada; University of Alberta","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Environmental science; Biogeochemical cycle; Arctic; Particulates; Total organic carbon; Particulate organic carbon; Watershed; Fluvial; Oceanography; Hydrology (agriculture); Carbon cycle; Physical geography; Environmental chemistry; Geology; Ecosystem; Nutrient; Geography; Phytoplankton; Ecology; Chemistry","score_opus":0.016186140296400323,"score_gpt":0.21495992034924197,"score_spread":0.19877378005284163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2512227809","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990144,0.00003462541,0.000067558976,0.000004277562,8.97738e-7,0.0000013377149,0.0006371616,0.000002379301,0.00023735242],"genre_scores_gemma":[0.99701107,0.000080350874,0.00021961419,0.0000073479464,0.0000036301087,0.0000055256555,0.0022985537,0.0000026105631,0.0003712854],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998909,0.000010373165,0.000010413547,0.000043129952,0.000029345138,0.000015827767],"domain_scores_gemma":[0.99971265,0.000035930007,0.000111057605,0.000015669362,0.000088331144,0.000036329697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027801984,0.00023948721,0.00014284479,0.00056727487,0.0003769592,0.0006783637,0.000117382384,0.000114038405,0.0003359783],"category_scores_gemma":[0.0003207863,0.00009972413,0.00018478403,0.0006483683,0.00014178171,0.00021225418,0.00030772632,0.00014413461,0.000072714545],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008247506,0.000017711154,0.9919376,0.000009037004,0.000052749063,0.000043893502,0.00009714332,0.00041450013,0.0041659316,0.000030957686,0.00009221199,0.0030557378],"study_design_scores_gemma":[0.0000011291388,0.000014702295,0.99892706,0.0000014941763,0.000008447384,0.000018781348,0.000079405385,0.00032338232,0.00042209824,0.000009143387,0.00019287349,0.0000014075214],"about_ca_topic_score_codex":0.048393946,"about_ca_topic_score_gemma":0.07986222,"teacher_disagreement_score":0.048393946,"about_ca_system_score_codex":0.00056854094,"about_ca_system_score_gemma":0.00036878206,"threshold_uncertainty_score":0.09622449},"labels":[],"label_agreement":null},{"id":"W2516269908","doi":"10.1002/2015gb005338","title":"Sources of uncertainties in 21st century projections of potential ocean ecosystem stressors","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":206,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Fisheries and Oceans Canada","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Aeronautics and Space Administration","keywords":"Thermocline; Environmental science; Climate change; Climatology; Ecosystem; Marine ecosystem; Effects of global warming on oceans; Ocean acidification; Sea surface temperature; Earth system science; Global change; Global warming; Ocean observations; Oceanography; Geology; Ecology","score_opus":0.007942688290822387,"score_gpt":0.21453260296803245,"score_spread":0.20658991467721005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2516269908","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9331091,0.0011748914,0.04115406,0.004260206,0.00017427617,0.000046406833,0.005076483,0.0001638132,0.014840793],"genre_scores_gemma":[0.9957561,0.00037142186,0.0021537363,0.00012846602,0.000027836908,0.000020852003,0.0011653018,0.000022015915,0.0003541627],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99882346,0.00043233173,0.00009488088,0.00019213221,0.00034237097,0.00011489491],"domain_scores_gemma":[0.99553525,0.002265093,0.0007881856,0.00027112543,0.0009545864,0.00018571748],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0040475624,0.0006704796,0.0003418286,0.00111369,0.00052359275,0.0019967346,0.0005433705,0.0009036719,0.0013308212],"category_scores_gemma":[0.012635783,0.0004212485,0.00093926396,0.0014157447,0.0005499733,0.0018194172,0.0019022496,0.0012416934,0.00019093965],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014073384,0.000025590094,0.08718143,0.00008495585,0.0002813307,0.00025214546,0.00014519735,0.88564676,0.0009324895,0.0126589835,0.0013895856,0.0112608345],"study_design_scores_gemma":[0.000033113945,0.00010079779,0.10901012,0.0002302901,0.00014907934,0.00020992062,0.00086343766,0.80378586,0.0022674522,0.0742602,0.008889655,0.00020015948],"about_ca_topic_score_codex":0.019096171,"about_ca_topic_score_gemma":0.010520172,"teacher_disagreement_score":0.019096171,"about_ca_system_score_codex":0.0018659764,"about_ca_system_score_gemma":0.0012175402,"threshold_uncertainty_score":0.037970006},"labels":[],"label_agreement":null},{"id":"W2522893336","doi":"10.1002/2016gb005419","title":"A multiyear estimate of methane fluxes in Alaska from CARVE atmospheric observations","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Dalhousie University","funders":"National Oceanic and Atmospheric Administration; Ames Research Center; National Aeronautics and Space Administration","keywords":"Environmental science; Permafrost; Flux (metallurgy); Arctic; Methane; Atmospheric sciences; Tundra; Climatology; Greenhouse gas; Atmospheric methane; Climate model; Climate change; Geology; Oceanography","score_opus":0.010186915566044218,"score_gpt":0.2286987971320531,"score_spread":0.21851188156600887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2522893336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957313,0.00006920631,0.0021067087,0.00001786881,0.0000066586645,0.0000034295877,0.0012219357,0.00008466801,0.0007582415],"genre_scores_gemma":[0.9968352,0.00005026872,0.0015599444,0.0000051009943,0.000003388332,0.000005151799,0.0013238874,0.0000067458454,0.00021038252],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999068,0.0000139439935,0.000008916822,0.000035873367,0.000023221677,0.00001120301],"domain_scores_gemma":[0.9997683,0.000051292063,0.00005840228,0.00003394993,0.000065803426,0.000022249413],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003090948,0.0002842948,0.00015281278,0.00069845066,0.0002948233,0.00034138665,0.00019508897,0.00031206524,0.0005440841],"category_scores_gemma":[0.0005810473,0.00020342077,0.00051411183,0.00046892196,0.00008964882,0.0005277082,0.00026610823,0.00020697765,0.00011419162],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007785756,0.000074303905,0.8940209,0.000040777235,0.00022081756,0.00007052848,0.00015571447,0.083949275,0.0048718937,0.0002856722,0.00050221715,0.015730068],"study_design_scores_gemma":[0.0000073053648,0.000052804695,0.8104922,0.000031953256,0.00009894868,0.000056517285,0.0002868328,0.1835565,0.0032737737,0.0003914493,0.001716856,0.000034946104],"about_ca_topic_score_codex":0.05456774,"about_ca_topic_score_gemma":0.0859559,"teacher_disagreement_score":0.05456774,"about_ca_system_score_codex":0.00049660675,"about_ca_system_score_gemma":0.000376537,"threshold_uncertainty_score":0.10850024},"labels":[],"label_agreement":null},{"id":"W2524578103","doi":"10.1002/2016gb005406","title":"Rising atmospheric methane: 2007–2014 growth and isotopic shift","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":556,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Royal Holloway, University of London; Sight Research UK; National Oceanic and Atmospheric Administration; Met Office; Natural Environment Research Council; Royal Society","keywords":"Methane; Atmospheric methane; Environmental science; Tropics; Atmospheric sciences; Wetland; Southern Hemisphere; Fossil fuel; Northern Hemisphere; Latitude; Atmosphere (unit); Environmental chemistry; Climatology; Chemistry; Ecology; Geology; Meteorology; Geography; Biology","score_opus":0.0043754149579767025,"score_gpt":0.20293090752326529,"score_spread":0.1985554925652886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2524578103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929997,0.00017432754,0.0001573864,0.0006144686,0.000044886914,0.000006414372,0.004085878,0.000026843618,0.0018900972],"genre_scores_gemma":[0.99537754,0.00013066443,0.00016810623,0.00010821559,0.000043454842,0.0000068406353,0.0035764808,0.000008182766,0.00058051344],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988115,0.000011381115,0.000008512923,0.000028314482,0.000037239275,0.000033501175],"domain_scores_gemma":[0.9996183,0.000025846266,0.000094277726,0.000018498537,0.00018150511,0.00006157611],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031357727,0.00019536821,0.00016200425,0.0007760023,0.0002561976,0.00041306246,0.00022133238,0.00039526325,0.0011327368],"category_scores_gemma":[0.0005191217,0.00011325144,0.00021896992,0.0011279264,0.00022884528,0.00034510033,0.00048425602,0.0003870927,0.0002727492],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040361937,0.00009071953,0.9693419,0.00006949919,0.00012505573,0.00015963617,0.00028635835,0.0008022017,0.010461236,0.0003768687,0.0038333514,0.014049564],"study_design_scores_gemma":[0.0000017852722,0.000013825049,0.99719954,0.0000046451687,0.00000791766,0.000024739633,0.00010870904,0.0004043743,0.000905277,0.000028090466,0.0012971514,0.0000039373067],"about_ca_topic_score_codex":0.042522825,"about_ca_topic_score_gemma":0.047066186,"teacher_disagreement_score":0.042522825,"about_ca_system_score_codex":0.0009389199,"about_ca_system_score_gemma":0.00070810446,"threshold_uncertainty_score":0.08455062},"labels":[],"label_agreement":null},{"id":"W2525934856","doi":"10.1002/2015gb005323","title":"Mercury isotope compositions across North American forests","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":216,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of Toronto","funders":"","keywords":"Mercury (programming language); Soil water; Plant litter; Environmental chemistry; Forest floor; Biogeochemical cycle; Terrestrial ecosystem; Ecosystem; Soil horizon; Environmental science; Isotope; Deposition (geology); Cycling; Forest ecology; Litter; Chemistry; Ecology; Geology; Soil science; Sediment; Forestry; Geomorphology","score_opus":0.012910597994135416,"score_gpt":0.2806042608498069,"score_spread":0.2676936628556715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2525934856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99908495,0.00011540362,0.000074740914,0.000005912089,8.5186826e-7,0.0000017211216,0.0002597347,0.000008983997,0.00044786165],"genre_scores_gemma":[0.9987985,0.00014544452,0.0002779713,0.000017847624,0.0000016240552,0.0000047198855,0.00050562236,0.000003110219,0.0002451736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999405,0.0000065572276,0.0000030754686,0.000023219207,0.000015384312,0.000011231565],"domain_scores_gemma":[0.99989605,0.000012019909,0.000026031306,0.0000068164245,0.00004454445,0.000014549113],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001197226,0.00017330072,0.00013107853,0.0008198235,0.00048205527,0.00027357426,0.00016419656,0.00010695557,0.00049104716],"category_scores_gemma":[0.0001228394,0.00010846165,0.0001026448,0.00081329176,0.00015139578,0.00013747347,0.00018043976,0.00007780927,0.00007807447],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000100938545,0.000028702672,0.9667672,0.000023682516,0.00007711488,0.00007947874,0.00022833508,0.00032945696,0.018822346,0.000038273934,0.00018066753,0.013323819],"study_design_scores_gemma":[0.0000011489616,0.0000072723615,0.9988992,0.0000017899752,0.000011767846,0.000022473372,0.00008770148,0.00016697936,0.00054722704,0.000015088787,0.00023782124,0.0000013946179],"about_ca_topic_score_codex":0.08579085,"about_ca_topic_score_gemma":0.24302639,"teacher_disagreement_score":0.9142091,"about_ca_system_score_codex":0.00039264152,"about_ca_system_score_gemma":0.00029906697,"threshold_uncertainty_score":0.17058295},"labels":[],"label_agreement":null},{"id":"W2526533082","doi":"10.1002/2016gb005463","title":"The role of metabolism in modulating CO<sub>2</sub> fluxes in boreal lakes","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Primary production; Environmental science; Autotroph; Ecosystem; Boreal; Carbon cycle; Ecosystem respiration; Heterotroph; Boreal ecosystem; Atmospheric sciences; Cycling; Ecology; Environmental chemistry; Chemistry; Biology; Geology","score_opus":0.005401091706156426,"score_gpt":0.19590142832465188,"score_spread":0.19050033661849544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2526533082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99949074,0.000086174616,0.00017159947,0.000009551436,7.1503354e-7,0.0000016733255,0.00006674852,0.000006745959,0.00016612049],"genre_scores_gemma":[0.99975127,0.000027250158,0.0001286489,0.000004907356,0.0000010914438,0.0000015830002,0.000046186924,0.000001614587,0.000037435715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993455,0.00001586108,0.000006015952,0.000020924173,0.00000793121,0.000014707007],"domain_scores_gemma":[0.9998155,0.000038500904,0.00008136748,0.0000111990175,0.000022880293,0.00003049247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026575857,0.00025800543,0.00020852411,0.00040308133,0.00037617466,0.0006096979,0.00012690754,0.00019138568,0.0003031384],"category_scores_gemma":[0.0003357225,0.00020371015,0.00020215489,0.00026590965,0.00036614004,0.0004285825,0.000368787,0.00010619823,0.000041647705],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052843045,0.000038339545,0.76425815,0.00006588027,0.00013745614,0.0001216125,0.0003887668,0.0023647493,0.22440992,0.00020706405,0.0000980697,0.007381629],"study_design_scores_gemma":[0.0000017063282,0.00003444024,0.99655116,0.0000013647852,0.000014461719,0.000027943192,0.000055814504,0.0015948587,0.0015878147,0.000041812742,0.00008465623,0.000003854287],"about_ca_topic_score_codex":0.010577413,"about_ca_topic_score_gemma":0.013110883,"teacher_disagreement_score":0.010577413,"about_ca_system_score_codex":0.0003815275,"about_ca_system_score_gemma":0.00022181153,"threshold_uncertainty_score":0.021031678},"labels":[],"label_agreement":null},{"id":"W2527273020","doi":"10.1002/2016gb005408","title":"Tracing dust input to the global ocean using thorium isotopes in marine sediments: ThoroMap","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Past Global Changes; National Centers for Environmental Information; National Oceanic and Atmospheric Administration; FP7 People: Marie-Curie Actions; National Science Foundation","keywords":"Geology; Oceanography; Last Glacial Maximum; Aeolian processes; Ice core; Holocene; Environmental science; Marine isotope stage; Earth science; Glacial period; Interglacial; Geomorphology","score_opus":0.019707555388640396,"score_gpt":0.2709354855743238,"score_spread":0.2512279301856834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2527273020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9815263,0.00022457974,0.005800486,0.000051534804,0.000015924623,0.000018937613,0.009741369,0.0004425416,0.0021783535],"genre_scores_gemma":[0.9835413,0.00018155228,0.00970867,0.00001753958,0.000011295334,0.000025410964,0.0061533907,0.000063513085,0.00029748929],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999273,0.000010125405,0.000005915166,0.000024862113,0.000023193625,0.000008558994],"domain_scores_gemma":[0.99971324,0.00005545149,0.00007552105,0.000049776838,0.00008586071,0.000020158937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021071662,0.0004373811,0.0001894674,0.0013537278,0.00020116963,0.00044860053,0.00023039574,0.00021370673,0.00037943738],"category_scores_gemma":[0.00055153976,0.0001663846,0.00041752568,0.001313488,0.0001266381,0.00023848825,0.00045721701,0.00018346503,0.0001559095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023497359,0.00006433808,0.8510457,0.00020700386,0.00047233462,0.00037330977,0.00018826484,0.059957452,0.03202016,0.00050352525,0.0019225855,0.053010214],"study_design_scores_gemma":[0.000053024203,0.00007432224,0.861905,0.000040649877,0.00013277426,0.00016237125,0.00013732226,0.10798287,0.022777062,0.0005897661,0.006097333,0.000047549904],"about_ca_topic_score_codex":0.02407786,"about_ca_topic_score_gemma":0.0314032,"teacher_disagreement_score":0.02407786,"about_ca_system_score_codex":0.00045389996,"about_ca_system_score_gemma":0.00035055703,"threshold_uncertainty_score":0.047875404},"labels":[],"label_agreement":null},{"id":"W2556425461","doi":"10.1002/2016gb005414","title":"Factors regulating the Great Calcite Belt in the Southern Ocean and its biogeochemical significance","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":183,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Centre National de la Recherche Scientifique; Dalhousie University; National Science Foundation","keywords":"Calcite; Biogeochemical cycle; Oceanography; Flux (metallurgy); Calcium carbonate; Particulates; Seawater; Coccolithophore; Carbonate; Geology; Atmosphere (unit); Environmental science; Mineralogy; Environmental chemistry; Phytoplankton; Chemistry; Nutrient; Geography; Meteorology","score_opus":0.017549772530927682,"score_gpt":0.2147590945572658,"score_spread":0.19720932202633812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2556425461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993291,0.00008433744,0.000043727658,0.0000209633,0.0000011490922,0.000002758033,0.000064844266,0.0000043058444,0.0004488822],"genre_scores_gemma":[0.9997489,0.00003427292,0.00006545454,0.000008505825,0.0000017230983,0.0000013476997,0.000061010862,0.0000010941811,0.00007777138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999281,0.0000088685365,0.0000039827505,0.000022524924,0.00001928052,0.000017269436],"domain_scores_gemma":[0.9998242,0.000022827922,0.00007018457,0.000009620951,0.000033074055,0.000040165054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001423493,0.0001706406,0.0001422744,0.00048283132,0.00040472564,0.00053386635,0.00016316089,0.00020142338,0.000403962],"category_scores_gemma":[0.00025725184,0.000100711884,0.000088944435,0.0004968392,0.00062295684,0.0001590171,0.00030381425,0.00009689876,0.00004390294],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019036786,0.00002983161,0.80514497,0.000044101846,0.00002849203,0.00014978413,0.00034455326,0.00036661557,0.18900792,0.00014870611,0.00006638028,0.0044781873],"study_design_scores_gemma":[0.000002990324,0.000019175535,0.99739826,0.0000023584364,0.0000053967237,0.000027433101,0.00027120908,0.00021379323,0.0018161457,0.000031357027,0.00020974228,0.0000021362284],"about_ca_topic_score_codex":0.052232806,"about_ca_topic_score_gemma":0.068108924,"teacher_disagreement_score":0.052232806,"about_ca_system_score_codex":0.00057174545,"about_ca_system_score_gemma":0.000419937,"threshold_uncertainty_score":0.10385752},"labels":[],"label_agreement":null},{"id":"W2560085714","doi":"10.1002/2016gb005483","title":"What proportion of riverine nutrients reaches the open ocean?","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":165,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"University of East Anglia; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Biogeochemical cycle; Plume; Oceanography; Pelagic zone; Environmental science; Nutrient; Continental shelf; Estuary; Salinity; Latitude; Deposition (geology); Residence time (fluid dynamics); Geology; Structural basin; Geography; Meteorology; Ecology","score_opus":0.01470872862309533,"score_gpt":0.22820030267944533,"score_spread":0.21349157405635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560085714","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97991735,0.0018966837,0.00433783,0.0005302889,0.000016479096,0.0000039536935,0.0020976614,0.00008280535,0.011116965],"genre_scores_gemma":[0.9968027,0.0009109805,0.00043064763,0.00010214146,0.000014795531,0.0000029075063,0.00052333315,0.00001824076,0.00119426],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990237,0.00001249112,0.000007287041,0.000042181022,0.000019582576,0.000016175985],"domain_scores_gemma":[0.99964905,0.00010605717,0.00011805631,0.000023339386,0.000061168066,0.00004227124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012513869,0.00015095339,0.0001865768,0.00040437392,0.0001608052,0.0012733593,0.0002465211,0.00023113063,0.0033875033],"category_scores_gemma":[0.0008505393,0.00012393986,0.00020293065,0.00081557734,0.00031186477,0.0012004565,0.0003639558,0.00015573952,0.0005885061],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010897143,0.00002889717,0.9015563,0.00021879199,0.00024390277,0.00027276718,0.00041175657,0.008914981,0.0081340065,0.005306363,0.0021975634,0.07260578],"study_design_scores_gemma":[0.000019698156,0.000063544845,0.9297546,0.00013398808,0.0001279797,0.0005292963,0.0017933984,0.022002533,0.0055273683,0.015288488,0.024720415,0.000038675964],"about_ca_topic_score_codex":0.009401272,"about_ca_topic_score_gemma":0.012503445,"teacher_disagreement_score":0.009401272,"about_ca_system_score_codex":0.00039318632,"about_ca_system_score_gemma":0.0001857891,"threshold_uncertainty_score":0.01869309},"labels":[],"label_agreement":null},{"id":"W2560806021","doi":"10.1002/2016gb005498","title":"Two centuries of nitrogen dynamics: Legacy sources and sinks in the Mississippi and Susquehanna River Basins","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":298,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Groundwater; Hydrology (agriculture); Environmental science; Drainage basin; Dominance (genetics); Sink (geography); Deposition (geology); Structural basin; Nitrate; Surface water; Geology; Ecology; Geography; Environmental engineering; Geomorphology","score_opus":0.005693458954460441,"score_gpt":0.21344928527188994,"score_spread":0.2077558263174295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560806021","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99896634,0.000046937017,0.00019391743,0.00008206362,0.0000014977949,0.0000021624471,0.00021982926,0.000008169002,0.00047906814],"genre_scores_gemma":[0.99892503,0.000065927496,0.0003875288,0.000018238083,0.0000016616285,0.0000040538757,0.0003043765,0.000005673858,0.00028752343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993825,0.00001487262,0.000003992511,0.000026351052,0.0000074049703,0.0000091803195],"domain_scores_gemma":[0.99985135,0.000036920374,0.00003453041,0.000016998141,0.000031358333,0.000028846009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026169384,0.00016892346,0.00013608733,0.00047320232,0.0005911948,0.0008176827,0.00047755853,0.00057021546,0.00096982863],"category_scores_gemma":[0.00056673633,0.00021531536,0.00032248785,0.00059737975,0.0003801394,0.0005501353,0.00055706524,0.00031906425,0.00006815977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000118402175,0.00010987967,0.85848385,0.000058549307,0.00021526037,0.0005148201,0.0014482155,0.116714165,0.0041047344,0.00254718,0.0009041016,0.014780951],"study_design_scores_gemma":[0.000042563504,0.00008261646,0.68864536,0.0000663342,0.00008424255,0.00016163042,0.001922572,0.29992485,0.0013390251,0.0016499336,0.006016503,0.00006439825],"about_ca_topic_score_codex":0.2321254,"about_ca_topic_score_gemma":0.30410516,"teacher_disagreement_score":0.2321254,"about_ca_system_score_codex":0.002085863,"about_ca_system_score_gemma":0.001278422,"threshold_uncertainty_score":0.46154857},"labels":[],"label_agreement":null},{"id":"W2564730929","doi":"10.1002/2016gb005459","title":"Increasing net ecosystem biomass production of Canada's boreal and temperate forests despite decline in dry climates","year":2016,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; University of British Columbia; Canadian Forest Service","funders":"Natural Resources Canada; University of British Columbia; Department of Environment and Conservation, Government of Newfoundland and Labrador; Ministry of Forests, Lands and Natural Resource Operations; Ministry of Natural Resources","keywords":"Environmental science; Biomass (ecology); Ecosystem; Sink (geography); Temperate climate; Carbon sink; Primary production; Taiga; Climate change; Greenhouse gas; Atmospheric sciences; Ecology; Temperate rainforest; Geography; Biology","score_opus":0.004342408440071824,"score_gpt":0.19537110167117183,"score_spread":0.1910286932311,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2564730929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984358,0.00009084247,0.00018994957,0.00004286207,0.000001659434,0.0000029288112,0.0005385178,0.0000147412575,0.0006826945],"genre_scores_gemma":[0.9992507,0.00003642626,0.00016866381,0.000014477735,8.821012e-7,0.0000020374312,0.00033615305,0.0000029282596,0.00018768603],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999866,0.000009347416,0.000005337041,0.00004231946,0.000029892226,0.000047033976],"domain_scores_gemma":[0.99971145,0.000032991447,0.000042985484,0.00001909912,0.000110899666,0.00008244861],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030511757,0.00027907308,0.00020865597,0.00041923986,0.0007500602,0.00087131414,0.00045075407,0.00019390858,0.00059902435],"category_scores_gemma":[0.00055325305,0.0001941554,0.00038174618,0.00051346415,0.0004732849,0.00025436562,0.0003667993,0.0002147458,0.000049865383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011868395,0.00002723612,0.96731055,0.00003980729,0.0001712426,0.00008510261,0.00019567918,0.016337387,0.007173217,0.0004500621,0.0005963261,0.007494746],"study_design_scores_gemma":[0.000004660058,0.000009376144,0.99114835,0.000003560955,0.000016819024,0.000020121768,0.0001287262,0.007881824,0.00027205065,0.000057463072,0.0004501832,0.0000069720913],"about_ca_topic_score_codex":0.9410462,"about_ca_topic_score_gemma":0.9698224,"teacher_disagreement_score":0.05895382,"about_ca_system_score_codex":0.008277999,"about_ca_system_score_gemma":0.005098727,"threshold_uncertainty_score":0.11860198},"labels":[],"label_agreement":null},{"id":"W2568176580","doi":"10.1002/2016gb005378","title":"Organic matter remineralization in marine sediments: A Pan‐Arctic synthesis","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Université du Québec à Rimouski","funders":"Natural Environment Research Council; Sight Research UK; ArcticNet; Agence Nationale de la Recherche; National Science Foundation","keywords":"Benthic zone; Arctic; Organic matter; Oceanography; Environmental science; Remineralisation; Ecosystem; Continental shelf; Sediment; Ecology; Geology; Chemistry; Biology; Geomorphology","score_opus":0.008226039899672393,"score_gpt":0.21856663117201577,"score_spread":0.2103405912723434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2568176580","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01217428,0.9842786,0.0007394553,0.0003494787,0.00023199947,0.00000554515,0.00078396586,0.000015161136,0.0014214584],"genre_scores_gemma":[0.062177528,0.93404734,0.0018594454,0.00020389445,0.0005020256,0.000011946992,0.0009147515,0.000013333261,0.00026977618],"study_design_codex":"design_other","study_design_gemma":"systematic_review","domain_scores_codex":[0.9995977,0.000068489506,0.000086903456,0.00014316334,0.000063761356,0.000040066447],"domain_scores_gemma":[0.9981018,0.0006854116,0.0003927722,0.00006932537,0.00065327476,0.00009753145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001980219,0.0010098496,0.00087697594,0.0060259006,0.00036327948,0.0022250188,0.00029450445,0.0003398081,0.0009673214],"category_scores_gemma":[0.001951056,0.0002797489,0.0007671633,0.009811906,0.00039861546,0.00087705953,0.00074190594,0.0005464702,0.00019890584],"study_design_candidate":"systematic_review","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041725262,0.00012731816,0.03980665,0.06269366,0.0024071222,0.00046990992,0.0012312545,0.0045558815,0.010902935,0.004217077,0.008684083,0.8644869],"study_design_scores_gemma":[0.000022189864,0.00061503734,0.40010026,0.04219252,0.0058739986,0.0011129634,0.0013885262,0.0021052386,0.005006032,0.0043550557,0.53709245,0.00013569652],"about_ca_topic_score_codex":0.018688167,"about_ca_topic_score_gemma":0.026899345,"teacher_disagreement_score":0.018688167,"about_ca_system_score_codex":0.0011200913,"about_ca_system_score_gemma":0.0024801865,"threshold_uncertainty_score":0.037158787},"labels":[],"label_agreement":null},{"id":"W2575973976","doi":"10.1002/2016gb005586","title":"A reevaluation of the magnitude and impacts of anthropogenic atmospheric nitrogen inputs on the ocean","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":264,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Dalhousie University","funders":"Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Biogeochemistry; Environmental science; Fluvial; Nitrogen; Nitrogen fixation; Nitrogen cycle; Reactive nitrogen; Continental shelf; Deep sea; Oceanography; Biogeochemical cycle; Denitrification; Atmosphere (unit); Geochemical cycle; Geology; Environmental chemistry; Chemistry; Meteorology","score_opus":0.01318714714995963,"score_gpt":0.23626147976233716,"score_spread":0.22307433261237752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2575973976","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7246116,0.21093918,0.023515327,0.012332153,0.0010838279,0.000060647337,0.007955409,0.00038189712,0.019119922],"genre_scores_gemma":[0.93238693,0.05190009,0.011613833,0.001174848,0.00028701243,0.000027570079,0.0012306273,0.00005675093,0.001322335],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99921465,0.00019314144,0.000118770935,0.00020994918,0.00022398584,0.00003959524],"domain_scores_gemma":[0.9955546,0.0013423876,0.0005496385,0.0003593872,0.0020671624,0.00012681625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0038314732,0.00086440437,0.00091220293,0.002143033,0.00034717997,0.002494094,0.00057209545,0.00045132654,0.0008193471],"category_scores_gemma":[0.005327857,0.0002995478,0.0006429079,0.002149034,0.00057460676,0.0022880232,0.00090722035,0.0008289614,0.00018309054],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012517439,0.00011430995,0.33693466,0.008773836,0.0042406,0.0006930787,0.0013020986,0.03599446,0.030815288,0.009161842,0.007714981,0.5630031],"study_design_scores_gemma":[0.00006636735,0.00065439043,0.7172787,0.0037703891,0.003734289,0.00050692476,0.00253956,0.03526645,0.030184118,0.014085747,0.19170803,0.00020507099],"about_ca_topic_score_codex":0.017277768,"about_ca_topic_score_gemma":0.029227912,"teacher_disagreement_score":0.017277768,"about_ca_system_score_codex":0.0023067214,"about_ca_system_score_gemma":0.0019349903,"threshold_uncertainty_score":0.03435445},"labels":[],"label_agreement":null},{"id":"W2580742740","doi":"10.1002/2016gb005471","title":"Mobility and transport of mercury and methylmercury in peat as a function of changes in water table regime and plant functional groups","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"U.S. Forest Service; Natural Sciences and Engineering Research Council of Canada; Northern Research Station; University of Toronto; U.S. Department of Agriculture; National Science Foundation","keywords":"Peat; Mesocosm; Environmental science; Methylmercury; Water table; Ericaceae; Wetland; Ecosystem; Ecology; Sphagnum; Hydrology (agriculture); Calluna; Periphyton; Environmental chemistry; Nutrient; Chemistry; Biology; Groundwater; Geology; Bioaccumulation","score_opus":0.016825249626306552,"score_gpt":0.24359524275900313,"score_spread":0.22676999313269658,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2580742740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99983656,0.000007748298,0.0000622906,0.0000026553264,4.373067e-7,0.0000016663453,0.000033187418,0.0000012656315,0.000054087897],"genre_scores_gemma":[0.9991252,0.000022711347,0.00029874736,0.000007372079,8.184452e-7,0.000009534803,0.000099105666,0.0000014609744,0.000435056],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995077,0.000007128881,0.0000024614865,0.00002134122,0.000007837926,0.000010435684],"domain_scores_gemma":[0.999912,0.000019312341,0.000017355143,0.000007611234,0.000016200747,0.000027428301],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013226767,0.00011465664,0.00013516936,0.00013920428,0.000219656,0.0002251968,0.00012417597,0.000111137066,0.00058129383],"category_scores_gemma":[0.0001068631,0.000094432085,0.0001333526,0.00009242924,0.00016977184,0.00022768589,0.00019343456,0.00019843437,0.000057936253],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00087597454,0.00017990344,0.11944267,0.000025401378,0.000051407802,0.000046134337,0.0002642798,0.0005513349,0.8748017,0.00007111666,0.00006732464,0.0036227282],"study_design_scores_gemma":[0.00002645694,0.0009882876,0.88562936,0.000004445574,0.00004785719,0.000065944674,0.0003929967,0.005916474,0.10637138,0.00010184026,0.00044506355,0.000009863539],"about_ca_topic_score_codex":0.01219357,"about_ca_topic_score_gemma":0.021147365,"teacher_disagreement_score":0.01219357,"about_ca_system_score_codex":0.00039453027,"about_ca_system_score_gemma":0.00025102065,"threshold_uncertainty_score":0.024245143},"labels":[],"label_agreement":null},{"id":"W2583727975","doi":"10.1002/2016gb005452","title":"Development of a global ocean mercury model with a methylation cycle: Outstanding issues","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Biogeochemistry; Oceanography; Sediment trap; Geochemical cycle; Environmental science; Mercury (programming language); Biogeochemical cycle; Carbon cycle; Seabed; Water column; Environmental chemistry; Geology; Chemistry; Ecology; Ecosystem","score_opus":0.026760189889021423,"score_gpt":0.3040673965679076,"score_spread":0.2773072066788862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2583727975","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.37832537,0.0007969813,0.57306534,0.0054794974,0.00061974267,0.0004799777,0.0035906543,0.0075759515,0.030066557],"genre_scores_gemma":[0.65078473,0.00076229253,0.33781275,0.00050059037,0.00014029104,0.0006134411,0.0018386429,0.0012022989,0.0063451],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998869,0.000035958557,0.0000071681015,0.000022541853,0.00003302702,0.000014494939],"domain_scores_gemma":[0.9996445,0.00011255843,0.000019497425,0.000060803355,0.00011073119,0.0000518574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069692044,0.000646442,0.0006831894,0.00017949339,0.00047813612,0.00077926693,0.00192955,0.0012857192,0.0021180664],"category_scores_gemma":[0.0013618739,0.0005283502,0.0008099346,0.000349357,0.00038589857,0.0012429991,0.0010368846,0.0012114721,0.00065730716],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006462417,0.00004975201,0.0033017343,0.000074794814,0.00005705957,0.00011132518,0.00004400165,0.97596073,0.0037849029,0.004338812,0.0010527867,0.011159476],"study_design_scores_gemma":[0.00006758365,0.00003134771,0.00036558163,0.000008667188,0.000016732192,0.000017407772,0.000010990101,0.9922328,0.0013860223,0.0018426498,0.0040068496,0.000013402244],"about_ca_topic_score_codex":0.01497416,"about_ca_topic_score_gemma":0.010149216,"teacher_disagreement_score":0.01497416,"about_ca_system_score_codex":0.00070467795,"about_ca_system_score_gemma":0.0022220733,"threshold_uncertainty_score":0.02977395},"labels":[],"label_agreement":null},{"id":"W2593315406","doi":"10.1002/2016gb005504","title":"Measurement of the <sup>13</sup>C isotopic signature of methane emissions from northern European wetlands","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":116,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Isotopic signature; Wetland; Methane; Environmental science; Flux (metallurgy); Atmospheric methane; Atmosphere (unit); Atmospheric sciences; Boreal; Taiga; Hydrology (agriculture); Isotope; Geology; Chemistry; Ecology; Meteorology; Physics","score_opus":0.009524391788953278,"score_gpt":0.20912888367899785,"score_spread":0.19960449189004456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2593315406","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990671,0.000041640553,0.00035119095,0.0000037772013,0.0000010599239,0.0000010866353,0.00011985773,0.000007927179,0.00040635729],"genre_scores_gemma":[0.99834216,0.000050577393,0.0011137539,0.000007994381,0.0000012264635,0.0000026725295,0.00023737668,0.0000054408865,0.00023884862],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999298,0.000009222502,0.0000025109784,0.000026827356,0.00001749496,0.0000141457895],"domain_scores_gemma":[0.9999232,0.000016631928,0.000017370523,0.000006794763,0.000025549554,0.00001047695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013057019,0.00018849115,0.00009411448,0.00019946154,0.0002473932,0.00021377766,0.00011738842,0.00012288286,0.00035843288],"category_scores_gemma":[0.00011956665,0.00007572337,0.000082067105,0.00018766818,0.00016485075,0.00011133245,0.00010685902,0.00009064252,0.00009984287],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029771565,0.000019493478,0.17306322,0.000029943592,0.00003897036,0.000060808154,0.00009015404,0.00049071776,0.8136954,0.00005527291,0.0000864695,0.012071787],"study_design_scores_gemma":[0.0000041078465,0.000056234443,0.84921056,0.000003624498,0.000020604899,0.00010536992,0.00008891775,0.0013418001,0.14828032,0.00002783698,0.0008524667,0.000008187016],"about_ca_topic_score_codex":0.015107964,"about_ca_topic_score_gemma":0.030488709,"teacher_disagreement_score":0.015107964,"about_ca_system_score_codex":0.00025291488,"about_ca_system_score_gemma":0.00014381405,"threshold_uncertainty_score":0.030040026},"labels":[],"label_agreement":null},{"id":"W2594550998","doi":"10.1002/2016gb005567","title":"N<sub>2</sub>O production and consumption from stable isotopic and concentration data in the Peruvian coastal upwelling system","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Office of Science; Deutsche Forschungsgemeinschaft; U.S. Department of Energy","keywords":"Denitrification; Nitrate; Environmental chemistry; Upwelling; Nitrous oxide; Isotopes of nitrogen; Organic matter; New production; Isotope analysis; Stable isotope ratio; Anoxic waters; Dominance (genetics); Isotopomers; Nitrite; Environmental science; Chemistry; Nutrient; Oceanography; Nitrogen; Geology; Phytoplankton","score_opus":0.02200791443226841,"score_gpt":0.2250819332691905,"score_spread":0.20307401883692208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2594550998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992072,0.00007240637,0.000101834914,0.000024909923,5.0222343e-7,0.0000032330338,0.00026076924,0.0000070671194,0.00032214864],"genre_scores_gemma":[0.99891937,0.00009520914,0.00023903002,0.000014666248,0.0000023761588,0.000010884996,0.00062075723,0.000003829259,0.000093980205],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990153,0.000025620539,0.000008772014,0.00002897053,0.000016122636,0.000019012641],"domain_scores_gemma":[0.9995757,0.00007612133,0.00017088746,0.00003505482,0.000105602594,0.000036719095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024975775,0.00031281973,0.00016668568,0.0010123088,0.0003603962,0.0005316001,0.00030993487,0.00039462923,0.0007908304],"category_scores_gemma":[0.00084401644,0.00022444119,0.00029866464,0.0010495841,0.0002895733,0.0003768345,0.0007350164,0.0001722078,0.0001817124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006950528,0.000015900685,0.983127,0.00003972854,0.00008483581,0.00014229062,0.00070053525,0.0006395422,0.010881558,0.00003335472,0.000099641315,0.0041661155],"study_design_scores_gemma":[0.000002358393,0.000014925474,0.99840194,0.0000052935666,0.0000111093705,0.000030859657,0.00024192162,0.0007788051,0.00028176783,0.000013252551,0.00021285408,0.000004895487],"about_ca_topic_score_codex":0.044710435,"about_ca_topic_score_gemma":0.06231489,"teacher_disagreement_score":0.044710435,"about_ca_system_score_codex":0.00046045776,"about_ca_system_score_gemma":0.0003232543,"threshold_uncertainty_score":0.08890039},"labels":[],"label_agreement":null},{"id":"W2610813618","doi":"10.1002/2016gb005548","title":"Contributions of wildland fire to terrestrial ecosystem carbon dynamics in North America from 1990 to 2012","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Center for Selective C-H Functionalization, National Science Foundation; U.S. Geological Survey; U.S. Department of Energy; Alaska Climate Adaptation Science Center, University of Alaska Fairbanks; National Science Foundation","keywords":"Environmental science; Ecosystem; Carbon sink; Terrestrial ecosystem; Carbon cycle; Biome; Disturbance (geology); Taiga; Fire regime; Carbon fibers; Atmospheric sciences; Primary production; Ecology; Geology","score_opus":0.005156685822496345,"score_gpt":0.2273359093753006,"score_spread":0.22217922355280426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2610813618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99851733,0.0001737326,0.00016934561,0.0000683053,0.000012444303,0.000004933672,0.00069498474,0.000023150807,0.00033580145],"genre_scores_gemma":[0.9985696,0.000121828336,0.00017536005,0.000024548084,0.0000072588637,0.00000912899,0.00083914894,0.000004679975,0.00024832724],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998895,0.000018138848,0.000008073858,0.000040845116,0.000017926344,0.00002548892],"domain_scores_gemma":[0.99977225,0.00004002692,0.0000551535,0.000014091564,0.00007618874,0.000042264033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028682945,0.0004089834,0.0002219099,0.00052554003,0.00034100102,0.0005598795,0.0003321483,0.00039089852,0.0007858973],"category_scores_gemma":[0.0005552002,0.0002480127,0.00072609197,0.0005610655,0.00017637106,0.00042382497,0.00034996637,0.0002973543,0.00008046693],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023564356,0.00013156653,0.89692026,0.00007986461,0.0003127175,0.00029790238,0.000120868186,0.088640906,0.0025304947,0.00020276156,0.0011593329,0.0093677305],"study_design_scores_gemma":[0.000026210837,0.000053460622,0.87138814,0.000021371108,0.00011456428,0.0000930847,0.0002240315,0.12597468,0.0007155609,0.0002879981,0.0010723561,0.000028498765],"about_ca_topic_score_codex":0.11094523,"about_ca_topic_score_gemma":0.14447397,"teacher_disagreement_score":0.11094523,"about_ca_system_score_codex":0.0013583992,"about_ca_system_score_gemma":0.0007306123,"threshold_uncertainty_score":0.22059888},"labels":[],"label_agreement":null},{"id":"W2611522945","doi":"10.1002/2016gb005493","title":"Seasonal and spatial variabilities in northern Gulf of Alaska surface water iron concentrations driven by shelf sediment resuspension, glacial meltwater, a Yakutat eddy, and dust","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Meltwater; Oceanography; Continental shelf; Sediment; Glacial period; Nitrate; Environmental science; Particulates; Geology; Flux (metallurgy); Surface water; Geomorphology; Chemistry","score_opus":0.006698379985310615,"score_gpt":0.2028896252105454,"score_spread":0.1961912452252348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2611522945","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996693,0.000016620332,0.000032089614,0.0000055721343,0.0000013807041,7.246024e-7,0.00010567072,0.000004430785,0.00016425973],"genre_scores_gemma":[0.99965155,0.000015424002,0.00004798132,0.0000023924033,0.000001110345,0.0000021103626,0.00016466774,0.0000011992006,0.00011366057],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999423,0.0000066916596,0.000006082213,0.00002457639,0.000010698086,0.000009673713],"domain_scores_gemma":[0.9997553,0.00004897275,0.00006962144,0.000018066514,0.00005776237,0.00005022963],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020902374,0.00017819245,0.00014585395,0.00052697764,0.00030117086,0.00040991255,0.00015316828,0.00021548316,0.00051487464],"category_scores_gemma":[0.00040920704,0.0001721876,0.0002002079,0.00038505482,0.00021304087,0.00022372481,0.0002833939,0.00013137134,0.00009432706],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000104082974,0.000023660386,0.98663414,0.000010714064,0.00004703514,0.00010545016,0.0003408589,0.0015751591,0.008345487,0.000039313985,0.000124429,0.0026497217],"study_design_scores_gemma":[0.0000021358064,0.000010877327,0.99720603,0.0000033597746,0.000010180746,0.000018045625,0.00024058654,0.00205218,0.00030791858,0.000019680954,0.00012529588,0.0000036586746],"about_ca_topic_score_codex":0.060412075,"about_ca_topic_score_gemma":0.07815075,"teacher_disagreement_score":0.060412075,"about_ca_system_score_codex":0.0004759693,"about_ca_system_score_gemma":0.00028194938,"threshold_uncertainty_score":0.12012088},"labels":[],"label_agreement":null},{"id":"W2618609623","doi":"10.1002/2017gb005648","title":"Understanding the unique biogeochemistry of the Mediterranean Sea: Insights from a coupled phosphorus and nitrogen model","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"University of Waterloo; Canada Excellence Research Chairs, Government of Canada","keywords":"Biogeochemical cycle; Biogeochemistry; Oceanography; Environmental science; Mediterranean sea; Denitrification; Mediterranean climate; Water column; Phosphorus; Ocean gyre; Reactive nitrogen; Nitrate; Nitrogen cycle; Environmental chemistry; Nitrogen; Chemistry; Ecology; Subtropics; Geology; Biology","score_opus":0.033123525895842124,"score_gpt":0.2227124943820834,"score_spread":0.1895889684862413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2618609623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9720639,0.00024992306,0.01645193,0.0007067407,0.000035309982,0.000028061457,0.000590991,0.00013955144,0.009733663],"genre_scores_gemma":[0.9955383,0.00012520149,0.0030991836,0.00008264083,0.000023430648,0.00002838485,0.0001949048,0.000021965008,0.00088589627],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999435,0.000016605813,0.0000032222738,0.000018230894,0.0000075233856,0.000010911068],"domain_scores_gemma":[0.99984324,0.0000684601,0.000021874172,0.000010755047,0.000025935104,0.000029622492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027404467,0.00057285966,0.0005413773,0.000287543,0.00041456148,0.0008776702,0.00093494926,0.0011511939,0.0011384028],"category_scores_gemma":[0.0007254823,0.00033850875,0.00072065083,0.00026541293,0.0004723708,0.000680722,0.0007215229,0.000428116,0.00011749403],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033767432,0.000026358164,0.0064078597,0.000016491875,0.0000611906,0.00008979582,0.00002616724,0.9894372,0.0011998953,0.0012849632,0.00021327595,0.0012030188],"study_design_scores_gemma":[0.000023215782,0.0000129147165,0.0014790454,0.000001935672,0.000013287265,0.000005336077,0.00001336749,0.9974056,0.00006292117,0.0008028863,0.0001746937,0.00000480797],"about_ca_topic_score_codex":0.05837431,"about_ca_topic_score_gemma":0.027885206,"teacher_disagreement_score":0.05837431,"about_ca_system_score_codex":0.0013586566,"about_ca_system_score_gemma":0.0009731116,"threshold_uncertainty_score":0.11606908},"labels":[],"label_agreement":null},{"id":"W2622869046","doi":"10.1002/2016gb005539","title":"No long‐term trends in <i>p</i>CO<sub>2</sub> despite increasing organic carbon concentrations in boreal lakes, streams, and rivers","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Sveriges Lantbruksuniversitet; Vetenskapsrådet; Naturvårdsverket; Global Lake Ecological Observatory Network; Knut och Alice Wallenbergs Stiftelse; European Commission","keywords":"Surface runoff; Dissolved organic carbon; Environmental science; Surface water; STREAMS; Hydrology (agriculture); Groundwater; Total organic carbon; Environmental chemistry; Carbon dioxide; Soil water; Boreal; Ecology; Chemistry; Soil science; Geology; Environmental engineering; Biology","score_opus":0.007952975104684434,"score_gpt":0.21509846732630686,"score_spread":0.20714549222162243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2622869046","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99912566,0.00007951871,0.00007489872,0.000019232648,0.0000028194463,0.0000018168488,0.0003152909,0.000005807754,0.00037495786],"genre_scores_gemma":[0.9993179,0.00003228319,0.00006296021,0.000009765703,0.0000032825883,0.0000033063561,0.00044503834,0.0000014780031,0.00012401793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997929,0.000018588551,0.000024063678,0.00007200879,0.0000484466,0.00004402464],"domain_scores_gemma":[0.99909735,0.00011727542,0.00036471675,0.000065964916,0.00024772645,0.00010697354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000319322,0.00013608746,0.00021264229,0.00058697315,0.00041765088,0.0006148545,0.00021156679,0.00027826778,0.0005379815],"category_scores_gemma":[0.00059677113,0.00013818964,0.00019472883,0.0007834597,0.00041081037,0.00027938455,0.00029810792,0.0002028378,0.00013999458],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018025919,0.000028200398,0.98175967,0.000029184699,0.00009756301,0.00008733465,0.00023264976,0.00016812327,0.013608612,0.00005062999,0.00016366912,0.003594178],"study_design_scores_gemma":[9.2225224e-7,0.000027838412,0.9989974,0.0000017885453,0.000015327805,0.0000249378,0.00013520982,0.00011484995,0.00046588085,0.000008690616,0.00020532467,0.0000020018535],"about_ca_topic_score_codex":0.013630398,"about_ca_topic_score_gemma":0.028852943,"teacher_disagreement_score":0.013630398,"about_ca_system_score_codex":0.00042741076,"about_ca_system_score_gemma":0.00033372038,"threshold_uncertainty_score":0.027102113},"labels":[],"label_agreement":null},{"id":"W2626480532","doi":"10.1029/2017gb005842","title":"Global Spatial and Temporal Variation of Cd:P in Euphotic Zone Particulates","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Ocean Sciences; Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Photic zone; Particulates; Spatial variability; Variation (astronomy); Environmental science; Atmospheric sciences; Geology; Ecology; Biology; Phytoplankton; Mathematics","score_opus":0.010210574193916834,"score_gpt":0.23180677167398386,"score_spread":0.22159619748006704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2626480532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991696,0.000037478607,0.00008476808,0.0000083119285,0.0000011396093,0.0000012470063,0.0005354946,0.000007941416,0.00015399912],"genre_scores_gemma":[0.9989365,0.000030536026,0.00014897143,0.0000046530286,0.00000179209,0.0000031624743,0.0007733302,0.000002845756,0.000098297656],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994373,0.000005035837,0.0000035412722,0.000029369925,0.00000892115,0.000009381617],"domain_scores_gemma":[0.9998247,0.00003376882,0.00004854837,0.000016433423,0.00004864681,0.000027952861],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018733476,0.00016996231,0.00019543584,0.0006413629,0.00019005762,0.0003295923,0.00016065165,0.0002472074,0.0004438888],"category_scores_gemma":[0.00020331025,0.00015022667,0.00020308646,0.0005530432,0.00017314745,0.00021619417,0.00024350687,0.00013114305,0.00010728019],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000120609606,0.000022128888,0.9694232,0.000024343683,0.00011548591,0.00007768152,0.00023983521,0.00093193346,0.024617916,0.000036510686,0.00014235917,0.0042480095],"study_design_scores_gemma":[9.3806193e-7,0.0000057959255,0.99924695,7.728748e-7,0.0000049979826,0.000010025374,0.000028596807,0.00028378502,0.00032717953,0.000004711987,0.00008504924,0.0000012482094],"about_ca_topic_score_codex":0.017692143,"about_ca_topic_score_gemma":0.020400323,"teacher_disagreement_score":0.017692143,"about_ca_system_score_codex":0.00032707938,"about_ca_system_score_gemma":0.000113267844,"threshold_uncertainty_score":0.035178363},"labels":[],"label_agreement":null},{"id":"W2742814356","doi":"10.1002/2017gb005829","title":"Oxygen Saturation Surrounding Deep Water Formation Events in the Labrador Sea From Argo‐O<sub>2</sub> Data","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche; Equipex","keywords":"Argo; Oxygen; Thermohaline circulation; Convection; Oceanography; Geology; Sink (geography); Seawater; Deep convection; Atmospheric sciences; Chemistry; Meteorology; Geography","score_opus":0.0171419192189145,"score_gpt":0.22201249640392043,"score_spread":0.20487057718500593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2742814356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99770314,0.000032023814,0.00014934165,0.000010160529,0.0000024831602,0.0000028594852,0.0016394049,0.00003420328,0.0004263734],"genre_scores_gemma":[0.99652135,0.000026757387,0.00037003332,0.000009181709,0.0000035805392,0.0000060447105,0.0029041395,0.000010326858,0.00014856394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982256,0.000018465596,0.00002012286,0.00005931643,0.000029000747,0.000050529892],"domain_scores_gemma":[0.99954283,0.000049654336,0.00022353521,0.00005674328,0.00007826429,0.00004892785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031603413,0.00035434935,0.00024051787,0.0011121702,0.0002229833,0.0005852807,0.00028672913,0.0002586379,0.0005391987],"category_scores_gemma":[0.0005457228,0.000117957214,0.00031100787,0.0011693432,0.00023130987,0.00032030407,0.00046147604,0.00015593358,0.00020755097],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025558262,0.00003820423,0.97406965,0.00003913044,0.00008957722,0.00011684698,0.00019925134,0.0024896923,0.011404041,0.00004336313,0.00047065452,0.010784095],"study_design_scores_gemma":[0.0000060393786,0.000022766786,0.99409395,0.0000058676565,0.00001821032,0.000026753934,0.00013082715,0.0024897538,0.00259588,0.000012281854,0.0005902223,0.0000074161894],"about_ca_topic_score_codex":0.045257717,"about_ca_topic_score_gemma":0.07344327,"teacher_disagreement_score":0.9547423,"about_ca_system_score_codex":0.0006101551,"about_ca_system_score_gemma":0.0003186077,"threshold_uncertainty_score":0.08998859},"labels":[],"label_agreement":null},{"id":"W2744145998","doi":"10.1002/2017gb005624","title":"North Atlantic Deep Water formation inhibits high Arctic contamination by continental perfluorooctane sulfonate discharges","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Per- and polyfluoroalkyl substances research","field":"Environmental Science","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Toronto; Natural Sciences and Engineering Research Council of Canada; European Commission; National Science Foundation; Richard and Susan Smith Family Foundation; Joint Research Centre; Stockholms Universitet","keywords":"Arctic; Oceanography; Perfluorooctane; North Atlantic Deep Water; Environmental science; Seawater; Continental shelf; Thermohaline circulation; Ocean current; Geology; Chemistry; Sulfonate","score_opus":0.008378275951282599,"score_gpt":0.2374957820223574,"score_spread":0.2291175060710748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2744145998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99740916,0.000034228957,0.00047154876,0.000063003,0.00000717918,0.0000037455004,0.00028962726,0.000033668475,0.0016878864],"genre_scores_gemma":[0.99918526,0.000026770158,0.00021255556,0.000013907419,0.0000014576261,0.0000020908144,0.00026321204,0.0000071482086,0.0002876919],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999324,0.000011262774,0.000004082761,0.000021373355,0.00001261378,0.000018268598],"domain_scores_gemma":[0.9998938,0.000016020358,0.000035236673,0.00000777327,0.000027179962,0.0000199575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000098863544,0.00026686356,0.00016745528,0.00013317507,0.00034791898,0.0005907138,0.00016774643,0.00025939383,0.0010618768],"category_scores_gemma":[0.00037217725,0.00017053763,0.00043617678,0.00012492324,0.00016846824,0.00022284748,0.00038965623,0.00022933085,0.0001695562],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037439133,0.00014473742,0.6253093,0.00009450922,0.00019300816,0.0003124872,0.00022860122,0.18070552,0.17863345,0.0013535438,0.0016096496,0.011040822],"study_design_scores_gemma":[0.00010823166,0.00027035075,0.59277344,0.000029919007,0.00015930217,0.000060906386,0.0004680379,0.3747136,0.02546015,0.00071884,0.005199499,0.00003789627],"about_ca_topic_score_codex":0.1196488,"about_ca_topic_score_gemma":0.09254566,"teacher_disagreement_score":0.1196488,"about_ca_system_score_codex":0.0013614284,"about_ca_system_score_gemma":0.0011705394,"threshold_uncertainty_score":0.23790479},"labels":[],"label_agreement":null},{"id":"W2763353102","doi":"10.1002/2017gb005749","title":"Widespread Increases in Iron Concentration in European and North American Freshwaters","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":117,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Ministry of the Environment, Conservation and Parks","funders":"Centre for Ecology and Hydrology; National Science Foundation of Sri Lanka; Leibniz-Gemeinschaft; Natural Environment Research Council; Norges Miljø- og Biovitenskapelige Universitet; Latvijas Universitate; Svenska Forskningsrådet Formas; Grantová Agentura České Republiky; U.S. Geological Survey; European Commission; Knut och Alice Wallenbergs Stiftelse; Global Lake Ecological Observatory Network; Vetenskapsrådet; National Science Foundation","keywords":"Biogeochemical cycle; Biogeochemistry; Environmental science; Deposition (geology); Ecosystem; Total organic carbon; Environmental chemistry; Boreal; Physical geography; Ecology; Geography; Chemistry; Geology; Sediment; Biology","score_opus":0.007960514039940683,"score_gpt":0.22058965124349958,"score_spread":0.2126291372035589,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763353102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990031,0.00017398794,0.0000573921,0.000029222889,0.000001396059,0.000001558834,0.00012565269,0.000003952098,0.0006036805],"genre_scores_gemma":[0.99936277,0.00012864074,0.00012612986,0.000023449482,0.0000034052496,0.0000024815572,0.00015490213,0.000001167442,0.0001971003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997732,0.00003409042,0.000018837887,0.00008943261,0.00004340114,0.000041010415],"domain_scores_gemma":[0.9993498,0.00010044404,0.00027403378,0.000030555417,0.00017325504,0.00007194805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004463454,0.0001407503,0.00024111873,0.0015568978,0.00041913657,0.000542233,0.0001860937,0.00027197122,0.00063700177],"category_scores_gemma":[0.0006591386,0.00012482751,0.00011675222,0.0016475533,0.0005443655,0.0003694359,0.00053011475,0.00010570984,0.000060723338],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000095850664,0.000016536833,0.98496115,0.0000333604,0.00005079209,0.00011444875,0.000491799,0.0001232578,0.0064320723,0.000072176554,0.00010635483,0.007502162],"study_design_scores_gemma":[6.8048314e-7,0.0000077093955,0.99937326,0.0000023952778,0.0000044192784,0.000029971987,0.00015655106,0.000037483245,0.00014197576,0.0000151465065,0.00022897616,0.000001458116],"about_ca_topic_score_codex":0.021067895,"about_ca_topic_score_gemma":0.04998875,"teacher_disagreement_score":0.021067895,"about_ca_system_score_codex":0.0004265641,"about_ca_system_score_gemma":0.000292128,"threshold_uncertainty_score":0.041890502},"labels":[],"label_agreement":null},{"id":"W2776677364","doi":"10.1002/2017gb005667","title":"Estimating the Cross‐Shelf Export of Riverine Materials: Part 1. General Relationships From an Idealized Numerical Model","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Plume; Environmental science; Biogeochemical cycle; Scaling; Biological oceanography; Latitude; Forcing (mathematics); Geology; Oceanography; Atmospheric sciences; Meteorology; Mathematics; Geodesy; Physics","score_opus":0.0335620635207671,"score_gpt":0.2764068020285855,"score_spread":0.24284473850781838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2776677364","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90439653,0.0005864268,0.0880253,0.0004263045,0.000023207156,0.00009139886,0.0010977293,0.00024117557,0.005111877],"genre_scores_gemma":[0.98486507,0.00023067302,0.013678296,0.000052815605,0.000012787827,0.000073316645,0.00045593746,0.000037761736,0.00059329683],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998055,0.000070387294,0.000021485039,0.000050009985,0.000029385335,0.000023167368],"domain_scores_gemma":[0.9983941,0.0009639618,0.00026386432,0.00014425104,0.0001697357,0.00006413077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00078925426,0.00087282155,0.0006320384,0.00069790205,0.00038657698,0.0011663457,0.0008393247,0.0012942578,0.0009935285],"category_scores_gemma":[0.00437739,0.00050022,0.00075381965,0.000598741,0.00087327574,0.0011234933,0.00085869076,0.0007776186,0.00014685917],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012330041,0.000020384245,0.0036120967,0.000021313992,0.00001171174,0.000036161568,0.000013121681,0.9933036,0.0010704937,0.0009700118,0.000056692665,0.0008720953],"study_design_scores_gemma":[0.0000049117643,0.000008410066,0.0005509797,0.00000351032,0.0000027494518,0.00000630294,0.000005011225,0.9988312,0.00017756438,0.0003538063,0.00005062215,0.000004944654],"about_ca_topic_score_codex":0.01969273,"about_ca_topic_score_gemma":0.0064781765,"teacher_disagreement_score":0.01969273,"about_ca_system_score_codex":0.00095013913,"about_ca_system_score_gemma":0.0006302014,"threshold_uncertainty_score":0.0391562},"labels":[],"label_agreement":null},{"id":"W2789756224","doi":"10.1002/2017gb005668","title":"Estimating the Cross‐Shelf Export of Riverine Materials: Part 2. Estimates of Global Freshwater and Nutrient Export","year":2017,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Environmental science; Nutrient; Biogeochemical cycle; Plume; Pelagic zone; Oceanography; Dissolved organic carbon; Eutrophication; Biogeochemistry; Dissolved silica; Hypoxia (environmental); Hydrology (agriculture); Environmental chemistry; Geology; Ecology; Chemistry; Biology; Geography","score_opus":0.013781509941824106,"score_gpt":0.24723267891228914,"score_spread":0.23345116897046503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789756224","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97177786,0.0010123857,0.01848291,0.0001628474,0.000008842817,0.000038820817,0.005845554,0.00017461264,0.0024962707],"genre_scores_gemma":[0.9776513,0.00084255444,0.014698574,0.000050801198,0.000015431586,0.000062611216,0.00579561,0.00008229853,0.0008008023],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998692,0.000020002835,0.000016102002,0.000048608024,0.000031394775,0.00001470069],"domain_scores_gemma":[0.9996014,0.00012702076,0.00010328477,0.00006429528,0.00008315327,0.000020764499],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070984423,0.0010485887,0.0003877834,0.001548817,0.00019022134,0.0011259875,0.00030331066,0.0004497249,0.0012487676],"category_scores_gemma":[0.0015264861,0.00031450304,0.00064917613,0.0017490266,0.00032700735,0.0012179902,0.0010828973,0.00029158875,0.00032872686],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007103972,0.000068608584,0.6670041,0.00025291674,0.000690799,0.00016304152,0.00016887236,0.23969142,0.013598277,0.0017527579,0.0010910038,0.07544713],"study_design_scores_gemma":[0.00003188431,0.000059349648,0.74417305,0.00008885382,0.00023187738,0.00010120827,0.000269287,0.23342,0.013123607,0.002586487,0.0058353767,0.000078906894],"about_ca_topic_score_codex":0.02071453,"about_ca_topic_score_gemma":0.01747765,"teacher_disagreement_score":0.02071453,"about_ca_system_score_codex":0.00062282325,"about_ca_system_score_gemma":0.0004697223,"threshold_uncertainty_score":0.041187882},"labels":[],"label_agreement":null},{"id":"W2791262758","doi":"10.1002/2017gb005792","title":"Refined Estimates of Net Community Production in the Subarctic Northeast Pacific Derived From ΔO<sub>2</sub>/Ar Measurements With N<sub>2</sub>O‐Based Corrections for Vertical Mixing","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Canadian Institute for Advanced Research; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Subarctic climate; Mixed layer; Hydrography; Upwelling; Environmental science; Thermocline; Vertical mixing; Mixing (physics); Atmospheric sciences; Flux (metallurgy); Oceanography; Geology; Physics; Chemistry","score_opus":0.02457442629379014,"score_gpt":0.22286299376141394,"score_spread":0.1982885674676238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791262758","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99658173,0.00010538654,0.0025859962,0.000010526515,0.000003145442,0.000009956661,0.00025826442,0.000022038143,0.00042307583],"genre_scores_gemma":[0.99319565,0.00008640412,0.0062066996,0.000012870057,0.0000041880176,0.000013944373,0.00034216637,0.000010333229,0.00012769751],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984133,0.000042642678,0.000011106729,0.0000497324,0.00004111099,0.000014049356],"domain_scores_gemma":[0.9994611,0.00012298644,0.00015784724,0.000061019073,0.00016054658,0.00003656258],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069964345,0.0004919814,0.00020922894,0.0006629514,0.00021354419,0.00038696616,0.00028197627,0.00017178747,0.00032863911],"category_scores_gemma":[0.0010669886,0.00024192147,0.00017112159,0.0004162425,0.0002462521,0.00039779991,0.00038931132,0.00023279757,0.00008993532],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020875073,0.000045778103,0.8920411,0.00007371416,0.00017598165,0.00008169014,0.00028537738,0.008760297,0.07764679,0.000076082026,0.00013750712,0.02046687],"study_design_scores_gemma":[0.000005293041,0.000025017522,0.9869528,0.000007253258,0.000030061452,0.00001705419,0.00009503377,0.008685158,0.003876934,0.000042355536,0.0002544747,0.000008453087],"about_ca_topic_score_codex":0.031851817,"about_ca_topic_score_gemma":0.07597836,"teacher_disagreement_score":0.031851817,"about_ca_system_score_codex":0.00043064126,"about_ca_system_score_gemma":0.00033611976,"threshold_uncertainty_score":0.063332856},"labels":[],"label_agreement":null},{"id":"W2791502245","doi":"10.1002/2017gb005783","title":"Carbon: Chlorophyll Ratios and Net Primary Productivity of Subarctic Pacific Surface Waters Derived From Autonomous Shipboard Sensors","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Institute for Advanced Research; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Phytoplankton; Subarctic climate; Oceanography; Environmental science; Hydrography; Upwelling; Productivity; Nutrient; Chlorophyll a; Primary production; Biology; Geology; Ecology; Ecosystem; Botany","score_opus":0.007856946104365808,"score_gpt":0.18610816528792073,"score_spread":0.17825121918355494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791502245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987099,0.00003737669,0.00017222123,0.000005971504,0.0000015398816,0.0000026584019,0.00071984425,0.000012004654,0.0003385187],"genre_scores_gemma":[0.99786574,0.00006308337,0.00061954063,0.000010360166,0.000002837313,0.000006876859,0.0012937777,0.0000042949005,0.00013353197],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999337,0.000008004821,0.00000630941,0.00002183867,0.00002006718,0.000010134677],"domain_scores_gemma":[0.9996933,0.000065306434,0.000095580785,0.000018244435,0.0000930235,0.0000345812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002396903,0.0003982482,0.00015058105,0.00076984335,0.00022782163,0.00046336136,0.00017332006,0.00016623823,0.0005591252],"category_scores_gemma":[0.00064044,0.00019313913,0.0002165841,0.0008147633,0.00015884919,0.00028012175,0.0002986857,0.00016993088,0.00014083527],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003358191,0.0000135704,0.9927785,0.000014650659,0.000045777353,0.000029890765,0.000068399764,0.00086963037,0.0023368704,0.000012758393,0.00009544333,0.0037010151],"study_design_scores_gemma":[0.0000016702388,0.000006159206,0.9981723,0.0000027494543,0.000008639081,0.000012983758,0.000057947662,0.0012686462,0.0003849256,0.000006189519,0.000075973716,0.0000018027168],"about_ca_topic_score_codex":0.06821977,"about_ca_topic_score_gemma":0.11225539,"teacher_disagreement_score":0.06821977,"about_ca_system_score_codex":0.00050541584,"about_ca_system_score_gemma":0.00030048084,"threshold_uncertainty_score":0.13564539},"labels":[],"label_agreement":null},{"id":"W2792164768","doi":"10.1002/2017gb005824","title":"Present and Future Mercury Concentrations in Chinese Rice: Insights From Modeling","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Mercury (programming language); Methylmercury; Environmental chemistry; Biogeochemical cycle; Environmental science; Paddy field; Rice plant; Chemistry; Agronomy; Bioaccumulation","score_opus":0.01148905288334764,"score_gpt":0.2658457383213984,"score_spread":0.2543566854380508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792164768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98120224,0.00015934867,0.0086539555,0.00041572552,0.000009785606,0.000016499554,0.0007864002,0.00010780199,0.008648226],"genre_scores_gemma":[0.99772316,0.00011835785,0.0010376914,0.000022466918,0.0000039287897,0.000011995161,0.00018687709,0.000010585259,0.0008848964],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999044,0.000023523176,0.0000047291196,0.000029274981,0.000015491863,0.000022519385],"domain_scores_gemma":[0.9998466,0.000065858934,0.000026967147,0.000014368604,0.000030882537,0.000015409983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029268558,0.0005355,0.00029183546,0.00039413388,0.00038917156,0.0007140182,0.0008792718,0.0005397718,0.001026368],"category_scores_gemma":[0.00065221643,0.0002857802,0.0006833594,0.00061099924,0.0004542226,0.00065620773,0.00056082645,0.00029835672,0.00007418567],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001863569,0.000012545152,0.012818357,0.000021792732,0.000029022232,0.00010009448,0.000048715254,0.98140717,0.0009300937,0.0027917516,0.00021715484,0.0016047063],"study_design_scores_gemma":[0.000009610993,0.000011419259,0.003182349,0.000002939106,0.000023854362,0.000010546243,0.00004242911,0.99504256,0.00031593262,0.0009791557,0.00036987095,0.000009329438],"about_ca_topic_score_codex":0.22759223,"about_ca_topic_score_gemma":0.096342996,"teacher_disagreement_score":0.22759223,"about_ca_system_score_codex":0.0026918922,"about_ca_system_score_gemma":0.0022490069,"threshold_uncertainty_score":0.45253497},"labels":[],"label_agreement":null},{"id":"W2792601296","doi":"10.1002/2017gb005759","title":"Nitrous Oxide Emissions Estimated With the CarbonTracker‐Lagrange North American Regional Inversion Framework","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Climate Program Office; National Oceanic and Atmospheric Administration","keywords":"Nitrous oxide; Fertilizer; Inversion (geology); Environmental science; Greenhouse gas; Precipitation; Nitrogen; Atmospheric sciences; Yield (engineering); Agronomy; Climatology; Meteorology; Geography; Geology; Chemistry; Oceanography","score_opus":0.007894035717554617,"score_gpt":0.21978327141549076,"score_spread":0.21188923569793613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792601296","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9610117,0.00015838162,0.027456168,0.00020266863,0.000018056595,0.000034945388,0.0054092873,0.00047802165,0.0052307127],"genre_scores_gemma":[0.9754608,0.000074492615,0.018088019,0.000041379968,0.000010886861,0.000047220965,0.00561333,0.000045136232,0.00061862706],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997613,0.00006777591,0.000010136622,0.000075505806,0.000043671662,0.000041690393],"domain_scores_gemma":[0.9997358,0.000050092694,0.000037234644,0.000031777636,0.00012298985,0.000022114195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010401306,0.00039311903,0.00031711187,0.0006464577,0.00037036574,0.00048731887,0.00068231527,0.0003596473,0.0008645983],"category_scores_gemma":[0.0011489366,0.00025679506,0.0007097147,0.00076691114,0.00024343007,0.00056803017,0.0005045044,0.00037148938,0.00018146931],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000267746,0.00014032253,0.16823588,0.00005889025,0.00040045445,0.00012671996,0.000090530804,0.78639466,0.005792452,0.0027778258,0.004392739,0.031321786],"study_design_scores_gemma":[0.000056766545,0.00002341303,0.048647687,0.000009706842,0.0000624388,0.000015358271,0.000044927194,0.94712985,0.0013191941,0.0007445202,0.0019124091,0.000033605364],"about_ca_topic_score_codex":0.2359147,"about_ca_topic_score_gemma":0.19090532,"teacher_disagreement_score":0.7640853,"about_ca_system_score_codex":0.00087379804,"about_ca_system_score_gemma":0.002070948,"threshold_uncertainty_score":0.46908307},"labels":[],"label_agreement":null},{"id":"W2792769926","doi":"10.1002/2017gb005722","title":"Recent Synchronous Declines in DIN:TP in Swedish Lakes","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Aquatic Ecosystems and Phytoplankton Dynamics","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Vetenskapsrådet; Carl Tryggers Stiftelse för Vetenskaplig Forskning","keywords":"Subarctic climate; Environmental science; Nutrient; Climate change; Precipitation; Deposition (geology); Ecosystem; Boreal; Physical geography; Period (music); STREAMS; Ecology; Geography; Biology; Sediment","score_opus":0.009425023798559716,"score_gpt":0.2465815425957255,"score_spread":0.2371565187971658,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792769926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99890566,0.00030867793,0.000091691036,0.000019575635,0.000004011061,0.0000012526297,0.00026845964,0.0000063186676,0.00039442896],"genre_scores_gemma":[0.9989994,0.00018868319,0.00017079627,0.000014547313,0.0000068530844,0.0000036591216,0.00045429694,0.0000028260429,0.00015892295],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998116,0.000024579225,0.000027957534,0.000070337395,0.000040282233,0.000025208099],"domain_scores_gemma":[0.9993824,0.000076664095,0.00030195108,0.000024951409,0.00016685663,0.000047060665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042407413,0.00021645735,0.00024847992,0.0008473251,0.00032987836,0.00070214027,0.00018658124,0.00020294923,0.00039824913],"category_scores_gemma":[0.00067614176,0.00014877661,0.00016756037,0.0012475129,0.00027264337,0.0003709785,0.0005406144,0.00017594107,0.000082319166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010408519,0.000012744219,0.98904246,0.000048351194,0.000075633376,0.00013260634,0.000443981,0.0002467295,0.002800694,0.000034202723,0.00016551687,0.0068929465],"study_design_scores_gemma":[0.0000012372216,0.000011788027,0.9988894,0.0000063069633,0.000014068089,0.000059800583,0.00019966175,0.00012851873,0.0002949543,0.000021725627,0.00037060148,0.0000018847771],"about_ca_topic_score_codex":0.012832359,"about_ca_topic_score_gemma":0.026141254,"teacher_disagreement_score":0.012832359,"about_ca_system_score_codex":0.0004965104,"about_ca_system_score_gemma":0.00031604286,"threshold_uncertainty_score":0.025515378},"labels":[],"label_agreement":null},{"id":"W2793069893","doi":"10.1002/2017gb005698","title":"Photochemical Mineralization of Terrigenous DOC to Dissolved Inorganic Carbon in Ocean","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University; Louisiana-Pacific (Canada)","funders":"Academy of Finland","keywords":"Dissolved organic carbon; Terrigenous sediment; Seawater; Photobleaching; Irradiance; Environmental science; Colored dissolved organic matter; Oceanography; Environmental chemistry; Total inorganic carbon; Flux (metallurgy); Chemistry; Geology; Phytoplankton; Carbon dioxide; Nutrient; Physics; Geomorphology; Sediment","score_opus":0.007489011171414683,"score_gpt":0.2126789181466332,"score_spread":0.20518990697521852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2793069893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983253,0.00027696154,0.00039779823,0.000015786594,0.0000025291333,0.000003922521,0.00012724791,0.0000054270927,0.0008451233],"genre_scores_gemma":[0.9974974,0.00035144566,0.00072880037,0.000022697495,0.0000021133535,0.000013021626,0.00028625922,0.0000071410964,0.0010910815],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999312,0.0000057171023,0.000003344713,0.00003489025,0.000014064467,0.000010748897],"domain_scores_gemma":[0.99993575,0.000015778396,0.000014840591,0.0000055615715,0.000019332554,0.000008762674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000112458314,0.00023149852,0.00015640384,0.00018693347,0.00020696879,0.00034591393,0.00012596908,0.00018144751,0.00062791054],"category_scores_gemma":[0.00017804097,0.00017174293,0.00019738497,0.00016696563,0.00018238522,0.00017860699,0.00023527755,0.0002564606,0.00018764475],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013007635,0.000020110887,0.08367413,0.00013038189,0.000035487385,0.00010538959,0.00011080742,0.001081721,0.90386236,0.00012410931,0.000059376474,0.0106661245],"study_design_scores_gemma":[0.000014512458,0.00019421674,0.6568637,0.000018171235,0.00004287214,0.00017687886,0.00041322867,0.004720282,0.33481008,0.00013902897,0.0025944992,0.0000125032675],"about_ca_topic_score_codex":0.006026374,"about_ca_topic_score_gemma":0.010107834,"teacher_disagreement_score":0.006026374,"about_ca_system_score_codex":0.00082892267,"about_ca_system_score_gemma":0.0003015599,"threshold_uncertainty_score":0.01198262},"labels":[],"label_agreement":null},{"id":"W2801024111","doi":"10.1029/2017gb005738","title":"Rapid Changes in Anthropogenic Carbon Storage and Ocean Acidification in the Intermediate Layers of the Eurasian Arctic Ocean: 1996–2015","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Svenska Forskningsrådet Formas; Royal Swedish Academy of Sciences","keywords":"Structural basin; Oceanography; Arctic; Ocean acidification; Carbonate; Carbon fibers; Geology; Total inorganic carbon; TRACER; Boundary current; Canada Basin; Environmental science; Ocean current; Carbon dioxide; Climate change; Geomorphology; Ecology; Chemistry","score_opus":0.010590784937218309,"score_gpt":0.22813983250657813,"score_spread":0.21754904756935983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801024111","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899656,0.000092366245,0.00017534086,0.000018236173,0.0000033486272,0.0000012772155,0.00047765631,0.000011412285,0.00022393375],"genre_scores_gemma":[0.99852365,0.00006343358,0.00023552123,0.000004379029,0.0000025058387,0.0000026419646,0.0010091305,0.0000041341764,0.0001545862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980956,0.00002461516,0.0000274686,0.00007907453,0.000029168763,0.000030164818],"domain_scores_gemma":[0.9995937,0.000061914114,0.0001870711,0.000035507528,0.00008111461,0.00004072849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00086713,0.00035704466,0.00021097194,0.00054568995,0.0001973289,0.0006159481,0.00031506483,0.00024236104,0.0005365704],"category_scores_gemma":[0.0010158157,0.00020906661,0.00070912443,0.0008198239,0.00024914724,0.00048307533,0.00061997486,0.00022789442,0.00010959257],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028783103,0.000025810325,0.97694814,0.000053433836,0.00033561216,0.00012879711,0.00015872016,0.011252509,0.0038721138,0.0001621615,0.00016166073,0.006613214],"study_design_scores_gemma":[0.0000050436993,0.000020852209,0.9920257,0.0000103020375,0.000039068855,0.00004359427,0.00009787304,0.006417459,0.0009234894,0.000042697582,0.00036649103,0.000007446935],"about_ca_topic_score_codex":0.052431315,"about_ca_topic_score_gemma":0.05222615,"teacher_disagreement_score":0.052431315,"about_ca_system_score_codex":0.00082256773,"about_ca_system_score_gemma":0.00048493274,"threshold_uncertainty_score":0.10425228},"labels":[],"label_agreement":null},{"id":"W2809101536","doi":"10.1029/2017gb005874","title":"Accurate Estimation of Net Community Production From O<sub>2</sub>/Ar Measurements","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; Fisheries and Oceans Canada; Canadian Hydrographic Service","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Upwelling; Atmosphere (unit); Flux (metallurgy); Mixed layer; Environmental science; Atmospheric sciences; Sea surface temperature; Meteorology; Climatology; Chemistry; Oceanography; Geology; Physics","score_opus":0.02827378945943166,"score_gpt":0.2363040855421508,"score_spread":0.20803029608271914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2809101536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8754151,0.0001383685,0.12082927,0.000089570305,0.000015243521,0.000032320277,0.0009009273,0.000486231,0.0020930194],"genre_scores_gemma":[0.9571955,0.00011218273,0.041587643,0.00002357518,0.000008032763,0.00004028784,0.00052464637,0.00005662067,0.00045146822],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99984074,0.000039749902,0.0000071896507,0.000058687692,0.000038968432,0.000014723898],"domain_scores_gemma":[0.9994854,0.00023176864,0.000100187666,0.00006524075,0.000082206,0.00003517592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004780762,0.0004690013,0.0003052005,0.0002506356,0.00019825886,0.00044483575,0.00047541337,0.00046520113,0.0005797236],"category_scores_gemma":[0.0019180037,0.0003254287,0.00037673736,0.0002442845,0.00021335352,0.00073605316,0.00044699703,0.00028454588,0.0001962659],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021333878,0.00009362619,0.10401802,0.00013225147,0.00011834985,0.00009431426,0.00008032397,0.750741,0.119727544,0.0014911944,0.0004423497,0.022847695],"study_design_scores_gemma":[0.0000105538875,0.000033370892,0.022580713,0.000004734737,0.000011224274,0.000014771698,0.000018198634,0.9694862,0.007138527,0.00045336504,0.00023025455,0.000018115396],"about_ca_topic_score_codex":0.01594585,"about_ca_topic_score_gemma":0.013012827,"teacher_disagreement_score":0.01594585,"about_ca_system_score_codex":0.00056934624,"about_ca_system_score_gemma":0.00059552514,"threshold_uncertainty_score":0.031706095},"labels":[],"label_agreement":null},{"id":"W2890187819","doi":"10.1029/2018gb005941","title":"Blue Carbon Storage Capacity of Temperate Eelgrass (<scp><i>Zostera marina</i></scp>) Meadows","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":225,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Université du Québec à Chicoutimi; University of Victoria","funders":"Åbo Akademi; Syddansk Universitet; Maj ja Tor Nesslingin Säätiö; Center for Hierarchical Manufacturing, National Science Foundation; National Science Foundation","keywords":"Zostera marina; Temperate climate; Environmental science; Seagrass; Blue carbon; Carbon fibers; Zostera; Ecology; Chemistry; Oceanography; Botany; Biology; Ecosystem; Geology; Materials science","score_opus":0.008325723279343363,"score_gpt":0.2072725410406108,"score_spread":0.19894681776126744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890187819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997516,0.00002037983,0.000025764435,0.0000013971504,1.682766e-7,6.107005e-7,0.00010566249,0.0000017915318,0.00009260432],"genre_scores_gemma":[0.99966586,0.000018263607,0.00006407886,0.0000023198147,4.762422e-7,0.0000017071195,0.00017653049,0.0000013260491,0.000069441754],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999366,0.000007638843,0.00000591389,0.000023126477,0.000011348656,0.000015401529],"domain_scores_gemma":[0.9997787,0.000027553282,0.00008701399,0.000017198276,0.000049928534,0.00003965104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001467686,0.00019337775,0.0001637046,0.000941612,0.0002297114,0.00042518118,0.00014754933,0.00010487277,0.0006234073],"category_scores_gemma":[0.00021751809,0.00012833464,0.00015448294,0.0004919124,0.00022440609,0.00019475537,0.00024402914,0.00008176815,0.00011894189],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008987789,0.000009372057,0.971068,0.000018848361,0.000077668454,0.00004073312,0.00024392304,0.00017579625,0.025238885,0.000019710817,0.00004174229,0.0029754105],"study_design_scores_gemma":[7.0656654e-7,0.000008971993,0.9994691,0.0000010292882,0.000004930083,0.000015159246,0.00006834499,0.00008527138,0.00029762948,0.0000031422326,0.00004463554,0.0000010160916],"about_ca_topic_score_codex":0.028871315,"about_ca_topic_score_gemma":0.06365959,"teacher_disagreement_score":0.028871315,"about_ca_system_score_codex":0.00038152133,"about_ca_system_score_gemma":0.00015379216,"threshold_uncertainty_score":0.057406545},"labels":[],"label_agreement":null},{"id":"W2892013549","doi":"10.1029/2018gb005919","title":"Behind the Scenes: Mechanisms Regulating Climatic Patterns of Dissolved Organic Carbon Uptake in Headwater Streams","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Agència de Gestió d'Ajuts Universitaris i de Recerca; Eusko Jaurlaritza","keywords":"STREAMS; Dissolved organic carbon; Environmental science; Total organic carbon; Carbon fibers; Carbon cycle; Hydrology (agriculture); Earth science; Physical geography; Geology; Environmental chemistry; Oceanography; Ecology; Ecosystem; Chemistry; Geography; Biology","score_opus":0.009985326734463465,"score_gpt":0.2111776796979146,"score_spread":0.20119235296345112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2892013549","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99914086,0.0001100501,0.00023059739,0.000013872586,0.0000017563095,0.000004197462,0.00023537505,0.0000073434385,0.00025591516],"genre_scores_gemma":[0.9994697,0.000064025604,0.0001601962,0.000009509101,0.0000033034166,0.0000038940693,0.00019839307,0.0000034762795,0.00008745032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998871,0.00002836895,0.000011076096,0.000039506922,0.000014118002,0.000019822955],"domain_scores_gemma":[0.9997305,0.000069616,0.00009532918,0.000014754238,0.000054903452,0.000034761535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032639722,0.000157664,0.00021741295,0.00055111095,0.0002133112,0.0008072885,0.00018178952,0.00023304207,0.00064172974],"category_scores_gemma":[0.00044355277,0.00015912358,0.00021643384,0.00049401994,0.0002498354,0.0004088807,0.00031132618,0.00011492483,0.00008731729],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031837853,0.000053642358,0.9177894,0.00006414935,0.00015279392,0.00008169473,0.00025641985,0.0013502694,0.07235864,0.0001510563,0.000119065386,0.0073044216],"study_design_scores_gemma":[0.000003061458,0.000016111126,0.9981153,0.000002491824,0.000011690305,0.000011513302,0.0000872088,0.000859667,0.0007563321,0.000037617472,0.000096011136,0.0000029083378],"about_ca_topic_score_codex":0.007019709,"about_ca_topic_score_gemma":0.008237867,"teacher_disagreement_score":0.007019709,"about_ca_system_score_codex":0.00031282302,"about_ca_system_score_gemma":0.0002450695,"threshold_uncertainty_score":0.013957679},"labels":[],"label_agreement":null},{"id":"W2893738650","doi":"10.1029/2018gb005949","title":"Effect of Dung Quantity and Quality on Greenhouse Gas Fluxes From Tropical Pastures in Kenya","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Agriculture and Agri-Food Canada","funders":"China Scholarship Council","keywords":"Temperate climate; Environmental science; Greenhouse gas; Nitrous oxide; Rangeland; Methane; Carbon dioxide; Animal science; Tropics; Agronomy; Ecology; Agroforestry; Biology","score_opus":0.014084378268340822,"score_gpt":0.26365047544790954,"score_spread":0.2495660971795687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2893738650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999635,0.000062841296,0.000022972463,0.000004680641,7.953504e-7,0.0000037176123,0.00013363152,8.92518e-7,0.00013547353],"genre_scores_gemma":[0.9992867,0.00010085263,0.00017808484,0.000012321143,0.0000016871331,0.000007831071,0.00025931955,0.0000023288167,0.00015093568],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998056,0.000034689503,0.000018040771,0.000060553248,0.000037927926,0.00004328623],"domain_scores_gemma":[0.9994247,0.00013714044,0.00022151452,0.000034477216,0.00009945753,0.000082706],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025517715,0.00039628363,0.00035466332,0.00048220117,0.0007377066,0.00063655816,0.0003137292,0.00023635881,0.00075269263],"category_scores_gemma":[0.00067174947,0.0002672004,0.0002471386,0.0006177182,0.00041619583,0.00043397228,0.00035114374,0.00018874166,0.00007460274],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00150279,0.000127987,0.8579361,0.00022876369,0.0002103707,0.00060391857,0.00060657604,0.00097193284,0.12980433,0.000048178008,0.000104753446,0.007854396],"study_design_scores_gemma":[0.000003901496,0.00006906234,0.99777347,0.0000045449924,0.000017048314,0.000041093277,0.00017287146,0.00016036234,0.0016109236,0.0000046552727,0.00013884214,0.0000032249668],"about_ca_topic_score_codex":0.042481218,"about_ca_topic_score_gemma":0.13580763,"teacher_disagreement_score":0.042481218,"about_ca_system_score_codex":0.0014433126,"about_ca_system_score_gemma":0.00033099798,"threshold_uncertainty_score":0.08446789},"labels":[],"label_agreement":null},{"id":"W2897111448","doi":"10.1029/2018gb005948","title":"Isotopic Constraints on Nitrogen Transformation Rates in the Deep Sedimentary Marine Biosphere","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Anoxic waters; Nitrate; Isotopes of nitrogen; Nitrite; Denitrification; Environmental chemistry; Nitrogen cycle; Nitrogen; Cycling; Stable isotope ratio; Sedimentary rock; Chemistry; Oceanography; Environmental science; Geology; Geochemistry","score_opus":0.008233810988009243,"score_gpt":0.21505924572753066,"score_spread":0.20682543473952142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897111448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991173,0.00007484676,0.00024696876,0.00001600314,9.0199285e-7,9.724317e-7,0.000105083804,0.0000060096827,0.00043187675],"genre_scores_gemma":[0.9996623,0.000046940833,0.00013393615,0.0000058745836,7.31669e-7,0.0000014060852,0.00009874505,0.0000023812754,0.00004762728],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990726,0.000012020284,0.00000654167,0.000034926637,0.00002071086,0.000018445124],"domain_scores_gemma":[0.9997156,0.00011732718,0.000056036188,0.000029160377,0.000049249757,0.000032595093],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003620669,0.00031897725,0.00025004012,0.00048339294,0.0002969667,0.00043775505,0.00028513055,0.0003446639,0.00051393296],"category_scores_gemma":[0.0007471008,0.0002890319,0.00016935632,0.00028367748,0.00034018,0.0003949431,0.0005218919,0.00018558107,0.00009721519],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032773212,0.00004613056,0.7148332,0.000079752914,0.00011803928,0.000106360196,0.00026334848,0.01246275,0.26272693,0.001055228,0.00008906428,0.007891515],"study_design_scores_gemma":[0.000020610554,0.00007079689,0.96262014,0.00001363179,0.00004166171,0.000047555444,0.00019993333,0.023706023,0.011421964,0.0011026675,0.00073749106,0.0000174914],"about_ca_topic_score_codex":0.015353212,"about_ca_topic_score_gemma":0.024294779,"teacher_disagreement_score":0.015353212,"about_ca_system_score_codex":0.00057832757,"about_ca_system_score_gemma":0.00026983034,"threshold_uncertainty_score":0.030527651},"labels":[],"label_agreement":null},{"id":"W2900238917","doi":"10.1029/2017gb005848","title":"Eutrophication Leads to Accumulation of Recalcitrant Autochthonous Organic Matter in Coastal Environment","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"Naturvidenskab og Teknologi, Aarhus Universitet; Ciência sem Fronteiras; Erzincan Üniversitesi; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Aarhus Universitet","keywords":"Eutrophication; Organic matter; Environmental science; Environmental chemistry; Oceanography; Ecology; Nutrient; Geology; Chemistry; Biology","score_opus":0.018586541601750325,"score_gpt":0.24344893870419998,"score_spread":0.22486239710244965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900238917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99977297,0.000026747768,0.000045234825,0.0000022677175,4.5974568e-7,7.0989825e-7,0.000040959007,0.0000029292034,0.000107745815],"genre_scores_gemma":[0.9991013,0.000057879148,0.00015972169,0.0000074090103,5.6648474e-7,0.0000028455308,0.00013108097,0.0000033454571,0.0005358092],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999461,0.0000057961324,0.000005671912,0.000017165203,0.000010787434,0.000014472041],"domain_scores_gemma":[0.99986327,0.000016771332,0.000057884085,0.000011080185,0.000020983447,0.000029921008],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000083955274,0.00019325112,0.00013643334,0.00020594319,0.00017737657,0.00030423424,0.000084744504,0.00015631334,0.00038292437],"category_scores_gemma":[0.00009601969,0.00019435487,0.00014026756,0.00015099514,0.00015102379,0.00010825086,0.0002755501,0.00015160901,0.00012689497],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010457982,0.000017189554,0.025215223,0.000021758744,0.000010159522,0.00015668359,0.00007685961,0.00014198502,0.9734591,0.00001983493,0.000023726425,0.0007528149],"study_design_scores_gemma":[0.000006264399,0.00019845524,0.8623723,0.00000728535,0.000019416691,0.00026253436,0.00034221107,0.0009534817,0.13506153,0.000051339637,0.00071701995,0.000008175383],"about_ca_topic_score_codex":0.0031547453,"about_ca_topic_score_gemma":0.0059479815,"teacher_disagreement_score":0.0031547453,"about_ca_system_score_codex":0.000270283,"about_ca_system_score_gemma":0.00014891032,"threshold_uncertainty_score":0.006272793},"labels":[],"label_agreement":null},{"id":"W2903896275","doi":"10.1029/2018gb005985","title":"Insights From the<sup>238</sup>U‐<sup>234</sup>Th Method Into the Coupling of Biological Export and the Cycling of Cadmium, Cobalt, and Manganese in the Southeast Pacific Ocean","year":2018,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Geotraces; Particulates; Manganese; Cadmium; Biogeochemical cycle; Sediment trap; Environmental science; Environmental chemistry; Cobalt; Flux (metallurgy); Phosphorus; Cycling; Oceanography; Seawater; Chemistry; Geology; Total organic carbon; Inorganic chemistry","score_opus":0.014432892410047271,"score_gpt":0.2320544312153064,"score_spread":0.2176215388052591,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903896275","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8441457,0.0011803501,0.13820657,0.00048249643,0.00006751651,0.000054497974,0.001345572,0.00046245675,0.014054657],"genre_scores_gemma":[0.9240058,0.0007750843,0.06980427,0.0000678589,0.000013997334,0.000058946378,0.00055712555,0.00021287535,0.0045040883],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99989474,0.000026472317,0.000008031171,0.00002284628,0.000039114035,0.000008843645],"domain_scores_gemma":[0.99974805,0.0001154364,0.000040087758,0.000034018147,0.000057516787,0.000004904631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060434174,0.00023764932,0.00013318688,0.0004688701,0.00016007302,0.0005214069,0.00022567225,0.0001762218,0.0012101174],"category_scores_gemma":[0.0008025794,0.00015656768,0.00015939055,0.00046270565,0.00034687197,0.00024624998,0.00021461479,0.0002511516,0.00021214127],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042142053,0.00004964179,0.09651626,0.0003186282,0.0001258644,0.0004307889,0.00019256493,0.014263262,0.7737197,0.005350592,0.00075455155,0.10785673],"study_design_scores_gemma":[0.00003184078,0.0001600903,0.09506806,0.000050937157,0.00013332604,0.00053810905,0.0004691479,0.09707293,0.7803073,0.002821838,0.023309147,0.000037235797],"about_ca_topic_score_codex":0.011335574,"about_ca_topic_score_gemma":0.026498137,"teacher_disagreement_score":0.011335574,"about_ca_system_score_codex":0.0004428979,"about_ca_system_score_gemma":0.0004898284,"threshold_uncertainty_score":0.022539198},"labels":[],"label_agreement":null},{"id":"W2908842421","doi":"10.1029/2018gb006106","title":"Large‐Scale Landscape Drivers of CO<sub>2</sub>, CH<sub>4</sub>, DOC, and DIC in Boreal River Networks","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; University of Alberta","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Boreal; Biome; Fluvial; Environmental science; Dissolved organic carbon; Taiga; STREAMS; Climate change; Scale (ratio); Hydrology (agriculture); Ecosystem; Physical geography; Ecology; Geology; Geography; Geomorphology; Oceanography; Structural basin; Cartography; Biology","score_opus":0.0025768110692731333,"score_gpt":0.1840894314266914,"score_spread":0.18151262035741828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908842421","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991217,0.00004623212,0.00020969556,0.00005191918,7.4279774e-7,0.000004447938,0.00022683854,0.0000098467,0.00032855265],"genre_scores_gemma":[0.99961096,0.00003127638,0.000102067934,0.000008681154,5.437236e-7,0.0000021782655,0.00010846151,0.0000017670843,0.00013411703],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999099,0.0000177965,0.000003521421,0.000032606153,0.000008463311,0.000027613802],"domain_scores_gemma":[0.99976367,0.00006127012,0.000048555452,0.000013769414,0.000059151604,0.00005370981],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022758477,0.00015534322,0.0001551857,0.00040391218,0.00037457168,0.0007407399,0.00028322372,0.0002495666,0.0010466833],"category_scores_gemma":[0.0005315626,0.00017032199,0.0002548127,0.00044411063,0.00052312406,0.00031552804,0.00029466706,0.00020198591,0.000053523225],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006633367,0.00002887933,0.9615389,0.000022012411,0.00010929004,0.00011698215,0.00032264186,0.027130345,0.004724287,0.00067851384,0.0004935175,0.0047680745],"study_design_scores_gemma":[0.000005147052,0.000008933677,0.9715233,0.0000055274395,0.000023116972,0.000020592961,0.00037988776,0.027450511,0.00010752222,0.00012742984,0.00033860287,0.000009455663],"about_ca_topic_score_codex":0.7945163,"about_ca_topic_score_gemma":0.881042,"teacher_disagreement_score":0.7945163,"about_ca_system_score_codex":0.0039996114,"about_ca_system_score_gemma":0.0011957347,"threshold_uncertainty_score":0.4133876},"labels":[],"label_agreement":null},{"id":"W2912260609","doi":"10.1029/2018gb005975","title":"Biogeochemical Cycling of Dissolved Zinc in the Western Arctic (Arctic GEOTRACES GN01)","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Argonne National Laboratory; Division of Ocean Sciences; U.S. Department of Energy; Office of Science; National Science Foundation","keywords":"Geotraces; Biogeochemical cycle; Oceanography; Arctic; Water column; Halocline; Canada Basin; Environmental science; Bioturbation; Geology; Sediment; Environmental chemistry; Chemistry; Seawater; Geomorphology; Salinity","score_opus":0.009789538609455044,"score_gpt":0.2394337293492485,"score_spread":0.22964419073979345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2912260609","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985103,0.00022417081,0.00009803903,0.000010924822,0.0000053637286,0.0000020917128,0.00053202093,0.0000078895855,0.0006091822],"genre_scores_gemma":[0.9980775,0.00023285356,0.00039832314,0.000016241704,0.00000384943,0.0000034036248,0.0007075859,0.000003809546,0.00055644393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999229,0.0000074096033,0.000005113624,0.000022795299,0.000027856446,0.000013873041],"domain_scores_gemma":[0.99984145,0.000010197397,0.0000357551,0.000004245179,0.000084439525,0.000023933932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000167592,0.0003151958,0.00020884744,0.0008031368,0.00044645218,0.0005316989,0.00013460971,0.00015305937,0.00028345443],"category_scores_gemma":[0.00014609908,0.00013507673,0.00017889607,0.0007207566,0.00014322858,0.0001314341,0.00029778492,0.00013260929,0.00011601588],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039075193,0.00003168133,0.8783971,0.000079954625,0.0001648495,0.00026086275,0.0003158996,0.0013075225,0.10264246,0.000109005116,0.00023474997,0.016065128],"study_design_scores_gemma":[0.000003815295,0.000045544475,0.9946673,0.000008192085,0.000032305295,0.000041106003,0.0001671352,0.0007462992,0.0034150525,0.000015204567,0.00085393945,0.000003976066],"about_ca_topic_score_codex":0.2433117,"about_ca_topic_score_gemma":0.36134058,"teacher_disagreement_score":0.2433117,"about_ca_system_score_codex":0.0009824852,"about_ca_system_score_gemma":0.00071594137,"threshold_uncertainty_score":0.48379093},"labels":[],"label_agreement":null},{"id":"W2914378285","doi":"10.1029/2018gb005997","title":"The Intraseasonal Dynamics of the Mixed Layer Pump in the Subpolar North Atlantic Ocean: A Biogeochemical‐Argo Float Approach","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"European Research Council; Horizon 2020 Framework Programme; Natural Environment Research Council; Sight Research UK","keywords":"Mixed layer; Mesopelagic zone; Spring bloom; Environmental science; Argo; Bloom; Oceanography; Biological pump; Biogeochemical cycle; Phytoplankton; Climatology; Pelagic zone; Geology; Nutrient; Ecology; Biology","score_opus":0.006805701150438161,"score_gpt":0.18406006948306394,"score_spread":0.17725436833262578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914378285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99900216,0.00006157379,0.00046623705,0.00002028572,0.0000034347456,0.000004490245,0.00017438961,0.000005333274,0.0002621423],"genre_scores_gemma":[0.9986966,0.000035416266,0.0009092485,0.000008494005,0.0000051770467,0.000005539909,0.00017669621,0.0000021675696,0.00016076624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999541,0.0000078497715,0.0000030324065,0.000020002472,0.000005697389,0.000009322555],"domain_scores_gemma":[0.9998518,0.00002795018,0.0000481098,0.000012468721,0.000027687323,0.000031948708],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018507268,0.0001994296,0.00020378533,0.0007318004,0.00028242747,0.00040870067,0.0002468247,0.00022954808,0.000544309],"category_scores_gemma":[0.00028638245,0.00014398694,0.00019901627,0.00047910903,0.00021106732,0.00029703186,0.0003441223,0.00012529592,0.00008743168],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000074925105,0.00009554805,0.9595891,0.00003037607,0.000120535726,0.000102691665,0.0003110094,0.011178384,0.015111549,0.00028653306,0.0002177813,0.012881476],"study_design_scores_gemma":[0.0000064064316,0.000037272235,0.94475883,0.0000067833653,0.000026092426,0.000020885112,0.00024819962,0.0540159,0.000288852,0.00013530049,0.00044701633,0.000008528108],"about_ca_topic_score_codex":0.02729565,"about_ca_topic_score_gemma":0.049144056,"teacher_disagreement_score":0.02729565,"about_ca_system_score_codex":0.00040325813,"about_ca_system_score_gemma":0.00023271723,"threshold_uncertainty_score":0.054273546},"labels":[],"label_agreement":null},{"id":"W2924211914","doi":"10.1029/2018gb006086","title":"Quantifying the Impact of Atmospheric Transport Uncertainty on CO<sub>2</sub> Surface Flux Estimates","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":258,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Aeronautics and Space Administration","keywords":"Environmental science; Flux (metallurgy); Atmospheric sciences; Carbon dioxide; Carbon dioxide in Earth's atmosphere; Distribution (mathematics); Chemistry; Geology; Mathematics","score_opus":0.009525731320093931,"score_gpt":0.2455924378622261,"score_spread":0.23606670654213216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2924211914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9671432,0.00018147599,0.030175125,0.0002535081,0.000018489061,0.000011254906,0.0007280986,0.0001423912,0.0013465493],"genre_scores_gemma":[0.99658185,0.000036585698,0.0029778178,0.000015958496,0.000006475916,0.0000046029727,0.00031272302,0.00001788542,0.000046002275],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99934405,0.0002997767,0.00004497682,0.00010829345,0.00014385309,0.00005895572],"domain_scores_gemma":[0.9946525,0.003795563,0.00059116364,0.00051064335,0.0003936422,0.00005636973],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021548008,0.0005779201,0.0002743644,0.00051263423,0.00032561054,0.000737019,0.00042780413,0.0006015088,0.0003809442],"category_scores_gemma":[0.012497789,0.00032165207,0.00037835594,0.0007819273,0.000417751,0.0012167217,0.0006031541,0.0005176892,0.000042311724],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009914477,0.000029229037,0.08675395,0.00003695101,0.00021385126,0.000055626944,0.000042514414,0.89766705,0.003484294,0.0020954618,0.00024616616,0.009275749],"study_design_scores_gemma":[0.000008069502,0.000033874392,0.03824272,0.000012282247,0.000051594183,0.00003077121,0.000033939355,0.9520672,0.007035749,0.0019617889,0.00049922004,0.00002274564],"about_ca_topic_score_codex":0.02955178,"about_ca_topic_score_gemma":0.021515137,"teacher_disagreement_score":0.02955178,"about_ca_system_score_codex":0.0010407969,"about_ca_system_score_gemma":0.00068285194,"threshold_uncertainty_score":0.05875951},"labels":[],"label_agreement":null},{"id":"W2937663245","doi":"10.1029/2018gb006152","title":"Seasonality of Dissolved Organic Carbon in the Upper Northeast Pacific Ocean","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; Fisheries and Oceans Canada; University of Washington; Conselho Nacional de Desenvolvimento Científico e Tecnológico; University of Miami; National Aeronautics and Space Administration; National Science Foundation","keywords":"Dissolved organic carbon; Biogeochemical cycle; Seasonality; Environmental science; Nitrate; Total organic carbon; Oceanography; Water column; Hydrology (agriculture); Environmental chemistry; Geology; Chemistry; Ecology; Biology","score_opus":0.006489509442866612,"score_gpt":0.1934852406608251,"score_spread":0.18699573121795848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937663245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973665,0.00015430005,0.000111516114,0.00004007687,0.000007937918,0.000005908109,0.001303653,0.000014994039,0.0009950448],"genre_scores_gemma":[0.99804354,0.00009488086,0.00022313757,0.00001930648,0.000007078378,0.000008664509,0.0012756077,0.0000044652566,0.0003233497],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999411,0.0000036472932,0.0000058947276,0.000020467549,0.000017663442,0.000011318033],"domain_scores_gemma":[0.9997664,0.000023319988,0.000078443365,0.000010927503,0.000073848314,0.00004703831],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016092147,0.00023463284,0.00015182485,0.000641838,0.00027398852,0.00043133023,0.00017248996,0.00015408588,0.00048153978],"category_scores_gemma":[0.00038036468,0.000129014,0.00016753338,0.00073652645,0.00018583925,0.00025364876,0.00033145712,0.00022286832,0.00009416439],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006366927,0.000021812153,0.9840858,0.00003409336,0.00006882524,0.0001213671,0.00017697315,0.0003322789,0.009466386,0.000027449702,0.00026750067,0.00533392],"study_design_scores_gemma":[8.939008e-7,0.000006214975,0.99901295,0.0000028131606,0.000006144367,0.000013497945,0.000055025645,0.0002528711,0.00029984463,0.0000050702465,0.00034287412,0.0000018274224],"about_ca_topic_score_codex":0.052790303,"about_ca_topic_score_gemma":0.082632184,"teacher_disagreement_score":0.052790303,"about_ca_system_score_codex":0.0005784789,"about_ca_system_score_gemma":0.00036383158,"threshold_uncertainty_score":0.104966104},"labels":[],"label_agreement":null},{"id":"W2942634271","doi":"10.1029/2018gb006134","title":"Remote Western Arctic Nutrients Fuel Remineralization in Deep Baffin Bay","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Chinese Academy of Agricultural Sciences; University of Connecticut; National Science Foundation","keywords":"Bay; Oceanography; Arctic; Environmental science; Benthic zone; Nitrogen cycle; Nutrient; Denitrification; Canada Basin; Geology; Nitrogen; Ecology; Chemistry","score_opus":0.0067831607998441274,"score_gpt":0.223683633783292,"score_spread":0.2169004729834479,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2942634271","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987643,0.00011487397,0.00004116469,0.00003403913,0.0000036916847,0.0000017372502,0.0002014813,0.0000056423846,0.0008331107],"genre_scores_gemma":[0.99883264,0.000088817826,0.00010874875,0.000021078065,0.000003224092,0.0000027707003,0.0002531102,0.000002800437,0.00068678375],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993634,0.000004002171,0.0000028522416,0.000021986263,0.00001599945,0.000018885754],"domain_scores_gemma":[0.9998809,0.000010047916,0.000023683317,0.000005784893,0.00004694738,0.00003257146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013175057,0.00031012288,0.00024340059,0.00061667146,0.00078875164,0.0006058987,0.0002442461,0.0003055449,0.0013879958],"category_scores_gemma":[0.00018228438,0.00022537078,0.00011971634,0.0004430459,0.0003030358,0.00034590292,0.00061281474,0.00019616171,0.00020163147],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006815909,0.00008997442,0.63478553,0.000109622626,0.00008451266,0.0005043391,0.0014632731,0.00088655186,0.34912497,0.000341235,0.00073289394,0.011195529],"study_design_scores_gemma":[0.000007193429,0.00003402081,0.99190944,0.000009390074,0.000015186896,0.000042141506,0.00073389075,0.0009146471,0.004966606,0.000053649237,0.0013056562,0.000008119879],"about_ca_topic_score_codex":0.25066134,"about_ca_topic_score_gemma":0.3481687,"teacher_disagreement_score":0.25066134,"about_ca_system_score_codex":0.0015686123,"about_ca_system_score_gemma":0.0007822679,"threshold_uncertainty_score":0.49840468},"labels":[],"label_agreement":null},{"id":"W2943101824","doi":"10.1029/2018gb006145","title":"Exposing the Distributions and Elemental Associations of Scavenged Particulate Phases in the Ocean Using Basin‐Scale Multi‐Element Data Sets","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Foundation of Sri Lanka","keywords":"Geotraces; Trace element; Particulates; Phytoplankton; Biogeochemical cycle; Environmental science; Authigenic; Mixed layer; Oceanography; Environmental chemistry; Chemistry; Geology; Mineralogy; Geochemistry; Diagenesis; Seawater; Nutrient","score_opus":0.03691632347407609,"score_gpt":0.27575399299808584,"score_spread":0.23883766952400975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2943101824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9819356,0.00011664797,0.008291705,0.00008940146,0.000005985048,0.000016576007,0.007739162,0.00025312387,0.0015517772],"genre_scores_gemma":[0.9775099,0.00008744768,0.015892006,0.00002582403,0.000009413677,0.000023729168,0.0059858975,0.000062491265,0.000403198],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985254,0.000018621742,0.00001508236,0.000054925604,0.00004313134,0.000015647229],"domain_scores_gemma":[0.9993362,0.00021277384,0.00013347849,0.000121389225,0.00016775579,0.000028450422],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039101293,0.00024750552,0.00017086252,0.0023498368,0.00023567877,0.00047360052,0.0002863101,0.00024278476,0.0009144904],"category_scores_gemma":[0.0009480259,0.00015491499,0.00047510694,0.0021748606,0.00020631445,0.0003470699,0.0007588142,0.00029701993,0.0001736375],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012072479,0.00006396298,0.86707723,0.00012627091,0.00031184423,0.00015197604,0.0005560386,0.019852621,0.058341976,0.0011155538,0.0009785346,0.051303294],"study_design_scores_gemma":[0.000007633139,0.000022445976,0.96385664,0.00001897486,0.000035811863,0.000053309777,0.0003517186,0.025729118,0.0055119717,0.00087717915,0.003512344,0.000022762322],"about_ca_topic_score_codex":0.027069973,"about_ca_topic_score_gemma":0.037183948,"teacher_disagreement_score":0.027069973,"about_ca_system_score_codex":0.0003023853,"about_ca_system_score_gemma":0.00027023559,"threshold_uncertainty_score":0.053824842},"labels":[],"label_agreement":null},{"id":"W2946072074","doi":"10.1029/2018gb005909","title":"Vegetation Functional Properties Determine Uncertainty of Simulated Ecosystem Productivity: A Traceability Analysis in the East Asian Monsoon Region","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; McMaster University; McMaster University Medical Centre","funders":"National Key Research and Development Program of China; Natural Sciences and Engineering Research Council of Canada; Jet Propulsion Laboratory; Oak Ridge National Laboratory; Biological and Environmental Research; National Natural Science Foundation of China; UT-Battelle; University of Montana; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy; California Institute of Technology; Battelle","keywords":"Primary production; Environmental science; Vegetation (pathology); Biosphere; Leaf area index; Terrestrial ecosystem; Productivity; East Asian Monsoon; Ecosystem; Normalized Difference Vegetation Index; Atmospheric sciences; Latitude; Biomass (ecology); Climatology; Monsoon; Global change; Climate change; Ecology; Geography; Geology; Biology","score_opus":0.012377970544744427,"score_gpt":0.1986931724834544,"score_spread":0.18631520193870996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946072074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985098,0.000018668292,0.0011517842,0.000017174483,0.0000012882336,0.0000030135186,0.00011923069,0.00003108818,0.00014782397],"genre_scores_gemma":[0.99957854,0.000004976133,0.0002665476,0.0000027739277,6.901021e-7,0.0000020113791,0.00012128118,0.000004265927,0.000018848394],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997241,0.0001052861,0.000023383247,0.00008196336,0.000029316634,0.00003602213],"domain_scores_gemma":[0.99829704,0.0010035589,0.00019187461,0.0002063666,0.00020940062,0.0000917267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018805795,0.00059732515,0.0002960567,0.0006639201,0.00036380126,0.0006762616,0.0008331152,0.0005419411,0.00046038575],"category_scores_gemma":[0.0032955583,0.0002932498,0.0010372975,0.0005539628,0.0004817179,0.0007659518,0.0005107345,0.00048319204,0.00004739062],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021842783,0.000080611695,0.15827803,0.000023569088,0.0002465845,0.00007989746,0.00009292854,0.83349895,0.0023525378,0.0004996323,0.00010075876,0.0045280107],"study_design_scores_gemma":[0.000016019998,0.000045176937,0.04717539,0.000004106209,0.000039278337,0.000016174512,0.000051018138,0.951242,0.0011105512,0.00022074764,0.00006684708,0.000012556698],"about_ca_topic_score_codex":0.044357,"about_ca_topic_score_gemma":0.01276168,"teacher_disagreement_score":0.044357,"about_ca_system_score_codex":0.0011202024,"about_ca_system_score_gemma":0.00052566075,"threshold_uncertainty_score":0.08819765},"labels":[],"label_agreement":null},{"id":"W2969681672","doi":"10.1029/2019gb006222","title":"Effects of Damming on River Nitrogen Fluxes: A Global Analysis","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Canada Excellence Research Chairs, Government of Canada","keywords":"Denitrification; Environmental science; Biogeochemical cycle; Hydrology (agriculture); Mineralization (soil science); Biogeochemistry; Nitrogen cycle; Nutrient; Nitrogen fixation; Nitrogen; Sedimentary rock; Phosphorus; Soil science; Geology; Oceanography; Environmental chemistry; Ecology; Chemistry; Soil water; Geochemistry","score_opus":0.0031528935785809765,"score_gpt":0.206315203362179,"score_spread":0.20316230978359803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969681672","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99754864,0.00008243109,0.0011338065,0.00005160034,0.0000031098546,0.0000040358696,0.0004020383,0.00004337699,0.0007310111],"genre_scores_gemma":[0.9989926,0.00007059733,0.0004438059,0.000011219421,0.0000025870827,0.0000040573095,0.0003431241,0.000011103018,0.00012085619],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99990475,0.0000346341,0.000003906192,0.000026779244,0.000010238661,0.00001961943],"domain_scores_gemma":[0.9997359,0.00011927786,0.000054023632,0.000031984386,0.000033174678,0.000025660429],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004611432,0.00052425667,0.00037469828,0.00046831623,0.00018104639,0.00039747276,0.00025959572,0.00040325796,0.0008687774],"category_scores_gemma":[0.00055922836,0.00021704099,0.00093228195,0.00078800827,0.00035977847,0.00057344086,0.00044171588,0.00021875916,0.000060519385],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020490785,0.00010721101,0.3052084,0.00009234573,0.00069823547,0.00049260777,0.00008240696,0.67317516,0.006578739,0.0017934811,0.0007509119,0.010815551],"study_design_scores_gemma":[0.00004128851,0.00020717524,0.37557805,0.000013436491,0.00030452298,0.00010754858,0.00014938308,0.6180598,0.0023696176,0.0015664635,0.001555343,0.00004744073],"about_ca_topic_score_codex":0.014023755,"about_ca_topic_score_gemma":0.009810739,"teacher_disagreement_score":0.014023755,"about_ca_system_score_codex":0.00052964425,"about_ca_system_score_gemma":0.00021795282,"threshold_uncertainty_score":0.027884245},"labels":[],"label_agreement":null},{"id":"W2971359887","doi":"10.1029/2018gb006157","title":"Sensitivity of Ozone Dry Deposition to Ecosystem‐Atmosphere Interactions: A Critical Appraisal of Observations and Simulations","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Oceanic and Atmospheric Administration; U.S. Department of Commerce","keywords":"Ozone; Atmosphere (unit); Environmental science; Atmospheric sciences; Deposition (geology); Ecosystem; Sensitivity (control systems); Environmental chemistry; Chemistry; Meteorology; Ecology; Geology; Geography; Geomorphology; Biology","score_opus":0.01408392649943846,"score_gpt":0.26075877964143385,"score_spread":0.2466748531419954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971359887","genre_codex":"empirical","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98371893,0.0039198073,0.004894545,0.00093641604,0.00007697108,0.000083139435,0.0024371874,0.00027972032,0.0036533296],"genre_scores_gemma":[0.99599165,0.0010428106,0.0019924047,0.00007296432,0.000045966615,0.000047339854,0.0006066003,0.00003090694,0.00016945812],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99961406,0.00018034365,0.000032562144,0.00007772197,0.000054243465,0.000041178584],"domain_scores_gemma":[0.99671245,0.0025522062,0.00025105898,0.00016648055,0.0002310796,0.00008673844],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025465703,0.00078934303,0.00070887926,0.000655161,0.00038760193,0.0009937742,0.0012906061,0.0010847951,0.0010159933],"category_scores_gemma":[0.004324793,0.00060000975,0.0010374152,0.0007088681,0.00048669797,0.0010354907,0.00068699656,0.0007320424,0.00008497562],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032737982,0.00018512084,0.0838293,0.0005519766,0.00073590776,0.00015320003,0.00012250172,0.8941281,0.0028124792,0.0017710911,0.0016502378,0.013732633],"study_design_scores_gemma":[0.00012373735,0.00014898129,0.050845634,0.00010006948,0.00019920352,0.000023768156,0.00012778446,0.9441405,0.0014002606,0.0012633766,0.0015802857,0.000046365767],"about_ca_topic_score_codex":0.04452436,"about_ca_topic_score_gemma":0.018942922,"teacher_disagreement_score":0.04452436,"about_ca_system_score_codex":0.0015108039,"about_ca_system_score_gemma":0.0005461859,"threshold_uncertainty_score":0.08853042},"labels":[],"label_agreement":null},{"id":"W2972727705","doi":"10.1029/2019gb006276","title":"Sediment Respiration Pulses in Intermittent Rivers and Ephemeral Streams","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"Horizon 2020 Framework Programme; Eusko Jaurlaritza; European Cooperation in Science and Technology; European Commission; Ministerio de Ciencia, Innovación y Universidades; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Ministerio de Economía y Competitividad; National Science Foundation","keywords":"STREAMS; Ephemeral key; Respiration; Sediment; Hydrology (agriculture); Environmental science; Geology; Oceanography; Ecology; Geomorphology; Biology; Geotechnical engineering","score_opus":0.00690520356791281,"score_gpt":0.2225075670722299,"score_spread":0.2156023635043171,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972727705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99966633,0.000035370518,0.00009239372,0.000002839791,6.3138646e-7,0.0000012504672,0.00008656399,0.0000031981533,0.00011145915],"genre_scores_gemma":[0.99963796,0.000024966812,0.0001251293,0.0000031596348,0.0000016186942,0.0000020903794,0.00012646262,0.000001467059,0.00007706229],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998921,0.000017721191,0.000011080694,0.00004277204,0.00001728297,0.000019066389],"domain_scores_gemma":[0.99967587,0.000045106808,0.00018788804,0.000019219615,0.0000426455,0.000029188846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001924296,0.00015693162,0.00017728019,0.0005345955,0.00016109864,0.00035521606,0.00012638983,0.00015553147,0.0004485708],"category_scores_gemma":[0.00037156872,0.00011818429,0.00014216022,0.0005992739,0.00022646978,0.00027788733,0.00027345613,0.0001506125,0.000052237818],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024900268,0.0000653392,0.941768,0.00003639956,0.000094642804,0.00014895582,0.0001726259,0.0012762398,0.04897914,0.000072139905,0.00007494721,0.007062498],"study_design_scores_gemma":[0.000001944786,0.000029015926,0.99805605,0.0000016295836,0.000008947841,0.000034754987,0.00005204748,0.0005631395,0.0011486699,0.000026281066,0.00007545304,0.000002143083],"about_ca_topic_score_codex":0.0028814152,"about_ca_topic_score_gemma":0.006438346,"teacher_disagreement_score":0.0028814152,"about_ca_system_score_codex":0.00021864446,"about_ca_system_score_gemma":0.0001068844,"threshold_uncertainty_score":0.005729258},"labels":[],"label_agreement":null},{"id":"W2979985574","doi":"10.1029/2018gb006135","title":"Underestimation of Global Photosynthesis in Earth System Models Due to Representation of Vegetation Structure","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Division of Graduate Education; Horizon 2020 Framework Programme; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; National Centre for Earth Observation; Natural Environment Research Council; Met Office; European Commission; Sight Research UK","keywords":"Biosphere; Environmental science; Shortwave radiation; Canopy; Atmospheric sciences; Photosynthetically active radiation; Photosynthesis; Carbon cycle; Shortwave; Interception; Vegetation (pathology); Radiation; Ecosystem; Radiative transfer; Ecology; Geology; Physics; Botany; Biology","score_opus":0.007569502610122832,"score_gpt":0.21885799025687075,"score_spread":0.21128848764674793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979985574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.986961,0.00023781684,0.009570693,0.00019835656,0.000027298136,0.000017891733,0.00051113596,0.00026795006,0.002207766],"genre_scores_gemma":[0.9981926,0.00006615927,0.0013169965,0.00002817317,0.0000037193709,0.000009642881,0.0001543538,0.000032343578,0.00019599166],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99964523,0.00017814888,0.000028022412,0.000054105763,0.000054704713,0.00003984353],"domain_scores_gemma":[0.99854857,0.000904666,0.00014360157,0.00021873834,0.00012779108,0.000056622324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00083857647,0.0005722353,0.00043961342,0.00023669236,0.00025619322,0.0007015072,0.0004399207,0.00058636814,0.00090614345],"category_scores_gemma":[0.0038521932,0.00032674466,0.00063552975,0.00049368193,0.0004111567,0.00082371844,0.0006479075,0.0005024603,0.00015297503],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052339852,0.000020173,0.015270018,0.000040068022,0.00006583314,0.000032744418,0.000030332336,0.97838587,0.0030179773,0.00040229334,0.00016790941,0.002514397],"study_design_scores_gemma":[0.000034273293,0.00006677903,0.0130164195,0.00001370599,0.000031642703,0.000022092738,0.000031754345,0.9841107,0.0019474531,0.00039842605,0.0003147268,0.000011956024],"about_ca_topic_score_codex":0.025056422,"about_ca_topic_score_gemma":0.015169967,"teacher_disagreement_score":0.025056422,"about_ca_system_score_codex":0.0008664415,"about_ca_system_score_gemma":0.0005049196,"threshold_uncertainty_score":0.04982114},"labels":[],"label_agreement":null},{"id":"W2984921292","doi":"10.1029/2019gb006261","title":"Natural Lakes Are a Minor Global Source of N<sub>2</sub>O to the Atmosphere","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Horizon 2020 Framework Programme","keywords":"Atmosphere (unit); Environmental science; Flux (metallurgy); Atmospheric sciences; Surface water; Natural (archaeology); Greenhouse gas; Hydrology (agriculture); Geology; Meteorology; Oceanography; Chemistry; Geography; Environmental engineering","score_opus":0.004665483211048428,"score_gpt":0.18506700015606606,"score_spread":0.18040151694501763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2984921292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9906611,0.0003734421,0.0023356264,0.00019960951,0.000010294167,0.000008995463,0.0024140973,0.0001735321,0.0038233723],"genre_scores_gemma":[0.99804914,0.00015339997,0.00065945025,0.000022883081,0.000003901896,0.000008120238,0.00080080656,0.0000130848875,0.00028928625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991107,0.000012635314,0.000005273038,0.000033269913,0.000020046948,0.000017753719],"domain_scores_gemma":[0.9998603,0.000028077024,0.000051890267,0.000015348185,0.00003200173,0.0000125261795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008946716,0.00022366745,0.0002120448,0.0001545659,0.0002016553,0.0006416408,0.000208856,0.00023205715,0.0015351928],"category_scores_gemma":[0.00029703326,0.00016711153,0.00035023302,0.00035012185,0.00023453264,0.00075711904,0.0003668715,0.00012463245,0.00017649893],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002620287,0.00009097052,0.7413592,0.0007470792,0.00049222726,0.00048640248,0.00019714182,0.10908841,0.109531395,0.0029158706,0.0038100367,0.031019289],"study_design_scores_gemma":[0.000063750354,0.000109633955,0.7898869,0.00007511556,0.00024852672,0.00021046758,0.00044056552,0.16780284,0.019362655,0.002413718,0.019309238,0.00007667258],"about_ca_topic_score_codex":0.021018712,"about_ca_topic_score_gemma":0.026798189,"teacher_disagreement_score":0.021018712,"about_ca_system_score_codex":0.0005062678,"about_ca_system_score_gemma":0.00055907166,"threshold_uncertainty_score":0.04179275},"labels":[],"label_agreement":null},{"id":"W2992149320","doi":"10.1029/2019gb006230","title":"Reduced CaCO<sub>3</sub>Flux to the Seafloor and Weaker Bottom Current Speeds Curtail Benthic CaCO<sub>3</sub>Dissolution Over the 21st Century","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seafloor spreading; Benthic zone; Bottom water; Dissolution; Geology; Abyssal zone; Oceanography; Sediment; Flux (metallurgy); Antarctic Bottom Water; Seabed; Deep sea; Ocean current; Current (fluid); Calcite; Environmental science; Mineralogy; Geomorphology; Chemistry","score_opus":0.008780813949656976,"score_gpt":0.22652336051884372,"score_spread":0.21774254656918673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2992149320","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9875438,0.00040808404,0.0021929396,0.0006738307,0.00006941429,0.000008873545,0.0019205018,0.00021792791,0.006964538],"genre_scores_gemma":[0.9983353,0.00018397109,0.0003141079,0.00005801641,0.000010139284,0.0000043127475,0.0004545679,0.00002895109,0.0006106271],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989665,0.00001888205,0.000008108175,0.000030858057,0.000015855701,0.000029601282],"domain_scores_gemma":[0.9996716,0.00007894097,0.000085018546,0.00004054598,0.00007144547,0.0000524707],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029703666,0.00044674185,0.00035383337,0.00025446116,0.00021971694,0.001353996,0.0005486005,0.0009043075,0.0020903442],"category_scores_gemma":[0.00097407954,0.00025657774,0.0011356577,0.00043054868,0.00035105235,0.00065250334,0.00045293284,0.0005132711,0.0003500419],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029298247,0.000085721054,0.11286951,0.00021786838,0.0004600608,0.00022684888,0.00007546129,0.86382926,0.008307763,0.0033246586,0.0027018718,0.0076080426],"study_design_scores_gemma":[0.00015352506,0.00015866349,0.106390655,0.000040864204,0.0003010933,0.00007175702,0.00015591196,0.8826813,0.0045062182,0.0016181377,0.0038706579,0.000051098723],"about_ca_topic_score_codex":0.06926717,"about_ca_topic_score_gemma":0.035565596,"teacher_disagreement_score":0.06926717,"about_ca_system_score_codex":0.0009783817,"about_ca_system_score_gemma":0.0010703263,"threshold_uncertainty_score":0.13772798},"labels":[],"label_agreement":null},{"id":"W2995331807","doi":"10.1029/2018gb006065","title":"Advancing Scientific Understanding of the Global Methane Budget in Support of the Paris Agreement","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":167,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Natural Environment Research Council; Sight Research UK; Gordon and Betty Moore Foundation","keywords":"Greenhouse gas; Environmental science; United Nations Framework Convention on Climate Change; Climate change; Wetland; Meteorology; Kyoto Protocol; Geography; Ecology","score_opus":0.007589795157183407,"score_gpt":0.21986652246571559,"score_spread":0.21227672730853217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995331807","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05568082,0.075999156,0.07666667,0.31839737,0.005730263,0.00015648175,0.0021081506,0.00055141305,0.46470967],"genre_scores_gemma":[0.83992666,0.08056069,0.039086066,0.010313725,0.0028991217,0.00023233816,0.0014021301,0.00022171364,0.025357587],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978116,0.0011006492,0.00007587967,0.00023817751,0.00053092034,0.0002428015],"domain_scores_gemma":[0.99291235,0.0029665946,0.00065424957,0.00061856175,0.0025755495,0.00027267367],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008050442,0.00076205784,0.00035779414,0.0027271956,0.0012771209,0.0054950695,0.0014645471,0.002019015,0.010193791],"category_scores_gemma":[0.015133514,0.00029130894,0.0005883569,0.002642026,0.0024546992,0.011418237,0.0025895024,0.0032540113,0.0012892786],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000069027745,0.000052223073,0.0057330728,0.0005718962,0.00006535734,0.00032176267,0.0014224359,0.030731825,0.0009373803,0.7966108,0.052986797,0.11049741],"study_design_scores_gemma":[0.000021315967,0.000041895342,0.008557987,0.0017149585,0.000027765493,0.0000806458,0.0028331135,0.02310567,0.0016982786,0.5128028,0.44900253,0.000113094786],"about_ca_topic_score_codex":0.034477256,"about_ca_topic_score_gemma":0.017080186,"teacher_disagreement_score":0.034477256,"about_ca_system_score_codex":0.010904652,"about_ca_system_score_gemma":0.006923321,"threshold_uncertainty_score":0.079119205},"labels":[],"label_agreement":null},{"id":"W2997778219","doi":"10.1029/2019gb006345","title":"A Synthesis of Blue Carbon Stocks, Sources, and Accumulation Rates in Eelgrass (<i>Zostera marina</i>) Meadows in the Northeast Pacific","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal plant biology","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Roads University; North Island College; Tula Foundation; Simon Fraser University","funders":"Hakai Institute; Commission for Environmental Cooperation; National Science Foundation","keywords":"Blue carbon; Seagrass; Zostera marina; Environmental science; Carbon sequestration; Temperate climate; Salt marsh; Sediment; Ecosystem; Greenhouse gas; Carbon fibers; Total organic carbon; Mangrove; Oceanography; Carbon dioxide; Ecology; Geology; Biology","score_opus":0.016991965385561667,"score_gpt":0.2204128116221373,"score_spread":0.20342084623657564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997778219","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917915,0.0017315706,0.00031699872,0.000017971312,0.0000036384965,0.000012170486,0.0049816803,0.0000132215755,0.0011313538],"genre_scores_gemma":[0.9905625,0.0016667864,0.0010407724,0.000023169225,0.000008076407,0.000027922244,0.0059308726,0.00000774003,0.0007321987],"study_design_codex":"observational","study_design_gemma":"meta_analysis","domain_scores_codex":[0.99989104,0.00001331433,0.000019872756,0.000039773517,0.000020005313,0.000015929301],"domain_scores_gemma":[0.99952054,0.00006805939,0.00016737108,0.00002389419,0.0001736761,0.000046334717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033149315,0.0003555698,0.00024119347,0.0040771407,0.00037987385,0.0006429998,0.00016679888,0.00013383706,0.0010430744],"category_scores_gemma":[0.00042048682,0.00017834712,0.00032089767,0.0030568356,0.00015992427,0.00034706361,0.00028827507,0.00011336283,0.00012916271],"study_design_candidate":"meta_analysis","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000108206994,0.000009791563,0.9750606,0.00023387515,0.00028378083,0.00007067387,0.0006017603,0.00020890828,0.0047493037,0.000025785426,0.00019538894,0.018451985],"study_design_scores_gemma":[7.9151766e-7,0.000008360847,0.9986457,0.000020107207,0.000053789205,0.000018513436,0.00029008923,0.000072084935,0.00021643669,0.000006358377,0.0006651738,0.0000025540976],"about_ca_topic_score_codex":0.14884779,"about_ca_topic_score_gemma":0.30674204,"teacher_disagreement_score":0.14884779,"about_ca_system_score_codex":0.00070628343,"about_ca_system_score_gemma":0.00048030226,"threshold_uncertainty_score":0.2959628},"labels":[],"label_agreement":null},{"id":"W2998006343","doi":"10.1029/2018gb006061","title":"Evolution of the Global Carbon Cycle and Climate Regulation on Earth","year":2019,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":211,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Science Foundation of Sri Lanka; NASA Astrobiology Institute; Heising-Simons Foundation; National Aeronautics and Space Administration","keywords":"Weathering; Carbon cycle; Carbon dioxide in Earth's atmosphere; Earth science; Earth (classical element); Environmental science; Carbon sink; Sink (geography); Atmosphere (unit); Earth system science; Silicate; Atmospheric sciences; Carbon dioxide; Climate change; Astrobiology; Carbon fibers; Geology; Oceanography; Chemistry; Ecology; Geochemistry; Meteorology; Materials science; Geography; Ecosystem","score_opus":0.007230887805746853,"score_gpt":0.22309252804830867,"score_spread":0.21586164024256183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2998006343","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36333564,0.5012804,0.01775157,0.022574984,0.0009173354,0.000034986464,0.0015103001,0.0003082571,0.0922865],"genre_scores_gemma":[0.90797895,0.0837525,0.0027176312,0.00178195,0.00044344057,0.0000139193,0.00028671115,0.00004057991,0.002984324],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.999874,0.000028547593,0.000006872939,0.000048952832,0.000022120752,0.000019390724],"domain_scores_gemma":[0.9998147,0.000039940376,0.000051558196,0.0000145654485,0.000053717777,0.000025501531],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045291858,0.0002380582,0.0001677602,0.000649927,0.00020228793,0.0010056989,0.00017878677,0.0007028948,0.0011657198],"category_scores_gemma":[0.0005659784,0.00009465964,0.00019764864,0.0011128585,0.0008935482,0.00094084843,0.0006224025,0.0005200439,0.00021111785],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030178163,0.00004291426,0.0500787,0.002033892,0.0007653925,0.0010244438,0.0011131171,0.027322162,0.046483207,0.39447168,0.013777334,0.46258542],"study_design_scores_gemma":[0.000024599418,0.00018300663,0.2633397,0.000664043,0.0002658116,0.00091419456,0.00069407024,0.009992067,0.0055168252,0.19835326,0.51991475,0.00013771933],"about_ca_topic_score_codex":0.0032874767,"about_ca_topic_score_gemma":0.0021886681,"teacher_disagreement_score":0.0032874767,"about_ca_system_score_codex":0.0010276468,"about_ca_system_score_gemma":0.00048122727,"threshold_uncertainty_score":0.007456124},"labels":[],"label_agreement":null},{"id":"W3002553555","doi":"10.1029/2019gb006349","title":"Tidal Wetland Gross Primary Production Across the Continental United States, 2000–2019","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Wetland; Primary production; Eddy covariance; Environmental science; Moderate-resolution imaging spectroradiometer; Carbon cycle; Hydrology (agriculture); Geology; Ecosystem; Ecology; Biology","score_opus":0.006954604834833982,"score_gpt":0.21540445657079607,"score_spread":0.2084498517359621,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3002553555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98909444,0.0001833414,0.00042954378,0.0001370785,0.000013272192,0.000008060132,0.008857276,0.00004584458,0.001231146],"genre_scores_gemma":[0.9927269,0.00008695897,0.0005669415,0.00004611644,0.0000067156993,0.000013610236,0.006038357,0.000005723856,0.0005086463],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999114,0.000013938579,0.000007335511,0.000032343884,0.00002242084,0.000012481421],"domain_scores_gemma":[0.9996086,0.00004342285,0.00009527311,0.00003963957,0.00016729564,0.00004577728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002592581,0.00023266088,0.00012174221,0.0005754719,0.00016956429,0.00037645802,0.00022005156,0.00019108481,0.0005256785],"category_scores_gemma":[0.00057425065,0.00010775149,0.00019441548,0.0011265198,0.0001303121,0.00039734945,0.0003728127,0.00020430169,0.0001226871],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000963383,0.000051076982,0.9696112,0.000038523245,0.0001681019,0.00014739232,0.00016658835,0.0063807094,0.0019046881,0.00015624236,0.0037642182,0.017514935],"study_design_scores_gemma":[0.000003261441,0.0000110591845,0.9933128,0.000006734637,0.000018333005,0.000021988697,0.00013140493,0.004226239,0.0003300386,0.00003836492,0.0018951059,0.000004638383],"about_ca_topic_score_codex":0.14732625,"about_ca_topic_score_gemma":0.2712119,"teacher_disagreement_score":0.14732625,"about_ca_system_score_codex":0.0010297367,"about_ca_system_score_gemma":0.0003617923,"threshold_uncertainty_score":0.2929374},"labels":[],"label_agreement":null},{"id":"W3004015853","doi":"10.1029/2020gb006788","title":"Quantifying Errors in Observationally Based Estimates of Ocean Carbon Sink Variability","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":217,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Southern Hemisphere; Environmental science; Amplitude; Climatology; Northern Hemisphere; Range (aeronautics); Carbon cycle; Sampling (signal processing); Geology; Atmospheric sciences; Meteorology; Computer science; Detector; Geography; Physics","score_opus":0.01636841120276211,"score_gpt":0.24047112959826805,"score_spread":0.22410271839550594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3004015853","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97447973,0.00018473952,0.022572488,0.00012816353,0.000029866387,0.000013200075,0.0013265889,0.00019182831,0.00107335],"genre_scores_gemma":[0.99601376,0.000029032455,0.0030883427,0.000018229572,0.0000085715155,0.000007104105,0.0007694582,0.000015537198,0.000049989467],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986792,0.00062719017,0.000128759,0.0002779341,0.00023222374,0.000054522643],"domain_scores_gemma":[0.9893756,0.0058896826,0.0015053105,0.0021728831,0.00095655385,0.000100013414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0054007415,0.00037168633,0.00023408046,0.00075691415,0.00016378485,0.0006506137,0.0004183454,0.00042984006,0.00039813298],"category_scores_gemma":[0.021301659,0.00024481496,0.0003061342,0.00066294754,0.00042264623,0.0009712564,0.00067645696,0.00032627865,0.00011881731],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002359952,0.000103469916,0.637303,0.00007707182,0.00067637727,0.00007185391,0.00013688348,0.31558102,0.0075149946,0.0012552453,0.00082446926,0.036219493],"study_design_scores_gemma":[0.000022708125,0.000055493987,0.4718899,0.00004206801,0.00005219386,0.000064638734,0.000081763326,0.5175136,0.006586317,0.0026326797,0.0010219438,0.000036679845],"about_ca_topic_score_codex":0.006605075,"about_ca_topic_score_gemma":0.0062613455,"teacher_disagreement_score":0.006605075,"about_ca_system_score_codex":0.00044071634,"about_ca_system_score_gemma":0.00031727005,"threshold_uncertainty_score":0.028562248},"labels":[],"label_agreement":null},{"id":"W3004718844","doi":"10.1029/2019gb006423","title":"Origin and Accumulation of an Anthropogenic CO<sub>2</sub> and <sup>13</sup>C Suess Effect in the Arctic Ocean","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Research Foundation of Korea; Joint Institute for the Study of the Atmosphere and Ocean; National Science Foundation","keywords":"Arctic; Canada Basin; Oceanography; Dissolved organic carbon; Halocline; Geotraces; Environmental science; Water mass; Carbon fibers; Seawater; Geology; Salinity","score_opus":0.02297387085081606,"score_gpt":0.27955330576637394,"score_spread":0.2565794349155579,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3004718844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992654,0.00008945233,0.00010546647,0.000016567039,0.000004137342,0.0000011992072,0.00014076867,0.000003669476,0.00037337356],"genre_scores_gemma":[0.9996247,0.000044871536,0.00007547152,0.000007802636,0.0000033929923,9.307995e-7,0.00013642116,0.0000022670354,0.00010411942],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999074,0.000013872721,0.0000064655683,0.00002568405,0.000028091737,0.000018468872],"domain_scores_gemma":[0.999708,0.000032651842,0.00009045865,0.000018122673,0.00010925681,0.000041478386],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029381146,0.00026757183,0.00017115538,0.00048289256,0.00029753265,0.00042092995,0.00014468595,0.00019059514,0.0003972146],"category_scores_gemma":[0.0003163639,0.0001470775,0.0002605511,0.00036201344,0.0003242287,0.00018769984,0.00032952163,0.0001843135,0.00008674481],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020901342,0.000013656253,0.964389,0.00002110411,0.00008068766,0.00012238673,0.000093675946,0.00076027494,0.031241618,0.00006265417,0.000079745645,0.0029260716],"study_design_scores_gemma":[8.5055245e-7,0.0000144604455,0.9978423,0.0000017471885,0.000010103224,0.000017359422,0.0000545359,0.00051251485,0.0013876846,0.000008978472,0.00014726729,0.0000022600082],"about_ca_topic_score_codex":0.07001325,"about_ca_topic_score_gemma":0.08152608,"teacher_disagreement_score":0.07001325,"about_ca_system_score_codex":0.00069534045,"about_ca_system_score_gemma":0.00047213,"threshold_uncertainty_score":0.13921148},"labels":[],"label_agreement":null},{"id":"W3009376267","doi":"10.1029/2019gb006356","title":"Linking Global Land Use/Land Cover to Hydrologic Soil Groups From 850 to 2015","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"University of Victoria; National Science Foundation","keywords":"Environmental science; Biogeochemical cycle; Soil water; Land use; Hydrology (agriculture); Land cover; Soil functions; Soil series; Soil type; Land management; Soil science; Soil classification; Soil biodiversity; Soil fertility; Geology; Ecology","score_opus":0.02538463609260596,"score_gpt":0.2331856119484899,"score_spread":0.20780097585588395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009376267","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898307,0.00012042244,0.00029407837,0.00003959509,0.0000049102905,0.0000067075216,0.008776687,0.000028347004,0.00089857244],"genre_scores_gemma":[0.99258053,0.000055425895,0.00029346958,0.000013576121,0.0000037247453,0.000005539374,0.006833502,0.0000034036702,0.00021087243],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998765,0.000018403513,0.000013845964,0.000044416658,0.000018877763,0.000028059705],"domain_scores_gemma":[0.9996973,0.000034369637,0.00011449577,0.00003163388,0.000079321086,0.000042811906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039721045,0.00021055978,0.00015445554,0.0011064305,0.0001408107,0.00047572414,0.00013750089,0.0001434005,0.0013164838],"category_scores_gemma":[0.0005846404,0.00009561749,0.00036417914,0.0018624434,0.00017476,0.0003620495,0.0005990812,0.00015465214,0.00022343681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039593648,0.000015285368,0.9908931,0.00003262107,0.000100703684,0.000024909134,0.000100940306,0.0024551477,0.0006104367,0.00016039802,0.00088868354,0.0046782037],"study_design_scores_gemma":[0.0000014958,0.0000079271995,0.9978167,0.000005768212,0.0000147014935,0.00001191698,0.000105421284,0.0012399779,0.00013700301,0.000045640518,0.00061070296,0.0000028289737],"about_ca_topic_score_codex":0.04176154,"about_ca_topic_score_gemma":0.05586094,"teacher_disagreement_score":0.04176154,"about_ca_system_score_codex":0.0005069753,"about_ca_system_score_gemma":0.00027562105,"threshold_uncertainty_score":0.08303696},"labels":[],"label_agreement":null},{"id":"W3033226544","doi":"10.1029/2020gb006547","title":"Low Molecular Weight Dissolved Organic Carbon: Aging, Compositional Changes, and Selective Utilization During Global Ocean Circulation","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"National Science Foundation","keywords":"Dissolved organic carbon; Carbon cycle; Environmental chemistry; Water column; Ultrafiltration (renal); Chemistry; Deep sea; Seawater; Composition (language); Total organic carbon; Oceanography; Environmental science; Geology; Ecology; Chromatography; Biology","score_opus":0.008996892674003528,"score_gpt":0.19965312922643313,"score_spread":0.1906562365524296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033226544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994469,0.00010575305,0.00009112398,0.000014603143,0.0000018096262,0.0000024631574,0.00013212994,0.0000035360918,0.00020161769],"genre_scores_gemma":[0.9995061,0.00007401449,0.00010638365,0.000018357157,0.0000029863104,0.0000036530257,0.0001498234,0.000002767359,0.00013590025],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000026808639,0.0000023246835,0.000019347779,0.000008982275,0.000009492857],"domain_scores_gemma":[0.99986994,0.000015567304,0.000051816194,0.000009032583,0.000030845345,0.000022751265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013367011,0.00024373383,0.00016268536,0.00036688586,0.00026712145,0.00036869015,0.00016569068,0.00021345016,0.0003400223],"category_scores_gemma":[0.00021387041,0.0001564829,0.000111807785,0.00038633423,0.00040123196,0.0003037074,0.0002489689,0.00025936143,0.00007723679],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021979724,0.00003897924,0.6170169,0.00006688801,0.00007939755,0.00015884876,0.00028850336,0.00033901457,0.37287146,0.00007439102,0.000080117,0.008765748],"study_design_scores_gemma":[0.0000014090153,0.000019778032,0.99570787,0.00000122382,0.00000629306,0.00001464959,0.00006650439,0.00016033405,0.0039107287,0.000011890944,0.00009750224,0.0000018705073],"about_ca_topic_score_codex":0.022163885,"about_ca_topic_score_gemma":0.026199393,"teacher_disagreement_score":0.022163885,"about_ca_system_score_codex":0.0004892388,"about_ca_system_score_gemma":0.00031067684,"threshold_uncertainty_score":0.044069767},"labels":[],"label_agreement":null},{"id":"W3038666536","doi":"10.1029/2020gb006716","title":"Nitrification and Nitrous Oxide Production in the Offshore Waters of the Eastern Tropical South Pacific","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Alfred P. Sloan Foundation; National Science Foundation","keywords":"Nitrification; Nitrite; Nitrate; Environmental chemistry; Nitrous oxide; Ammonia; Biogeochemistry; Photic zone; Nitrogen cycle; Ammonium; New production; Reactive nitrogen; Environmental science; Nitrogen; Oceanography; Chemistry; Nutrient; Geology","score_opus":0.013020933945135255,"score_gpt":0.18797833229800678,"score_spread":0.17495739835287152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3038666536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99964285,0.000022336993,0.000022690394,0.000006005502,6.368741e-7,0.0000016983992,0.00009244689,0.0000010640481,0.00021038137],"genre_scores_gemma":[0.9989937,0.000074327516,0.0001755731,0.000011117567,0.0000030213632,0.000008146501,0.00044823752,0.0000020122473,0.00028392288],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999254,0.0000069188814,0.0000056110002,0.000025004541,0.00002148487,0.000015686319],"domain_scores_gemma":[0.9996947,0.00004375538,0.000116438794,0.000012605251,0.00006959857,0.00006293004],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017581464,0.0004043444,0.000159756,0.00054434506,0.00046285984,0.00037280362,0.00018243879,0.00020171839,0.0004410843],"category_scores_gemma":[0.00036202156,0.00022827325,0.00019778854,0.0005209449,0.0003301892,0.0002295717,0.0004593814,0.00020235467,0.00008270337],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018732638,0.000028307282,0.92463434,0.0000661274,0.00007500852,0.00032480856,0.0012090099,0.0004906143,0.06921061,0.000020926316,0.000084259984,0.0036686733],"study_design_scores_gemma":[0.0000027857486,0.000025504376,0.9984322,0.000003617321,0.000007631396,0.00003603062,0.00028939423,0.00019386939,0.0008881187,0.0000054385027,0.000113271475,0.0000022066147],"about_ca_topic_score_codex":0.054068025,"about_ca_topic_score_gemma":0.07674526,"teacher_disagreement_score":0.054068025,"about_ca_system_score_codex":0.00036276606,"about_ca_system_score_gemma":0.00042636634,"threshold_uncertainty_score":0.10750663},"labels":[],"label_agreement":null},{"id":"W3041864671","doi":"10.1029/2019gb006430","title":"Hydrologic Export Is a Major Component of Coastal Wetland Carbon Budgets","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of Lethbridge","funders":"","keywords":"Wetland; Environmental science; Ecosystem; Productivity; Marsh; Carbon sequestration; Brackish water; Salt marsh; Ecosystem services; Terrestrial ecosystem; Ecology; Hydrology (agriculture); Carbon dioxide; Salinity; Biology; Geology","score_opus":0.009627228327274593,"score_gpt":0.21024490825058667,"score_spread":0.2006176799233121,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041864671","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954169,0.00008943031,0.00068442867,0.000055448105,0.0000020494767,0.000004867342,0.0020717566,0.00004354613,0.0016316171],"genre_scores_gemma":[0.99735487,0.00011063972,0.00038661904,0.000014836772,0.000004894655,0.0000071278632,0.001375446,0.000018005818,0.00072760467],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999565,0.000004674223,0.000005692335,0.000012059227,0.0000119703,0.000009083383],"domain_scores_gemma":[0.999721,0.000041354113,0.000115474446,0.000023045848,0.000068376095,0.00003065525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001263044,0.0002483049,0.00014660355,0.00041417143,0.00014974413,0.00044421264,0.00013935077,0.000099267294,0.0016157004],"category_scores_gemma":[0.0003802262,0.00011971884,0.00017064078,0.00049287814,0.0001081807,0.0004328082,0.00030283423,0.00010998328,0.00018563753],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012795335,0.000035977115,0.9180643,0.000110393914,0.0002497095,0.00018415286,0.000094973024,0.011414287,0.03790961,0.0005041027,0.00085418066,0.03045035],"study_design_scores_gemma":[0.0000036705771,0.000014927949,0.9894728,0.000007134408,0.00002654708,0.00004778466,0.000044096836,0.0073102964,0.0017327587,0.0001993891,0.0011329444,0.000007666111],"about_ca_topic_score_codex":0.010428992,"about_ca_topic_score_gemma":0.014969,"teacher_disagreement_score":0.010428992,"about_ca_system_score_codex":0.00034481572,"about_ca_system_score_gemma":0.0002931662,"threshold_uncertainty_score":0.020736575},"labels":[],"label_agreement":null},{"id":"W3043249414","doi":"10.1029/2019gb006495","title":"Delineating the Continuum of Dissolved Organic Matter in Temperate River Networks","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Trois-Rivières","funders":"Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Dissolved organic carbon; Biogeochemical cycle; Environmental science; Hydrology (agriculture); Aquatic ecosystem; Temperate climate; Ecology; Drainage basin; Ecosystem; Geology; Geography; Biology","score_opus":0.008542964684608703,"score_gpt":0.19356546783288595,"score_spread":0.18502250314827723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043249414","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99835664,0.00005626305,0.0010823448,0.000015747619,7.098519e-7,0.000002721711,0.00008556889,0.0000063427296,0.00039369537],"genre_scores_gemma":[0.9993926,0.000019708013,0.00045364196,0.0000039074653,0.0000012445921,0.0000027652195,0.000086178814,9.06879e-7,0.000039134156],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987555,0.00002931126,0.000009486055,0.00004706171,0.000014964705,0.000023551003],"domain_scores_gemma":[0.999559,0.00012079377,0.00013910545,0.000031631826,0.00008442605,0.00006502864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040815945,0.00007619601,0.00015656633,0.0010888884,0.0003089516,0.0006331149,0.00017865656,0.00018753171,0.0004147502],"category_scores_gemma":[0.0008199602,0.000088847126,0.00013542105,0.0006847826,0.0004648283,0.0005177606,0.0005841074,0.000113617476,0.00004276427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012452048,0.000030150915,0.96333724,0.0000312395,0.000035558696,0.0001331115,0.0008663008,0.002896997,0.022877874,0.0011290652,0.0000964166,0.00844141],"study_design_scores_gemma":[0.0000022631689,0.000029285753,0.9887272,0.000008173958,0.000008860521,0.00004622841,0.00067493,0.008643814,0.00081812503,0.00064023124,0.00039467885,0.0000060905772],"about_ca_topic_score_codex":0.004572247,"about_ca_topic_score_gemma":0.007535153,"teacher_disagreement_score":0.004572247,"about_ca_system_score_codex":0.00032178304,"about_ca_system_score_gemma":0.00019348806,"threshold_uncertainty_score":0.009091258},"labels":[],"label_agreement":null},{"id":"W3043952142","doi":"10.1029/2020gb006581","title":"Arctic Continental Margin Sediments as Possible Fe and Mn Sources to Seawater as Sea Ice Retreats: Insights From the Eurasian Margin","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"European Commission","keywords":"Geology; Biogeochemical cycle; Oceanography; Arctic; Continental margin; Sea ice; Sediment; Continental shelf; Plateau (mathematics); Arctic ice pack; Carbon cycle; Seafloor spreading; Geochemistry; Geomorphology; Ecosystem; Paleontology; Environmental chemistry","score_opus":0.008385570886958982,"score_gpt":0.21733265783791977,"score_spread":0.2089470869509608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043952142","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981493,0.0007258255,0.00008005757,0.00002652212,0.0000037066675,0.0000016128746,0.00016369058,0.0000027347678,0.00084676885],"genre_scores_gemma":[0.9984158,0.00056336913,0.00027988685,0.000023174849,0.0000048273064,0.0000019998834,0.00023748794,0.000004956078,0.00046837077],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993396,0.00000850443,0.0000071905406,0.000021221991,0.00001013669,0.00001908458],"domain_scores_gemma":[0.9998909,0.000009014667,0.00002975514,0.000004727428,0.00004942931,0.000016047623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028972546,0.0003088217,0.0003312423,0.0012501761,0.0006073759,0.0009195931,0.00016188425,0.00027811766,0.0005700782],"category_scores_gemma":[0.00016653458,0.00014218976,0.0003099718,0.0011811936,0.00022784791,0.00041756564,0.00048590743,0.00019425686,0.00015225848],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039904827,0.00003132352,0.91129774,0.00013203024,0.000108184584,0.00072222756,0.0016296571,0.00062359887,0.066410854,0.00013220763,0.00011280766,0.018400399],"study_design_scores_gemma":[0.0000016165591,0.000026593205,0.996723,0.000018830953,0.00002360942,0.00008436293,0.001028174,0.00026246576,0.0011371502,0.000029634233,0.0006612364,0.00000335923],"about_ca_topic_score_codex":0.040245872,"about_ca_topic_score_gemma":0.061529838,"teacher_disagreement_score":0.040245872,"about_ca_system_score_codex":0.0005024219,"about_ca_system_score_gemma":0.00041631272,"threshold_uncertainty_score":0.08002323},"labels":[],"label_agreement":null},{"id":"W3044905498","doi":"10.1029/2019gb006520","title":"Improving a Biogeochemical Model to Simulate Surface Energy, Greenhouse Gas Fluxes, and Radiative Forcing for Different Land Use Types in Northeastern United States","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Environmental science; Biogeochemical cycle; Radiative forcing; Greenhouse gas; Atmospheric sciences; Sensible heat; Biogeochemistry; Land use, land-use change and forestry; Climate model; Climatology; Climate change; Land use; Ecology; Oceanography; Geology","score_opus":0.011510205969079314,"score_gpt":0.2112928718086129,"score_spread":0.19978266583953358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3044905498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949503,0.000059695612,0.0029333148,0.00011946326,0.000015140065,0.000021880405,0.00037377994,0.00015006072,0.0013763381],"genre_scores_gemma":[0.99570674,0.00003739052,0.003378102,0.00003447915,0.000005119993,0.000027830723,0.0003874707,0.000016174237,0.00040680906],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987316,0.000037635637,0.000009050539,0.000040606792,0.00001671628,0.000022875263],"domain_scores_gemma":[0.99962986,0.00014477145,0.000049464874,0.00003549726,0.000092889866,0.000047458434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060779834,0.00072091806,0.00039322607,0.00035702068,0.00066436117,0.0006275145,0.00085309206,0.0007443566,0.0008637271],"category_scores_gemma":[0.00086759904,0.0004540421,0.00060341286,0.00033788985,0.00035671805,0.00044659304,0.00039719,0.00055526046,0.00009773171],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039913404,0.00007529804,0.016513737,0.000007735434,0.00003192302,0.000036607427,0.000018036351,0.9807184,0.0007691369,0.0001507591,0.00017767948,0.0014607913],"study_design_scores_gemma":[0.00002446353,0.000014468143,0.0028113672,0.0000015185659,0.000009954294,0.0000030349704,0.000009083295,0.99676764,0.00019640313,0.000042301897,0.00011623956,0.000003591442],"about_ca_topic_score_codex":0.23064844,"about_ca_topic_score_gemma":0.16512088,"teacher_disagreement_score":0.23064844,"about_ca_system_score_codex":0.002253247,"about_ca_system_score_gemma":0.0014861809,"threshold_uncertainty_score":0.45861185},"labels":[],"label_agreement":null},{"id":"W3044987811","doi":"10.1029/2019gb006453","title":"Time of Emergence and Large Ensemble Intercomparison for Ocean Biogeochemical Trends","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate variability and models","field":"Environmental Science","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions","funders":"Horizon 2020; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Biogeochemistry; Biogeochemical cycle; Environmental science; Earth system science; Forcing (mathematics); Climatology; Climate change; Oceanography; Ecology; Geology","score_opus":0.020558710746539335,"score_gpt":0.26299332174742157,"score_spread":0.24243461100088223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3044987811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9874401,0.000045104596,0.0112534445,0.00007654432,0.000034717847,0.00001342911,0.00047829826,0.000087267916,0.00057099364],"genre_scores_gemma":[0.9961261,0.000011778827,0.003062995,0.000016452113,0.0000068741797,0.00002269017,0.00065285683,0.000013800057,0.00008641461],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99952626,0.00024804444,0.0000246444,0.000114352886,0.000048162154,0.00003852535],"domain_scores_gemma":[0.9965823,0.001989558,0.0002678559,0.00081723044,0.0002370369,0.00010598004],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0035884515,0.0002931173,0.00021928204,0.00020055618,0.0004308907,0.00039030533,0.000386828,0.0002897335,0.0005328313],"category_scores_gemma":[0.004930383,0.00015621947,0.0005503144,0.00022110078,0.0002030789,0.0007224346,0.0006067363,0.000742923,0.000054546505],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007927777,0.0003621436,0.31243452,0.0000541783,0.0013438064,0.00007897291,0.00022171767,0.6277133,0.011101358,0.0029481177,0.0020136565,0.04093536],"study_design_scores_gemma":[0.000069536196,0.00018118708,0.12290104,0.000008186965,0.00011500236,0.000019585417,0.00007039587,0.86806196,0.005635194,0.0020710574,0.0008360809,0.000030728934],"about_ca_topic_score_codex":0.0061663175,"about_ca_topic_score_gemma":0.007815929,"teacher_disagreement_score":0.0061663175,"about_ca_system_score_codex":0.00037627327,"about_ca_system_score_gemma":0.0003787101,"threshold_uncertainty_score":0.018977761},"labels":[],"label_agreement":null},{"id":"W3048558434","doi":"10.1029/2020gb006612","title":"Decadal‐Scale Recovery of Carbon Stocks After Wildfires Throughout the Boreal Forests","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University; Université du Québec en Abitibi-Témiscamingue; Université du Québec à Montréal","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Academy of Finland; Russian Foundation for Basic Research","keywords":"Environmental science; Taiga; Boreal; Climate change; Atmospheric sciences; Physical geography; Ecology; Hydrology (agriculture); Agroforestry; Forestry; Geography; Geology; Biology","score_opus":0.006023511994135343,"score_gpt":0.2260377521576714,"score_spread":0.22001424016353607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048558434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99919254,0.0000800379,0.00011647057,0.000014477443,0.00000551643,0.0000017754323,0.0003886342,0.000010006232,0.0001905573],"genre_scores_gemma":[0.9994448,0.00002340163,0.00007120495,0.0000061574433,0.000004063244,0.0000021206865,0.00038026096,0.000001774753,0.00006626987],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998652,0.000021639338,0.000014211156,0.0000425708,0.00002484227,0.000031662796],"domain_scores_gemma":[0.99926585,0.00011973681,0.00028836614,0.000092920614,0.00013894972,0.00009418797],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00064316497,0.00020778441,0.00024345373,0.00049776805,0.00028291688,0.0004556578,0.000261139,0.00027101763,0.0005694841],"category_scores_gemma":[0.0007642057,0.00009521995,0.00036377003,0.0003905618,0.00020572887,0.00035449734,0.00023374014,0.0002712565,0.00011541419],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003493196,0.00006257726,0.98021793,0.00002515991,0.0001888234,0.00008742265,0.00012692488,0.001110943,0.009129596,0.00004421492,0.00028188454,0.008375225],"study_design_scores_gemma":[0.0000010990999,0.000020481095,0.99929726,9.650142e-7,0.00000907408,0.000022876984,0.000034347202,0.0003452283,0.00018796202,0.000009875931,0.00006860768,0.0000022887862],"about_ca_topic_score_codex":0.007773159,"about_ca_topic_score_gemma":0.012103309,"teacher_disagreement_score":0.007773159,"about_ca_system_score_codex":0.0002637008,"about_ca_system_score_gemma":0.000107843385,"threshold_uncertainty_score":0.015455842},"labels":[],"label_agreement":null},{"id":"W3080785158","doi":"10.1029/2020gb006592","title":"Ironing Out Fe Residence Time in the Dynamic Upper Ocean","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Vrije Universiteit Brussel; Ocean Frontier Institute; Fonds Wetenschappelijk Onderzoek; National Aeronautics and Space Administration; Agence Nationale de la Recherche; National Science Foundation","keywords":"Iron fertilization; Geotraces; Residence time (fluid dynamics); Biogeochemical cycle; Sediment trap; Environmental science; Oceanography; Residence; Cycling; Ocean current; Deep sea; Sediment; Carbon cycle; Climatology; Geology; Seawater; Water column; Phytoplankton; Geography; Ecosystem; Chemistry; Environmental chemistry; Nutrient; Ecology","score_opus":0.010169991418400493,"score_gpt":0.21238410787501874,"score_spread":0.20221411645661824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080785158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969988,0.00022037032,0.0011008176,0.000035272904,0.0000050651324,0.0000013524955,0.00041446913,0.000024714516,0.0011992432],"genre_scores_gemma":[0.9992505,0.000048991922,0.0002451094,0.000008115681,0.000002618309,0.0000013166664,0.00016751059,0.000005527377,0.00027029772],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996185,0.000002398017,0.0000017788084,0.00001713479,0.0000072481066,0.000009517748],"domain_scores_gemma":[0.9998425,0.00004266844,0.000050249393,0.0000131820125,0.00003457703,0.000016685759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014569715,0.00012481726,0.00015172499,0.0004679231,0.00017189511,0.00038639462,0.00018014958,0.00015298801,0.0007715178],"category_scores_gemma":[0.00041746063,0.0001199492,0.000111570494,0.00037736315,0.0001833568,0.00034499855,0.00029976093,0.00018851738,0.0001877813],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047849977,0.00004885587,0.62803906,0.00010164363,0.000092251845,0.00022602362,0.00039582181,0.0059694974,0.33143213,0.001282645,0.0005960321,0.031337578],"study_design_scores_gemma":[0.00000710574,0.0000622033,0.93986565,0.000012216696,0.000037878584,0.00008155653,0.00020694766,0.029857604,0.026537165,0.000640132,0.0026706187,0.000021030835],"about_ca_topic_score_codex":0.017070446,"about_ca_topic_score_gemma":0.015520303,"teacher_disagreement_score":0.017070446,"about_ca_system_score_codex":0.00042194378,"about_ca_system_score_gemma":0.00021261511,"threshold_uncertainty_score":0.033942163},"labels":[],"label_agreement":null},{"id":"W3081334618","doi":"10.1029/2020gb006626","title":"Long‐Term Shifts in U.S. Nitrogen Sources and Sinks Revealed by the New TREND‐Nitrogen Data Set (1930–2017)","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Ontario Ministry of Research, Innovation and Science","keywords":"Environmental science; Agriculture; Land use; Population; Surface runoff; Soil water; Nitrogen balance; Hydrology (agriculture); Atmospheric sciences; Geography; Nitrogen; Ecology; Soil science; Chemistry","score_opus":0.021996504073620016,"score_gpt":0.24574963357238724,"score_spread":0.22375312949876722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3081334618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5831936,0.0006626532,0.0017612918,0.0005037727,0.00009157735,0.000031185005,0.4094488,0.00028455738,0.0040226094],"genre_scores_gemma":[0.5002304,0.00063455076,0.0042984956,0.00016651824,0.000056584136,0.00015590324,0.49319622,0.00008519109,0.001176139],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997706,0.000029180033,0.000027013795,0.00007954484,0.00006489964,0.000028678724],"domain_scores_gemma":[0.999203,0.000084596235,0.00018841396,0.000115756004,0.00035112852,0.000057092824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048346483,0.00027816405,0.00024111047,0.0013406804,0.00030189904,0.00038867941,0.00034682383,0.00020485662,0.00085213705],"category_scores_gemma":[0.0015129837,0.00012557965,0.0003689658,0.0032903387,0.00019974055,0.0004284081,0.0007366349,0.00036969694,0.0004680862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014892212,0.00008394471,0.89281523,0.00020114948,0.00029371536,0.00015206353,0.0004219466,0.007995072,0.0014016709,0.001558377,0.06955146,0.025376454],"study_design_scores_gemma":[0.00003158477,0.0000343407,0.9075605,0.00010142387,0.00006918612,0.000085828295,0.0006217052,0.010854148,0.0011279889,0.0008369629,0.07864791,0.000028510438],"about_ca_topic_score_codex":0.15965201,"about_ca_topic_score_gemma":0.22232385,"teacher_disagreement_score":0.15965201,"about_ca_system_score_codex":0.0007325418,"about_ca_system_score_gemma":0.0011158973,"threshold_uncertainty_score":0.31744546},"labels":[],"label_agreement":null},{"id":"W3082018805","doi":"10.1029/2020gb006672","title":"Assessing the Potential for Mobilization of Old Soil Carbon After Permafrost Thaw: A Synthesis of <sup>14</sup>C Measurements From the Northern Permafrost Region","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; University of Guelph; University of Alberta","funders":"H2020 European Research Council; Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Permafrost; Thermokarst; Peat; Tundra; Soil water; Environmental science; Soil carbon; Hydrology (agriculture); Dissolved organic carbon; Total organic carbon; Anoxic waters; Geology; Physical geography; Environmental chemistry; Arctic; Soil science; Oceanography; Ecology; Chemistry","score_opus":0.041488272617773096,"score_gpt":0.24921434140849721,"score_spread":0.2077260687907241,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082018805","genre_codex":"empirical","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99175256,0.0028684898,0.0014019997,0.000055424887,0.000009189628,0.00002201368,0.0018646528,0.00003282019,0.001992822],"genre_scores_gemma":[0.99251336,0.0013175104,0.0035794561,0.000060066493,0.000021179823,0.00003345526,0.0021869228,0.00002643305,0.0002616211],"study_design_codex":"observational","study_design_gemma":"systematic_review","domain_scores_codex":[0.99971884,0.000058572296,0.000027959019,0.000102123064,0.00006490303,0.000027430797],"domain_scores_gemma":[0.9987255,0.00046977572,0.00025706994,0.00007570561,0.00039052073,0.000081460814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011559796,0.00039706263,0.0003867799,0.001773281,0.0005385212,0.000734778,0.00034227502,0.00036271228,0.0007251681],"category_scores_gemma":[0.0010690357,0.00023701572,0.00042810885,0.0021019252,0.0004859271,0.00047787227,0.00037879532,0.0002226971,0.00014075647],"study_design_candidate":"systematic_review","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036893203,0.00003729985,0.86974573,0.00070618937,0.00054770976,0.00040517072,0.0010407303,0.0017143267,0.060201395,0.000058449896,0.00034750393,0.06482656],"study_design_scores_gemma":[0.0000019047725,0.000030486652,0.99541426,0.000026666048,0.00007050543,0.00008055467,0.00022585786,0.0005182189,0.002464611,0.000026605643,0.0011312845,0.000008999563],"about_ca_topic_score_codex":0.019661615,"about_ca_topic_score_gemma":0.05263974,"teacher_disagreement_score":0.019661615,"about_ca_system_score_codex":0.0006216378,"about_ca_system_score_gemma":0.0007231589,"threshold_uncertainty_score":0.03909433},"labels":[],"label_agreement":null},{"id":"W3086852369","doi":"10.1029/2020gb006821","title":"Glacial Dust Surpasses Both Volcanic Ash and Desert Dust in Its Iron Fertilization Potential","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Dean of the Faculty of Arts and Sciences, Dartmouth College; Colby College","keywords":"Iron fertilization; Volcanic ash; Geology; Subarctic climate; Glacial period; Sediment; Glacier; Geochemistry; Volcano; Environmental chemistry; Mineralogy; Oceanography; Geomorphology; Chemistry; Nutrient; Phytoplankton","score_opus":0.009879687235458602,"score_gpt":0.21152973882951992,"score_spread":0.20165005159406132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3086852369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983924,0.00026788062,0.00003896512,0.000017497672,0.0000023117145,0.000001203097,0.00007860916,0.0000031106688,0.0011980655],"genre_scores_gemma":[0.9994591,0.000096217715,0.00007118927,0.000013003547,0.0000027514689,6.687912e-7,0.000101346464,0.0000012885905,0.00025443992],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998987,0.000011433424,0.000007883441,0.000030117833,0.000023642959,0.000028315328],"domain_scores_gemma":[0.9997955,0.00002888883,0.000052443585,0.000012609744,0.00005065228,0.000059920563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022606892,0.00019715776,0.0002001762,0.00048612428,0.00035645373,0.0007292034,0.00015338503,0.00018625098,0.0011840125],"category_scores_gemma":[0.0003438693,0.00010823065,0.00012643117,0.00033904068,0.00024796967,0.00034446485,0.00033758188,0.00014945057,0.00025409728],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012339771,0.000023937006,0.9653435,0.000027332382,0.000056435332,0.00020889092,0.00022910367,0.00015324907,0.021673923,0.00010994034,0.00014321349,0.011907094],"study_design_scores_gemma":[0.000001926233,0.0000440276,0.9971718,0.0000063681177,0.000014193935,0.0000951515,0.00047616765,0.00013391742,0.0011517099,0.000049416987,0.0008531917,0.0000021575356],"about_ca_topic_score_codex":0.020522166,"about_ca_topic_score_gemma":0.052633263,"teacher_disagreement_score":0.020522166,"about_ca_system_score_codex":0.00045241593,"about_ca_system_score_gemma":0.00035191467,"threshold_uncertainty_score":0.04080546},"labels":[],"label_agreement":null},{"id":"W3092371870","doi":"10.1029/2019gb006456","title":"Spatiotemporal Variability in Modeled Bottom Ice and Sea Surface Dimethylsulfide Concentrations and Fluxes in the Arctic During 1979–2015","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; University of Victoria","funders":"ArcticNet","keywords":"Sea ice; Arctic ice pack; Environmental science; Arctic; Oceanography; Pelagic zone; Biogeochemical cycle; Dimethylsulfoniopropionate; Climatology; Arctic geoengineering; Atmospheric sciences; Antarctic sea ice; Geology; Phytoplankton; Chemistry","score_opus":0.01131559501825098,"score_gpt":0.22250980287978459,"score_spread":0.21119420786153362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092371870","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977968,0.00007021407,0.00041738694,0.00003273108,0.000009627509,0.000003502226,0.0012170975,0.00003260587,0.00042008562],"genre_scores_gemma":[0.9981312,0.000060473227,0.00025099664,0.0000073166157,0.0000030546476,0.000004309589,0.0014043142,0.000004630393,0.00013358086],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999143,0.000010787563,0.000008387441,0.00003451533,0.00000991022,0.000022218119],"domain_scores_gemma":[0.9998995,0.000020008667,0.000022049055,0.000010185665,0.0000319605,0.000016346368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035385415,0.00055452617,0.00028920965,0.0002890437,0.00041058034,0.0005137077,0.00048649876,0.00043921088,0.00051192305],"category_scores_gemma":[0.00035793945,0.00030681558,0.0010977419,0.00036584924,0.00021559268,0.00035797444,0.00025760528,0.00021929291,0.0001312624],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029536147,0.00012396085,0.29659897,0.00006712771,0.000408443,0.00028181061,0.00007869848,0.6885494,0.008078088,0.0005610629,0.00088385225,0.0040732413],"study_design_scores_gemma":[0.00006554028,0.00009746168,0.23439679,0.000021242251,0.00018653033,0.00006509937,0.00014714112,0.75963134,0.004005593,0.00024139808,0.0010956944,0.00004615884],"about_ca_topic_score_codex":0.21902336,"about_ca_topic_score_gemma":0.12680507,"teacher_disagreement_score":0.21902336,"about_ca_system_score_codex":0.0018086359,"about_ca_system_score_gemma":0.0010654823,"threshold_uncertainty_score":0.435497},"labels":[],"label_agreement":null},{"id":"W3092760830","doi":"10.1029/2020gb006599","title":"Annual Net Community Production of Particulate and Dissolved Organic Carbon From a Decade of Biogeochemical Profiling Float Observations in the Northeast Pacific","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Health Canada; National Science Foundation","keywords":"Biogeochemical cycle; Dissolved organic carbon; Environmental science; Carbon cycle; Total organic carbon; Particulates; Biological pump; Biogeochemistry; Total inorganic carbon; Carbon sink; Sink (geography); Alkalinity; Carbon fibers; Carbon sequestration; Carbon dioxide; Oceanography; Environmental chemistry; Geology; Chemistry; Ecosystem; Climate change; Ecology","score_opus":0.021251813454880628,"score_gpt":0.21126763192015457,"score_spread":0.19001581846527393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092760830","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99804866,0.000054782344,0.00031047,0.000015117821,0.0000029434905,0.0000038896414,0.0012829344,0.000014179549,0.00026694516],"genre_scores_gemma":[0.99679714,0.00006679808,0.00083298853,0.000010114456,0.0000053257518,0.000009170649,0.0021218583,0.0000048005304,0.00015179087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999119,0.00000851084,0.000008797523,0.000036159563,0.000024611714,0.000010009072],"domain_scores_gemma":[0.99950325,0.00006691851,0.00015910533,0.000042143038,0.00017279797,0.00005586108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046937386,0.00022975806,0.00012798951,0.0007946032,0.00025619444,0.00033363007,0.00023600618,0.0002336704,0.00027953615],"category_scores_gemma":[0.00083251763,0.00016084644,0.0002319689,0.0006844296,0.00013012486,0.00043735275,0.00025904438,0.00015788937,0.00008362903],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026829133,0.000021073496,0.9859357,0.000019770925,0.0000699433,0.00004982308,0.00008517454,0.0020274206,0.0035859398,0.00003115203,0.00029217958,0.007854943],"study_design_scores_gemma":[0.0000017680456,0.000007978587,0.99387085,0.000003823359,0.000012479438,0.000021590478,0.00003283964,0.005322532,0.0004778176,0.000012745187,0.00023239836,0.0000031149982],"about_ca_topic_score_codex":0.07603152,"about_ca_topic_score_gemma":0.110092856,"teacher_disagreement_score":0.07603152,"about_ca_system_score_codex":0.0006287085,"about_ca_system_score_gemma":0.00036142275,"threshold_uncertainty_score":0.15117788},"labels":[],"label_agreement":null},{"id":"W3093279768","doi":"10.1029/2011gb004054","title":"Contribution of winter soil respiration to annual soil CO<sub>2</sub> emission in a Mollisol under different tillage practices in northeast China","year":2012,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Agriculture and Agri-Food Canada","funders":"National Natural Science Foundation of China","keywords":"Tillage; Environmental science; Soil respiration; Growing season; Mollisol; Agronomy; Soil carbon; Soil water; Animal science; Soil science; Biology","score_opus":0.01354690683770529,"score_gpt":0.2556951572265953,"score_spread":0.24214825038889,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093279768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998932,0.000021786529,0.000023859417,0.0000035198748,3.1910287e-7,9.594349e-7,0.000024656572,0.0000016255207,0.000029992127],"genre_scores_gemma":[0.9996803,0.000030113006,0.000048483016,0.000008469627,7.2150664e-7,0.0000028744078,0.00011148834,0.0000018601203,0.00011578589],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998528,0.000013618453,0.000015073103,0.000057025543,0.000023887138,0.00003766388],"domain_scores_gemma":[0.9997501,0.000019211368,0.00010036877,0.000016623768,0.00004276287,0.000070946306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029006682,0.00045521738,0.00037604073,0.00060161913,0.0003614143,0.00039099468,0.00028363042,0.00019831368,0.00023706997],"category_scores_gemma":[0.00017336667,0.00017173636,0.00040895905,0.00045449982,0.0002955181,0.00031256754,0.00031549312,0.0001397048,0.000045467452],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007212217,0.00011190368,0.78152233,0.00007212543,0.00018391317,0.00027161225,0.00071652513,0.00088023266,0.20802888,0.000037829876,0.000048568872,0.007404933],"study_design_scores_gemma":[0.0000030183398,0.0000477517,0.9983205,9.849729e-7,0.000014526617,0.000012754295,0.00008729838,0.00038155285,0.0010829908,0.000005868786,0.000039539365,0.000003172519],"about_ca_topic_score_codex":0.041385304,"about_ca_topic_score_gemma":0.08450487,"teacher_disagreement_score":0.041385304,"about_ca_system_score_codex":0.001128431,"about_ca_system_score_gemma":0.00054971856,"threshold_uncertainty_score":0.0822888},"labels":[],"label_agreement":null},{"id":"W3100943079","doi":"10.1029/2020gb006719","title":"Stream Dissolved Organic Matter in Permafrost Regions Shows Surprising Compositional Similarities but Negative Priming and Nutrient Effects","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Institute of General Medical Sciences; Natural Sciences and Engineering Research Council of Canada; Netherlands Earth System Science Centre; Montana Agricultural Experiment Station; National Science Foundation","keywords":"Dissolved organic carbon; Nutrient; Environmental chemistry; Mineralization (soil science); Colored dissolved organic matter; Ecosystem; Chemistry; Organic matter; Permafrost; Environmental science; Nutrient cycle; Ecology; Nitrogen; Biology; Phytoplankton","score_opus":0.021543395027868555,"score_gpt":0.2310716080588081,"score_spread":0.20952821303093955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3100943079","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999212,0.00016962318,0.00011731193,0.000011632614,0.0000013963111,0.000004055783,0.00011982322,0.000005417185,0.00035862735],"genre_scores_gemma":[0.9988752,0.0001009326,0.00050532713,0.00002221462,0.0000029678613,0.0000075012063,0.00022396934,0.0000033209478,0.00025847025],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999025,0.000010110787,0.00000912554,0.000039171264,0.000021685593,0.000017379905],"domain_scores_gemma":[0.99987423,0.000017090402,0.000048021902,0.00000723402,0.000025151494,0.000028246375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010464661,0.00021679072,0.00023270192,0.0003611584,0.0002955105,0.00031128374,0.00010668106,0.00019664841,0.00043064126],"category_scores_gemma":[0.00013550746,0.00012715429,0.00016103828,0.00023316186,0.0002689145,0.00018115673,0.00023635001,0.00016085166,0.000060629944],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002510366,0.000036368623,0.11111796,0.000091230206,0.000040523835,0.00011493524,0.00013514425,0.00017936963,0.8808258,0.000047190246,0.00003790205,0.0071225027],"study_design_scores_gemma":[0.0000043774007,0.00012636164,0.95123345,0.000005275688,0.000019265155,0.00010932122,0.00013080944,0.000300002,0.047526505,0.00004707931,0.0004915921,0.00000597693],"about_ca_topic_score_codex":0.003364164,"about_ca_topic_score_gemma":0.007761436,"teacher_disagreement_score":0.003364164,"about_ca_system_score_codex":0.00030052007,"about_ca_system_score_gemma":0.00021616799,"threshold_uncertainty_score":0.006689191},"labels":[],"label_agreement":null},{"id":"W3107448918","doi":"10.1029/2020gb006671","title":"Controls on the <sup>14</sup>C Content of Dissolved and Particulate Organic Carbon Mobilized Across the Mackenzie River Basin, Canada","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Svenska Forskningsrådet Formas","keywords":"Tributary; Dissolved organic carbon; Permafrost; Total organic carbon; Bedrock; Hydrology (agriculture); Drainage basin; Biogeochemistry; Particulates; Environmental science; Turbidity; Geology; Oceanography; Environmental chemistry; Geomorphology; Ecology; Chemistry; Geography","score_opus":0.030971335893423393,"score_gpt":0.22535372487342192,"score_spread":0.19438238897999854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3107448918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997322,0.0001687636,0.00007936691,0.000055461962,0.0000024942974,0.000006645277,0.0008480947,0.000009250405,0.0015078662],"genre_scores_gemma":[0.9985844,0.00009210994,0.00013299563,0.000028004877,8.626865e-7,0.0000056103895,0.00037669032,0.0000074077484,0.00077201927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997558,0.00001473158,0.000012136267,0.00009922299,0.000052509313,0.00006552988],"domain_scores_gemma":[0.99952376,0.00003907999,0.0000786329,0.000018610115,0.00024614518,0.00009374041],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017417825,0.00028325236,0.00020177187,0.00071593345,0.001352756,0.0008890142,0.0004831868,0.00014314803,0.0010715062],"category_scores_gemma":[0.00041581216,0.00020202307,0.00019584043,0.0006972233,0.00075426657,0.00020049998,0.0005185335,0.00021009933,0.000120482255],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054337137,0.000040754327,0.8742257,0.0001016164,0.00022246239,0.00021534279,0.000949736,0.0008732814,0.11029396,0.00062705594,0.0009227169,0.010984036],"study_design_scores_gemma":[0.0000026419518,0.000008415577,0.996906,0.0000038138264,0.000016655806,0.000015111346,0.00037647272,0.00018710602,0.0017270707,0.000024738034,0.00072644884,0.0000055220817],"about_ca_topic_score_codex":0.9307648,"about_ca_topic_score_gemma":0.96595484,"teacher_disagreement_score":0.069235206,"about_ca_system_score_codex":0.0084407,"about_ca_system_score_gemma":0.004832791,"threshold_uncertainty_score":0.13928586},"labels":[],"label_agreement":null},{"id":"W3108480344","doi":"10.1029/2020gb006629","title":"Summertime Biogenic Silica Production and Silicon Limitation in the Pacific Arctic Region From 2006 to 2016","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Biogenic silica; Silicic acid; Photic zone; Phytoplankton; Nitrate; Diatom; Oceanography; New production; Arctic; Environmental science; Irradiance; Dissolved silica; Particulates; Plankton; Environmental chemistry; Atmospheric sciences; Nutrient; Geology; Chemistry","score_opus":0.017403049382604417,"score_gpt":0.20370905681575147,"score_spread":0.18630600743314704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3108480344","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982905,0.00027786937,0.000055992652,0.000018409524,0.0000074349928,0.000002229934,0.0009479597,0.0000046472446,0.00039515522],"genre_scores_gemma":[0.99783784,0.0002456597,0.00015474795,0.000012195735,0.000013469407,0.0000047593862,0.0013755584,0.000002339949,0.00035347784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992,0.000006749616,0.000009044026,0.00002516848,0.00001932071,0.00001971046],"domain_scores_gemma":[0.99961156,0.000023707056,0.00012872687,0.0000127696685,0.00015701233,0.00006626324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003031358,0.0002654757,0.00021744262,0.0008660425,0.00046148113,0.00044176367,0.00014089639,0.00017014377,0.00031472888],"category_scores_gemma":[0.00029614763,0.00013263179,0.0002024695,0.0008525232,0.0001681508,0.00026378199,0.0002855498,0.0001647161,0.0000901137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017423618,0.000021374663,0.9864374,0.000055922923,0.000079632955,0.000116095,0.00037541098,0.00035410703,0.0057909903,0.00002687101,0.00026296813,0.006305153],"study_design_scores_gemma":[7.309796e-7,0.00001258749,0.99882895,0.0000054310012,0.0000082013175,0.000024058483,0.00012990386,0.00013461517,0.00038584098,0.000004151198,0.000463823,0.0000017960887],"about_ca_topic_score_codex":0.08094385,"about_ca_topic_score_gemma":0.14582999,"teacher_disagreement_score":0.08094385,"about_ca_system_score_codex":0.0006230916,"about_ca_system_score_gemma":0.00063394173,"threshold_uncertainty_score":0.16094542},"labels":[],"label_agreement":null},{"id":"W3109703770","doi":"10.1029/2020gb006613","title":"Climate‐Driven Variability and Trends in Plant Productivity Over Recent Decades Based on Three Global Products","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Environment and Climate Change Canada","funders":"Natural Environment Research Council; Sight Research UK; Nuclear Safety and Security Commission; European Space Agency; National Aeronautics and Space Administration","keywords":"Environmental science; Biosphere; Climatology; FluxNet; Tropics; Primary production; Carbon cycle; Atmospheric sciences; Latitude; Vegetation (pathology); Climate change; Global change; Temporal scales; Ecosystem; Geography; Ecology; Eddy covariance; Geology","score_opus":0.01210731510071357,"score_gpt":0.22559357271795463,"score_spread":0.21348625761724105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3109703770","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9746397,0.00030063873,0.0007442349,0.00008376108,0.000012235722,0.000005236865,0.023047946,0.00009779923,0.001068533],"genre_scores_gemma":[0.9660243,0.00021226592,0.0012645018,0.000028991364,0.0000138421365,0.000016679012,0.0321478,0.000033827913,0.0002578168],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987185,0.000016950944,0.000011813528,0.00005901336,0.00002314479,0.000017276092],"domain_scores_gemma":[0.9990439,0.00021439751,0.00032193813,0.000121272264,0.00022686372,0.00007158442],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006476988,0.00039802236,0.00016016357,0.0012169315,0.00010109995,0.00046243606,0.00028333554,0.00022707108,0.00078119524],"category_scores_gemma":[0.0013115099,0.00011541815,0.0004790994,0.002550204,0.0001494728,0.000529175,0.00036659357,0.00024691486,0.00023615743],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012568079,0.000029258505,0.9751247,0.00010291945,0.0004406573,0.00008121684,0.00021232157,0.0062749125,0.0019410715,0.00028423828,0.0017970555,0.0135858925],"study_design_scores_gemma":[0.00000472548,0.0000203205,0.9943658,0.000011970393,0.00006575521,0.00006586605,0.000057084024,0.0034096267,0.0003588232,0.000089193025,0.0015433809,0.0000073895008],"about_ca_topic_score_codex":0.011793493,"about_ca_topic_score_gemma":0.013115142,"teacher_disagreement_score":0.011793493,"about_ca_system_score_codex":0.0003120337,"about_ca_system_score_gemma":0.00018047435,"threshold_uncertainty_score":0.023449719},"labels":[],"label_agreement":null},{"id":"W3115379833","doi":"10.1029/2019gb006218","title":"Estimating Greenhouse Gas Emissions From Peat Combustion in Wildfires on Indonesian Peatlands, and Their Uncertainty","year":2020,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Canadian Forest Service","funders":"","keywords":"Peat; Greenhouse gas; Environmental science; Variance (accounting); Monte Carlo method; Combustion; Atmospheric sciences; Environmental engineering; Hydrology (agriculture); Soil science; Meteorology; Statistics; Mathematics; Chemistry; Geology; Ecology; Geography","score_opus":0.009471067808072995,"score_gpt":0.21850648246070944,"score_spread":0.20903541465263645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3115379833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91416675,0.013562803,0.06886469,0.00024953188,0.000059190897,0.00010530546,0.001468347,0.00012864696,0.0013948525],"genre_scores_gemma":[0.9896253,0.0016063361,0.008122316,0.000037978753,0.00001189853,0.000046245957,0.00042446802,0.000014816887,0.00011067695],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9983701,0.001032573,0.00013757966,0.00025891076,0.00015528819,0.00004558664],"domain_scores_gemma":[0.9933513,0.005457716,0.0005114155,0.00034973645,0.00028942438,0.00004044559],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008861127,0.0009305319,0.0011541289,0.0022898123,0.00026407163,0.0013636663,0.00075427914,0.0005805665,0.0003584011],"category_scores_gemma":[0.0089416895,0.00048187378,0.0041448497,0.0014563348,0.00041004585,0.00087972695,0.0005340315,0.00046976705,0.000048231435],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004900392,0.00010770585,0.17345655,0.0012808385,0.01888325,0.00033047155,0.00009751575,0.7698552,0.0022779552,0.0022059914,0.00021701684,0.030797405],"study_design_scores_gemma":[0.000103304315,0.0001919439,0.07862352,0.00047050844,0.0092346165,0.00015290905,0.00021488048,0.8934807,0.006119067,0.009635865,0.0016703155,0.00010234196],"about_ca_topic_score_codex":0.014231862,"about_ca_topic_score_gemma":0.009215611,"teacher_disagreement_score":0.014231862,"about_ca_system_score_codex":0.0011938654,"about_ca_system_score_gemma":0.00081104203,"threshold_uncertainty_score":0.04686266},"labels":[],"label_agreement":null},{"id":"W3120346597","doi":"10.1029/2020gb006721","title":"Consistent Relationships Among Productivity Rate Methods in the NE Subarctic Pacific","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Productivity; Environmental science; Upwelling; Primary production; Carbon cycle; Phytoplankton; Subarctic climate; Carbon fibers; Dissolved organic carbon; Chlorophyll a; Atmospheric sciences; Environmental chemistry; Ecosystem; Chemistry; Nutrient; Oceanography; Ecology; Geology; Biology; Mathematics","score_opus":0.03274419035608174,"score_gpt":0.2608655853941226,"score_spread":0.22812139503804085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3120346597","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9886002,0.0020083,0.0057338793,0.00010027194,0.000027997565,0.00004105325,0.0007055479,0.000070456794,0.002712185],"genre_scores_gemma":[0.9927401,0.00047834596,0.0052060816,0.00007385878,0.000012634591,0.000046785342,0.0005963601,0.000029497187,0.00081635994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988605,0.00031479506,0.00010992998,0.00037160201,0.00028547077,0.000057789366],"domain_scores_gemma":[0.98941094,0.0044719344,0.002210577,0.00079280074,0.0029334456,0.00018024739],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027514098,0.00052500906,0.00024949643,0.00088735035,0.00036069748,0.0008542203,0.000512442,0.00035535867,0.0003835568],"category_scores_gemma":[0.0073681828,0.00040244494,0.00023351025,0.0007552019,0.00036685736,0.00042058344,0.00042393265,0.00035358703,0.00013004993],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019466493,0.00006914729,0.94644576,0.00014664751,0.00035688144,0.000071139046,0.0005163462,0.0011179578,0.035268325,0.00009730791,0.00020105313,0.0155147435],"study_design_scores_gemma":[0.0000048360175,0.00007207978,0.98818386,0.000016611933,0.000064392116,0.00006039805,0.00023396831,0.0011095861,0.009511398,0.000049408827,0.0006849869,0.000008453153],"about_ca_topic_score_codex":0.019037845,"about_ca_topic_score_gemma":0.033594962,"teacher_disagreement_score":0.019037845,"about_ca_system_score_codex":0.0007690745,"about_ca_system_score_gemma":0.0004260712,"threshold_uncertainty_score":0.037854075},"labels":[],"label_agreement":null},{"id":"W3120427812","doi":"10.1029/2020gb006717","title":"Spatially Resolved Measurements in Tropical Reservoirs Reveal Elevated Methane Ebullition at River Inflows and at High Productivity","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"FP7 Ideas: European Research Council; Fundação de Amparo à Pesquisa do Estado de Minas Gerais; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Environmental science; Hydrology (agriculture); Tropics; Methane; Productivity; Hypolimnion; Atmospheric sciences; Eutrophication; Geology; Nutrient; Ecology","score_opus":0.013085392492999282,"score_gpt":0.21870181819403336,"score_spread":0.20561642570103408,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3120427812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991897,0.00003337606,0.00035053884,0.000007357503,7.727067e-7,0.0000018495604,0.00014114972,0.000013840201,0.0002614163],"genre_scores_gemma":[0.99957687,0.000013860982,0.00029266605,0.0000031006498,5.029082e-7,0.000002652688,0.00005611996,0.0000027499407,0.00005151424],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992096,0.00000899884,0.000005493457,0.000024565088,0.000015980782,0.000023965897],"domain_scores_gemma":[0.999798,0.000048248672,0.00006201247,0.000016426873,0.000044663564,0.000030702115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016134906,0.00017916903,0.00018655225,0.0005044066,0.00024222893,0.0002971307,0.0001800941,0.0001957025,0.0006172724],"category_scores_gemma":[0.0004094679,0.00020180302,0.00014519441,0.00044114736,0.00027184602,0.00034221157,0.00040181624,0.00015663696,0.000092523595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017626488,0.000044702272,0.7052348,0.00006988175,0.00005826396,0.00018672759,0.0010207102,0.0018866076,0.28200382,0.000097719036,0.0000946293,0.009125819],"study_design_scores_gemma":[0.0000030555027,0.000032156553,0.98735493,0.000006651015,0.000015339387,0.000054109285,0.00031983186,0.0032440966,0.008764493,0.000025333775,0.0001708611,0.000009061267],"about_ca_topic_score_codex":0.014076605,"about_ca_topic_score_gemma":0.024411827,"teacher_disagreement_score":0.014076605,"about_ca_system_score_codex":0.0002092437,"about_ca_system_score_gemma":0.00017811517,"threshold_uncertainty_score":0.027989328},"labels":[],"label_agreement":null},{"id":"W3121947077","doi":"10.1029/2020gb006651","title":"Summertime Evolution of Net Community Production and CO<sub>2</sub> Flux in the Western Arctic Ocean","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China; National Science Foundation","keywords":"Arctic; Flux (metallurgy); Oceanography; Sea ice; New production; Environmental science; Saturation (graph theory); Arctic ice pack; Atmospheric sciences; Nutrient; Climatology; Chemistry; Geology; Phytoplankton","score_opus":0.011491918681978772,"score_gpt":0.21930749471764893,"score_spread":0.20781557603567016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3121947077","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996177,0.000016319458,0.000046871017,0.000005694299,0.0000013680791,5.894616e-7,0.00018176726,0.000004761242,0.00012487834],"genre_scores_gemma":[0.99951684,0.000013314628,0.00006729175,0.0000037307611,0.000001935076,0.0000020855628,0.0002905916,0.000002033702,0.00010214021],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999614,0.0000061366545,0.0000025047675,0.000013647184,0.0000072008943,0.000009221369],"domain_scores_gemma":[0.99981683,0.000022618915,0.000044051823,0.0000117956415,0.00006353142,0.000041149407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001778365,0.00021457835,0.00017744557,0.00031528325,0.00024571104,0.00030568475,0.00009644438,0.00015644396,0.00048588336],"category_scores_gemma":[0.0002781601,0.00012525124,0.00015270295,0.00026104692,0.00012275227,0.00018281875,0.00017499628,0.000109443456,0.00012649978],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002551158,0.00003102151,0.97401947,0.000013944061,0.000054646804,0.0000778956,0.00018963659,0.0013213445,0.02085579,0.000044426353,0.00021993782,0.0029169028],"study_design_scores_gemma":[9.69551e-7,0.000012899441,0.9979698,0.0000012431533,0.000004117192,0.000012145115,0.00006620036,0.0015792545,0.00025390965,0.000008171781,0.000089422785,0.000001813503],"about_ca_topic_score_codex":0.04974826,"about_ca_topic_score_gemma":0.07022745,"teacher_disagreement_score":0.04974826,"about_ca_system_score_codex":0.00036796558,"about_ca_system_score_gemma":0.00022078017,"threshold_uncertainty_score":0.098917425},"labels":[],"label_agreement":null},{"id":"W3125117975","doi":"10.1029/2020gb006850","title":"Declining Summertime <i>p</i>CO<sub>2</sub> in Tundra Lakes in a Granitic Landscape","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Agnico Eagle (Canada); University of Alberta; University of Guelph","funders":"","keywords":"Tundra; Environmental science; Alkalinity; Arctic; Climate change; Greenhouse gas; Global warming; Ecosystem; Bedrock; Carbon dioxide; Precipitation; Atmospheric sciences; Physical geography; Oceanography; Ecology; Geology; Geography; Chemistry","score_opus":0.024739684958488987,"score_gpt":0.250301298192515,"score_spread":0.22556161323402601,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3125117975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993856,0.00005155116,0.000026924527,0.000016185628,7.836975e-7,0.0000013279829,0.00021922651,0.0000042746196,0.0002940858],"genre_scores_gemma":[0.9996538,0.000025213569,0.000053566364,0.0000067332658,7.844163e-7,0.00000124189,0.00016301438,0.0000016579527,0.00009402661],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998995,0.000008562266,0.000006555314,0.000032338474,0.000018328883,0.00003470732],"domain_scores_gemma":[0.9997248,0.000018784214,0.000085832806,0.000013048278,0.00008996461,0.00006761173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021307277,0.00019054771,0.00017747807,0.00089232944,0.0009609721,0.000864047,0.00036840996,0.00027382557,0.0005937359],"category_scores_gemma":[0.00031889728,0.0001415954,0.0002606336,0.0013521153,0.00046238536,0.0002944935,0.0003590259,0.00014560687,0.00008559345],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009041905,0.0000073415194,0.9942788,0.000011874285,0.000042939482,0.0000770446,0.00033667625,0.00040418297,0.0028016954,0.000029607692,0.00009084283,0.001828589],"study_design_scores_gemma":[0.000001134314,0.000004170173,0.998825,0.0000021590258,0.0000069727575,0.000021446987,0.00033468168,0.00040866138,0.00020087863,0.0000068568297,0.00018622103,0.000001825767],"about_ca_topic_score_codex":0.7121256,"about_ca_topic_score_gemma":0.85577613,"teacher_disagreement_score":0.7121256,"about_ca_system_score_codex":0.00380384,"about_ca_system_score_gemma":0.0016162904,"threshold_uncertainty_score":0.5791395},"labels":[],"label_agreement":null},{"id":"W3126916403","doi":"10.1029/2020gb006769","title":"Global Ocean Sediment Composition and Burial Flux in the Deep Sea","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":141,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Australian Research Council; Russian Science Foundation; European Commission; Past Global Changes; Akademie der Naturwissenschaften; National Science Foundation","keywords":"Authigenic; Seafloor spreading; Sedimentary rock; Geology; Deep sea; Total organic carbon; Sediment; Oceanography; Carbon cycle; Biogenic silica; Carbonate; Mineralogy; Geochemistry; Paleontology; Environmental chemistry; Ecosystem","score_opus":0.01185105624429055,"score_gpt":0.24865882690293334,"score_spread":0.23680777065864278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3126916403","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99708813,0.00016049859,0.00035050765,0.000021220665,0.0000031560987,0.000001535299,0.0019092909,0.0000301024,0.0004355371],"genre_scores_gemma":[0.9961248,0.00014472284,0.00053773366,0.000014012251,0.000003752325,0.0000047118097,0.0029498031,0.000015101276,0.00020530185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999516,0.000008526866,0.0000047375315,0.000020373334,0.00000869331,0.0000059726194],"domain_scores_gemma":[0.9998118,0.00003472745,0.00007154604,0.000022443552,0.00004049262,0.000019018842],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024645223,0.00041192287,0.00016370241,0.0009809877,0.000097328724,0.00041654354,0.00012370985,0.00018903216,0.00045121],"category_scores_gemma":[0.00038406192,0.00015445893,0.0002794943,0.0011635665,0.00016160836,0.0003629695,0.0002855928,0.00014756467,0.00014474681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016406644,0.00001631819,0.94898444,0.00008764541,0.00031785094,0.00011041677,0.0001080587,0.010362043,0.026810803,0.00030390586,0.0004456829,0.01228866],"study_design_scores_gemma":[0.0000053379626,0.000017471071,0.99662554,0.0000043344103,0.000027838027,0.000028718936,0.000025927116,0.0015976335,0.0010325186,0.000090368274,0.00053937896,0.000004931458],"about_ca_topic_score_codex":0.0074482807,"about_ca_topic_score_gemma":0.0077835484,"teacher_disagreement_score":0.0074482807,"about_ca_system_score_codex":0.00041860872,"about_ca_system_score_gemma":0.00015703445,"threshold_uncertainty_score":0.014809847},"labels":[],"label_agreement":null},{"id":"W3127802927","doi":"10.1029/2020gb006709","title":"Molecular Signatures of Glacial Dissolved Organic Matter From Svalbard and Greenland","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Polar Research and Ecology","field":"Environmental Science","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Lethbridge","funders":"High Magnetic Field Laboratory, Chinese Academy of Sciences; Division of Chemistry; Division of Materials Research; National High Magnetic Field Laboratory; Nationale Geologiske Undersøgelser for Danmark og Grønland; Rijksuniversiteit Groningen; National Science Foundation","keywords":"Glacier; Meltwater; Glacial period; Geology; Greenland ice sheet; Arctic; Dissolved organic carbon; Physical geography; Oceanography; Geomorphology; Geography","score_opus":0.0051288056122676005,"score_gpt":0.22642946078213785,"score_spread":0.22130065516987024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127802927","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99915874,0.000112304566,0.000039946543,0.000006451763,0.0000018319539,0.000001785092,0.0004252606,0.00000711388,0.00024652484],"genre_scores_gemma":[0.99716717,0.00013409996,0.00028480968,0.000024004146,0.000003074031,0.0000037016364,0.0019784726,0.000008097526,0.00039658454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999136,0.000004390649,0.0000040378022,0.000031811367,0.000017740036,0.000028456358],"domain_scores_gemma":[0.99991846,0.000008210538,0.000020058647,0.0000038797925,0.00002196114,0.000027527218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011008726,0.00024556936,0.00023383909,0.001136935,0.00040427642,0.0006118888,0.00013045619,0.00017888498,0.00035084374],"category_scores_gemma":[0.00014689362,0.00011005651,0.0001510598,0.00066840637,0.0002182383,0.0001403853,0.00029444773,0.0001252503,0.00009520706],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026100592,0.00006898861,0.8400836,0.000043353422,0.000101390244,0.00033606734,0.00095429795,0.00028163716,0.14474751,0.00011485722,0.00036827044,0.01263902],"study_design_scores_gemma":[0.0000013104311,0.00001111939,0.99752575,0.0000026121202,0.000009297131,0.000040237774,0.00019752006,0.00018528696,0.0016952776,0.000010839718,0.0003189048,0.0000019295646],"about_ca_topic_score_codex":0.046959165,"about_ca_topic_score_gemma":0.08341135,"teacher_disagreement_score":0.046959165,"about_ca_system_score_codex":0.00059442443,"about_ca_system_score_gemma":0.00030036827,"threshold_uncertainty_score":0.09337163},"labels":[],"label_agreement":null},{"id":"W3130945207","doi":"10.1029/2021gb006976","title":"Glaciers and Nutrients in the Canadian Arctic Archipelago Marine System","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Geological Survey of Canada; University of British Columbia; University of Alberta","funders":"","keywords":"Meltwater; Glacier; Oceanography; Glacial period; Arctic; Ablation zone; Geology; Water column; Environmental science; Upwelling; Archipelago; Physical geography; Geomorphology; Geography","score_opus":0.012661859084833858,"score_gpt":0.20761347422017307,"score_spread":0.1949516151353392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3130945207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99363697,0.0006012999,0.000025918118,0.00022318738,0.00000888645,0.000007657531,0.0027962457,0.000008662782,0.0026912284],"genre_scores_gemma":[0.99814665,0.0003425412,0.00007131669,0.00004376214,0.0000031085394,0.000004013858,0.0008842645,0.0000023325354,0.00050204317],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980694,0.000012357951,0.000012343475,0.000033464014,0.000057149617,0.00007781989],"domain_scores_gemma":[0.99898475,0.000055420172,0.0001766609,0.000028426617,0.0005424658,0.00021231054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000239387,0.00019153555,0.0001888468,0.0017506168,0.0019424389,0.0011498585,0.00049890974,0.00023277203,0.001998068],"category_scores_gemma":[0.00096628786,0.00012776916,0.00028981856,0.0034723617,0.0005283875,0.0002577684,0.00058835413,0.0003233135,0.00012476681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027077858,0.000010946528,0.9945381,0.000024583975,0.000059959413,0.000051533152,0.0003628529,0.00030815418,0.0003614991,0.0001220245,0.00081035885,0.0033229145],"study_design_scores_gemma":[9.698182e-7,0.0000024235874,0.9988047,0.000008305906,0.0000080951195,0.000008524757,0.0005368698,0.00011891156,0.000019421517,0.0000153568,0.000473908,0.0000026308242],"about_ca_topic_score_codex":0.9903467,"about_ca_topic_score_gemma":0.9965965,"teacher_disagreement_score":0.010660002,"about_ca_system_score_codex":0.010660002,"about_ca_system_score_gemma":0.011085111,"threshold_uncertainty_score":0.07734412},"labels":[],"label_agreement":null},{"id":"W3132800685","doi":"10.1029/2020gb006659","title":"Permafrost Causes Unique Fine‐Scale Spatial Variability Across Tundra Soils","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Horizon 2020 Framework Programme; Vetenskapsrådet; Aurora Research Institute","keywords":"Permafrost; Tundra; Spatial variability; Landform; Terrain; Physical geography; Geology; Soil water; Spatial ecology; Soil carbon; Arctic; Soil map; Soil science; Environmental science; Hydrology (agriculture); Geomorphology; Geography; Ecology; Oceanography; Cartography","score_opus":0.022204675620256444,"score_gpt":0.2653880651217356,"score_spread":0.24318338950147914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3132800685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99954516,0.000048968483,0.000107758875,0.0000046108908,6.6407057e-7,0.0000010812131,0.00011670094,0.0000050792987,0.00016996865],"genre_scores_gemma":[0.99983406,0.00001192174,0.000038045586,0.0000030145382,8.127599e-7,6.98067e-7,0.00008662881,9.627153e-7,0.000023826853],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998636,0.00002836271,0.00001157022,0.00004382793,0.000023228073,0.000029408577],"domain_scores_gemma":[0.99964297,0.00006713442,0.00014736781,0.000043521813,0.000059289603,0.00003958521],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001559822,0.000116953015,0.00020234098,0.0007269189,0.0002840959,0.00039292197,0.00016337339,0.00014035734,0.00044222397],"category_scores_gemma":[0.0003711867,0.0000952096,0.00016959921,0.0009881698,0.0002928821,0.00013558748,0.00034608578,0.00011177347,0.00006154094],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016739703,0.00003109495,0.92817974,0.000030675852,0.000102451864,0.00053911546,0.0002576202,0.0006527835,0.06331097,0.00009321199,0.000079082034,0.0065558627],"study_design_scores_gemma":[5.4051236e-7,0.000007320707,0.99905986,0.0000011287527,0.000004228653,0.000106018815,0.00009457309,0.00019818675,0.00044938546,0.00002099708,0.00005648408,0.0000014019129],"about_ca_topic_score_codex":0.01483082,"about_ca_topic_score_gemma":0.016642582,"teacher_disagreement_score":0.01483082,"about_ca_system_score_codex":0.00027818553,"about_ca_system_score_gemma":0.0001614608,"threshold_uncertainty_score":0.02948898},"labels":[],"label_agreement":null},{"id":"W3134195618","doi":"10.1029/2020gb006871","title":"Pan‐Arctic Riverine Dissolved Organic Matter: Synchronous Molecular Stability, Shifting Sources and Subsidies","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Aurora College; University of Alberta","funders":"National Science Foundation","keywords":"Dissolved organic carbon; Arctic; Environmental science; Permafrost; Oceanography; Environmental chemistry; Chemistry; Geology","score_opus":0.014367796324315896,"score_gpt":0.22140327491749892,"score_spread":0.20703547859318303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134195618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99816555,0.00022744575,0.0003120396,0.000029522656,0.0000032857333,0.000001837897,0.0003928559,0.000011209662,0.00085627777],"genre_scores_gemma":[0.998985,0.00012309797,0.00032473993,0.000014375198,0.0000046628506,0.0000020155906,0.00027292955,0.000004716267,0.00026841438],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999311,0.0000065322747,0.000004447501,0.000027133401,0.000016510121,0.000014294057],"domain_scores_gemma":[0.9997565,0.000023722821,0.00007074556,0.000014349153,0.0001122731,0.000022324137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002547197,0.00012471483,0.00019178902,0.0005749829,0.0004838733,0.0005167405,0.00013428422,0.00012579406,0.0005050364],"category_scores_gemma":[0.0002522502,0.000083474864,0.00012534707,0.00057699764,0.00018434478,0.00020599582,0.0002861821,0.00015353326,0.00006986871],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030970084,0.00003392805,0.7996826,0.00007399106,0.000116608484,0.00014387422,0.0004516862,0.0008516006,0.17451611,0.00044079055,0.0002909839,0.023088198],"study_design_scores_gemma":[0.000002097131,0.000024204413,0.99240196,0.000004922328,0.000017114937,0.00005897836,0.00017716327,0.000810734,0.0051434776,0.000097847056,0.0012578535,0.0000037100624],"about_ca_topic_score_codex":0.015959647,"about_ca_topic_score_gemma":0.02853752,"teacher_disagreement_score":0.015959647,"about_ca_system_score_codex":0.00045258884,"about_ca_system_score_gemma":0.00028576088,"threshold_uncertainty_score":0.031733513},"labels":[],"label_agreement":null},{"id":"W3136175182","doi":"10.1029/2020gb006684","title":"Stable Carbon Isotopes Suggest Large Terrestrial Carbon Inputs to the Global Ocean","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Carbon cycle; Environmental science; Terrestrial ecosystem; Global change; Carbon fibers; Isotopes of carbon; Oceanography; Carbon flux; Ecosystem; Climate change; Total organic carbon; Geology; Ecology; Environmental chemistry; Chemistry","score_opus":0.005845379838190816,"score_gpt":0.2146534104998047,"score_spread":0.20880803066161388,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3136175182","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917407,0.00027614817,0.0022947765,0.00014873908,0.000010717398,0.0000054800385,0.0005739488,0.000075751464,0.0048737545],"genre_scores_gemma":[0.99886227,0.00007635067,0.0005678033,0.000036019337,0.0000025863358,0.0000025764073,0.0001996868,0.000007966261,0.00024463804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999473,0.000004102857,0.0000034133914,0.000022929467,0.000012256264,0.000009944754],"domain_scores_gemma":[0.9999056,0.000017533335,0.00002587871,0.0000107170745,0.000028665068,0.000011687597],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013209386,0.00028639092,0.00016187577,0.00041958308,0.00024342471,0.0006034439,0.00017718706,0.00041476268,0.0012077603],"category_scores_gemma":[0.00023925921,0.00019792814,0.00016879835,0.0005039323,0.00038299084,0.00033488846,0.00025906856,0.00019412207,0.00025523774],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015197502,0.000041487478,0.71915114,0.000059391805,0.000115265306,0.0001880848,0.00010028549,0.0065024304,0.25639316,0.0014445044,0.00045052034,0.015401817],"study_design_scores_gemma":[0.000029881436,0.000079046455,0.9449587,0.000017733075,0.0000837837,0.000170192,0.00024155709,0.019402636,0.030196613,0.0021675106,0.0026312734,0.00002113474],"about_ca_topic_score_codex":0.008153283,"about_ca_topic_score_gemma":0.011066267,"teacher_disagreement_score":0.008153283,"about_ca_system_score_codex":0.00036570505,"about_ca_system_score_gemma":0.00030988108,"threshold_uncertainty_score":0.016211689},"labels":[],"label_agreement":null},{"id":"W3138402703","doi":"10.1029/2020gb006759","title":"Deep Chlorophyll Maxima in the Global Ocean: Occurrences, Drivers and Characteristics","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":206,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"H2020 European Research Council; Fondation BNP Paribas; Agence Nationale de la Recherche","keywords":"Phytoplankton; Environmental science; Biogeochemical cycle; Argo; Chlorophyll a; Deep sea; Deep chlorophyll maximum; Oceanography; Particulate organic carbon; Biomass (ecology); Water column; Ocean color; Chlorophyll; Nutrient; Atmospheric sciences; Geology; Satellite; Ecology; Biology; Photic zone","score_opus":0.008335383128089102,"score_gpt":0.20477941332033006,"score_spread":0.19644403019224096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3138402703","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99826163,0.00028499615,0.00023740914,0.000020677997,0.0000017763867,0.0000037817006,0.0006811227,0.000011605712,0.0004969404],"genre_scores_gemma":[0.9988643,0.000140607,0.0002633632,0.000008404306,0.000004348412,0.0000041178687,0.00062587997,0.0000035070098,0.0000855082],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999162,0.000011182919,0.000009234399,0.000031199554,0.000013349732,0.000018913095],"domain_scores_gemma":[0.9997054,0.00004949985,0.00015556766,0.000025999328,0.000030964755,0.00003256133],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002625673,0.00017804537,0.00015492091,0.00094216614,0.00011486906,0.00039369042,0.00009473053,0.00015587783,0.00047774593],"category_scores_gemma":[0.00038407213,0.000092900926,0.00017845158,0.0013676324,0.00023947856,0.00036368385,0.0005036799,0.0001179761,0.00009894125],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023450364,0.00001481202,0.9881159,0.00003256198,0.000034386274,0.00003736327,0.0001523803,0.0003794093,0.0035290665,0.00009820825,0.0001191111,0.007463339],"study_design_scores_gemma":[4.0140267e-7,0.0000055778987,0.9993493,0.000002654969,0.0000039721704,0.00001963164,0.000095094285,0.00019545529,0.000070982016,0.000036619553,0.00021889995,0.0000014509566],"about_ca_topic_score_codex":0.0046283207,"about_ca_topic_score_gemma":0.0065868846,"teacher_disagreement_score":0.0046283207,"about_ca_system_score_codex":0.00018734511,"about_ca_system_score_gemma":0.00013407183,"threshold_uncertainty_score":0.009202778},"labels":[],"label_agreement":null},{"id":"W3149879777","doi":"10.1029/2020gb006887","title":"Nitrate Supply Routes and Impact of Internal Cycling in the North Atlantic Ocean Inferred From Nitrate Isotopic Composition","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Vlaamse regering; Vrije Universiteit Brussel; Ocean Frontier Institute; Fonds Wetenschappelijk Onderzoek; Dalhousie University; Belgian Federal Science Policy Office; Canada First Research Excellence Fund; Agence Nationale de la Recherche; Institut Français de Recherche pour l'Exploitation de la Mer","keywords":"Ocean gyre; Oceanography; Upwelling; Geology; Nitrate; Geotraces; North Atlantic Deep Water; Mode water; Water mass; Subtropics; Thermohaline circulation; Transect; Chemistry; Ecology","score_opus":0.0089669409905691,"score_gpt":0.2202990935343211,"score_spread":0.21133215254375198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3149879777","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990752,0.000045668196,0.00006831603,0.000015774785,0.00000248862,0.0000013055804,0.00020764924,0.000003554423,0.0005800005],"genre_scores_gemma":[0.9992749,0.000044346903,0.00012308978,0.000007759388,0.0000021464043,0.000001871115,0.00032807604,0.0000032007845,0.00021463165],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994695,0.000008054326,0.00000435759,0.000017225171,0.000012623303,0.000010680633],"domain_scores_gemma":[0.99983025,0.000029009656,0.00004578935,0.000013124751,0.00005477906,0.0000269583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015277475,0.00017462124,0.00014174359,0.00028789465,0.00024942294,0.00045437764,0.0001232228,0.00018450675,0.00063045823],"category_scores_gemma":[0.00037478743,0.00015351379,0.00018547705,0.00024303049,0.00015019358,0.00024421394,0.0003352044,0.00014677251,0.0001250689],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000110987356,0.000014774651,0.9762131,0.000013481177,0.000047744674,0.00005702438,0.000102871236,0.00059287855,0.01899672,0.00004941133,0.00007571979,0.003725181],"study_design_scores_gemma":[0.0000022086656,0.000013510903,0.99818856,0.0000031678492,0.000009738158,0.000010586287,0.000078099685,0.0010482145,0.0004503867,0.000016807699,0.00017636394,0.0000024566405],"about_ca_topic_score_codex":0.049851704,"about_ca_topic_score_gemma":0.11355456,"teacher_disagreement_score":0.049851704,"about_ca_system_score_codex":0.00039831025,"about_ca_system_score_gemma":0.00033099073,"threshold_uncertainty_score":0.09912312},"labels":[],"label_agreement":null},{"id":"W3163425839","doi":"10.1029/2021gb007000","title":"Improved Constraints on Global Methane Emissions and Sinks Using <i>δ</i><sup>13</sup>C‐CH<sub>4</sub>","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":186,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Sink (geography); Environmental science; Methane; Atmospheric sciences; Fractionation; Troposphere; Atmospheric chemistry; Fossil fuel; TRACER; Emission inventory; Atmospheric methane; Chemistry; Environmental chemistry; Meteorology; Physics; Air quality index; Ozone; Nuclear physics; Geography","score_opus":0.008675041421469017,"score_gpt":0.2258847754929056,"score_spread":0.21720973407143657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3163425839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9542783,0.00018594376,0.036434032,0.00043164458,0.00003032876,0.00002140856,0.0028570958,0.000289264,0.005471945],"genre_scores_gemma":[0.99604946,0.00004789609,0.0027465408,0.000040957264,0.000008205338,0.000014474136,0.00083463185,0.000045984456,0.00021191455],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985385,0.000051960495,0.000008080086,0.00003473414,0.000017568247,0.00003376252],"domain_scores_gemma":[0.9993088,0.00039683428,0.0000987624,0.000071603,0.000078866724,0.000045122248],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009155584,0.0010070835,0.00047314953,0.00046026052,0.00030899164,0.00066595356,0.0010722986,0.00077829027,0.0022866246],"category_scores_gemma":[0.0022522511,0.0005826076,0.0010233124,0.0005446442,0.00042749758,0.0013705101,0.00064714346,0.000493833,0.00022824842],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011189787,0.000029528024,0.017518695,0.000031072886,0.000049583443,0.000068664864,0.000016036021,0.97476757,0.0027555502,0.0027295486,0.0002663081,0.0016554862],"study_design_scores_gemma":[0.00005836829,0.000030865296,0.0061117695,0.000011791813,0.00003097103,0.000012319813,0.000026184845,0.98866034,0.0017984932,0.002736365,0.0005021721,0.000020433466],"about_ca_topic_score_codex":0.03286384,"about_ca_topic_score_gemma":0.014867253,"teacher_disagreement_score":0.03286384,"about_ca_system_score_codex":0.0013187132,"about_ca_system_score_gemma":0.0012416253,"threshold_uncertainty_score":0.06534511},"labels":[],"label_agreement":null},{"id":"W3163953034","doi":"10.1029/2021gb006954","title":"Soil Microbial Community Response to Permafrost Degradation in Palsa Fields of the Hudson Bay Lowlands: Implications for Greenhouse Gas Production in a Warming Climate","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Forest Research Institute; Ministry of Natural Resources and Forestry; Université Laval; Center for Northern Studies; Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Peat; Permafrost; Thermokarst; Environmental science; Greenhouse gas; Methanogenesis; Methane; Soil science; Hydrology (agriculture); Ecology; Geology; Oceanography","score_opus":0.03572326640818165,"score_gpt":0.27411367127854613,"score_spread":0.23839040487036448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3163953034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998497,0.000019354391,0.000013624621,0.0000032384773,3.259188e-7,0.0000011625021,0.00006247507,7.428046e-7,0.000049385428],"genre_scores_gemma":[0.99968934,0.000022551762,0.000039266357,0.0000067991045,0.0000011469945,0.00000303975,0.00013475682,4.823041e-7,0.000102641825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999211,0.000010140989,0.0000050727267,0.000024792962,0.000013822134,0.000024994184],"domain_scores_gemma":[0.9998042,0.000025375135,0.000053663247,0.0000067511264,0.0000357355,0.000074248266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016530282,0.00021603922,0.00022054727,0.00053421553,0.0003321955,0.00056614354,0.0001640548,0.00015636551,0.000756797],"category_scores_gemma":[0.00017991131,0.00014564146,0.0001655825,0.00035800872,0.00032854386,0.00022856354,0.00031827405,0.00015107032,0.0000729548],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032062386,0.00007169077,0.9171621,0.000045913737,0.000060539995,0.00016177673,0.00085988484,0.0003107765,0.0773697,0.000030601892,0.000057053338,0.0035492552],"study_design_scores_gemma":[0.0000019330541,0.00003542233,0.9988286,0.0000013268315,0.0000044144867,0.000015725356,0.0004060034,0.00012726798,0.0005379495,0.000005097487,0.0000351684,0.0000011572686],"about_ca_topic_score_codex":0.043484155,"about_ca_topic_score_gemma":0.056640893,"teacher_disagreement_score":0.95651585,"about_ca_system_score_codex":0.0006602313,"about_ca_system_score_gemma":0.00038161592,"threshold_uncertainty_score":0.08646208},"labels":[],"label_agreement":null},{"id":"W3165173431","doi":"10.1029/2020gb006888","title":"Year‐2020 Global Distribution and Pathways of Reservoir Methane and Carbon Dioxide Emissions According to the Greenhouse Gas From Reservoirs (G‐res) Model","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":134,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Division of Environmental Biology; Society for Mathematical Biology; Stanford University; Groupe de recherche interuniversitaire en limnologie; National Science Foundation","keywords":"Greenhouse gas; Environmental science; Carbon dioxide; Flux (metallurgy); Methane; Atmospheric sciences; Global warming; Subtropics; Carbon cycle; Climate change; Ecosystem; Geology; Chemistry; Oceanography; Ecology","score_opus":0.01090606585629794,"score_gpt":0.22364550028529095,"score_spread":0.212739434428993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3165173431","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92502046,0.0005100588,0.022921197,0.0009176891,0.00010751135,0.000055951696,0.030150205,0.0014038937,0.018913131],"genre_scores_gemma":[0.97874326,0.00023657986,0.004645023,0.000120563454,0.000013385711,0.00006943306,0.013804385,0.00009738884,0.0022699388],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990416,0.000024607629,0.000003983559,0.000030981195,0.000012881596,0.000023488983],"domain_scores_gemma":[0.99979264,0.00006526467,0.000032385567,0.000026235763,0.0000607142,0.000022795199],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044217083,0.00061512674,0.00036216894,0.00050780666,0.00021426292,0.0005793375,0.00082285394,0.00075954356,0.003674001],"category_scores_gemma":[0.00086142746,0.00027995196,0.0008745456,0.0009447721,0.00030575675,0.00083903334,0.00039395734,0.00041475377,0.00063429226],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009792006,0.000019794237,0.00920361,0.000032402466,0.00008668108,0.00004981028,0.000014155939,0.9834553,0.0006393209,0.0016486857,0.00207905,0.002673205],"study_design_scores_gemma":[0.00005193624,0.000034096982,0.0070793917,0.000013351845,0.000040294442,0.000037681784,0.00003875315,0.9874057,0.0005990814,0.002166081,0.0025099437,0.00002360307],"about_ca_topic_score_codex":0.038369548,"about_ca_topic_score_gemma":0.022619495,"teacher_disagreement_score":0.038369548,"about_ca_system_score_codex":0.0009227396,"about_ca_system_score_gemma":0.00074512773,"threshold_uncertainty_score":0.076292396},"labels":[],"label_agreement":null},{"id":"W3170594992","doi":"10.1029/2020gb006796","title":"Unravelling Surface Seawater DMS Concentration and Sea‐To‐Air Flux Changes After Sea Ice Retreat in the Western Arctic Ocean","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Chinese Arctic and Antarctic Administration; China Scholarship Council; National Natural Science Foundation of China; Ministry of Natural Resources of the People's Republic of China","keywords":"Sea ice; Oceanography; Seawater; Arctic; Environmental science; Arctic ice pack; Arctic sea ice decline; Arctic geoengineering; Phytoplankton; Nutrient; Biogeochemical cycle; Geology; Antarctic sea ice; Chemistry; Environmental chemistry","score_opus":0.0097467117003628,"score_gpt":0.214899705320824,"score_spread":0.2051529936204612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3170594992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993006,0.00013886354,0.000042183547,0.000025026959,0.0000037372852,0.0000015357942,0.0002476729,0.0000045898996,0.00023583983],"genre_scores_gemma":[0.9992537,0.000108819695,0.00009408207,0.000015999145,0.0000049447976,0.0000027185924,0.00035114767,0.0000021857675,0.00016630648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999559,0.0000047794692,0.0000033156468,0.00001282963,0.000008049292,0.000015061697],"domain_scores_gemma":[0.9998785,0.000012001074,0.000030718496,0.0000064429646,0.000045368746,0.000026907459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022980648,0.0002946856,0.00030020336,0.0006068309,0.00040062884,0.00059008243,0.00013433903,0.00025827566,0.0004603173],"category_scores_gemma":[0.00019803667,0.00014004837,0.00023711723,0.0005927817,0.0002426068,0.00033497054,0.0002754285,0.0002593842,0.00008852804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027505518,0.000053047985,0.95779794,0.000035208202,0.0001230962,0.00017683473,0.00032815058,0.0006928907,0.033823296,0.000063842774,0.00022133703,0.0064092525],"study_design_scores_gemma":[0.000001600472,0.00001246836,0.99839646,0.0000025296658,0.000010220126,0.000010461522,0.00016333855,0.00050154014,0.0006642706,0.000010968474,0.00022392241,0.0000022871984],"about_ca_topic_score_codex":0.13740435,"about_ca_topic_score_gemma":0.16551068,"teacher_disagreement_score":0.13740435,"about_ca_system_score_codex":0.0008509216,"about_ca_system_score_gemma":0.00066141906,"threshold_uncertainty_score":0.27320915},"labels":[],"label_agreement":null},{"id":"W3171214386","doi":"10.1029/2020gb006829","title":"Anthropogenic and Climatic Contributions to Observed Carbon System Trends in the Northeast Pacific","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Fisheries and Oceans Canada; University of British Columbia","funders":"Marine Environmental Observation Prediction and Response Network","keywords":"Oceanography; Thermocline; Environmental science; Salinity; Dissolved organic carbon; Hydrography; Ocean acidification; Remineralisation; Aragonite; Pacific decadal oscillation; Water column; Subarctic climate; Seawater; Sea surface temperature; Geology; Chemistry; Calcite; Mineralogy","score_opus":0.015806376081682363,"score_gpt":0.25245688451561904,"score_spread":0.23665050843393667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3171214386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986324,0.00014040514,0.000086124914,0.00005973783,0.0000055663963,0.000001794003,0.00066667795,0.0000074524987,0.000399724],"genre_scores_gemma":[0.99938285,0.00007930861,0.00005965481,0.000009669748,0.0000062976887,0.0000019384956,0.00040494767,0.0000020627547,0.00005327916],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986553,0.000025799583,0.000019705796,0.00004453268,0.000027931777,0.000016563177],"domain_scores_gemma":[0.9991085,0.0001271885,0.0004273728,0.00007613925,0.00017949389,0.000081347556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041409637,0.00015820345,0.00010790973,0.00053321314,0.00019699447,0.0005329118,0.00017210422,0.00014652863,0.00077262765],"category_scores_gemma":[0.0012752588,0.00011139435,0.00019829346,0.0012161429,0.00028662718,0.00024488688,0.00030048657,0.00020163071,0.0000659068],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018883251,0.0000064090177,0.99704915,0.00001273612,0.000055430977,0.000023788785,0.00006320317,0.00024332943,0.0010021047,0.000038250342,0.00006710783,0.0014195446],"study_design_scores_gemma":[4.912724e-7,0.000002762642,0.99952424,0.0000014033244,0.0000042813367,0.000009083735,0.00003120988,0.00027210437,0.000050430728,0.000011921071,0.000091120855,9.117979e-7],"about_ca_topic_score_codex":0.041223377,"about_ca_topic_score_gemma":0.059591036,"teacher_disagreement_score":0.041223377,"about_ca_system_score_codex":0.000488524,"about_ca_system_score_gemma":0.000504872,"threshold_uncertainty_score":0.08196688},"labels":[],"label_agreement":null},{"id":"W3179895477","doi":"10.1029/2021gb006979","title":"Probing the Bioavailability of Dissolved Iron to Marine Eukaryotic Phytoplankton Using In Situ Single Cell Iron Quotas","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"H2020 European Research Council; Natural Environment Research Council; Israel Science Foundation; National Science Foundation; German-Israeli Foundation for Scientific Research and Development; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Sight Research UK","keywords":"Bioavailability; Phytoplankton; Environmental chemistry; In situ; Chemistry; Nutrient; Oceanography; Ecology; Biology; Geology; Bioinformatics","score_opus":0.013888768143549952,"score_gpt":0.21239350575016297,"score_spread":0.19850473760661302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3179895477","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97750443,0.00046314648,0.019048829,0.000049811795,0.00001791445,0.000024247614,0.001655176,0.00008558472,0.0011506896],"genre_scores_gemma":[0.9846489,0.00021728656,0.0134306075,0.000045601064,0.000009188133,0.000051566098,0.00082448026,0.000024706553,0.00074772624],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99972016,0.000021718892,0.000016361275,0.00014460692,0.00007264002,0.000024479432],"domain_scores_gemma":[0.99965036,0.000103646846,0.000078382596,0.00004497126,0.000088675144,0.000033932138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032606005,0.0003399706,0.0005751791,0.0005488877,0.0003325881,0.0005656829,0.00042199288,0.0004761016,0.0006731456],"category_scores_gemma":[0.00060984964,0.00026706158,0.0003374215,0.0004067867,0.0002742258,0.0004943353,0.0004980393,0.00046092502,0.0002992809],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010962147,0.00001913389,0.026285533,0.000102044636,0.000036295718,0.000039762283,0.00012264452,0.0011081991,0.96719587,0.00007836579,0.00005608268,0.0048463875],"study_design_scores_gemma":[0.00001442049,0.0003643706,0.23186105,0.000019013783,0.00010782854,0.00028419512,0.00039480918,0.035478063,0.727963,0.00045063221,0.003005728,0.000056925575],"about_ca_topic_score_codex":0.00469179,"about_ca_topic_score_gemma":0.007790479,"teacher_disagreement_score":0.00469179,"about_ca_system_score_codex":0.00060815737,"about_ca_system_score_gemma":0.00023844508,"threshold_uncertainty_score":0.009328961},"labels":[],"label_agreement":null},{"id":"W3180510126","doi":"10.1029/2020gb006916","title":"Continental and Ecoregion‐Specific Drivers of Atmospheric NO<sub>2</sub> and NH<sub>3</sub> Seasonality Over Africa Revealed by Satellite Observations","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Goddard Space Flight Center; Universities Space Research Association; National Aeronautics and Space Administration","keywords":"Seasonality; Environmental science; Ecoregion; Precipitation; Atmospheric sciences; Ecology; Meteorology; Geography; Geology","score_opus":0.007703786431442882,"score_gpt":0.18795655724614818,"score_spread":0.1802527708147053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3180510126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99925345,0.00008498502,0.00004757281,0.000020903202,0.0000015107379,0.0000018252703,0.00037238566,0.0000026767607,0.00021461639],"genre_scores_gemma":[0.99953294,0.000063106985,0.00007372026,0.000006635734,0.0000026977812,0.000002947885,0.0002631613,0.000002074262,0.000052783053],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998976,0.00002484881,0.0000065902664,0.00003055255,0.000010021537,0.000030420699],"domain_scores_gemma":[0.9995596,0.000065347725,0.00023400312,0.000031146756,0.000053612475,0.000056306508],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021423676,0.00016273113,0.00016718709,0.0005362309,0.00017752004,0.00043588044,0.0001569882,0.00014068803,0.0007039],"category_scores_gemma":[0.0005378992,0.00015067354,0.00023639823,0.00091877417,0.00022951678,0.00029538939,0.0003278189,0.00013768482,0.000103217215],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005050176,0.000008407902,0.9925113,0.00001784845,0.000103385886,0.00006893733,0.00022932327,0.0003628596,0.0040103216,0.000054237084,0.00014355186,0.0024394533],"study_design_scores_gemma":[9.270315e-7,0.000002820251,0.9993356,0.000003448603,0.000008807902,0.000012178275,0.00014682626,0.00027158353,0.00007699792,0.000007790729,0.0001318157,0.000001321118],"about_ca_topic_score_codex":0.031338245,"about_ca_topic_score_gemma":0.04683512,"teacher_disagreement_score":0.031338245,"about_ca_system_score_codex":0.00023698682,"about_ca_system_score_gemma":0.00015512845,"threshold_uncertainty_score":0.06231165},"labels":[],"label_agreement":null},{"id":"W3181673049","doi":"10.1029/2020gb006774","title":"Global Uptake of Atmospheric Methane by Soil From 1900 to 2100","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Natural Environment Research Council; European Commission; Natural Sciences and Engineering Research Council of Canada; Horizon 2020 Framework Programme; Consejo Nacional de Ciencia y Tecnología; Sight Research UK","keywords":"Sink (geography); Environmental science; Atmospheric sciences; Methane; Northern Hemisphere; Global change; Environmental chemistry; Climate change; Hydrology (agriculture); Ecology; Chemistry; Biology; Geology","score_opus":0.005212761202288177,"score_gpt":0.21319831345184587,"score_spread":0.2079855522495577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3181673049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99049604,0.00024939064,0.0006981905,0.00021968363,0.000032932203,0.0000068503427,0.0063177934,0.0001441284,0.0018349959],"genre_scores_gemma":[0.9956006,0.00012726735,0.00035905535,0.000041076193,0.000008268245,0.000010086844,0.0036718894,0.00001886666,0.00016289575],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999099,0.000013330996,0.000005653222,0.000037460442,0.0000116693045,0.000022006825],"domain_scores_gemma":[0.9998846,0.000026940592,0.00002285337,0.000013363296,0.000025829198,0.000026300455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002908813,0.00074257865,0.00029406534,0.0004349679,0.00023246177,0.00039438214,0.0003933048,0.0006423861,0.0014533568],"category_scores_gemma":[0.000506507,0.0003492188,0.0010294748,0.0005373734,0.00029684216,0.0006331804,0.00043657218,0.0003916509,0.00027654416],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006080893,0.00014630318,0.395667,0.00029198753,0.0006241755,0.00034919466,0.0001144564,0.5721765,0.013440272,0.0017948468,0.0038512489,0.010935895],"study_design_scores_gemma":[0.00028646522,0.0003797397,0.6032839,0.00006512877,0.0003484405,0.00020481272,0.00022534255,0.3803827,0.0067776195,0.0017584023,0.006162618,0.00012494883],"about_ca_topic_score_codex":0.039997835,"about_ca_topic_score_gemma":0.01528028,"teacher_disagreement_score":0.039997835,"about_ca_system_score_codex":0.0014019782,"about_ca_system_score_gemma":0.0005819338,"threshold_uncertainty_score":0.07953006},"labels":[],"label_agreement":null},{"id":"W3181866418","doi":"10.1029/2021gb006953","title":"Gradients of Anthropogenic Nutrient Enrichment Alter N Composition and DOM Stoichiometry in Freshwater Ecosystems","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"New Hampshire Agricultural Experiment Station; Natural Environment Research Council; Sight Research UK; U.S. Department of Agriculture; National Institute of Food and Agriculture; National Science Foundation","keywords":"Dissolved organic carbon; Biogeochemical cycle; Nutrient; Environmental chemistry; Ecological stoichiometry; Chemistry; Ecosystem; Biome; Organic matter; Biogeochemistry; Composition (language); Ecology; Biology","score_opus":0.006274254686377587,"score_gpt":0.226872153535671,"score_spread":0.22059789884929343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3181866418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990507,0.000107137814,0.00021484292,0.000019246801,0.0000020441182,0.0000024725816,0.00016447321,0.000009730762,0.00042932457],"genre_scores_gemma":[0.99941194,0.000069082795,0.00025937482,0.00002804009,0.0000017082914,0.000003423767,0.0001425768,0.0000027138988,0.00008116315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998536,0.000023571205,0.000018671233,0.000050796578,0.00002840823,0.000024910401],"domain_scores_gemma":[0.9997924,0.00003099138,0.00008148503,0.000014650941,0.00005261972,0.000027835762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024010085,0.0001604312,0.00021536567,0.0005734015,0.00034449404,0.00046226743,0.00019525665,0.00021741235,0.00048652824],"category_scores_gemma":[0.00040771047,0.00012869209,0.00018135202,0.00054153445,0.00043175253,0.00039050687,0.00062438933,0.00012027861,0.000074605225],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014873804,0.000036105754,0.8107984,0.00009847733,0.00015678898,0.00013719649,0.00020488161,0.0013169626,0.17783265,0.00022012745,0.00015428623,0.008895388],"study_design_scores_gemma":[0.0000023075831,0.00003035077,0.9954816,0.000004288138,0.00001254606,0.00004158206,0.00017273627,0.00085797446,0.0027946604,0.00012576002,0.00046930768,0.0000067611177],"about_ca_topic_score_codex":0.008135807,"about_ca_topic_score_gemma":0.015510978,"teacher_disagreement_score":0.008135807,"about_ca_system_score_codex":0.0005722004,"about_ca_system_score_gemma":0.00035010366,"threshold_uncertainty_score":0.01617688},"labels":[],"label_agreement":null},{"id":"W3196863676","doi":"10.1029/2020gb006901","title":"Isoscape Models of the Southern Ocean: Predicting Spatial and Temporal Variability in Carbon and Nitrogen Isotope Compositions of Particulate Organic Matter","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Isotope Analysis in Ecology","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Tula Foundation; University of British Columbia; Fisheries and Oceans Canada","funders":"H2020 Marie Skłodowska-Curie Actions; Division of Grants and Agreements; Natural Sciences and Engineering Research Council of Canada; Hakai Institute; G. Unger Vetlesen Foundation; Bundesministerium für Bildung und Frauen; University of British Columbia; Ministry of Business, Innovation and Employment; Agence Nationale de la Recherche","keywords":"Environmental science; Biogeochemical cycle; Spatial variability; Trophic level; Oceanography; Spatial ecology; Ecology; Ecosystem; Food web; Biology; Geology","score_opus":0.0054700540281154,"score_gpt":0.2016013804802119,"score_spread":0.1961313264520965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3196863676","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98117226,0.000051747447,0.01792082,0.000076609314,0.000006402446,0.0000066185203,0.00019119815,0.00012248543,0.00045179605],"genre_scores_gemma":[0.9955532,0.000018895798,0.003919074,0.000014409698,0.000004317088,0.000008457399,0.00026436485,0.000009075784,0.00020824495],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998815,0.000034326702,0.000006129655,0.0000469767,0.000015439518,0.000015571508],"domain_scores_gemma":[0.999419,0.0002980957,0.00011182897,0.000038652255,0.000065909044,0.0000665026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008600303,0.00036151233,0.00039669353,0.0005702619,0.00027295915,0.0005514683,0.000772476,0.00049199193,0.0005965971],"category_scores_gemma":[0.0019517378,0.0003211664,0.0006785066,0.00033463188,0.00051495706,0.0004265251,0.0005733723,0.0005147073,0.00010702352],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057269863,0.000033331988,0.037635475,0.000005588484,0.000041153857,0.000023485578,0.000019379124,0.9581848,0.00059822696,0.00036825004,0.00009184213,0.0029413078],"study_design_scores_gemma":[0.0000034433226,0.000006047711,0.0019456027,6.77038e-7,0.0000024487147,0.0000021939961,0.000004377487,0.9977265,0.00005616424,0.00023256797,0.000018570809,0.0000013132097],"about_ca_topic_score_codex":0.049090542,"about_ca_topic_score_gemma":0.032645565,"teacher_disagreement_score":0.049090542,"about_ca_system_score_codex":0.0009103544,"about_ca_system_score_gemma":0.0007487829,"threshold_uncertainty_score":0.09760958},"labels":[],"label_agreement":null},{"id":"W3200228180","doi":"10.1029/2021gb007058","title":"Canadian Arctic Archipelago Shelf‐Ocean Interactions: A Major Iron Source to Pacific Derived Waters Transiting to the Atlantic","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia; Canada Foundation for Innovation","keywords":"Oceanography; Archipelago; Arctic; Bay; Geology; Continental shelf; Sediment; Sound (geography); Arctic dipole anomaly; Environmental science; Arctic ice pack; Paleontology","score_opus":0.007033598152376813,"score_gpt":0.19489032247647978,"score_spread":0.18785672432410297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3200228180","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99112844,0.00045861964,0.00012114673,0.00023288127,0.000014621178,0.000011772493,0.002128431,0.000011323936,0.00589272],"genre_scores_gemma":[0.9966948,0.0003292951,0.00024487966,0.000051422954,0.0000029863945,0.0000053482554,0.00075915223,0.000004542357,0.0019075333],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988496,0.00000465386,0.0000033448805,0.000025323418,0.000032283588,0.000049427363],"domain_scores_gemma":[0.9997466,0.000009479794,0.000023199742,0.000005486856,0.00015826321,0.000056952096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000114702256,0.00031229024,0.0002019678,0.0008177855,0.0023897043,0.0009089845,0.00034234172,0.00023538143,0.0020325389],"category_scores_gemma":[0.00031448563,0.00014378662,0.00022184006,0.0013450262,0.0003139042,0.00019280976,0.00041337562,0.0002664662,0.00013310449],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022681897,0.00003203705,0.96638966,0.00007565613,0.00009495026,0.00031144483,0.0006339381,0.0013711783,0.011287565,0.0006128982,0.0025041483,0.016459752],"study_design_scores_gemma":[0.000005209677,0.000009987943,0.99412715,0.000015094783,0.00003002772,0.000037103164,0.00097554334,0.00078150677,0.00058110175,0.00005179861,0.003376953,0.000008493472],"about_ca_topic_score_codex":0.98628366,"about_ca_topic_score_gemma":0.99387145,"teacher_disagreement_score":0.01371634,"about_ca_system_score_codex":0.009002718,"about_ca_system_score_gemma":0.010095332,"threshold_uncertainty_score":0.0653196},"labels":[],"label_agreement":null},{"id":"W3208309832","doi":"10.1029/2021gb006977","title":"Iron Isotope Biogeochemical Cycling in the Western Arctic Ocean","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geotraces; Biogeochemical cycle; Oceanography; Arctic; Seawater; Canada Basin; Geology; Continental shelf; Cycling; Geochemical cycle; Transect; Environmental chemistry; Geochemistry; Chemistry","score_opus":0.01878924117156074,"score_gpt":0.26208525134095256,"score_spread":0.2432960101693918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3208309832","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99787045,0.0002780212,0.00010174136,0.000021882495,0.000007045641,0.0000026549694,0.00033213114,0.000008358189,0.001377715],"genre_scores_gemma":[0.9979584,0.00029930795,0.0005051581,0.000028466664,0.000008785252,0.000004059446,0.00055865134,0.000006859484,0.00063023175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999031,0.000008887457,0.00000888611,0.000034039684,0.00002609761,0.000018892799],"domain_scores_gemma":[0.9998374,0.000007429964,0.000038144462,0.000005185576,0.000094000745,0.000017812426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022634478,0.00033150832,0.00021101903,0.0009669519,0.0007285356,0.000701759,0.00012206711,0.000142347,0.00031451831],"category_scores_gemma":[0.0001772229,0.00014712912,0.0001677119,0.0008068021,0.00020014547,0.00019208605,0.00036891236,0.00014062539,0.00012210448],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017758504,0.00002758478,0.91233814,0.000054057065,0.000120932484,0.00023268812,0.000579543,0.00068629184,0.07147407,0.00011168629,0.0002633633,0.013933945],"study_design_scores_gemma":[0.0000024196831,0.000026337364,0.9949008,0.000013817827,0.000023554192,0.00006379794,0.0003803055,0.00052518136,0.0023354415,0.00002389037,0.0016989793,0.000005333011],"about_ca_topic_score_codex":0.19926842,"about_ca_topic_score_gemma":0.2698898,"teacher_disagreement_score":0.19926842,"about_ca_system_score_codex":0.00084496394,"about_ca_system_score_gemma":0.00076451123,"threshold_uncertainty_score":0.39621705},"labels":[],"label_agreement":null},{"id":"W3215516198","doi":"10.1029/2020gb006922","title":"Characterizing Methane Emission Hotspots From Thawing Permafrost","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Global Institute for Water Security; University of Alberta; University of Saskatchewan","funders":"U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Permafrost; Thermokarst; Hotspot (geology); Arctic; Environmental science; Wetland; Methane; Physical geography; Atmospheric sciences; Hydrology (agriculture); Geology; Oceanography; Ecology; Geography","score_opus":0.03019062143145999,"score_gpt":0.2569550017366986,"score_spread":0.22676438030523863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3215516198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996835,0.000018503712,0.00009058497,0.0000014076431,2.416856e-7,9.525235e-7,0.000069011076,0.0000041677745,0.00013163403],"genre_scores_gemma":[0.9995852,0.000017386028,0.00015156013,0.0000021911833,7.2849076e-7,0.0000015776706,0.00015549142,0.0000013259194,0.00008442786],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997544,0.0000018883313,0.0000010695937,0.000008687135,0.0000054989773,0.000007478687],"domain_scores_gemma":[0.99994946,0.000008294801,0.00001853743,0.0000029856412,0.00000991504,0.000010759051],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000055828306,0.00010574412,0.00009198346,0.00046066364,0.00023864499,0.00021855692,0.00009770655,0.00010655407,0.0005597298],"category_scores_gemma":[0.0000863532,0.00009444875,0.000084102474,0.0003314492,0.00011681915,0.000121561,0.00018041463,0.00005964092,0.000071381844],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001313645,0.000016100004,0.9234138,0.000024322873,0.000026940404,0.00021349503,0.00042287182,0.0007966174,0.068700485,0.00004391775,0.00008533423,0.006124639],"study_design_scores_gemma":[8.875285e-7,0.000013301501,0.99619055,0.0000018199705,0.0000063153543,0.00006901757,0.00016965659,0.00086699054,0.0025353276,0.000015203155,0.000128961,0.0000018263306],"about_ca_topic_score_codex":0.0073321783,"about_ca_topic_score_gemma":0.017253503,"teacher_disagreement_score":0.0073321783,"about_ca_system_score_codex":0.00014451843,"about_ca_system_score_gemma":0.00009088235,"threshold_uncertainty_score":0.014578998},"labels":[],"label_agreement":null},{"id":"W4200279109","doi":"10.1029/2021gb007032","title":"The Changing CO<sub>2</sub>Sink in the Western Arctic Ocean From 1994 to 2019","year":2021,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Sea ice; Arctic sea ice decline; Arctic; Arctic geoengineering; Oceanography; Sink (geography); Arctic ice pack; Environmental science; Biogeochemical cycle; Canada Basin; Climatology; Pelagic zone; Sea ice thickness; Geology; Geography; Chemistry","score_opus":0.007994614286876861,"score_gpt":0.21661047016527918,"score_spread":0.2086158558784023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200279109","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982267,0.000078952806,0.00018262681,0.00006206919,0.0000048311763,0.0000024968742,0.000942324,0.0000177289,0.00048213362],"genre_scores_gemma":[0.99861395,0.0000583121,0.00020793753,0.00001578973,0.0000030722144,0.000003083139,0.0008959224,0.000003766203,0.00019814061],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999145,0.00000954422,0.00000628905,0.000030140522,0.000017935223,0.000021567117],"domain_scores_gemma":[0.999793,0.000018459277,0.00005180539,0.000013770618,0.00010408551,0.000018862673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002447641,0.0002944755,0.00018877134,0.000470701,0.0002890699,0.0005986257,0.00020346363,0.00031340573,0.00048298345],"category_scores_gemma":[0.00033770438,0.0001276351,0.0003181803,0.0006629119,0.00019647185,0.0005038862,0.00021396097,0.00018327429,0.00012003238],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000344876,0.000049832768,0.9637349,0.000057760397,0.00014532004,0.00023324927,0.00014339708,0.012251998,0.010760013,0.00024453737,0.0006843686,0.011349757],"study_design_scores_gemma":[0.000003457432,0.000021500518,0.98657656,0.0000067138517,0.000037456284,0.000031457093,0.0001362833,0.010995733,0.001408421,0.000045737248,0.0007255612,0.000011158747],"about_ca_topic_score_codex":0.3012424,"about_ca_topic_score_gemma":0.3138618,"teacher_disagreement_score":0.3012424,"about_ca_system_score_codex":0.001865331,"about_ca_system_score_gemma":0.000938525,"threshold_uncertainty_score":0.598978},"labels":[],"label_agreement":null},{"id":"W4206125224","doi":"10.1029/2021gb007178","title":"Partitioning the Export of Distinct Biogenic Carbon Pools in the Northeast Pacific Ocean Using a Biogeochemical Profiling Float","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization","funders":"National Oceanic and Atmospheric Administration; Fisheries and Oceans Canada; David and Lucile Packard Foundation","keywords":"Biogeochemical cycle; Environmental science; Carbon cycle; Dissolved organic carbon; Primary production; Biogeochemistry; Particulates; Oceanography; Cycling; Total organic carbon; Biological pump; Geochemical cycle; Atmospheric sciences; Environmental chemistry; Ecosystem; Chemistry; Geology; Ecology; Biology","score_opus":0.016034716012605366,"score_gpt":0.21761906484603255,"score_spread":0.20158434883342718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206125224","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991335,0.000011409366,0.0006160723,0.000004919937,7.8728226e-7,0.000005313383,0.000081102866,0.000008321812,0.00013850706],"genre_scores_gemma":[0.9955264,0.000025914384,0.0039062668,0.0000130336775,0.0000025667525,0.000013058897,0.00029752342,0.000006112771,0.00020908707],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994254,0.000007507797,0.0000028180402,0.0000246925,0.000014098992,0.000008321444],"domain_scores_gemma":[0.99982774,0.00003869935,0.000048645146,0.000014175648,0.00003810722,0.000032616474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002386955,0.00030920558,0.00018830359,0.00047068507,0.00032119302,0.0003148411,0.00025694468,0.00020179397,0.0002854899],"category_scores_gemma":[0.0003664421,0.00023467446,0.00021945316,0.00025544857,0.00014452201,0.0004183434,0.0002325185,0.00010234757,0.000063578],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018559545,0.00011116654,0.8011274,0.000029189001,0.00010670776,0.00011898753,0.00036300241,0.005443222,0.17343116,0.000089093075,0.00014978679,0.018844765],"study_design_scores_gemma":[0.000009019581,0.00011587101,0.9534946,0.0000059776457,0.00002787816,0.000044346216,0.00011188174,0.040289152,0.0056113326,0.000040620045,0.00023623825,0.000013147967],"about_ca_topic_score_codex":0.02770633,"about_ca_topic_score_gemma":0.042089816,"teacher_disagreement_score":0.02770633,"about_ca_system_score_codex":0.00048025098,"about_ca_system_score_gemma":0.00026897553,"threshold_uncertainty_score":0.05509013},"labels":[],"label_agreement":null},{"id":"W4210737025","doi":"10.1029/2021gb007057","title":"Latitude, Elevation, and Mean Annual Temperature Predict Peat Organic Matter Chemistry at a Global Scale","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Forest Research Institute; McGill University; University of Saskatchewan; University of Alberta; Laurentian University","funders":"Northern Research Station; Natural Environment Research Council; Sight Research UK; U.S. Department of Agriculture; U.S. Forest Service; National Science Foundation","keywords":"Peat; Latitude; Organic matter; Mineralization (soil science); Environmental chemistry; Chemistry; Environmental science; Soil water; Soil science; Geology; Ecology; Organic chemistry; Biology","score_opus":0.002679427845635749,"score_gpt":0.19294839484240098,"score_spread":0.19026896699676524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210737025","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99938464,0.000045238696,0.0001765805,0.0000074871955,0.0000013529874,9.376563e-7,0.00017527252,0.000005855799,0.00020267985],"genre_scores_gemma":[0.9996592,0.0000201462,0.000108068394,0.000002480355,0.0000011187334,9.2373045e-7,0.00013916081,0.0000016196182,0.00006736722],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999949,0.000013621153,0.0000036881797,0.0000142111,0.000008325484,0.000011162487],"domain_scores_gemma":[0.9997205,0.000090082016,0.000087290675,0.00002400844,0.000037583446,0.000040559455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021192174,0.00013441425,0.00013066547,0.00027178382,0.00011763124,0.0003681582,0.000067584835,0.00017065249,0.0010300624],"category_scores_gemma":[0.000377814,0.00013165601,0.0002130441,0.00031585098,0.00009707207,0.00019787945,0.00016039357,0.00011644668,0.0002248443],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022235647,0.0000058467335,0.99602157,0.000004045286,0.000036641264,0.000014873297,0.000020437197,0.000595302,0.002140139,0.000013302428,0.000036514255,0.0010890742],"study_design_scores_gemma":[5.778281e-7,0.0000050705316,0.999111,8.881844e-7,0.000004935871,0.000010858518,0.00003497719,0.0006777141,0.000088697314,0.000013165448,0.00005116584,8.379372e-7],"about_ca_topic_score_codex":0.005981915,"about_ca_topic_score_gemma":0.0089558605,"teacher_disagreement_score":0.005981915,"about_ca_system_score_codex":0.000088367866,"about_ca_system_score_gemma":0.00008100579,"threshold_uncertainty_score":0.011894226},"labels":[],"label_agreement":null},{"id":"W4210766152","doi":"10.1029/2021gb007047","title":"Watershed Classification Predicts Streamflow Regime and Organic Carbon Dynamics in the Northeast Pacific Coastal Temperate Rainforest","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Tula Foundation; University of Alberta; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Hakai Institute; Simon Fraser University; Tula Foundation","keywords":"Watershed; Streamflow; Hydrology (agriculture); Environmental science; Surface runoff; Biogeochemistry; Biogeochemical cycle; Watershed area; Snowmelt; Drainage basin; Geology; Ecology; Oceanography; Geography","score_opus":0.011833563735841083,"score_gpt":0.19693410789570168,"score_spread":0.1851005441598606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210766152","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99941754,0.000010208309,0.00015245762,0.000010610751,5.8446295e-7,0.0000046435684,0.0002140096,0.000009575909,0.00018032246],"genre_scores_gemma":[0.9988223,0.000011948493,0.0003597747,0.00000389598,0.0000013099738,0.0000054821903,0.00072057435,0.000002549859,0.0000721463],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988747,0.000019946756,0.00000970969,0.000033329623,0.000019851283,0.000029663579],"domain_scores_gemma":[0.99943024,0.00013582308,0.00016036352,0.00003237228,0.000103858096,0.00013728409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042555487,0.0002503846,0.00021296227,0.0013434106,0.00031206282,0.000833465,0.00018206882,0.00023906605,0.00077879213],"category_scores_gemma":[0.0010254087,0.00013237631,0.00028799378,0.0010829304,0.00018961415,0.00034143854,0.00033855974,0.00018032572,0.00014473785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016723352,0.000030522464,0.99558145,0.0000023327127,0.000018579667,0.00001977352,0.000029652221,0.001968942,0.0003905564,0.000017941846,0.00014247585,0.0017811699],"study_design_scores_gemma":[0.0000045725014,0.0000072271932,0.9770364,0.0000037786886,0.000006145795,0.000011909516,0.000112265014,0.022596974,0.00008328312,0.00004488068,0.00009077471,0.0000017786288],"about_ca_topic_score_codex":0.06754376,"about_ca_topic_score_gemma":0.072531566,"teacher_disagreement_score":0.06754376,"about_ca_system_score_codex":0.0007280469,"about_ca_system_score_gemma":0.0005729497,"threshold_uncertainty_score":0.13430119},"labels":[],"label_agreement":null},{"id":"W4210927544","doi":"10.1029/2020gb006851","title":"Simulated Future Trends in Marine Nitrogen Fixation Are Sensitive to Model Iron Implementation","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Nitrogen cycle; Biogeochemical cycle; Upwelling; New production; Environmental science; Nutrient; Nitrogen; Primary production; Oxygen minimum zone; Nitrogen fixation; Ecosystem; Biogeochemistry; Reactive nitrogen; Climate change; Oceanography; Atmospheric sciences; Ecology; Environmental chemistry; Phytoplankton; Chemistry; Biology; Geology","score_opus":0.008996833101004624,"score_gpt":0.2374548363250202,"score_spread":0.22845800322401558,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210927544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949195,0.00003772073,0.0026086732,0.00007928111,0.00001263926,0.000011203211,0.0006296349,0.000100621895,0.001600666],"genre_scores_gemma":[0.99872833,0.000016335382,0.00069268903,0.000018117351,0.0000014138328,0.000012681441,0.00034814072,0.000013572762,0.00016875677],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998554,0.000047591984,0.000010562615,0.00004029295,0.000014504135,0.000031598414],"domain_scores_gemma":[0.9991856,0.00046723793,0.0001137533,0.00007316236,0.00010516308,0.000054986314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069841766,0.0004677713,0.00029492844,0.00027843576,0.0002802492,0.00057623896,0.0005814374,0.0007708028,0.0012262879],"category_scores_gemma":[0.0022781813,0.000315516,0.0005479371,0.0002601475,0.00039572982,0.000465615,0.0003143076,0.00051643816,0.000104419836],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006423667,0.000031033956,0.013809486,0.00001097547,0.000039525505,0.000022048656,0.00001004432,0.98404944,0.0007634851,0.00024012409,0.00014766949,0.00081208925],"study_design_scores_gemma":[0.000040364375,0.000055811524,0.0065686177,0.0000062660847,0.000022864235,0.00000930617,0.000019393523,0.99177647,0.0010919475,0.00020358857,0.00019367141,0.000011678376],"about_ca_topic_score_codex":0.03691866,"about_ca_topic_score_gemma":0.016885942,"teacher_disagreement_score":0.03691866,"about_ca_system_score_codex":0.0008705847,"about_ca_system_score_gemma":0.00054968137,"threshold_uncertainty_score":0.07340753},"labels":[],"label_agreement":null},{"id":"W4212765608","doi":"10.1029/2021gb007163","title":"Global Patterns and Controls of Nutrient Immobilization on Decomposing Cellulose in Riverine Ecosystems","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Freshwater macroinvertebrate diversity and ecology","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of New Brunswick; University of British Columbia; Trent University; Ontario Tech University; University of Regina; Memorial University of Newfoundland; International Institute for Sustainable Development; Université du Québec à Montréal","funders":"Biological and Environmental Research; Natural Sciences and Engineering Research Council of Canada; Office of Science; Secretaría de Educación Superior, Ciencia, Tecnología e Innovación; Oak Ridge National Laboratory; Huron Mountain Wildlife Foundation; UT-Battelle; Battelle; U.S. Department of Energy","keywords":"Nutrient; Riparian zone; Phosphorus; Nutrient cycle; Environmental science; Organic matter; Ecosystem; Litter; Environmental chemistry; Eutrophication; Substrate (aquarium); Ecology; Decomposition; Chemistry; Biology","score_opus":0.006544080566268519,"score_gpt":0.20347824505507456,"score_spread":0.19693416448880605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4212765608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99967515,0.000047306356,0.000073196046,0.000004541642,2.9661774e-7,0.0000011837822,0.000077381905,0.000002268218,0.0001187431],"genre_scores_gemma":[0.99972755,0.000027853926,0.00008416309,0.0000037211457,8.038606e-7,0.000002598291,0.00010262637,0.0000012739638,0.000049427217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997944,0.00004545965,0.000018811877,0.000087396926,0.000025122086,0.000028760975],"domain_scores_gemma":[0.9995371,0.00010099794,0.0002048096,0.000037993468,0.00006823404,0.00005079716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041249307,0.00021164892,0.000313513,0.0010270968,0.0003034559,0.0006039186,0.0001846847,0.00027714542,0.00055349775],"category_scores_gemma":[0.0004750508,0.00017500695,0.00018707379,0.0007530349,0.0005727122,0.0003327197,0.00056726596,0.00013851801,0.0000645568],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012623862,0.00003084331,0.90759426,0.000049373655,0.00018052573,0.00005987171,0.00047991995,0.00081629655,0.08486577,0.0001497079,0.00005377963,0.005593392],"study_design_scores_gemma":[0.0000014191087,0.000015211919,0.9989832,0.0000016152602,0.0000073106216,0.000015707286,0.000080192185,0.0003377359,0.00046799518,0.000028894776,0.00005795924,0.0000027210153],"about_ca_topic_score_codex":0.0039356034,"about_ca_topic_score_gemma":0.010024618,"teacher_disagreement_score":0.0039356034,"about_ca_system_score_codex":0.00030652146,"about_ca_system_score_gemma":0.00015296058,"threshold_uncertainty_score":0.007825375},"labels":[],"label_agreement":null},{"id":"W4212779748","doi":"10.1029/2021gb007126","title":"The Biogeochemical Legacy of Arctic Subglacial Sediments Exposed by Glacier Retreat","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Biogeochemical cycle; Glacier; Geology; Deglaciation; Arctic; Glacial period; Oceanography; Sediment; Physical geography; Biogeochemistry; Earth science; Geochemistry; Geomorphology; Ecology","score_opus":0.013176440433913425,"score_gpt":0.24136947762488792,"score_spread":0.2281930371909745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4212779748","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948263,0.00017936257,0.00003290162,0.0000055547007,0.00000176826,8.465243e-7,0.00011917159,0.0000031849872,0.00017454589],"genre_scores_gemma":[0.9993007,0.00016162638,0.00007975405,0.000010465925,0.000004774161,0.000001578305,0.000309304,0.0000029116475,0.00012895088],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989974,0.000011316312,0.0000070623055,0.000031962063,0.000020715386,0.000029162466],"domain_scores_gemma":[0.99977154,0.000018882138,0.00009870339,0.000011987654,0.000060288494,0.00003862911],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019145248,0.00039868007,0.00027566624,0.0015315032,0.00068225805,0.00080662186,0.00016370788,0.00027086187,0.00073964667],"category_scores_gemma":[0.0002126137,0.00019244096,0.00017057781,0.0010657285,0.0004577019,0.0003051557,0.0004408729,0.00019803725,0.0001869971],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031334374,0.000031596177,0.8668908,0.00006109583,0.00013198299,0.00029144078,0.0007182894,0.00027996278,0.124302074,0.000055447246,0.00006284566,0.0068611633],"study_design_scores_gemma":[9.352878e-7,0.00002194835,0.998492,0.0000025846225,0.000010124795,0.00003943209,0.00019611347,0.000060140515,0.0010240696,0.000011760145,0.00013925505,0.000001555029],"about_ca_topic_score_codex":0.014128728,"about_ca_topic_score_gemma":0.017798504,"teacher_disagreement_score":0.014128728,"about_ca_system_score_codex":0.00040648843,"about_ca_system_score_gemma":0.00024217974,"threshold_uncertainty_score":0.02809298},"labels":[],"label_agreement":null},{"id":"W4220703582","doi":"10.1029/2021gb007185","title":"Interannual Variability in Methane and Nitrous Oxide Concentrations and Sea‐Air Fluxes Across the North American Arctic Ocean (2015–2019)","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; University of British Columbia","funders":"Fisheries and Oceans Canada; Natural Sciences and Engineering Research Council of Canada; ArcticNet","keywords":"Arctic; Water column; Oceanography; Environmental science; Beaufort sea; Trace gas; Methane; Arctic geoengineering; Canada Basin; Flux (metallurgy); Seawater; Geology; Atmospheric sciences; Climatology; Arctic ice pack; Chemistry; Drift ice","score_opus":0.004147567151911547,"score_gpt":0.22379227412807554,"score_spread":0.21964470697616398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220703582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99728405,0.00014685807,0.00010477102,0.000049312333,0.000014364907,0.0000029029077,0.0019840281,0.000011345676,0.00040225088],"genre_scores_gemma":[0.9971488,0.00008169447,0.000120574696,0.000024192428,0.000010532645,0.000008717442,0.0023236726,0.000002743761,0.0002790871],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997744,0.00003145359,0.00002436347,0.00008280503,0.000047526126,0.00003943915],"domain_scores_gemma":[0.9991974,0.000083860934,0.00032323948,0.000052361152,0.0002437528,0.00009936543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005679363,0.0001753084,0.00019371067,0.000732878,0.0003556764,0.00050988304,0.00021075962,0.00020940475,0.00048983935],"category_scores_gemma":[0.00069160876,0.00013555477,0.00032174194,0.0008833994,0.00019363128,0.00031495938,0.00046446596,0.00022328495,0.00012962872],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042499378,0.000013469776,0.99650323,0.000011124997,0.000090397436,0.000032181364,0.00010695578,0.00025646322,0.0006084189,0.000019727873,0.00041902144,0.0018966014],"study_design_scores_gemma":[5.038613e-7,0.000004597479,0.999255,0.0000028187626,0.000008759849,0.000009617601,0.00008359699,0.00031723498,0.00005886721,0.0000050322583,0.00025251953,0.0000014019098],"about_ca_topic_score_codex":0.09244619,"about_ca_topic_score_gemma":0.15786572,"teacher_disagreement_score":0.09244619,"about_ca_system_score_codex":0.00060306466,"about_ca_system_score_gemma":0.00052484113,"threshold_uncertainty_score":0.1838162},"labels":[],"label_agreement":null},{"id":"W4220910376","doi":"10.1029/2021gb007213","title":"Large Soil Carbon Storage in Terrestrial Ecosystems of Canada","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Forest Service; World Wildlife Fund Canada; University of Toronto; Natural Resources Canada; McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Terrestrial ecosystem; Environmental science; Soil water; Peat; Ecosystem; Soil carbon; Climate change; Boreal; Taiga; Terrestrial plant; Carbon cycle; Global warming; Detritus; Ecology; Soil science; Forestry; Geography","score_opus":0.005448799267503454,"score_gpt":0.2002374332205766,"score_spread":0.19478863395307316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220910376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99114835,0.00049546204,0.000524975,0.00005102675,0.0000023551206,0.000009619293,0.005143412,0.00004536837,0.0025792967],"genre_scores_gemma":[0.99846435,0.00012311139,0.00035910343,0.0000069420857,5.1221105e-7,0.0000025439645,0.0007904579,0.0000029047058,0.00025013613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998615,0.0000043920613,0.0000049197106,0.000030077734,0.00006295902,0.000036239315],"domain_scores_gemma":[0.99948007,0.000035097826,0.00006311797,0.000015825413,0.00034536837,0.000060447],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013062387,0.00022456214,0.00023306673,0.0015607383,0.0011912981,0.0010219641,0.00044116523,0.00013650229,0.0010094051],"category_scores_gemma":[0.00045932017,0.00013131097,0.0002006396,0.0030294433,0.00032990417,0.00027758334,0.0004295222,0.0001262867,0.00009644981],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014313436,0.00002835543,0.93310815,0.0001643913,0.0001920866,0.00026654324,0.00055130816,0.01097503,0.011850393,0.0010376684,0.0017086299,0.039974242],"study_design_scores_gemma":[0.000002953762,0.000006598429,0.9927779,0.00001881737,0.000021602365,0.000045836474,0.00042259315,0.004153261,0.0010766217,0.00019446116,0.0012650337,0.000014269212],"about_ca_topic_score_codex":0.98322946,"about_ca_topic_score_gemma":0.9894991,"teacher_disagreement_score":0.016770542,"about_ca_system_score_codex":0.0100807035,"about_ca_system_score_gemma":0.008014522,"threshold_uncertainty_score":0.07314104},"labels":[],"label_agreement":null},{"id":"W4220974539","doi":"10.1029/2021gb007146","title":"Using Machine Learning to Predict Inland Aquatic CO<sub>2</sub> and CH<sub>4</sub> Concentrations and the Effects of Wildfires in the Yukon‐Kuskokwim Delta, Alaska","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Fish and Wildlife Service; Nuclear Safety and Security Commission; National Aeronautics and Space Administration; National Science Foundation","keywords":"Tundra; Environmental science; Permafrost; Dissolved organic carbon; Arctic; Aquatic ecosystem; Thermokarst; Total organic carbon; Surface water; Hydrology (agriculture); Ecosystem; Delta; Physical geography; Environmental chemistry; Atmospheric sciences; Ecology; Oceanography; Chemistry; Environmental engineering; Geology; Geography","score_opus":0.014382886077984757,"score_gpt":0.23297105829218104,"score_spread":0.21858817221419627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220974539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961345,0.00006759396,0.002779065,0.000079771344,0.000012226765,0.0000109695375,0.00040972233,0.00009083418,0.00041543876],"genre_scores_gemma":[0.99770266,0.0000239595,0.0014908713,0.000015052843,0.000005546601,0.000009699208,0.0004907081,0.0000037370248,0.00025772135],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998023,0.00005644956,0.000015171648,0.00007368831,0.000020055244,0.0000324375],"domain_scores_gemma":[0.9992537,0.000393871,0.00010623079,0.000039252278,0.00013968929,0.000067195935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096914655,0.00078084395,0.00037052308,0.0008815083,0.00037737415,0.0008911751,0.00041735117,0.0006342219,0.0006311839],"category_scores_gemma":[0.0014102893,0.0003219619,0.000564956,0.00047879535,0.00024475614,0.0004993701,0.0003429457,0.00040629125,0.00025029984],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021388097,0.0004401273,0.55514115,0.000023169456,0.0002476812,0.000063634005,0.00005386803,0.42287156,0.0016044247,0.00007728229,0.0005986713,0.018664587],"study_design_scores_gemma":[0.000007865821,0.00004022427,0.05480404,0.000006524957,0.000024908097,0.000008802675,0.000047435562,0.9443727,0.00042082593,0.00014878802,0.000110144676,0.000007747402],"about_ca_topic_score_codex":0.079667315,"about_ca_topic_score_gemma":0.06716013,"teacher_disagreement_score":0.079667315,"about_ca_system_score_codex":0.0013423145,"about_ca_system_score_gemma":0.0008142755,"threshold_uncertainty_score":0.15840721},"labels":[],"label_agreement":null},{"id":"W4221073257","doi":"10.1029/2021gb007242","title":"Heterogeneous Patterns of Aged Organic Carbon Export Driven by Hydrologic Flow Paths, Soil Texture, Fire, and Thaw in Discontinuous Permafrost Headwaters","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina; University of Lethbridge","funders":"","keywords":"Permafrost; Thermokarst; Dissolved organic carbon; Soil water; Hydrology (agriculture); Environmental science; STREAMS; Snowmelt; Soil carbon; Total organic carbon; Physical geography; Snow; Geology; Soil science; Geomorphology; Ecology; Oceanography; Geography","score_opus":0.011525738672169484,"score_gpt":0.20695884392034994,"score_spread":0.19543310524818044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221073257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998847,0.0000067793103,0.000035831883,0.0000013822046,1.3936652e-7,6.0636745e-7,0.000030091374,0.0000020008704,0.000038453843],"genre_scores_gemma":[0.99983585,0.0000051584398,0.000043608077,0.0000014888857,5.035805e-7,0.0000011587528,0.00007423185,9.2653545e-7,0.00003704225],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993944,0.000009560327,0.00000423127,0.000021399,0.00000771544,0.000017707838],"domain_scores_gemma":[0.99977726,0.000053914795,0.0000699212,0.000016068981,0.000030491332,0.00005228602],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014871435,0.00011274393,0.0001962253,0.00057033147,0.0003097715,0.0004899026,0.00017918575,0.00015902483,0.0004983216],"category_scores_gemma":[0.00031469527,0.00013126415,0.00015027939,0.00041436352,0.00033017446,0.00022261472,0.00030308694,0.00013399695,0.000060042727],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012851886,0.000026578182,0.98420227,0.0000070405968,0.00003353174,0.000102196864,0.00041817478,0.0006063759,0.012138367,0.000055226108,0.00003493606,0.002246746],"study_design_scores_gemma":[0.0000012578097,0.000009327387,0.99842215,0.0000010247251,0.0000038029832,0.000022404447,0.00014989804,0.0011076911,0.00022338427,0.00002695121,0.000030319461,0.0000018953892],"about_ca_topic_score_codex":0.010715472,"about_ca_topic_score_gemma":0.01650929,"teacher_disagreement_score":0.010715472,"about_ca_system_score_codex":0.00031052285,"about_ca_system_score_gemma":0.00014815768,"threshold_uncertainty_score":0.021306217},"labels":[],"label_agreement":null},{"id":"W4224210951","doi":"10.1029/2021gb007107","title":"Natural Variations in Dissolved Silicon Isotopes Across the Arctic Ocean From the Pacific to the Atlantic","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"H2020 Marie Skłodowska-Curie Actions; Natural Sciences and Engineering Research Council of Canada","keywords":"Oceanography; Geotraces; Geology; Bay; Arctic; Seawater; Isotopes of silicon; Water column; Water mass; Biogenic silica; Diatom; Silicon; Chemistry","score_opus":0.012137740332416536,"score_gpt":0.25012109141948397,"score_spread":0.23798335108706742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224210951","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990521,0.00007082333,0.0000810015,0.000014763587,0.0000055062737,0.0000018965961,0.00021020552,0.0000040433133,0.0005596717],"genre_scores_gemma":[0.99928147,0.000061039595,0.00012261994,0.000012023087,0.000003023643,0.0000033757983,0.00034458147,0.0000024072906,0.00016956979],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982613,0.000020952933,0.000009077228,0.000055751265,0.000056129884,0.000032024174],"domain_scores_gemma":[0.9995073,0.000060188697,0.000097934884,0.000018333421,0.00022930453,0.00008698855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003612197,0.000308458,0.00024226517,0.0008243922,0.00082608603,0.0006696044,0.00023266242,0.00018393096,0.0003559661],"category_scores_gemma":[0.0006278908,0.00026965057,0.00020318756,0.0007060812,0.0004262296,0.000196411,0.00038293476,0.00022444547,0.00007661269],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017550852,0.000018306417,0.9731599,0.000013615984,0.000109672066,0.00004366591,0.00035169526,0.00027593807,0.021998418,0.000055398967,0.00010860554,0.0036892146],"study_design_scores_gemma":[0.0000022296472,0.000015099281,0.9985649,0.000002794778,0.000013591174,0.000016575537,0.00019163678,0.00030962707,0.0006504521,0.000011598991,0.00021837965,0.0000030888032],"about_ca_topic_score_codex":0.26786894,"about_ca_topic_score_gemma":0.45325363,"teacher_disagreement_score":0.26786894,"about_ca_system_score_codex":0.0016789696,"about_ca_system_score_gemma":0.0011601195,"threshold_uncertainty_score":0.53261954},"labels":[],"label_agreement":null},{"id":"W4225284452","doi":"10.1029/2021gb007191","title":"Arctic – Atlantic Exchange of the Dissolved Micronutrients Iron, Manganese, Cobalt, Nickel, Copper and Zinc With a Focus on Fram Strait","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; University of British Columbia","funders":"","keywords":"Geotraces; Arctic; Oceanography; Environmental science; Micronutrient; Manganese; Deep sea; Seawater; Arctic dipole anomaly; Trace element; Flux (metallurgy); Zinc; Geology; Chemistry; Geochemistry; Arctic ice pack","score_opus":0.006552844186697975,"score_gpt":0.1960290438709883,"score_spread":0.18947619968429033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225284452","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9900726,0.0003568439,0.00024236186,0.00016763885,0.000037158105,0.0000036041654,0.0021428752,0.000021397202,0.0069554783],"genre_scores_gemma":[0.9963527,0.0001971941,0.0004906057,0.00005647927,0.000014305346,0.000003803042,0.001240788,0.0000146603925,0.0016295345],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998944,0.000008167948,0.000006628233,0.00003869776,0.000028029985,0.000024013849],"domain_scores_gemma":[0.9998253,0.00001586979,0.000042580712,0.0000091920365,0.00008474852,0.000022424105],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020438216,0.00021839027,0.0002221237,0.00059704453,0.00062003813,0.00071425835,0.00015651945,0.00023193461,0.0012849859],"category_scores_gemma":[0.0002494396,0.00014604363,0.00033480165,0.0007453223,0.00019921028,0.00028842903,0.0005919681,0.00024402284,0.00028092842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044186597,0.000026000484,0.956672,0.000098846984,0.00017928207,0.00025565267,0.00097588805,0.00084283965,0.023081182,0.00039831724,0.0018443454,0.015183758],"study_design_scores_gemma":[0.0000065321774,0.000023692353,0.9939673,0.000027984734,0.00003422306,0.00003795456,0.00057534844,0.00058850826,0.0010291416,0.000053010514,0.0036492902,0.0000070791175],"about_ca_topic_score_codex":0.27903676,"about_ca_topic_score_gemma":0.38074592,"teacher_disagreement_score":0.27903676,"about_ca_system_score_codex":0.0011103706,"about_ca_system_score_gemma":0.0009242944,"threshold_uncertainty_score":0.5548252},"labels":[],"label_agreement":null},{"id":"W4281680503","doi":"10.1029/2021gb007161","title":"Hydrologic Export of Soil Organic Carbon: Continental Variation and Implications","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Fonds de recherche du Québec – Nature et technologies; National Science Foundation","keywords":"Environmental science; Arid; Soil carbon; Sink (geography); Carbon cycle; Hydrology (agriculture); Total organic carbon; Soil water; Soil organic matter; Carbon sink; Drainage basin; Soil science; Environmental chemistry; Climate change; Ecosystem; Ecology; Geology; Oceanography; Geography; Chemistry","score_opus":0.0061660810230866735,"score_gpt":0.20174698584979903,"score_spread":0.19558090482671237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281680503","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99646395,0.00074090494,0.00039112114,0.00019191044,0.000007626201,0.0000027443932,0.00073927734,0.000020162868,0.001442324],"genre_scores_gemma":[0.999345,0.00016308045,0.0000666254,0.000016867096,0.000008234521,7.746236e-7,0.00032169535,0.0000052436526,0.00007240635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998479,0.000048331127,0.000009573859,0.000060255676,0.000015659785,0.000018310799],"domain_scores_gemma":[0.9990152,0.00034566515,0.00023944197,0.00010555425,0.00018770552,0.00010635331],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077047484,0.00016695131,0.00015654841,0.00089473114,0.00016976116,0.00061735214,0.00025064492,0.0001700651,0.0012887961],"category_scores_gemma":[0.001144325,0.00010457389,0.0003138252,0.0012229781,0.0004532734,0.0004447024,0.00047552332,0.00020535318,0.00013278745],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000075121825,0.000011872132,0.9884849,0.000018610772,0.00026478688,0.000057267676,0.00010284527,0.0013853653,0.0012569763,0.00024814482,0.00026502338,0.007829076],"study_design_scores_gemma":[0.0000015884419,0.0000057832017,0.9986235,0.0000046874957,0.000014770769,0.00002061098,0.00006222422,0.0008032072,0.00010734148,0.00010597766,0.0002478251,0.0000024694532],"about_ca_topic_score_codex":0.010062937,"about_ca_topic_score_gemma":0.008104096,"teacher_disagreement_score":0.010062937,"about_ca_system_score_codex":0.00021668366,"about_ca_system_score_gemma":0.000117396376,"threshold_uncertainty_score":0.020008743},"labels":[],"label_agreement":null},{"id":"W4282924640","doi":"10.1029/2021gb007024","title":"Anthropogenic Carbon Increase has Caused Critical Shifts in Aragonite Saturation Across a Sensitive Coastal System","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Environment and Climate Change Canada; Fisheries and Oceans Canada; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aragonite; Biogeochemical cycle; Environmental science; Estuary; Oceanography; Context (archaeology); Carbonate; Total inorganic carbon; Carbon cycle; Ocean acidification; Saturation (graph theory); Carbon fibers; Atmospheric sciences; Carbon dioxide; Seawater; Geology; Environmental chemistry; Ecosystem; Chemistry; Ecology; Materials science","score_opus":0.013500782233134173,"score_gpt":0.2551070915067276,"score_spread":0.24160630927359344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4282924640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996189,0.0000041348526,0.000055725093,0.000024399042,0.0000014242269,0.0000016433589,0.000051086794,0.000007020192,0.00023573189],"genre_scores_gemma":[0.9998274,0.0000068951235,0.000053627453,0.000008163725,5.120536e-7,0.0000018072462,0.000049537724,0.000001275134,0.000050774706],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994636,0.000008362751,0.0000043302375,0.000016918275,0.0000057209527,0.000018388413],"domain_scores_gemma":[0.9998838,0.000022231703,0.00002220505,0.000014094279,0.000019458435,0.000038294504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011049595,0.0002159974,0.00018609547,0.000194133,0.0004534746,0.0006696127,0.00039775454,0.00045385907,0.0014663131],"category_scores_gemma":[0.00037303046,0.00017622515,0.00043421786,0.00031708408,0.00046299002,0.0003187128,0.0005015865,0.00042024298,0.00006138743],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006296712,0.00033978547,0.6091369,0.00008731291,0.00035704157,0.00071371446,0.00027517416,0.32673505,0.05217544,0.0012730472,0.0010413993,0.007235472],"study_design_scores_gemma":[0.00014322752,0.00043854292,0.5694851,0.000012474398,0.00013443461,0.00013358728,0.0012900605,0.42018107,0.0061936686,0.00076732447,0.0011795925,0.000040857652],"about_ca_topic_score_codex":0.059098497,"about_ca_topic_score_gemma":0.061121784,"teacher_disagreement_score":0.059098497,"about_ca_system_score_codex":0.0016224958,"about_ca_system_score_gemma":0.0007414826,"threshold_uncertainty_score":0.11750901},"labels":[],"label_agreement":null},{"id":"W4283360230","doi":"10.1029/2022gb007304","title":"Extreme Nitrate Deficits in the Western Arctic Ocean: Origin, Decadal Changes, and Implications for Denitrification on a Polar Marginal Shelf","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Nitrate; Oceanography; Denitrification; Arctic; Environmental science; Canada Basin; Climatology; Geology; Nitrogen; Ecology; Chemistry; Biology","score_opus":0.02779333173713008,"score_gpt":0.24636829173559088,"score_spread":0.2185749599984608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283360230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995154,0.00012068637,0.000028924427,0.000023594555,0.0000027592998,8.009882e-7,0.000117963886,0.000001137482,0.0001887252],"genre_scores_gemma":[0.9996352,0.000097316515,0.000041204912,0.0000069281236,0.0000035140704,0.0000012704394,0.0001463083,5.2115905e-7,0.00006773358],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995625,0.0000057671996,0.000005123225,0.00001271299,0.00000790714,0.000012275522],"domain_scores_gemma":[0.9997483,0.000017544327,0.0000980414,0.000010843694,0.00008011428,0.00004519874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002739138,0.00014849316,0.00016386704,0.00045154302,0.00036288815,0.00043061332,0.000096921765,0.00013774668,0.00033055208],"category_scores_gemma":[0.0002943411,0.000076658434,0.00014203489,0.00058409985,0.00023549076,0.000259446,0.00033382318,0.00016718039,0.00004050579],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078024794,0.000011935437,0.9941397,0.000011586053,0.000042686268,0.00008202852,0.00017218849,0.00019380548,0.0026719852,0.000033375298,0.00006873389,0.0024940127],"study_design_scores_gemma":[5.155194e-7,0.0000067978667,0.99936825,0.0000029007272,0.000006092023,0.000012532844,0.00017699083,0.00016707863,0.00010891378,0.000012710097,0.00013601065,0.0000010627863],"about_ca_topic_score_codex":0.045089502,"about_ca_topic_score_gemma":0.07109349,"teacher_disagreement_score":0.045089502,"about_ca_system_score_codex":0.00042478618,"about_ca_system_score_gemma":0.00034010204,"threshold_uncertainty_score":0.08965415},"labels":[],"label_agreement":null},{"id":"W4285008794","doi":"10.1029/2022gb007407","title":"Changes in Canada's Phosphorus Cycle 1961–2018: Surpluses and Deficits","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ste. Anne's Hospital; McGill University","funders":"China Scholarship Council; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Cycling; Eutrophication; Phosphorus; Manure; Fertilizer; Environmental science; Agriculture; Nutrient cycle; Geography; Nutrient; Pasture; Ecology; Forestry; Biology; Archaeology; Chemistry","score_opus":0.00637543319064264,"score_gpt":0.19099506522487855,"score_spread":0.18461963203423593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285008794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9757414,0.00042234125,0.0009112737,0.000667546,0.000020006202,0.00003675502,0.01681267,0.000105847445,0.005282051],"genre_scores_gemma":[0.99371135,0.00036207042,0.0008142686,0.00007026684,0.0000041937424,0.000015751595,0.003191457,0.000012594091,0.0018181105],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998317,0.0000058930536,0.0000058071155,0.00003576287,0.000068273286,0.000052539395],"domain_scores_gemma":[0.99954873,0.000022202943,0.000057228815,0.000011486396,0.00030272658,0.000057632304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019170859,0.00038072618,0.0002545609,0.0010594719,0.0013543203,0.0011033267,0.0006157708,0.00032233293,0.0017247226],"category_scores_gemma":[0.0006165527,0.00018402954,0.000494765,0.002059801,0.0005171756,0.00035914092,0.00041642817,0.00034321117,0.00013223602],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026252551,0.00006277299,0.9004449,0.00020380582,0.00023032243,0.0003100344,0.0006866335,0.05258598,0.0047625755,0.0022121153,0.009224609,0.029013706],"study_design_scores_gemma":[0.000037363094,0.000025630517,0.9291427,0.00006318497,0.0000911752,0.00005434111,0.0010198927,0.050801203,0.001231606,0.0004310197,0.017049225,0.000052630447],"about_ca_topic_score_codex":0.997024,"about_ca_topic_score_gemma":0.99668294,"teacher_disagreement_score":0.03297641,"about_ca_system_score_codex":0.03297641,"about_ca_system_score_gemma":0.03174441,"threshold_uncertainty_score":0.23926175},"labels":[],"label_agreement":null},{"id":"W4290075774","doi":"10.1029/2022gb007320","title":"Sediments in Sea Ice Drive the Canada Basin Surface Mn Maximum: Insights From an Arctic Mn Ocean Model","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia; Compute Canada","keywords":"Sea ice; Oceanography; Biogeochemical cycle; Arctic; Geotraces; Geology; Arctic ice pack; Arctic sea ice decline; Canada Basin; Cryosphere; Environmental science; Bay; Drift ice; Seawater","score_opus":0.007799172550752006,"score_gpt":0.19998966934508444,"score_spread":0.19219049679433245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4290075774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99013025,0.00014410127,0.0018659858,0.0004704084,0.00002750205,0.00002308595,0.0014410724,0.000084107734,0.005813537],"genre_scores_gemma":[0.9966702,0.00010221617,0.0011448831,0.000071117945,0.000008706529,0.000015333308,0.00092520425,0.000032001826,0.0010304345],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999058,0.000020476884,0.000004169036,0.000021145957,0.000014081786,0.000034353343],"domain_scores_gemma":[0.9996458,0.000106283325,0.00003931347,0.000015725906,0.00010715359,0.00008569247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033981682,0.0007301574,0.000444829,0.0005098845,0.0010672152,0.0013011595,0.0011953231,0.0011260615,0.0017986061],"category_scores_gemma":[0.0010277017,0.0004448118,0.0008844247,0.000512645,0.00067448226,0.00034903025,0.00070862524,0.00071274413,0.00013622404],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000061074505,0.000041858562,0.022683369,0.000018388711,0.000055022516,0.00009068271,0.000034901568,0.97399116,0.00067775603,0.0009608853,0.0005689771,0.0008160257],"study_design_scores_gemma":[0.00003271577,0.00001738768,0.00535707,0.000007745964,0.000027077333,0.000005481628,0.00006410864,0.9937868,0.00012598225,0.00018762745,0.00037542725,0.000012481833],"about_ca_topic_score_codex":0.8237181,"about_ca_topic_score_gemma":0.697308,"teacher_disagreement_score":0.17628193,"about_ca_system_score_codex":0.0047601378,"about_ca_system_score_gemma":0.0065502655,"threshold_uncertainty_score":0.35464013},"labels":[],"label_agreement":null},{"id":"W4293072796","doi":"10.1029/2022gb007341","title":"Representing the Dynamic Response of Vegetation to Nitrogen Limitation via Biological Nitrogen Fixation in the CLASSIC Land Model","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Sink (geography); Biogeochemical cycle; Nitrogen cycle; Carbon sink; Nitrogen; Carbon cycle; Nitrogen fixation; Cycling; Carbon sequestration; Terrestrial ecosystem; Global change; Vegetation (pathology); Environmental change; Ecology; Climate change; Ecosystem; Chemistry; Biology; Geography; Forestry","score_opus":0.016192048386818928,"score_gpt":0.2532972749434214,"score_spread":0.2371052265566025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293072796","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9359862,0.00048189558,0.043721747,0.00087179575,0.000051576702,0.00004662154,0.0016759258,0.00031243393,0.016851878],"genre_scores_gemma":[0.9939917,0.00017664775,0.0034222628,0.00007277538,0.000008573772,0.000023822147,0.00018828173,0.000030480498,0.0020854727],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988663,0.000027301816,0.0000044250505,0.00003109743,0.00001851658,0.00003201686],"domain_scores_gemma":[0.9997609,0.000085652486,0.00003188964,0.000023265879,0.000055347413,0.000042950116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002452432,0.00045375217,0.00038415857,0.00035787496,0.0004984235,0.0008782516,0.0014232289,0.0007883507,0.0013063082],"category_scores_gemma":[0.0007379667,0.00020412743,0.0004417479,0.00053649314,0.00089812983,0.0007134869,0.0005027144,0.000440147,0.00009804329],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002224104,0.000009314268,0.0026910203,0.000017365885,0.00002205521,0.000026960779,0.0000232977,0.99052787,0.0015087806,0.0038479117,0.0001726475,0.001130563],"study_design_scores_gemma":[0.000012042921,0.0000096044305,0.0020309906,0.0000036481083,0.000015157314,0.0000075287458,0.000025188974,0.99568874,0.00022741231,0.0014550682,0.00051428063,0.000010333345],"about_ca_topic_score_codex":0.645433,"about_ca_topic_score_gemma":0.50667715,"teacher_disagreement_score":0.645433,"about_ca_system_score_codex":0.0048720804,"about_ca_system_score_gemma":0.0033542104,"threshold_uncertainty_score":0.71331024},"labels":[],"label_agreement":null},{"id":"W4293445905","doi":"10.1029/2022gb007403","title":"Permafrost Landscape History Shapes Fluvial Chemistry, Ecosystem Carbon Balance, and Potential Trajectories of Future Change","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University; Wilfrid Laurier University; Government of Northwest Territories; Trent University; Université de Montréal; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Permafrost; Fluvial; Environmental science; Thermokarst; Ecosystem; Carbon cycle; Total organic carbon; Soil carbon; Weathering; Hydrology (agriculture); Dissolved organic carbon; Earth science; Geology; Ecology; Environmental chemistry; Oceanography; Soil science; Geomorphology; Chemistry; Soil water","score_opus":0.014600734637203896,"score_gpt":0.20056857480797974,"score_spread":0.18596784017077583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293445905","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995141,0.000047864633,0.000054685024,0.000014560834,4.975012e-7,0.0000011768068,0.00011826088,0.000002940829,0.00024606418],"genre_scores_gemma":[0.9998037,0.000018610286,0.000041532352,0.0000042263523,4.029275e-7,6.94995e-7,0.00008046206,8.5600215e-7,0.000049498394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999466,0.000009871413,0.0000021727633,0.000014084106,0.000006073504,0.000021250979],"domain_scores_gemma":[0.99984527,0.000023870061,0.0000448363,0.000009687019,0.000035029312,0.0000413084],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019063277,0.00010874375,0.00012213721,0.00040067278,0.0003673762,0.00056952017,0.00013336595,0.00019220295,0.00072895637],"category_scores_gemma":[0.00034243445,0.00009141481,0.00012417148,0.00037767156,0.00028199883,0.00020796675,0.00016685933,0.000117447205,0.000047936002],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046626024,0.000014568424,0.9930736,0.000006087798,0.000041210787,0.00004923201,0.00011015785,0.0007558309,0.003052508,0.00008462737,0.0000917793,0.0026737489],"study_design_scores_gemma":[6.5743075e-7,0.0000045920524,0.9987495,0.0000015533548,0.0000039441934,0.000011603313,0.00009601709,0.00095901743,0.0000588022,0.000035352303,0.000077886885,0.0000010668336],"about_ca_topic_score_codex":0.16109672,"about_ca_topic_score_gemma":0.35117498,"teacher_disagreement_score":0.16109672,"about_ca_system_score_codex":0.00072869315,"about_ca_system_score_gemma":0.00051828666,"threshold_uncertainty_score":0.32031804},"labels":[],"label_agreement":null},{"id":"W4294891729","doi":"10.1029/2022gb007316","title":"Nutrient and Silicon Isotope Dynamics in the Laptev Sea and Implications for Nutrient Availability in the Transpolar Drift","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Canada First Research Excellence Fund; Ocean Frontier Institute; Bundesministerium für Bildung und Forschung","keywords":"Oceanography; Nutrient; Environmental science; Geology; Arctic; Colored dissolved organic matter; Sea ice; Surface water; Water column; Phytoplankton; Ecology","score_opus":0.009983766265466773,"score_gpt":0.22544759449326268,"score_spread":0.21546382822779592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294891729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993231,0.00006221724,0.000046945006,0.000012205597,0.000002678372,0.0000010800919,0.00012413051,0.00000447707,0.00042328527],"genre_scores_gemma":[0.999355,0.000056488054,0.00010063459,0.000012386302,0.0000024527487,0.0000025748427,0.00027465002,0.0000036108986,0.00019221999],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999516,0.000004168459,0.000004300046,0.00001786022,0.000009714658,0.0000124059125],"domain_scores_gemma":[0.99995005,0.000005370397,0.000013266216,0.0000033106542,0.000016392562,0.000011617107],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016178643,0.00041331866,0.0002614988,0.0007036535,0.0003651355,0.0007345032,0.00024276348,0.00027618633,0.0005689451],"category_scores_gemma":[0.00011512566,0.00020347022,0.00031314587,0.0006081785,0.00027089543,0.00028353903,0.000456942,0.00017455981,0.00011245994],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039567277,0.000047849906,0.8953278,0.000050572264,0.00016469386,0.00043893195,0.00029419808,0.003699064,0.08956755,0.00024000916,0.00017883709,0.009594853],"study_design_scores_gemma":[0.000019944939,0.00010984121,0.98739946,0.000011540206,0.000036412344,0.00008266048,0.00046551964,0.00471738,0.0062202495,0.00010739399,0.0008174804,0.000012165453],"about_ca_topic_score_codex":0.027861034,"about_ca_topic_score_gemma":0.031945296,"teacher_disagreement_score":0.027861034,"about_ca_system_score_codex":0.00081594614,"about_ca_system_score_gemma":0.0004941763,"threshold_uncertainty_score":0.05539775},"labels":[],"label_agreement":null},{"id":"W4297984228","doi":"10.1029/2022gb007452","title":"Evaluation of Biological Carbon Pump Metrics in the Subtropical Gulf of Aqaba, Northern Red Sea","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Photic zone; Environmental science; Oceanography; Biological pump; Atmospheric sciences; Total organic carbon; Context (archaeology); Ecosystem; Carbon cycle; Phytoplankton; Geology; Nutrient; Ecology; Environmental chemistry; Chemistry","score_opus":0.03188764647891987,"score_gpt":0.24071778742513605,"score_spread":0.2088301409462162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297984228","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99905735,0.000049361497,0.00014882827,0.00002278717,0.0000040394884,0.0000045160764,0.00035125684,0.000022131308,0.0003396493],"genre_scores_gemma":[0.99882656,0.000035492627,0.00037953517,0.000012806441,0.0000029860564,0.000007017478,0.00060001813,0.0000045605975,0.00013103032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987376,0.000017957167,0.000014151325,0.00003315872,0.000034640292,0.000026273521],"domain_scores_gemma":[0.99954444,0.00006163501,0.00012183347,0.000028630702,0.00018696843,0.000056558976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005911911,0.0004673559,0.00023040036,0.0010574039,0.00038729,0.00063118746,0.0002738436,0.00022892427,0.0004743094],"category_scores_gemma":[0.0009187747,0.00014647472,0.00029827535,0.0011913588,0.0002775791,0.000451461,0.0003751785,0.00021226631,0.000096217394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000113593676,0.000067430774,0.97169346,0.000041680876,0.00008477385,0.00015108811,0.00027875623,0.0075416584,0.009030105,0.00009663794,0.00023768637,0.010663203],"study_design_scores_gemma":[0.000008431974,0.000035840105,0.98608506,0.0000069279463,0.000019421052,0.000026359732,0.000301866,0.01240363,0.0007229045,0.000026369815,0.00035478052,0.000008395473],"about_ca_topic_score_codex":0.16644602,"about_ca_topic_score_gemma":0.19162792,"teacher_disagreement_score":0.16644602,"about_ca_system_score_codex":0.0008802552,"about_ca_system_score_gemma":0.0008417071,"threshold_uncertainty_score":0.33095443},"labels":[],"label_agreement":null},{"id":"W4313397282","doi":"10.1029/2022gb007523","title":"The Outsized Role of Salps in Carbon Export in the Subarctic Northeast Pacific Ocean","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; Memorial University of Newfoundland","funders":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration","keywords":"Photic zone; Subarctic climate; Oceanography; Pelagic zone; Marine snow; Biological pump; Zooplankton; Gelatinous zooplankton; Mesopelagic zone; Environmental science; Phytoplankton; Geology; Water column; Ecology; Nutrient; Biology","score_opus":0.006003524010247731,"score_gpt":0.1874830447680471,"score_spread":0.18147952075779938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313397282","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947816,0.000054508942,0.000070380294,0.000013952325,0.0000015919801,0.0000014039197,0.00013920023,0.0000061953706,0.00023475541],"genre_scores_gemma":[0.99957615,0.000054885397,0.000087864675,0.0000128528945,0.000002138632,0.0000020112057,0.00013121846,0.0000023371015,0.00013044913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996555,0.000002889475,0.000002949248,0.000012996954,0.0000074605905,0.0000080784475],"domain_scores_gemma":[0.9998423,0.000019140496,0.00006200682,0.000009929183,0.000031934876,0.00003467728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000121046396,0.00036653786,0.00013436287,0.00033266898,0.000335847,0.00040131898,0.00013262103,0.000176185,0.00085233443],"category_scores_gemma":[0.00016550689,0.00016837157,0.00021263964,0.00020320828,0.00023100969,0.00029644425,0.00035319946,0.00018703277,0.00011812605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002031761,0.000023584746,0.90207887,0.00006941277,0.00006369424,0.00023480692,0.00018542403,0.0010486578,0.09234751,0.00005620332,0.00009156187,0.0035971827],"study_design_scores_gemma":[0.0000021102521,0.000023980541,0.9972065,0.0000034946443,0.000010429042,0.000020691077,0.00010941061,0.000719015,0.0017575419,0.000014364694,0.00013053416,0.0000019617205],"about_ca_topic_score_codex":0.024768637,"about_ca_topic_score_gemma":0.029842112,"teacher_disagreement_score":0.024768637,"about_ca_system_score_codex":0.0004936212,"about_ca_system_score_gemma":0.00028832097,"threshold_uncertainty_score":0.049248934},"labels":[],"label_agreement":null},{"id":"W4313577893","doi":"10.1029/2022gb007495","title":"Hydrologic and Landscape Controls on Dissolved Organic Matter Composition Across Western North American Arctic Lakes","year":2022,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Wilfrid Laurier University; University of Waterloo","funders":"High Magnetic Field Laboratory, Chinese Academy of Sciences; Global Water Futures; Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; Nuclear Safety and Security Commission; National High Magnetic Field Laboratory; Division of Materials Research; National Aeronautics and Space Administration; Division of Chemistry; Parks Canada; National Science Foundation","keywords":"Dissolved organic carbon; Colored dissolved organic matter; Tundra; Arctic; Boreal; Environmental science; Permafrost; Taiga; Precipitation; Wetland; Organic matter; Aquatic ecosystem; Physical geography; Oceanography; Ecology; Geology; Geography; Phytoplankton; Nutrient","score_opus":0.005836282306421158,"score_gpt":0.2041912901389667,"score_spread":0.19835500783254553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313577893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99958163,0.000044965083,0.000021269634,0.000018633109,0.0000013216878,0.000001328085,0.00010219907,0.000002530742,0.00022614488],"genre_scores_gemma":[0.9996636,0.00004069387,0.000046489284,0.000010065027,0.0000027396823,0.0000031155682,0.00010891138,0.0000016848218,0.00012269164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988556,0.000023857277,0.000007164183,0.00003541784,0.000019094943,0.000028911389],"domain_scores_gemma":[0.9996184,0.000056617184,0.000112388276,0.00001538392,0.000103875274,0.00009327779],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025743808,0.00014512037,0.00018993478,0.00058689207,0.0007074677,0.0006623069,0.00018774944,0.0001590861,0.00055522396],"category_scores_gemma":[0.00041752428,0.00015956572,0.00017877942,0.0008600943,0.0003796031,0.00026587618,0.0003491444,0.00013377925,0.00004503609],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014758468,0.000038677805,0.98961675,0.000015756093,0.000081823855,0.00007912939,0.00061734096,0.0003146396,0.005843955,0.00006641108,0.00018342739,0.002994487],"study_design_scores_gemma":[9.841123e-7,0.000003117693,0.99946517,0.0000012586711,0.000007346951,0.000005588418,0.00024480763,0.00014935664,0.00004486587,0.000007962508,0.00006853119,0.0000011222111],"about_ca_topic_score_codex":0.26336205,"about_ca_topic_score_gemma":0.49935687,"teacher_disagreement_score":0.26336205,"about_ca_system_score_codex":0.0011834127,"about_ca_system_score_gemma":0.00092493347,"threshold_uncertainty_score":0.5236582},"labels":[],"label_agreement":null},{"id":"W4315434541","doi":"10.1029/2021gb007255","title":"Global Climate Change Increases Terrestrial Soil CH<sub>4</sub> Emissions","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Université du Québec à Montréal","funders":"National Key Research and Development Program of China; Priority Academic Program Development of Jiangsu Higher Education Institutions; China Scholarship Council; National Natural Science Foundation of China","keywords":"Environmental science; Terrestrial ecosystem; Ecosystem; Wetland; Precipitation; Soil water; Climate change; Greenhouse gas; Global warming; Sink (geography); Atmospheric sciences; Radiative forcing; Ecology; Soil science; Geography; Geology","score_opus":0.017070279207673567,"score_gpt":0.25329678414121226,"score_spread":0.2362265049335387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4315434541","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5252976,0.44067386,0.00899826,0.0045399577,0.00085798476,0.00006819073,0.014964808,0.0007015889,0.003897895],"genre_scores_gemma":[0.97293484,0.022653345,0.0011162546,0.00075009506,0.00017058835,0.000024141791,0.0020631715,0.00006584674,0.00022171688],"study_design_codex":"meta_analysis","study_design_gemma":"observational","domain_scores_codex":[0.99865854,0.0004957884,0.00012614223,0.0005108006,0.00011447534,0.00009409608],"domain_scores_gemma":[0.9975405,0.0012115845,0.0004472499,0.00046635384,0.00021674029,0.00011752036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030783082,0.0013471363,0.00172234,0.0020334618,0.00035031667,0.0015738837,0.0007687232,0.00084657175,0.002723686],"category_scores_gemma":[0.0029494155,0.0004678774,0.0076445355,0.00328735,0.0005298649,0.00077086006,0.0010573167,0.0009678219,0.00032494694],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018342615,0.00008131921,0.42310244,0.021850472,0.46155024,0.00065536663,0.00032188607,0.014830056,0.017037435,0.0017137445,0.0058467896,0.05117602],"study_design_scores_gemma":[0.00026057867,0.0003856873,0.62668145,0.0023236433,0.33045873,0.00046738674,0.00044484687,0.0075881514,0.005309514,0.0038640986,0.02209986,0.00011611199],"about_ca_topic_score_codex":0.009163983,"about_ca_topic_score_gemma":0.006516449,"teacher_disagreement_score":0.009163983,"about_ca_system_score_codex":0.0005222619,"about_ca_system_score_gemma":0.0006068601,"threshold_uncertainty_score":0.01822126},"labels":[],"label_agreement":null},{"id":"W4317829457","doi":"10.1029/2022gb007368","title":"Enhanced Transport of Dissolved Methane From the Chukchi Sea to the Central Arctic","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Halocline; Oceanography; Sea ice; Arctic sea ice decline; Arctic ice pack; Arctic; Arctic geoengineering; Geology; Seawater; Environmental science; Canada Basin; Antarctic sea ice; Climatology; Salinity","score_opus":0.010307324382529237,"score_gpt":0.2219929346907133,"score_spread":0.21168561030818406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317829457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994997,0.000059242444,0.00005374189,0.000012096326,0.0000028333586,0.0000014668785,0.0000903785,0.0000047306103,0.0002756666],"genre_scores_gemma":[0.99953914,0.00005172229,0.000098167475,0.000009988952,0.0000024534697,0.0000019557838,0.00011722293,0.0000013014768,0.00017803183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999553,0.0000026673886,0.000003310501,0.000010811097,0.000007119354,0.000020704509],"domain_scores_gemma":[0.99977654,0.00001873779,0.00006723745,0.000009474357,0.000082098464,0.000045914705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010040245,0.00034899148,0.00019322534,0.0006978166,0.0007528989,0.00053403556,0.0001730684,0.00018097201,0.00048928196],"category_scores_gemma":[0.00015084086,0.00021507774,0.00021415202,0.000954512,0.00022628091,0.00021907223,0.00036436785,0.00021127009,0.00005594401],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027353957,0.000030461857,0.88270503,0.00014570187,0.0001453161,0.00055075774,0.000819774,0.0012477003,0.10570268,0.00016776277,0.0002912258,0.007919997],"study_design_scores_gemma":[0.000006029531,0.000027122505,0.9936341,0.000015510013,0.00005274624,0.00009646541,0.0006533224,0.0018091709,0.0032830692,0.000024425657,0.0003889792,0.000008932715],"about_ca_topic_score_codex":0.23852387,"about_ca_topic_score_gemma":0.25286633,"teacher_disagreement_score":0.23852387,"about_ca_system_score_codex":0.0011819421,"about_ca_system_score_gemma":0.0010505399,"threshold_uncertainty_score":0.474271},"labels":[],"label_agreement":null},{"id":"W4353086307","doi":"10.1029/2022gb007651","title":"Memory and Management: Competing Controls on Long‐Term Nitrate Trajectories in U.S. Rivers","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Global Water Futures; Canada First Research Excellence Fund; Pennsylvania State University","keywords":"Environmental science; Eutrophication; Water quality; Watershed; Hydrology (agriculture); Nitrate; Ecosystem; Nutrient; Deposition (geology); Ecology; Structural basin","score_opus":0.00861552342514152,"score_gpt":0.22305814405291458,"score_spread":0.21444262062777306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4353086307","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999116,0.000042635973,0.00028750603,0.00012206473,0.0000019942706,0.0000029404064,0.00010683738,0.0000073153606,0.0003126911],"genre_scores_gemma":[0.9997036,0.000016264024,0.000070681526,0.000014091323,0.0000015152444,0.000002280762,0.00008368199,0.0000023559992,0.000105526204],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99952865,0.00016946232,0.000037284735,0.00013555073,0.000037074224,0.00009199021],"domain_scores_gemma":[0.9945702,0.0032332332,0.0010574191,0.00041350507,0.00028459018,0.00044102475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020083531,0.00018027484,0.0003302135,0.00074543024,0.0005497319,0.0013015388,0.00062253245,0.00072405214,0.0016329202],"category_scores_gemma":[0.009575566,0.0002339861,0.0004893538,0.00066508754,0.0008281017,0.0011105657,0.0010003914,0.00048427907,0.00013842068],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019906151,0.000107109176,0.97150403,0.000013495566,0.00012723594,0.00012836467,0.0004250527,0.018768921,0.0009690642,0.0015452085,0.0003801662,0.0058322735],"study_design_scores_gemma":[0.000012836937,0.000078084195,0.90873015,0.000014434029,0.00003893191,0.00006085444,0.00076317944,0.08697485,0.0002682715,0.0027323612,0.0002971214,0.000028898705],"about_ca_topic_score_codex":0.040678445,"about_ca_topic_score_gemma":0.05630525,"teacher_disagreement_score":0.040678445,"about_ca_system_score_codex":0.0012195697,"about_ca_system_score_gemma":0.0005895245,"threshold_uncertainty_score":0.080883324},"labels":[],"label_agreement":null},{"id":"W4365998692","doi":"10.1029/2023gb007715","title":"Linking Dissolved Organic Matter to CO<sub>2</sub> and CH<sub>4</sub> Concentrations in Canadian and Chilean Peatland Pools","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Agencia Nacional de Investigación y Desarrollo; Groupe de recherche interuniversitaire en limnologie","keywords":"Peat; Dissolved organic carbon; Environmental science; Nutrient; Primary production; Environmental chemistry; Organic matter; Ecosystem; Greenhouse gas; Precipitation; Vegetation (pathology); Hydrology (agriculture); Physical geography; Ecology; Chemistry; Geology; Geography; Biology","score_opus":0.006448654571897196,"score_gpt":0.21872928960779706,"score_spread":0.21228063503589986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4365998692","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99934214,0.000037820173,0.00003304673,0.000008519726,2.3789774e-7,0.0000028908587,0.00030556016,0.000002642164,0.0002672157],"genre_scores_gemma":[0.9993563,0.000032275628,0.00008427759,0.0000053020935,3.0550956e-7,0.0000045034435,0.00030405814,0.000001409814,0.00021150116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999398,0.0000047032763,0.0000025603674,0.000019718089,0.000008440253,0.000024825507],"domain_scores_gemma":[0.999736,0.000036178553,0.000053219974,0.000014215392,0.00010181752,0.000058490856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016989865,0.00018440139,0.0001591776,0.0006590362,0.0006216594,0.0006668418,0.00030298438,0.00013688224,0.0009072233],"category_scores_gemma":[0.0003964463,0.00014560285,0.00014885608,0.0007436289,0.00037472526,0.00017427975,0.00036063165,0.0001427628,0.0000745745],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017652757,0.000024321398,0.9820286,0.000037456215,0.00007034134,0.000114016846,0.00061562785,0.00077725895,0.012244868,0.00009016181,0.00013948933,0.0036812813],"study_design_scores_gemma":[0.0000030629888,0.000005084825,0.99820304,0.0000040923896,0.000010364409,0.000013226782,0.00046518727,0.0005361943,0.0005693458,0.000018515293,0.00016835591,0.0000036370773],"about_ca_topic_score_codex":0.8610367,"about_ca_topic_score_gemma":0.8865308,"teacher_disagreement_score":0.13896328,"about_ca_system_score_codex":0.0030867674,"about_ca_system_score_gemma":0.002665992,"threshold_uncertainty_score":0.2795633},"labels":[],"label_agreement":null},{"id":"W4367054207","doi":"10.1029/2022gb007658","title":"Inland Water Greenhouse Gas Budgets for RECCAP2: 2. Regionalization and Homogenization of Estimates","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Key Research and Development Program of China; Natural Environment Research Council; HORIZON EUROPE Framework Programme; Svenska Forskningsrådet Formas; European Commission; Sight Research UK; European Resuscitation Council; Agence Nationale de la Recherche; National Aeronautics and Space Administration; National Science Foundation","keywords":"Greenhouse gas; Environmental science; Nitrous oxide; Carbon dioxide; Methane; STREAMS; Hydrology (agriculture); Atmospheric sciences; Global warming; Carbon dioxide equivalent; Climate change; Oceanography; Chemistry; Geology","score_opus":0.008402186887283586,"score_gpt":0.2214747238301547,"score_spread":0.21307253694287112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367054207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86702013,0.0014928912,0.029809257,0.0005699501,0.0000360522,0.0001745028,0.071821734,0.0007958837,0.028279621],"genre_scores_gemma":[0.9320808,0.0006788783,0.027267303,0.000107446256,0.000026855367,0.00025215448,0.037230074,0.00029070367,0.0020657824],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999741,0.00007360808,0.000017258024,0.00007836907,0.000058091948,0.000031723055],"domain_scores_gemma":[0.99966764,0.000041116316,0.000067162895,0.00005368489,0.00015469987,0.000015636533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000615664,0.00063903944,0.00030664945,0.0011268379,0.00014495509,0.00062420993,0.00046922197,0.00027419627,0.001446819],"category_scores_gemma":[0.0007810925,0.00028184592,0.00066303636,0.0026898102,0.00014689963,0.00069197366,0.0004914531,0.00018468434,0.0004579609],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00071571005,0.00019812101,0.23510331,0.001000271,0.0017512497,0.0003016551,0.00046165666,0.550901,0.041930564,0.010624277,0.011234387,0.14577782],"study_design_scores_gemma":[0.00023217087,0.00018986898,0.5996024,0.00020634923,0.0009097702,0.0001884897,0.0005434778,0.25740355,0.046318658,0.00604093,0.088242434,0.000121935096],"about_ca_topic_score_codex":0.030329205,"about_ca_topic_score_gemma":0.029860811,"teacher_disagreement_score":0.030329205,"about_ca_system_score_codex":0.0011432791,"about_ca_system_score_gemma":0.00056256,"threshold_uncertainty_score":0.060305297},"labels":[],"label_agreement":null},{"id":"W4367054220","doi":"10.1029/2022gb007657","title":"Inland Water Greenhouse Gas Budgets for RECCAP2: 1. State‐Of‐The‐Art of Global Scale Assessments","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"HORIZON EUROPE European Research Council; Natural Environment Research Council; National Key Research and Development Program of China; Svenska Forskningsrådet Formas; Ministero dell’Istruzione, dell’Università e della Ricerca; European Commission; Agence Nationale de la Recherche; HORIZON EUROPE Framework Programme; Univerzita Karlova v Praze; Dipartimenti di Eccellenza; Sight Research UK; National Aeronautics and Space Administration; Vetenskapsrådet; National Science Foundation","keywords":"Greenhouse gas; Environmental science; Water cycle; Carbon cycle; Methane; Scale (ratio); Carbon sequestration; Surface water; Carbon dioxide; Nitrous oxide; Atmosphere (unit); Atmospheric sciences; Hydrology (agriculture); Climatology; Meteorology; Environmental engineering; Geography; Oceanography; Ecology; Geology; Ecosystem","score_opus":0.011243674040966923,"score_gpt":0.2402995553242828,"score_spread":0.22905588128331586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367054220","genre_codex":"empirical","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.48161528,0.100034565,0.21048947,0.009101185,0.0005899083,0.00040301387,0.08634248,0.0035258646,0.10789832],"genre_scores_gemma":[0.87263906,0.027872337,0.07388358,0.00065802335,0.00023066433,0.00031918098,0.021191964,0.00046896123,0.002736331],"study_design_codex":"simulation_or_modeling","study_design_gemma":"not_applicable","domain_scores_codex":[0.999694,0.00009775077,0.000017014083,0.00007437033,0.00008868485,0.000028255452],"domain_scores_gemma":[0.99927634,0.00014965731,0.00012862151,0.000079953905,0.000332581,0.00003279725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015044915,0.0011598455,0.00040131324,0.0012155981,0.00018335697,0.001378001,0.0007660836,0.00068807375,0.0012337087],"category_scores_gemma":[0.0013169253,0.00026287066,0.0004851498,0.002390845,0.00035315502,0.0024775795,0.000828078,0.00046096143,0.00037135853],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039472774,0.0001524787,0.05877092,0.0030835501,0.0010199101,0.00019795897,0.00016040458,0.4643633,0.020485803,0.028863909,0.026477868,0.3960292],"study_design_scores_gemma":[0.00009103672,0.00031414995,0.13118254,0.0018792727,0.00074846856,0.00018776362,0.0005361093,0.5548055,0.03502432,0.053095,0.22185245,0.00028346648],"about_ca_topic_score_codex":0.016981551,"about_ca_topic_score_gemma":0.014921642,"teacher_disagreement_score":0.016981551,"about_ca_system_score_codex":0.0014313938,"about_ca_system_score_gemma":0.0007399899,"threshold_uncertainty_score":0.033765376},"labels":[],"label_agreement":null},{"id":"W4368363948","doi":"10.1029/2022gb007616","title":"Oxygen Depletion in Arctic Lakes: Circumpolar Trends, Biogeochemical Processes, and Implications of Climate Change","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Center for Northern Studies; Makivik Corporation","funders":"Natural Sciences and Engineering Research Council of Canada; Canada First Research Excellence Fund; Fonds de recherche du Québec – Nature et technologies; Université Laval","keywords":"Biogeochemical cycle; Circumpolar star; Oceanography; Climate change; Arctic; Environmental science; The arctic; Oxygen; Climatology; Geology; Environmental chemistry; Chemistry","score_opus":0.017142648272148165,"score_gpt":0.2533798355739851,"score_spread":0.2362371873018369,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4368363948","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3477111,0.64846396,0.0006714251,0.0006766447,0.000118064585,0.0000127568255,0.0014019427,0.000010183284,0.0009339914],"genre_scores_gemma":[0.85584426,0.14221883,0.0008840057,0.00023301758,0.0001545875,0.000016377184,0.0005156896,0.0000031943323,0.00013007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99965143,0.00013528545,0.00006539862,0.0000799464,0.000045923323,0.000022058744],"domain_scores_gemma":[0.99825233,0.00079858233,0.00056194514,0.000038713544,0.00028998742,0.000058410064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013805347,0.00025847027,0.0004092925,0.0024554853,0.00022041461,0.0008699599,0.00015244064,0.00021668593,0.00026821805],"category_scores_gemma":[0.0017633892,0.00014106899,0.00077035005,0.0034979957,0.00024530586,0.000359195,0.00030947695,0.00019696067,0.00003262278],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002733752,0.000043012442,0.84472334,0.012663244,0.0055911043,0.00016671693,0.0007514524,0.0014181233,0.0024518764,0.0005982931,0.0009204007,0.1303991],"study_design_scores_gemma":[0.000010223743,0.00012787574,0.98599917,0.0023422297,0.0029089926,0.00012307569,0.00071639154,0.0010174834,0.00046056058,0.00050538854,0.0057721864,0.000016474758],"about_ca_topic_score_codex":0.022941466,"about_ca_topic_score_gemma":0.037151426,"teacher_disagreement_score":0.022941466,"about_ca_system_score_codex":0.0004705877,"about_ca_system_score_gemma":0.0007410735,"threshold_uncertainty_score":0.045615852},"labels":[],"label_agreement":null},{"id":"W4379876208","doi":"10.1029/2022gb007680","title":"Bioavailability of Macro and Micronutrients Across Global Topsoils: Main Drivers and Global Change Impacts","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Aquatic Ecosystems and Phytoplankton Dynamics","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Northern British Columbia; Agriculture and Agri-Food Canada; Wildlife Conservation Society Canada; McGill University; University of Regina; Fiducie de Recherche sur la Forêt des Cantons-de-l’Est; University of Alberta; Université Laval; Lakehead University; University of Waterloo; Université TÉLUQ","funders":"National Institute of Food and Agriculture; Ministerio de Ciencia e Innovación","keywords":"Biogeochemical cycle; Bioavailability; Topsoil; Environmental chemistry; Context (archaeology); Environmental science; Ecosystem; Global change; Terrestrial ecosystem; Environmental change; Chemistry; Earth science; Soil science; Soil water; Climate change; Ecology; Geology; Biology","score_opus":0.013957407761110036,"score_gpt":0.2666779361234339,"score_spread":0.25272052836232384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379876208","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949393,0.0016057733,0.0011931176,0.00012221398,0.000010042923,0.000012303556,0.0011686428,0.000035133435,0.00091335236],"genre_scores_gemma":[0.9982735,0.00042451403,0.00073256047,0.000043850298,0.0000065969216,0.0000064383858,0.0003468163,0.000008048304,0.00015781027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997423,0.00002766025,0.000015581683,0.00014107849,0.000041827036,0.000031509415],"domain_scores_gemma":[0.9995086,0.000077118624,0.00017343255,0.00004278427,0.00016379598,0.000034145065],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045946005,0.00036219918,0.00040490893,0.00074674666,0.00038016637,0.00083702535,0.00027389475,0.0004936248,0.00081539823],"category_scores_gemma":[0.00042158517,0.00019359139,0.00028573687,0.0010325374,0.00043080485,0.0006121157,0.000549414,0.00032216334,0.0001768925],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030414108,0.000038047143,0.5816988,0.00045258863,0.00039745294,0.00014738136,0.00044423412,0.0013677906,0.3941028,0.0002450357,0.00023936322,0.020562334],"study_design_scores_gemma":[0.0000040175264,0.00008592652,0.98623925,0.000016576825,0.00006400997,0.000070495356,0.00055237307,0.00097170623,0.010081425,0.000320103,0.0015795596,0.000014605758],"about_ca_topic_score_codex":0.0136990165,"about_ca_topic_score_gemma":0.014412005,"teacher_disagreement_score":0.0136990165,"about_ca_system_score_codex":0.0005003087,"about_ca_system_score_gemma":0.00029806272,"threshold_uncertainty_score":0.027238548},"labels":[],"label_agreement":null},{"id":"W4382981940","doi":"10.1029/2023gb007759","title":"Remote Sensing Soil Freeze‐Thaw Status and North American N <sub>2</sub> O Emissions From a Regional Inversion","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Growing season; Nitrous oxide; Fertilizer; Atmospheric sciences; Inversion (geology); Nitrogen; Seasonality; Annual cycle; Climatology; Agronomy; Hydrology (agriculture); Ecology; Chemistry; Geology; Biology","score_opus":0.029055397213471883,"score_gpt":0.23604246836138165,"score_spread":0.20698707114790976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382981940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997809,0.000019606914,0.00037467052,0.000024728397,0.0000031694663,0.0000032995038,0.0011621045,0.00004467101,0.0005586769],"genre_scores_gemma":[0.9972535,0.000018231298,0.0005270655,0.000008505991,0.0000028805473,0.000003302904,0.0020629494,0.00000482823,0.000118919175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993336,0.000009832236,0.0000033815397,0.000022956323,0.000013118433,0.000017352882],"domain_scores_gemma":[0.9998822,0.000017838845,0.00002669233,0.000013606171,0.000044950943,0.000014680622],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002638069,0.00022225462,0.00012958831,0.00033435415,0.00019258432,0.00022786683,0.00018614871,0.0001542667,0.0005433006],"category_scores_gemma":[0.00036968352,0.00011489864,0.00032522832,0.00047755035,0.00012209365,0.00022427304,0.00017796629,0.00018965466,0.00008896421],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005460941,0.0001629637,0.86823356,0.000044567943,0.00025517508,0.0001458083,0.00015448823,0.08251525,0.02015855,0.00033952342,0.0025858406,0.024858117],"study_design_scores_gemma":[0.000052539588,0.000038932933,0.8933964,0.000009089371,0.00007502973,0.00003404601,0.00013784927,0.101454064,0.0029356526,0.00013314065,0.0017105677,0.000022826456],"about_ca_topic_score_codex":0.1540747,"about_ca_topic_score_gemma":0.25086477,"teacher_disagreement_score":0.1540747,"about_ca_system_score_codex":0.00049932866,"about_ca_system_score_gemma":0.000560962,"threshold_uncertainty_score":0.30635577},"labels":[],"label_agreement":null},{"id":"W4385667909","doi":"10.1029/2023gb007813","title":"The Role of Wildfires in the Interplay of Forest Carbon Stocks and Wood Harvest in the Contiguous United States During the 20th Century","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"HORIZON EUROPE European Research Council; Universität für Bodenkultur Wien; Austrian Science Fund; European Commission","keywords":"Environmental science; Stock (firearms); Ecosystem; Climate change; Biomass (ecology); Agroforestry; Forestry; Land use, land-use change and forestry; Carbon sequestration; Primary production; Land use; Grazing; Forest ecology; Ecology; Geography; Carbon dioxide; Biology","score_opus":0.0028804593916430207,"score_gpt":0.20603952479418963,"score_spread":0.2031590654025466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385667909","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994255,0.0013832399,0.00019224879,0.00078848196,0.000037688093,0.0000035164946,0.00086753,0.000008087441,0.0024642118],"genre_scores_gemma":[0.9981589,0.00072585116,0.000103408835,0.00013806665,0.000034913046,0.000003735882,0.0005325313,0.0000050674294,0.0002976986],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998406,0.00003046591,0.00002065642,0.00004440464,0.000027431679,0.000036433343],"domain_scores_gemma":[0.9992236,0.000104707724,0.00033947863,0.00004725591,0.00015167879,0.0001333169],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058327266,0.00016695035,0.00013315209,0.00067061314,0.00049207447,0.0010696047,0.00025116262,0.00030473442,0.0010653432],"category_scores_gemma":[0.0014915329,0.00015416363,0.00018464171,0.0009240003,0.00048710272,0.0006070782,0.0008452104,0.00050458836,0.000110581124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000055596935,0.000032545835,0.97822773,0.000037821654,0.0000858493,0.000145561,0.0008112394,0.00082854123,0.00035800476,0.00090546865,0.0013898684,0.017121648],"study_design_scores_gemma":[0.000002366798,0.0000112161715,0.9958348,0.000032295688,0.000024058232,0.000044882785,0.0006835423,0.00080572115,0.00010031436,0.000376366,0.002076945,0.0000073367723],"about_ca_topic_score_codex":0.080879994,"about_ca_topic_score_gemma":0.14841732,"teacher_disagreement_score":0.080879994,"about_ca_system_score_codex":0.00074441725,"about_ca_system_score_gemma":0.0005059179,"threshold_uncertainty_score":0.1608184},"labels":[],"label_agreement":null},{"id":"W4385794468","doi":"10.1029/2023gb007854","title":"Quantification of Discharge‐Specific Effects on Dissolved Organic Matter Export From Major Arctic Rivers From 1982 Through 2019","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Goddard Space Flight Center; National Aeronautics and Space Administration; National Science Foundation","keywords":"Dissolved organic carbon; Colored dissolved organic matter; Environmental science; Arctic; Discharge; Hydrology (agriculture); Surface runoff; Organic matter; Oceanography; Drainage basin; Geology; Phytoplankton; Ecology; Nutrient; Geography","score_opus":0.011550040051339762,"score_gpt":0.21234409168866217,"score_spread":0.20079405163732242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385794468","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979615,0.00004449725,0.00014953568,0.000013271514,0.00000235778,0.0000025022864,0.0013770021,0.0000117031595,0.0004375995],"genre_scores_gemma":[0.9958897,0.000073347175,0.0002313592,0.00001055786,0.0000048249435,0.000008263898,0.0034029777,0.000005794053,0.0003731695],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987876,0.000016776967,0.000010781379,0.00004716039,0.000028439576,0.000018009634],"domain_scores_gemma":[0.99964786,0.0000774557,0.00011766007,0.000023008542,0.00009982606,0.000034242046],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000316576,0.00024150895,0.00018533581,0.0004212186,0.00022355423,0.00050695986,0.00014472335,0.00016565545,0.00040129296],"category_scores_gemma":[0.00063907413,0.00013064928,0.00033210177,0.000706617,0.00010831448,0.00026726484,0.00032160236,0.00016873817,0.00013041143],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013947152,0.00001922974,0.98975146,0.000021069,0.00007422458,0.000065396474,0.000086392945,0.0017728652,0.004099861,0.00003407475,0.0001339698,0.0038020932],"study_design_scores_gemma":[0.0000011479502,0.000011087182,0.9982445,0.0000017197245,0.000009475703,0.000010270154,0.00003328371,0.0010363596,0.00042831042,0.00000611669,0.00021566026,0.000002020561],"about_ca_topic_score_codex":0.037031103,"about_ca_topic_score_gemma":0.060402833,"teacher_disagreement_score":0.037031103,"about_ca_system_score_codex":0.00078459864,"about_ca_system_score_gemma":0.0003336558,"threshold_uncertainty_score":0.07363117},"labels":[],"label_agreement":null},{"id":"W4386316720","doi":"10.1029/2023gb007820","title":"Decadal Changes in Anthropogenic Inputs and Precipitation Influence Riverine Exports of Carbon, Nitrogen, and Phosphorus, and Alter Ecosystem Level Stoichiometry","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ecosystem; Environmental science; Precipitation; Phosphorus; Ecological stoichiometry; Temperate climate; Drainage basin; Hydrology (agriculture); Nitrogen; Nutrient; Environmental chemistry; Ecology; Geography; Chemistry; Geology; Biology","score_opus":0.009677925145632116,"score_gpt":0.2340977153031352,"score_spread":0.22441979015750307,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386316720","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972742,0.000091848655,0.00032181136,0.000025040294,0.0000023172834,0.0000034954417,0.0014151762,0.000012551032,0.0008535394],"genre_scores_gemma":[0.9987319,0.00007409377,0.00019525854,0.000011463905,0.0000019018447,0.0000036767906,0.00060490816,0.0000032534138,0.0003734421],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994457,0.000005893146,0.0000033083222,0.000018095529,0.000016376753,0.000011760551],"domain_scores_gemma":[0.9997563,0.000018940933,0.00006961527,0.000013941842,0.0001165674,0.00002465778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017350444,0.00012806582,0.000095065174,0.00041931722,0.00031181483,0.0005211865,0.00016297151,0.00010897669,0.0006577555],"category_scores_gemma":[0.0002867559,0.00006402336,0.000118003336,0.00069935416,0.00022183817,0.00019103491,0.0001712378,0.00012382433,0.00008091168],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027104748,0.0000085408365,0.9885183,0.000016048562,0.00007545299,0.000033216747,0.00011799687,0.0011148321,0.0053036446,0.00006805015,0.00027210743,0.004444806],"study_design_scores_gemma":[4.3424285e-7,0.0000024352764,0.9989907,0.000001277504,0.0000033185047,0.0000062367158,0.000041661555,0.0005180105,0.00013721194,0.000008470946,0.00028902284,0.0000011110532],"about_ca_topic_score_codex":0.46494487,"about_ca_topic_score_gemma":0.66085404,"teacher_disagreement_score":0.46494487,"about_ca_system_score_codex":0.001694442,"about_ca_system_score_gemma":0.0007394884,"threshold_uncertainty_score":0.92447716},"labels":[],"label_agreement":null},{"id":"W4386956082","doi":"10.1029/2022gb007644","title":"Arctic Permafrost Thawing Enhances Sulfide Oxidation","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Defense Science and Engineering Graduate; Resnick Sustainability Institute for Science, Energy and Sustainability, California Institute of Technology; California Institute of Technology; U.S. Department of Energy; National Science Foundation","keywords":"Permafrost; Weathering; Alkalinity; Biogeochemical cycle; Sulfate; Environmental chemistry; Carbon cycle; Dissolved organic carbon; Arctic; Sulfide; Carbon dioxide; Sediment; Total organic carbon; Biogeochemistry; Environmental science; Sulfur cycle; Geology; Oceanography; Geochemistry; Chemistry; Geomorphology","score_opus":0.029721825482438846,"score_gpt":0.26220436996888824,"score_spread":0.2324825444864494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386956082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995758,0.000016462582,0.00011925512,0.0000037229056,9.697637e-7,5.644942e-7,0.00007937136,0.00000889344,0.00019488696],"genre_scores_gemma":[0.9997526,0.0000109135,0.000068114474,0.0000030299684,3.4594072e-7,5.0834615e-7,0.00007224774,0.0000015614487,0.000090706904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996614,0.0000030392437,0.000002164696,0.000013950567,0.000006400767,0.000008236881],"domain_scores_gemma":[0.99995875,0.0000072714433,0.000011205345,0.0000037964187,0.000011670342,0.000007251956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000062632804,0.0001483389,0.00012655939,0.00013474315,0.000254013,0.00024723122,0.00008552354,0.00012658534,0.0007825796],"category_scores_gemma":[0.00010271734,0.00010670294,0.00014511857,0.00014557634,0.000120192395,0.00014647821,0.00016598908,0.00011838902,0.00006714358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003276452,0.000054929722,0.5416629,0.00007514279,0.000085666274,0.00024183189,0.00026337014,0.011781625,0.43506694,0.00016592324,0.00021863323,0.010055364],"study_design_scores_gemma":[0.000005339182,0.00007165212,0.93225455,0.000005442432,0.000026309513,0.000056939814,0.00035090843,0.023586234,0.043057844,0.00009054835,0.0004842421,0.000009999201],"about_ca_topic_score_codex":0.0226348,"about_ca_topic_score_gemma":0.032820348,"teacher_disagreement_score":0.0226348,"about_ca_system_score_codex":0.00036507263,"about_ca_system_score_gemma":0.00024187536,"threshold_uncertainty_score":0.045006096},"labels":[],"label_agreement":null},{"id":"W4387783386","doi":"10.1029/2023gb007878","title":"Global Nitrogen Mass Flux From the Active Freshwater Aquifer Element Pool","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Aquifer; Groundwater recharge; Flux (metallurgy); Groundwater; Hydrology (agriculture); Nitrogen; Water mass; Geology; Continental shelf; Environmental science; Oceanography; Chemistry","score_opus":0.011375006825404016,"score_gpt":0.22168376786364935,"score_spread":0.21030876103824533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387783386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9715522,0.00062266825,0.004900489,0.00034242054,0.000022257365,0.000013441042,0.013331866,0.00026671716,0.008947929],"genre_scores_gemma":[0.989638,0.0004802888,0.0018363653,0.00006324663,0.000013160095,0.00003125339,0.006740276,0.0000335369,0.0011639817],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999503,0.0000084948015,0.0000034695,0.00001860521,0.000014072558,0.00000508721],"domain_scores_gemma":[0.9998882,0.00002237354,0.000031391806,0.000008621895,0.000042969306,0.000006512351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020410036,0.00034859494,0.00014911393,0.0006674134,0.00009766808,0.0002952514,0.00021412446,0.00022034589,0.00122427],"category_scores_gemma":[0.0003562399,0.00010976619,0.0002656137,0.00079295115,0.00012472649,0.00042868304,0.00030190914,0.00011439574,0.0002305441],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024620444,0.00004493986,0.7747464,0.0003811591,0.00058600504,0.00035360144,0.00017495679,0.089961395,0.04046874,0.005185364,0.005997713,0.0818535],"study_design_scores_gemma":[0.000038033773,0.000056100704,0.9255197,0.000067834866,0.0001576402,0.00016404748,0.00009340852,0.033770774,0.010488851,0.0036543459,0.0259427,0.000046561174],"about_ca_topic_score_codex":0.011689087,"about_ca_topic_score_gemma":0.0070812013,"teacher_disagreement_score":0.011689087,"about_ca_system_score_codex":0.0006736141,"about_ca_system_score_gemma":0.00018906209,"threshold_uncertainty_score":0.023242116},"labels":[],"label_agreement":null},{"id":"W4387817862","doi":"10.1029/2023gb007959","title":"Shifts in the Isotopic Composition of Nitrous Oxide Between El Niño and La Niña in the Eastern Tropical South Pacific","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Upwelling; Biogeochemical cycle; Nitrous oxide; Biogeochemistry; Atmosphere (unit); Oceanography; Water column; Oxygen minimum zone; New production; Environmental chemistry; Environmental science; Geology; Chemistry; Ecology; Biology; Nutrient; Phytoplankton","score_opus":0.013014399332449526,"score_gpt":0.22159976534179912,"score_spread":0.2085853660093496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387817862","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992405,0.00010427561,0.000028622517,0.00003050849,0.0000060860593,0.0000015596328,0.00022432022,0.0000025938275,0.0003616197],"genre_scores_gemma":[0.9989502,0.0001212528,0.00005920333,0.000051755793,0.00000961596,0.000009408545,0.0005136346,0.0000034717202,0.00028149242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994004,0.000006446373,0.000004289732,0.000020559692,0.0000099434965,0.000018740318],"domain_scores_gemma":[0.9997714,0.000028518187,0.00007381791,0.00000797787,0.00005951443,0.000058907182],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015899709,0.00017160509,0.00014190262,0.00040117823,0.00034652028,0.0003929879,0.00014947893,0.00021377255,0.0006016048],"category_scores_gemma":[0.00026250424,0.000118180586,0.00014298869,0.00034002,0.00031278905,0.000267192,0.00033877528,0.00023347151,0.00008684049],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058364094,0.00005575204,0.8920647,0.00006541251,0.0001256351,0.0002273201,0.0009978227,0.0002191817,0.09974211,0.00008521211,0.00027978024,0.005553506],"study_design_scores_gemma":[0.0000022229722,0.000010599949,0.9991603,0.0000022925396,0.000006405815,0.000013280589,0.00021845444,0.00006263834,0.00037085757,0.000008509326,0.0001424452,0.0000019943288],"about_ca_topic_score_codex":0.031234019,"about_ca_topic_score_gemma":0.052838776,"teacher_disagreement_score":0.031234019,"about_ca_system_score_codex":0.00043918326,"about_ca_system_score_gemma":0.00031678192,"threshold_uncertainty_score":0.062104464},"labels":[],"label_agreement":null},{"id":"W4388023630","doi":"10.1029/2023gb007744","title":"Central Role of Nitrogen Fertilizer Relative to Water Management in Determining Direct Nitrous Oxide Emissions From Global Rice‐Based Ecosystems","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University; Université du Québec à Montréal","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; China Scholarship Council","keywords":"Environmental science; Fertilizer; Ecosystem; Biogeochemical cycle; Nitrous oxide; Agriculture; Greenhouse gas; Paddy field; Agronomy; Irrigation; Agroecosystem; Nitrogen; Atmospheric sciences; Environmental chemistry; Ecology; Chemistry; Biology","score_opus":0.008871217308024221,"score_gpt":0.23043165646636188,"score_spread":0.22156043915833765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388023630","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99734735,0.00023420644,0.0014099055,0.000034719676,0.00000679975,0.000009976444,0.00016579588,0.000018317265,0.0007729734],"genre_scores_gemma":[0.99907446,0.00013982561,0.00060532545,0.000009180598,0.000001096534,0.000004615308,0.000078275225,0.0000035133855,0.0000837052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998915,0.000017680126,0.000005851086,0.000053584725,0.000017337368,0.000014076495],"domain_scores_gemma":[0.99989855,0.000042649106,0.000024085371,0.0000068392383,0.000020926173,0.0000069326256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003871547,0.0004429226,0.00016651078,0.00024545184,0.0001675444,0.0003631399,0.00017732904,0.00029285473,0.00030494048],"category_scores_gemma":[0.00041555002,0.00013027272,0.00031931803,0.00028023717,0.00025487784,0.0005288301,0.00023679911,0.0001316339,0.0000449893],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032227967,0.0000818503,0.672833,0.00023923094,0.0002406423,0.0003458585,0.000093121496,0.115879096,0.17937349,0.00064310903,0.00022183241,0.029726408],"study_design_scores_gemma":[0.000035728277,0.0001534524,0.72634786,0.000033074593,0.00015500427,0.0000834873,0.00032932032,0.2372557,0.033186384,0.0010327919,0.0013516472,0.000035584646],"about_ca_topic_score_codex":0.019230882,"about_ca_topic_score_gemma":0.023025606,"teacher_disagreement_score":0.019230882,"about_ca_system_score_codex":0.0006918405,"about_ca_system_score_gemma":0.00048574604,"threshold_uncertainty_score":0.03823787},"labels":[],"label_agreement":null},{"id":"W4388682634","doi":"10.1029/2023gb007844","title":"Trace Element Geochemistry in North Pacific Red Clay Sediment Porewaters and Implications for Water‐Column Studies","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Geology; Trace element; Water column; Sediment; Environmental chemistry; Pelagic sediment; Benthic zone; Sulfate; Manganese; Trace metal; Mineralogy; Geochemistry; Oceanography; Chemistry; Metal; Geomorphology","score_opus":0.018244186929173352,"score_gpt":0.25127987145547587,"score_spread":0.23303568452630252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388682634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985959,0.00032559226,0.00012908316,0.00002695446,0.000002246354,0.0000049101113,0.00026654525,0.0000116319625,0.0006372279],"genre_scores_gemma":[0.9984236,0.00036410952,0.00043135774,0.000024153644,0.0000025069473,0.0000059492354,0.00024138804,0.0000042874685,0.00050273567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991024,0.0000079599695,0.000006334535,0.00003584941,0.00002352771,0.000016184134],"domain_scores_gemma":[0.9998272,0.000021268186,0.000053399213,0.000006702551,0.00006197845,0.000029431578],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019314411,0.0002821718,0.00020570711,0.00087371224,0.00061946246,0.0007229463,0.00032043082,0.00027003957,0.0005779422],"category_scores_gemma":[0.00024078517,0.0001883519,0.0001597021,0.0009853232,0.00035049923,0.00033107845,0.0002719388,0.00016678615,0.00011030088],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014646974,0.000031774212,0.9230072,0.000106840365,0.00006205528,0.00017805785,0.00074134266,0.00049384276,0.06357401,0.00009822351,0.00010028151,0.011459807],"study_design_scores_gemma":[0.0000022946456,0.00003079563,0.9958411,0.000010755717,0.000014544465,0.000030794276,0.00060123764,0.0004058691,0.0024323286,0.000025136454,0.00060011895,0.0000049216546],"about_ca_topic_score_codex":0.1788321,"about_ca_topic_score_gemma":0.18255393,"teacher_disagreement_score":0.1788321,"about_ca_system_score_codex":0.0011545231,"about_ca_system_score_gemma":0.0007179668,"threshold_uncertainty_score":0.35558242},"labels":[],"label_agreement":null},{"id":"W4390115824","doi":"10.1029/2023gb007804","title":"Neutral Tropical African CO <sub>2</sub> Exchange Estimated From Aircraft and Satellite Observations","year":2023,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Nuclear Safety and Security Commission; University of Oklahoma; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Satellite; Environmental science; Atmospheric sciences; Flux (metallurgy); Carbon cycle; Tropical Atlantic; Climatology; Dry season; Carbon flux; Geography; Sea surface temperature; Geology; Physics; Chemistry; Ecology","score_opus":0.017846104436991087,"score_gpt":0.23027898653497392,"score_spread":0.21243288209798283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390115824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99826616,0.000046712878,0.0002506734,0.000024110992,0.0000035441756,0.0000027376193,0.0009165243,0.000014230315,0.0004753315],"genre_scores_gemma":[0.9985393,0.000031033764,0.0002158186,0.00000593046,0.0000044209423,0.000003312867,0.0011401081,0.0000048114716,0.000055226723],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998951,0.000021951206,0.0000080315585,0.000029847857,0.000017897471,0.00002721382],"domain_scores_gemma":[0.9997354,0.00005645149,0.000086605236,0.000034658402,0.000065072876,0.000021727883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000295203,0.00037705264,0.00019467367,0.000498659,0.00028827618,0.0004850164,0.0002261543,0.00025764506,0.0007288234],"category_scores_gemma":[0.00088065956,0.00016796892,0.00030563696,0.00071624026,0.00014479099,0.00056651735,0.00028712853,0.00019062585,0.00016164873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031963483,0.000065043874,0.94284344,0.00006874123,0.00025378255,0.00018534981,0.00011973123,0.02734111,0.017732244,0.0002849055,0.0008814643,0.00990457],"study_design_scores_gemma":[0.000020274856,0.000023792805,0.9576714,0.00001631495,0.00006663643,0.000060297756,0.00010363727,0.038509067,0.0026294466,0.00010857478,0.000776178,0.000014238829],"about_ca_topic_score_codex":0.04153914,"about_ca_topic_score_gemma":0.048636302,"teacher_disagreement_score":0.04153914,"about_ca_system_score_codex":0.00044542897,"about_ca_system_score_gemma":0.00030887383,"threshold_uncertainty_score":0.08259469},"labels":[],"label_agreement":null},{"id":"W4391051693","doi":"10.1029/2023gb007803","title":"A Synthesis of Global Coastal Ocean Greenhouse Gas Fluxes","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Climate Program Office; National Oceanic and Atmospheric Administration; Nuclear Safety and Security Commission; Fonds Wetenschappelijk Onderzoek; European Commission; Belgian Federal Science Policy Office; National Aeronautics and Space Administration; National Science Foundation","keywords":"Environmental science; Biogeochemical cycle; Sink (geography); Greenhouse gas; Oceanography; Latitude; Climatology; Atmospheric sciences; Carbon cycle; Geology; Chemistry; Geography; Environmental chemistry; Ecosystem; Ecology","score_opus":0.007702287345748736,"score_gpt":0.20830757636128724,"score_spread":0.2006052890155385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391051693","genre_codex":"dataset","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13361536,0.073855825,0.20233488,0.0069114445,0.0058129034,0.00052946474,0.41237807,0.008777498,0.1557846],"genre_scores_gemma":[0.5781633,0.06947732,0.13347465,0.0011036791,0.0015365664,0.0008244115,0.19168559,0.0013825202,0.022351932],"study_design_codex":"design_other","study_design_gemma":"systematic_review","domain_scores_codex":[0.9997813,0.000026218408,0.000027825155,0.0000829307,0.00006280766,0.000019026133],"domain_scores_gemma":[0.9995005,0.00006807243,0.000060263297,0.000065822824,0.00027004787,0.000035267618],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006433661,0.0015194165,0.0006867426,0.0036189817,0.00032970705,0.001774763,0.00033421325,0.00052897853,0.011406982],"category_scores_gemma":[0.0011553311,0.00038030578,0.0010290061,0.006763335,0.00014107075,0.0014818665,0.00089857954,0.00053016626,0.0024431136],"study_design_candidate":"systematic_review","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034620258,0.00009906081,0.034747347,0.0069013475,0.0013485348,0.00042701987,0.00022500608,0.11162218,0.016329983,0.036076963,0.09461715,0.6972592],"study_design_scores_gemma":[0.000118183816,0.00014770907,0.0975351,0.0021788338,0.0010278447,0.00015915056,0.0004502452,0.0695613,0.009711839,0.036448047,0.7824993,0.00016247456],"about_ca_topic_score_codex":0.02415221,"about_ca_topic_score_gemma":0.016311863,"teacher_disagreement_score":0.02415221,"about_ca_system_score_codex":0.0013813154,"about_ca_system_score_gemma":0.0019218761,"threshold_uncertainty_score":0.048023283},"labels":[],"label_agreement":null},{"id":"W4393223911","doi":"10.1029/2023gb008051","title":"Overwinter and Spring Thaw Nitrous Oxide Fluxes in a Northern Prairie Cropland Are Limited but a Significant Proportion of Annual Emissions","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; University of Guelph","funders":"Saskatchewan Wheat Development Commission; Saskatchewan Canola Development Commission; Ministry of Agriculture - Saskatchewan","keywords":"Nitrous oxide; Environmental science; Growing season; Atmospheric sciences; Nitrate; Climate change; Hydrology (agriculture); Animal science; Agronomy; Climatology; Ecology; Biology","score_opus":0.009816848160974011,"score_gpt":0.22097356312405433,"score_spread":0.21115671496308033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393223911","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998047,0.000012397408,0.000021087855,0.000004084038,2.5213936e-7,9.4823025e-7,0.000070525384,0.0000010796801,0.0000849476],"genre_scores_gemma":[0.999501,0.000032545424,0.00010745467,0.0000047693293,7.669155e-7,0.000002719893,0.00022358535,8.40089e-7,0.00012637742],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994004,0.0000059980425,0.0000038484754,0.000021879709,0.000010723691,0.000017489167],"domain_scores_gemma":[0.99979323,0.00004108859,0.00006021464,0.000014123261,0.000044302968,0.000046996523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019759871,0.00016715282,0.00016174895,0.00035566557,0.00048236278,0.00033644805,0.00026276917,0.000161276,0.0004117904],"category_scores_gemma":[0.00024498845,0.00015706995,0.00013727005,0.00036922088,0.0003181976,0.00029627726,0.00022583973,0.0001704362,0.00006314803],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011131764,0.000053015614,0.972779,0.000018891586,0.000050782215,0.00012679395,0.0004843668,0.0006890529,0.021992525,0.00002368196,0.00009029465,0.0035801793],"study_design_scores_gemma":[0.0000019635606,0.000011736889,0.99904865,0.0000012450218,0.0000044793674,0.000013038805,0.00014651725,0.00047454773,0.00022043227,0.000005976817,0.00006982335,0.0000016743537],"about_ca_topic_score_codex":0.3186622,"about_ca_topic_score_gemma":0.60333097,"teacher_disagreement_score":0.3186622,"about_ca_system_score_codex":0.0010718002,"about_ca_system_score_gemma":0.0008020099,"threshold_uncertainty_score":0.6336148},"labels":[],"label_agreement":null},{"id":"W4393947366","doi":"10.1029/2023gb007953","title":"The Net GHG Balance and Budget of the Permafrost Region (2000–2020) From Ecosystem Flux Upscaling","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Horizon 2020 Framework Programme; HORIZON EUROPE Framework Programme; Svenska Forskningsrådet Formas; Global Foundation for Eating Disorders; Academy of Finland; Gordon and Betty Moore Foundation; National Science Foundation","keywords":"Permafrost; Flux (metallurgy); Environmental science; Ecosystem; Balance (ability); Greenhouse gas; Atmospheric sciences; Hydrology (agriculture); Earth science; Physical geography; Geology; Ecology; Geography; Oceanography; Chemistry; Biology","score_opus":0.012855784327405967,"score_gpt":0.22136127815258555,"score_spread":0.20850549382517958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393947366","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9568969,0.0011321913,0.011902102,0.00015103005,0.00004287808,0.00003813466,0.024982804,0.00064455986,0.0042094723],"genre_scores_gemma":[0.95168215,0.0006125047,0.01791507,0.0000756008,0.000034560228,0.00005465988,0.02882763,0.00008264155,0.00071510096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998115,0.000031635922,0.000015632046,0.00005617956,0.000064865664,0.000020343494],"domain_scores_gemma":[0.9996592,0.00004649103,0.00007713105,0.00005025652,0.00013930061,0.000027617463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073624647,0.00079528306,0.0003248258,0.0015098102,0.0002047914,0.0006733682,0.00044702878,0.0003706298,0.0011736444],"category_scores_gemma":[0.0008188756,0.00035117284,0.0008221963,0.001776657,0.00014634838,0.0010705313,0.00034003248,0.00021779783,0.0004623208],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040983135,0.0001882462,0.52516484,0.00045818026,0.0012191753,0.00029640796,0.00010352716,0.24618974,0.029538631,0.0010940629,0.0050671143,0.19027022],"study_design_scores_gemma":[0.000078172736,0.00013141092,0.71864563,0.00015228937,0.0003714101,0.00017618162,0.0000975154,0.24695782,0.014401203,0.002261584,0.016644176,0.00008264162],"about_ca_topic_score_codex":0.027672889,"about_ca_topic_score_gemma":0.02705754,"teacher_disagreement_score":0.027672889,"about_ca_system_score_codex":0.0010084357,"about_ca_system_score_gemma":0.0006248566,"threshold_uncertainty_score":0.05502361},"labels":[],"label_agreement":null},{"id":"W4394850093","doi":"10.1029/2023gb007909","title":"A Carbon Source in a Carbon Sink: Carbon Dioxide and Methane Dynamics in Open‐Water Peatland Pools","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Hydro-Québec; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Groupe de recherche interuniversitaire en limnologie; Hydro-Québec; Université du Québec à Montréal","keywords":"Peat; Carbon dioxide; Environmental chemistry; Methanogenesis; Environmental science; Water table; Dissolved organic carbon; Greenhouse gas; Carbon sink; Carbon fibers; Biogeochemical cycle; Carbon cycle; Methane; Bog; Sink (geography); Chemistry; Hydrology (agriculture); Ecosystem; Groundwater; Ecology; Geology; Oceanography","score_opus":0.007180463448040572,"score_gpt":0.23535465910747175,"score_spread":0.22817419565943117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394850093","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997485,0.000023332317,0.000055823497,0.0000030595038,2.8074928e-7,0.0000011890082,0.0000604588,0.0000016522816,0.00010575521],"genre_scores_gemma":[0.999703,0.000017351764,0.00009146585,0.0000018071763,3.587245e-7,0.0000016349601,0.00007418661,7.970728e-7,0.00010943458],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999633,0.000003509509,0.0000022548638,0.00000885026,0.000006747089,0.000015252538],"domain_scores_gemma":[0.9999019,0.000012867669,0.000021645641,0.00000407577,0.000028109567,0.000031359174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000110113826,0.00014201159,0.00012545493,0.0004404637,0.00029985065,0.00041788007,0.00016860965,0.00016285127,0.00041620218],"category_scores_gemma":[0.00013763482,0.000100006386,0.00011218842,0.00032813378,0.00025563568,0.000267352,0.0001700108,0.000057911177,0.00007117595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037350185,0.000078794576,0.8296011,0.00006080811,0.00008128725,0.00045032994,0.0004669047,0.005066739,0.15466765,0.00018817445,0.00014429927,0.008820502],"study_design_scores_gemma":[0.0000036647564,0.000032128584,0.98917925,0.000004636036,0.000010601766,0.00004354341,0.00029574326,0.0060372865,0.0040953667,0.000077467,0.0002136262,0.0000067096053],"about_ca_topic_score_codex":0.1646039,"about_ca_topic_score_gemma":0.20475355,"teacher_disagreement_score":0.1646039,"about_ca_system_score_codex":0.00078879227,"about_ca_system_score_gemma":0.00071649934,"threshold_uncertainty_score":0.32729155},"labels":[],"label_agreement":null},{"id":"W4400688879","doi":"10.1029/2023gb008048","title":"Physical Mechanisms Sustaining Silica Production Following the Demise of the Diatom Phase of the North Atlantic Spring Phytoplankton Bloom During EXPORTS","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Ocean Frontier Institute; National Aeronautics and Space Administration; Earth Sciences Division; National Science Foundation","keywords":"Diatom; Phytoplankton; Spring bloom; Bloom; Oceanography; Spring (device); Demise; Algal bloom; Environmental science; Plankton; Geology; Ecology; Biology; Nutrient","score_opus":0.006746619701326969,"score_gpt":0.2129134987196025,"score_spread":0.20616687901827552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400688879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985475,0.00014883222,0.00012148397,0.00006119548,0.000004025865,0.000008719801,0.00021219047,0.00000839859,0.00088761956],"genre_scores_gemma":[0.99909234,0.000059145666,0.00008718011,0.00003514885,0.0000045190604,0.000009188558,0.00022063834,0.0000023830562,0.0004894021],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994946,0.000003204916,0.000004082741,0.000014366617,0.000015541216,0.000013405929],"domain_scores_gemma":[0.9997806,0.000024549272,0.00007507759,0.0000089905525,0.000056125184,0.00005469861],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017171916,0.00014222869,0.0002975559,0.00027564968,0.000455985,0.00058281503,0.00021687154,0.0003011129,0.00083529],"category_scores_gemma":[0.00025990378,0.00023900546,0.00017602045,0.00015477104,0.00025016148,0.0002900751,0.0004003475,0.0003554376,0.00018716783],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005632971,0.000055685763,0.3007378,0.00007360531,0.00005679577,0.000342172,0.00042789712,0.00043761145,0.69118315,0.0001936006,0.00038558888,0.0055427505],"study_design_scores_gemma":[0.0000048345405,0.000054269985,0.99475974,0.0000025993581,0.0000061821684,0.00002825081,0.00016735999,0.0004633192,0.0041381666,0.00003774619,0.00033384393,0.0000037651723],"about_ca_topic_score_codex":0.016670097,"about_ca_topic_score_gemma":0.03159977,"teacher_disagreement_score":0.016670097,"about_ca_system_score_codex":0.0011043177,"about_ca_system_score_gemma":0.0003183757,"threshold_uncertainty_score":0.033146143},"labels":[],"label_agreement":null},{"id":"W4400736037","doi":"10.1029/2023gb008010","title":"The Modeled Seasonal Cycles of Surface N <sub>2</sub> O Fluxes and Atmospheric N <sub>2</sub> O","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Dalhousie University","funders":"University of Bern; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Troposphere; Atmospheric sciences; Seasonality; Environmental science; Stratosphere; Flux (metallurgy); Northern Hemisphere; Amplitude; Southern Hemisphere; Ozone; Greenhouse gas; Nitrous oxide; Climatology; Atmosphere (unit); Meteorology; Chemistry; Oceanography; Geology; Geography; Physics","score_opus":0.004678206767177873,"score_gpt":0.20054672623794026,"score_spread":0.1958685194707624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400736037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970348,0.000028664825,0.0010883543,0.000041010804,0.000012921814,0.0000060825996,0.00071069406,0.00010261677,0.00097485975],"genre_scores_gemma":[0.998108,0.000022144823,0.0007268636,0.000014139072,0.0000040153604,0.000013476679,0.00086032593,0.000022633767,0.00022832844],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992216,0.000012785166,0.000004331826,0.00002952732,0.000012579966,0.000018568151],"domain_scores_gemma":[0.9998969,0.000033331875,0.000019486266,0.000011873178,0.000024570023,0.0000138958785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021523962,0.0006799949,0.00030349378,0.00020036334,0.0002912442,0.000482504,0.00045849048,0.00055557257,0.0009655512],"category_scores_gemma":[0.0003063336,0.00031555092,0.00079665554,0.00032453053,0.00023792319,0.00045154602,0.00024106908,0.00032699085,0.00015898496],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000325815,0.00012163467,0.13336323,0.000051422576,0.00031497263,0.00011915982,0.000053420514,0.8400285,0.019099763,0.0003095929,0.0009324605,0.005279948],"study_design_scores_gemma":[0.00010066454,0.00006480544,0.064974345,0.0000062830495,0.00008400055,0.00002202419,0.00007134326,0.9287523,0.0050155125,0.00024630202,0.00063932204,0.000023069353],"about_ca_topic_score_codex":0.04531959,"about_ca_topic_score_gemma":0.035155885,"teacher_disagreement_score":0.04531959,"about_ca_system_score_codex":0.0008204229,"about_ca_system_score_gemma":0.0005513968,"threshold_uncertainty_score":0.09011161},"labels":[],"label_agreement":null},{"id":"W4400829989","doi":"10.1029/2024gb008102","title":"Trends and Drivers of Terrestrial Sources and Sinks of Carbon Dioxide: An Overview of the TRENDY Project","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Carbon sink; Environmental science; Carbon cycle; Biosphere; Global change; Sink (geography); Arid; Climate change; Terrestrial ecosystem; Atmospheric carbon cycle; Biogeochemical cycle; Climatology; Vegetation (pathology); Land cover; Land use, land-use change and forestry; Primary production; Greenhouse gas; Ecosystem; Atmospheric sciences; Land use; Ecology; Geography; Geology","score_opus":0.015261307442571238,"score_gpt":0.2529306717434836,"score_spread":0.23766936430091237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400829989","genre_codex":"empirical","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.56766146,0.17607816,0.1241257,0.022743788,0.0011138447,0.0012716224,0.037355755,0.0023360692,0.0673137],"genre_scores_gemma":[0.7429877,0.13026795,0.08899522,0.0011919757,0.0008953645,0.0010633,0.027419364,0.00080460584,0.0063745757],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994356,0.00013742906,0.000044712266,0.00015930529,0.00016161118,0.000061364735],"domain_scores_gemma":[0.9978956,0.00050060375,0.00034153595,0.00016818757,0.00090334925,0.00019066803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003973236,0.00081187254,0.00037116755,0.00334069,0.00029731344,0.0017288416,0.0006988468,0.00040758206,0.0015129354],"category_scores_gemma":[0.0035307943,0.0002827238,0.0007657281,0.0055792243,0.00038035744,0.0022432928,0.0015699047,0.0007509298,0.00020675341],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002790295,0.00020651464,0.17168532,0.0010240756,0.0003622952,0.00011738762,0.0002789521,0.029512119,0.0015239951,0.019933859,0.015052059,0.76002437],"study_design_scores_gemma":[0.000121652316,0.00080980087,0.51822394,0.0028553773,0.00048388584,0.00030016,0.0012217149,0.15082398,0.0060993773,0.039038807,0.27985105,0.00017019182],"about_ca_topic_score_codex":0.016869145,"about_ca_topic_score_gemma":0.006005081,"teacher_disagreement_score":0.016869145,"about_ca_system_score_codex":0.0012291231,"about_ca_system_score_gemma":0.0027439126,"threshold_uncertainty_score":0.033541918},"labels":[],"label_agreement":null},{"id":"W4401955006","doi":"10.1029/2024gb008230","title":"Observed APO Seasonal Cycle in the Pacific: Estimation of Autumn O <sub>2</sub> Oceanic Emissions","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Japan Society for the Promotion of Science; Ministry of the Environment, Government of Japan","keywords":"Environmental science; Oceanography; Seasonality; Pacific ocean; Climatology; Atmospheric sciences; Geology; Biology; Ecology","score_opus":0.008951601086289217,"score_gpt":0.21973264937856546,"score_spread":0.21078104829227623,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401955006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99765366,0.000033146654,0.001495153,0.00002044846,0.000003492792,0.0000045055394,0.00020150866,0.00005861217,0.0005296224],"genre_scores_gemma":[0.9990814,0.00002042711,0.00064230524,0.000005136028,0.0000021956057,0.0000038083913,0.00017962429,0.0000098160845,0.000055334694],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999578,0.0000074324394,0.000002969591,0.00001639985,0.000007510618,0.000007851853],"domain_scores_gemma":[0.999871,0.000036993,0.000032345848,0.000013690766,0.000027115602,0.00001898014],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018070801,0.0003303341,0.00019097498,0.0002623551,0.00018603978,0.000307653,0.0003038192,0.00033463442,0.00043643694],"category_scores_gemma":[0.00043303875,0.00019752806,0.00030076457,0.00027169674,0.00016847916,0.0003427287,0.00019200053,0.00021519343,0.000066430395],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003352102,0.00013949221,0.7350921,0.0001158049,0.00019425768,0.00030663027,0.00019153842,0.20696105,0.039152764,0.00032467447,0.00054757117,0.016638884],"study_design_scores_gemma":[0.000041694082,0.00006414727,0.43467972,0.000009256373,0.000048932885,0.000062924366,0.00011491746,0.55543125,0.008674322,0.00021579763,0.00063555967,0.000021480824],"about_ca_topic_score_codex":0.020420816,"about_ca_topic_score_gemma":0.018473994,"teacher_disagreement_score":0.020420816,"about_ca_system_score_codex":0.00029289577,"about_ca_system_score_gemma":0.00034580976,"threshold_uncertainty_score":0.040603936},"labels":[],"label_agreement":null},{"id":"W4403783425","doi":"10.1029/2023gb007969","title":"Permafrost Region Greenhouse Gas Budgets Suggest a Weak CO<sub>2</sub> Sink and CH<sub>4</sub> and N<sub>2</sub>O Sources, But Magnitudes Differ Between Top‐Down and Bottom‐Up Methods","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Agence Nationale de la Recherche; Natural Environment Research Council; Sight Research UK","keywords":"Permafrost; Sink (geography); Greenhouse gas; Environmental science; Atmospheric sciences; Geology; Mineralogy; Geography; Oceanography","score_opus":0.023170230986512417,"score_gpt":0.2659486441287394,"score_spread":0.242778413142227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403783425","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9797284,0.00030587948,0.0065079937,0.00016270767,0.000019808038,0.000015149348,0.0048847976,0.00050640455,0.007868795],"genre_scores_gemma":[0.994406,0.000105630075,0.002888859,0.000042023392,0.000005269474,0.000010710115,0.001999701,0.000038890048,0.0005029534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988735,0.000009518428,0.0000046220243,0.0000452931,0.000035086152,0.000018172432],"domain_scores_gemma":[0.9999187,0.000011608636,0.000020344452,0.000010962926,0.000026113652,0.000012293314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017084998,0.00040919203,0.0001708806,0.00041631405,0.00022372653,0.0004686871,0.00035015776,0.00035232154,0.0017104832],"category_scores_gemma":[0.00023859425,0.0001946605,0.00041327556,0.0004683551,0.00019982629,0.0005837579,0.0002306318,0.00016698077,0.00027984413],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005186216,0.00013438308,0.7415553,0.00030287736,0.00047843004,0.00015682621,0.00010284207,0.10268026,0.08304244,0.0013882079,0.0025767076,0.067063235],"study_design_scores_gemma":[0.00005910411,0.00008699274,0.82472265,0.00003501726,0.00019295969,0.00008072783,0.00010962138,0.13863762,0.029969236,0.001735922,0.0043157553,0.000054386415],"about_ca_topic_score_codex":0.03184122,"about_ca_topic_score_gemma":0.038042113,"teacher_disagreement_score":0.03184122,"about_ca_system_score_codex":0.0006563816,"about_ca_system_score_gemma":0.00045983904,"threshold_uncertainty_score":0.063311756},"labels":[],"label_agreement":null},{"id":"W4404326113","doi":"10.1029/2024gb008176","title":"Organic Coatings Reduce Dissolution Rate by an Order of Magnitude for Carbonate Minerals Produced by Marine Fish","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Calcium Carbonate Crystallization and Inhibition","field":"Materials Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Ocean Sciences; Natural Sciences and Engineering Research Council of Canada","keywords":"Dissolution; Carbonate; Fish <Actinopterygii>; Mineralogy; Carbonate minerals; Environmental science; Environmental chemistry; Chemistry; Calcite; Materials science; Metallurgy; Fishery; Biology","score_opus":0.011702397028827973,"score_gpt":0.26518624100485927,"score_spread":0.2534838439760313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404326113","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985103,0.00015342343,0.0005121839,0.000018808563,0.000005690101,0.000008284979,0.00013777809,0.00001096599,0.00064251013],"genre_scores_gemma":[0.9972398,0.00011109373,0.0010213171,0.000026330816,0.0000018499727,0.000010694142,0.00017018482,0.000008962035,0.0014096688],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998869,0.0000061807514,0.000006682896,0.000032857122,0.000034047993,0.000033322707],"domain_scores_gemma":[0.999813,0.000040574927,0.00005593592,0.000016654047,0.00003986025,0.000034023145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000968209,0.0002985089,0.00014181281,0.00017927926,0.00011832695,0.0003422267,0.00014144197,0.00023245843,0.0012428813],"category_scores_gemma":[0.00026774002,0.00012333352,0.00021680995,0.000103230304,0.00023166918,0.00013084625,0.00029064482,0.00023248701,0.00013023967],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006486957,0.000010570857,0.0051464085,0.00002748304,0.000010316701,0.000017375456,0.000012200922,0.00007900503,0.9930333,0.0000096364665,0.000014535595,0.0015743573],"study_design_scores_gemma":[0.0000070583073,0.0002655837,0.13967139,0.000008033289,0.00003210501,0.00006969915,0.00009968491,0.0012118657,0.85758996,0.000018960338,0.0010209737,0.0000046991436],"about_ca_topic_score_codex":0.004742685,"about_ca_topic_score_gemma":0.008145374,"teacher_disagreement_score":0.004742685,"about_ca_system_score_codex":0.00030835983,"about_ca_system_score_gemma":0.00017453119,"threshold_uncertainty_score":0.00943017},"labels":[],"label_agreement":null},{"id":"W4405479257","doi":"10.1029/2023gb007926","title":"Dissolved Nitrogen Cycling in the Eastern Canadian Arctic Archipelago and Baffin Bay From Stable Isotopic Data","year":2024,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Esri (Canada); University of Calgary; Université Laval","funders":"Canada Foundation for Innovation; ArcticNet; Université Laval; National Science Foundation","keywords":"Bay; Phytoplankton; Oceanography; Arctic; Environmental science; Archipelago; Nitrate; Meltwater; Chlorophyll a; δ15N; Stable isotope ratio; Nutrient; Environmental chemistry; Glacial period; Geology; Ecology; Chemistry; δ13C","score_opus":0.019151847389930098,"score_gpt":0.2256295344283553,"score_spread":0.2064776870384252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405479257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99483514,0.0006073245,0.00017437698,0.000052036987,0.00000849073,0.000018985635,0.0021530692,0.000018412706,0.0021322146],"genre_scores_gemma":[0.9943234,0.00045369117,0.00076857215,0.00005352484,0.0000049133805,0.000022633907,0.0035061245,0.0000058691166,0.000861421],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997602,0.000011229894,0.000013346325,0.000047145717,0.00010434706,0.000063659914],"domain_scores_gemma":[0.99942786,0.00002346056,0.000056539116,0.000014385054,0.00040530632,0.00007234981],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036741965,0.00037587623,0.00024542984,0.0018424944,0.0016757279,0.0012058704,0.0005711752,0.00028522,0.0007874517],"category_scores_gemma":[0.000641135,0.0002129781,0.00028342064,0.0025477053,0.000312009,0.00023300585,0.0003674827,0.00022902647,0.00012476681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000120244134,0.000027808725,0.97801447,0.00006403499,0.000113920985,0.000110670175,0.00037783184,0.0010880716,0.0075119627,0.000081642385,0.0009014166,0.011587909],"study_design_scores_gemma":[0.0000036128288,0.0000046595237,0.99744153,0.000009166798,0.000018863047,0.00001582371,0.00024308116,0.00082144176,0.00034955848,0.000013972888,0.0010706342,0.000007683216],"about_ca_topic_score_codex":0.98319167,"about_ca_topic_score_gemma":0.99343115,"teacher_disagreement_score":0.016808331,"about_ca_system_score_codex":0.009576461,"about_ca_system_score_gemma":0.008092942,"threshold_uncertainty_score":0.069482386},"labels":[],"label_agreement":null},{"id":"W4408384783","doi":"10.1029/2024gb008183","title":"Divergent Responses of CH<sub>4</sub> Emissions and Uptake to Global Change Drivers","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Environmental science; Global change; Climate change; Atmospheric sciences; Environmental chemistry; Chemistry; Oceanography; Geology","score_opus":0.0101293054517033,"score_gpt":0.2360698356325784,"score_spread":0.22594053018087512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408384783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978302,0.00038078811,0.00044371394,0.000029800796,0.000005251707,0.000011508498,0.0005071182,0.000016416194,0.00077512715],"genre_scores_gemma":[0.99911517,0.00011626957,0.00015026898,0.000022520675,0.000005473651,0.0000139611775,0.00038118399,0.0000048651173,0.00019037798],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994641,0.00014517864,0.00003691713,0.000189958,0.000107051594,0.00005684491],"domain_scores_gemma":[0.99861574,0.0006332232,0.00029534832,0.00018114419,0.00022053688,0.00005391732],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013184808,0.00026622292,0.0003179435,0.00052607455,0.00012132778,0.0004961641,0.00022376195,0.00026406712,0.00083557545],"category_scores_gemma":[0.0012506966,0.00015893237,0.00043470366,0.0006165148,0.0003676619,0.00039305555,0.00038130482,0.00019148807,0.00013319908],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000575357,0.00005893689,0.8250075,0.00022442968,0.0004254673,0.00012101139,0.00024836275,0.0021470678,0.15461718,0.00015400177,0.00020794554,0.01621278],"study_design_scores_gemma":[0.0000035586575,0.000048893595,0.994672,0.0000027026097,0.000037798767,0.00001852342,0.00008702962,0.00062528026,0.0041200332,0.00004356852,0.00033531888,0.0000053173326],"about_ca_topic_score_codex":0.0040265606,"about_ca_topic_score_gemma":0.0060138595,"teacher_disagreement_score":0.0040265606,"about_ca_system_score_codex":0.0004490376,"about_ca_system_score_gemma":0.00019020375,"threshold_uncertainty_score":0.008006275},"labels":[],"label_agreement":null},{"id":"W4408477705","doi":"10.1029/2024gb008209","title":"Agricultural Land Use Impacts Aquatic Greenhouse Gas Emissions From Wetlands in the Canadian Prairie Pothole Region","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ducks Unlimited Canada; University of Lethbridge","funders":"Natural Sciences and Engineering Research Council of Canada; Institute for Wetland and Waterfowl Research, Ducks Unlimited Canada; Beef Cattle Research Council; University of Lethbridge; Canada Research Chairs; Canada Foundation for Innovation","keywords":"Pothole (geology); Wetland; Environmental science; Greenhouse gas; Agricultural land; Agriculture; Land use; Environmental protection; Hydrology (agriculture); Water resource management; Geography; Ecology; Oceanography; Geology","score_opus":0.011664096879417902,"score_gpt":0.23352147530452916,"score_spread":0.22185737842511125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408477705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956722,0.00015928314,0.00024487585,0.00010266356,0.0000032920236,0.000026630869,0.0016265482,0.00001654643,0.0021479297],"genre_scores_gemma":[0.9985361,0.000115936404,0.00046607023,0.000029519535,0.000001222409,0.000011592363,0.0004247756,0.000004519479,0.00041034818],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99951255,0.000036321006,0.0000130499975,0.00011114969,0.00018960575,0.00013732434],"domain_scores_gemma":[0.9991579,0.000064536194,0.00010538726,0.00003692962,0.00051195885,0.0001233475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003351667,0.0002686352,0.00019738235,0.00080521,0.0016026328,0.00092932873,0.0006803332,0.00023148394,0.00090030686],"category_scores_gemma":[0.00075585715,0.00018546714,0.000370789,0.0018002627,0.0006428485,0.00039067425,0.00056555617,0.00029889823,0.00007761216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000114559116,0.00006977154,0.96160764,0.000096385134,0.00020913672,0.00020349037,0.0012198855,0.0025189887,0.012121892,0.00035594613,0.0014312238,0.02005118],"study_design_scores_gemma":[0.0000018366081,0.0000053598237,0.99814594,0.0000044544086,0.000011853889,0.000015630088,0.00044339636,0.00062767323,0.0001568702,0.000017872537,0.0005622272,0.000006972192],"about_ca_topic_score_codex":0.98971635,"about_ca_topic_score_gemma":0.9966696,"teacher_disagreement_score":0.012849943,"about_ca_system_score_codex":0.012849943,"about_ca_system_score_gemma":0.0094698975,"threshold_uncertainty_score":0.09323329},"labels":[],"label_agreement":null},{"id":"W4408580231","doi":"10.1029/2024gb008239","title":"Blue Carbon Stocks Along the Pacific Coast of North America Are Mainly Driven by Local Rather Than Regional Factors","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Parks Canada; Simon Fraser University; Tula Foundation","funders":"Hakai Institute; National Institute of Food and Agriculture; U.S. Geological Survey; National Oceanic and Atmospheric Administration; Tula Foundation; U.S. Department of Agriculture; Florida International University; Pew Charitable Trusts; National Estuarine Research Reserve System; U.S. Environmental Protection Agency","keywords":"Oceanography; Pacific ocean; Carbon fibers; Environmental science; Geography; Geology; Physical geography","score_opus":0.004973981737539367,"score_gpt":0.19698690046712633,"score_spread":0.19201291872958695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408580231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999181,0.00006838069,0.000046985126,0.000021366095,0.0000017771547,0.0000014526864,0.00020870284,0.0000023712794,0.00046784637],"genre_scores_gemma":[0.99940324,0.000068773305,0.00006177942,0.000013902788,0.0000022616875,0.0000021922995,0.00025803066,0.000001480885,0.0001883132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999448,0.000008449848,0.000004090805,0.000019634947,0.000011948992,0.000011114554],"domain_scores_gemma":[0.999613,0.000045137793,0.00016345167,0.00002272898,0.00010034696,0.000055357275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001694518,0.00014580306,0.0001052588,0.0004884923,0.00021381966,0.0003126325,0.00010998443,0.000090295114,0.00080125814],"category_scores_gemma":[0.000409894,0.00011146087,0.00009239214,0.00062348094,0.00020732568,0.00022979618,0.00021997708,0.0001115822,0.000081359656],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014739041,0.0000044508365,0.9967417,0.000005804499,0.00003164095,0.000022458606,0.000085759115,0.000055164583,0.0007904325,0.000015663121,0.0001031811,0.002128972],"study_design_scores_gemma":[3.1114268e-7,0.0000016911138,0.99978346,0.0000012584189,0.0000034524423,0.000006442082,0.00006055635,0.000055522854,0.000024280256,0.000007662172,0.000054992513,4.5841824e-7],"about_ca_topic_score_codex":0.049828447,"about_ca_topic_score_gemma":0.14268292,"teacher_disagreement_score":0.049828447,"about_ca_system_score_codex":0.00022110227,"about_ca_system_score_gemma":0.00020950001,"threshold_uncertainty_score":0.09907681},"labels":[],"label_agreement":null},{"id":"W4408779096","doi":"10.1029/2024gb008409","title":"Water Column Structure and Nutrient Supply on the Northwest Atlantic Shelf: A Nitrate Isotope Study","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Isotope Analysis in Ecology","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Dalhousie University","funders":"Ocean Frontier Institute","keywords":"Water column; Nitrate; Oceanography; Nutrient; Environmental science; Isotope; Geology; Stable isotope ratio; Water mass; Chemistry","score_opus":0.004497639122788435,"score_gpt":0.21658930549361288,"score_spread":0.21209166637082444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408779096","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99957794,0.000031490235,0.000023158429,0.000005776999,0.0000010662604,0.0000014300712,0.00014445542,7.3180894e-7,0.00021394355],"genre_scores_gemma":[0.9993656,0.00003781021,0.00008859157,0.000011482059,0.0000014085234,0.0000018170824,0.00024437322,9.33771e-7,0.00024787875],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999936,0.000005972686,0.000004837479,0.000017966886,0.000020626203,0.000014541204],"domain_scores_gemma":[0.9997545,0.000021412596,0.00005211716,0.000012641254,0.00009874794,0.000060535778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014377222,0.00012464623,0.00015741105,0.00037038446,0.00048065514,0.00042248896,0.00015706426,0.00021151455,0.0005263328],"category_scores_gemma":[0.00019247492,0.000111293375,0.00018503968,0.0004914569,0.00025260425,0.00018126905,0.0002576372,0.00014173237,0.00012897034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000101656566,0.00002196981,0.98861957,0.0000071652507,0.000024998477,0.000082114806,0.00017345384,0.00008918877,0.00891517,0.000018086288,0.00005043233,0.0018961997],"study_design_scores_gemma":[9.593103e-7,0.0000127761505,0.9994916,0.0000015630596,0.0000045563934,0.000014504886,0.00012881201,0.0001363507,0.00012405604,0.0000030049048,0.000080758844,0.0000010582374],"about_ca_topic_score_codex":0.26314637,"about_ca_topic_score_gemma":0.48697275,"teacher_disagreement_score":0.26314637,"about_ca_system_score_codex":0.0009269101,"about_ca_system_score_gemma":0.0007405967,"threshold_uncertainty_score":0.52322936},"labels":[],"label_agreement":null},{"id":"W4408858150","doi":"10.1029/2024gb008358","title":"Biological Responses to Ocean Acidification Are Changing the Global Ocean Carbon Cycle","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"National Oceanic and Atmospheric Administration","keywords":"Ocean acidification; Carbon cycle; Oceanography; Environmental science; Effects of global warming on oceans; Biological pump; Global change; Carbon flux; Climate change; Geology; Global warming; Ecosystem; Ecology; Biology","score_opus":0.014919624055693586,"score_gpt":0.2546359863133647,"score_spread":0.23971636225767112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408858150","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972863,0.0003190086,0.0002494603,0.00024247565,0.00001666413,0.0000041040616,0.00020633372,0.000021379625,0.0016543171],"genre_scores_gemma":[0.99946946,0.0001564497,0.00007704614,0.00009303887,0.000005505123,0.0000023942498,0.000080455255,0.0000020316013,0.0001136429],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992347,0.000018550529,0.000004466288,0.000018283634,0.000015111318,0.000020175237],"domain_scores_gemma":[0.99982184,0.00003587456,0.00005967919,0.000015303895,0.000032292293,0.0000349953],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019097317,0.00022225418,0.00013392731,0.00020511952,0.00015949864,0.0004069628,0.00010095294,0.00045480183,0.0010104442],"category_scores_gemma":[0.0005500493,0.00009433677,0.00018049621,0.00028327425,0.0003246515,0.00021610121,0.00038657276,0.00020802605,0.00012522009],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024718238,0.0000864967,0.69254744,0.00014293668,0.00026619862,0.0002915091,0.00015761513,0.012566492,0.2716473,0.00060612126,0.00093562837,0.020505166],"study_design_scores_gemma":[0.0000072283483,0.00010493146,0.99069536,0.0000060876923,0.000021958444,0.00007071399,0.00023126557,0.002057877,0.0049567507,0.00037959355,0.001461518,0.0000068066915],"about_ca_topic_score_codex":0.0046283957,"about_ca_topic_score_gemma":0.0043750317,"teacher_disagreement_score":0.0046283957,"about_ca_system_score_codex":0.00032925722,"about_ca_system_score_gemma":0.00015601478,"threshold_uncertainty_score":0.009202898},"labels":[],"label_agreement":null},{"id":"W4408984811","doi":"10.1029/2024gb008179","title":"Tracing Pan‐Canadian Arctic Water Masses and Dissolved Inorganic Carbon Cycling Using Stable and Radiocarbon Isotopes","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; University of Calgary; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Radiocarbon dating; Cycling; Dissolved organic carbon; Arctic; Isotope; Isotopes of carbon; Carbon fibers; Oceanography; Environmental science; Tracing; Carbon cycle; Stable isotope ratio; Environmental chemistry; Seawater; Geology; Chemistry; Total organic carbon; Geography; Archaeology; Ecology; Paleontology; Materials science","score_opus":0.007454366205548879,"score_gpt":0.217496940772706,"score_spread":0.21004257456715714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408984811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879981,0.0010371003,0.0010433722,0.000108471955,0.000016015994,0.000021029151,0.0047313,0.00005870818,0.00498575],"genre_scores_gemma":[0.99328023,0.0006084621,0.0023748851,0.00005352358,0.000006155361,0.000015602653,0.0020680798,0.000014002571,0.0015790821],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997191,0.000010123674,0.000008489177,0.000062728745,0.00014525515,0.00005435367],"domain_scores_gemma":[0.9993961,0.000016448199,0.00006022023,0.000014269034,0.00046590785,0.00004707989],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033992392,0.00047628814,0.00021272645,0.0019106759,0.0018309627,0.0007766829,0.00047155112,0.0002441939,0.0006833848],"category_scores_gemma":[0.00034825614,0.00022261855,0.00024438562,0.0027791958,0.0002860356,0.00020849885,0.000385545,0.00023877606,0.00017116875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014711698,0.000026772634,0.93454605,0.00009991231,0.00017924576,0.00011381283,0.0004443504,0.0016121455,0.030837098,0.000181006,0.0012484193,0.030564066],"study_design_scores_gemma":[0.0000030001872,0.000011942693,0.98971283,0.000012078031,0.000029708655,0.00002926157,0.00029322066,0.0016772264,0.004556103,0.000021776419,0.0036394533,0.000013411713],"about_ca_topic_score_codex":0.95747185,"about_ca_topic_score_gemma":0.98578715,"teacher_disagreement_score":0.042528152,"about_ca_system_score_codex":0.007494553,"about_ca_system_score_gemma":0.005389018,"threshold_uncertainty_score":0.08555716},"labels":[],"label_agreement":null},{"id":"W4409190563","doi":"10.1029/2024gb008310","title":"The North American Greenhouse Gas Budget: Emissions, Removals, and Integration for CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O (2010–2019): Results From the Second REgional Carbon Cycle Assessment and Processes Study (RECCAP2)","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Natural Resources Canada; Canadian Forest Service","funders":"Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México; National Natural Science Foundation of China; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Greenhouse gas; Environmental science; Geology; Oceanography","score_opus":0.007033979078767538,"score_gpt":0.2339123130632461,"score_spread":0.22687833398447857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409190563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91093904,0.0031030355,0.002655324,0.0027819395,0.00014516474,0.00008057343,0.0681088,0.00055698043,0.0116291065],"genre_scores_gemma":[0.9399701,0.0019295146,0.0052657104,0.0005517991,0.00005553306,0.00013829411,0.04731272,0.00009015531,0.004686029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997962,0.000033553675,0.000011111874,0.000048906895,0.00008216344,0.000028104478],"domain_scores_gemma":[0.9996582,0.000026101574,0.00005623028,0.000024451365,0.00020522959,0.000029784778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077317527,0.0006898923,0.00028880683,0.00062580185,0.0003614243,0.00088812603,0.00040334716,0.0004412647,0.00069883885],"category_scores_gemma":[0.00049145194,0.00028983073,0.0006126921,0.0019234447,0.00020560848,0.0007871651,0.00036585235,0.00043620405,0.00023463574],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009261861,0.00044239184,0.7023984,0.00083652715,0.002047889,0.00049601606,0.0003794653,0.10795244,0.013814079,0.0020712907,0.08751932,0.08111595],"study_design_scores_gemma":[0.00008693594,0.000042322266,0.89687395,0.00006686328,0.0005101266,0.00005509451,0.00038930343,0.060576867,0.0072906637,0.0005947927,0.033447098,0.000066108754],"about_ca_topic_score_codex":0.5075333,"about_ca_topic_score_gemma":0.5959057,"teacher_disagreement_score":0.5075333,"about_ca_system_score_codex":0.0026283395,"about_ca_system_score_gemma":0.003264737,"threshold_uncertainty_score":0.99073386},"labels":[],"label_agreement":null},{"id":"W4410479257","doi":"10.1029/2024gb008431","title":"Global Patterns of Leaf Litter C:N:P Stoichiometry Under Current and Future Climate Scenarios","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Science Foundation of Fujian Province; National Natural Science Foundation of China; Glenrose Rehabilitation Hospital","keywords":"Current (fluid); Stoichiometry; Litter; Environmental science; Physical geography; Ecology; Geography; Forestry; Biology; Atmospheric sciences; Oceanography; Geology; Chemistry","score_opus":0.01153563318328857,"score_gpt":0.23080903932784747,"score_spread":0.2192734061445589,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410479257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981232,0.00007591668,0.0002805222,0.000022230097,0.0000013240079,0.000001537758,0.0012486983,0.00001710025,0.00022939243],"genre_scores_gemma":[0.9984107,0.000055070253,0.00027152555,0.000007873158,0.0000014386204,0.000003993969,0.0012087418,0.0000037916263,0.000036919846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989057,0.000022504733,0.000009379749,0.000047217247,0.000013696414,0.000016559265],"domain_scores_gemma":[0.9996439,0.00009782094,0.00012685849,0.000041924148,0.00005844487,0.00003096527],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000494661,0.00017160771,0.00017073256,0.00081622927,0.00013058787,0.00037423454,0.00020847918,0.00031722742,0.00053135795],"category_scores_gemma":[0.00064942864,0.00012034229,0.00030846568,0.000850438,0.00020721501,0.0003692832,0.00024731515,0.000110096815,0.000113044705],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012565183,0.00001957153,0.9596822,0.00007030631,0.0002499917,0.00009710685,0.00006854131,0.020984275,0.011746631,0.00019716915,0.00034556695,0.0064130058],"study_design_scores_gemma":[0.000008054754,0.000023887696,0.97753215,0.0000073642423,0.00003994603,0.00007430596,0.00007766127,0.020571318,0.0009904805,0.00018507605,0.00047896602,0.000010837181],"about_ca_topic_score_codex":0.004114466,"about_ca_topic_score_gemma":0.004295248,"teacher_disagreement_score":0.004114466,"about_ca_system_score_codex":0.00029137533,"about_ca_system_score_gemma":0.00012024651,"threshold_uncertainty_score":0.0081810355},"labels":[],"label_agreement":null},{"id":"W4410622319","doi":"10.1029/2024gb008425","title":"Methane Emissions and Dynamics in the Weddell and Scotia Seas","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"British Antarctic Survey; Natural Environment Research Council; Fonds De La Recherche Scientifique - FNRS","keywords":"Nova scotia; Methane; Oceanography; Environmental science; Geology; Chemistry","score_opus":0.004459322238697816,"score_gpt":0.22392761247627868,"score_spread":0.21946829023758085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410622319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992747,0.000037950795,0.000012417902,0.000011019597,0.000001461798,0.000002406666,0.00025525398,0.0000011754863,0.0004036641],"genre_scores_gemma":[0.9992085,0.000048209513,0.000047015423,0.00001356597,0.0000010168317,0.000002666922,0.00024378898,7.418874e-7,0.00043454097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995947,0.00000476306,0.0000037292891,0.000009961363,0.0000090735575,0.000013083616],"domain_scores_gemma":[0.9998129,0.00001914647,0.000055772758,0.0000081403305,0.0000599853,0.000044081648],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001098221,0.00016168141,0.000091096925,0.00042170152,0.00029459878,0.00035874278,0.00010971125,0.00011024715,0.00059407635],"category_scores_gemma":[0.00020644217,0.00008924587,0.00014832617,0.00044273562,0.00016843788,0.00011543938,0.00029568438,0.00010500937,0.000091423615],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008291965,0.000008066384,0.993952,0.000013995174,0.00002325294,0.00015440649,0.00025748,0.0002734349,0.0031541982,0.000022198206,0.00008602108,0.0019721289],"study_design_scores_gemma":[0.0000012739159,0.00000875986,0.99938214,0.000003873635,0.0000031743243,0.00001501483,0.00022079161,0.000112890055,0.00011458866,0.0000027391304,0.00013406754,7.9030167e-7],"about_ca_topic_score_codex":0.46799153,"about_ca_topic_score_gemma":0.6930837,"teacher_disagreement_score":0.46799153,"about_ca_system_score_codex":0.0010868959,"about_ca_system_score_gemma":0.000698076,"threshold_uncertainty_score":0.930535},"labels":[],"label_agreement":null},{"id":"W4410856449","doi":"10.1029/2025gb008525","title":"The Global Biogeochemical Cycle of Chromium at the Earth's Surface","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Chromium effects and bioremediation","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Ocean Networks Canada Society; University of Victoria","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Biogeochemical cycle; Earth (classical element); Chromium; Environmental science; Geochemical cycle; Earth science; Geology; Environmental chemistry; Chemistry; Materials science; Metallurgy; Physics","score_opus":0.004444345931522803,"score_gpt":0.23033677624310256,"score_spread":0.22589243031157977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410856449","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.42902502,0.5267713,0.006995043,0.00286679,0.00027353576,0.00004532554,0.004011896,0.00043722268,0.029573807],"genre_scores_gemma":[0.8479299,0.14212312,0.004237213,0.0005843561,0.00014703274,0.000017160231,0.0011053622,0.000050756153,0.0038050788],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999273,0.0000075489793,0.00000422488,0.00002709906,0.000025058636,0.000008866491],"domain_scores_gemma":[0.99992883,0.000008746367,0.000018923905,0.0000031420384,0.000033775523,0.000006542877],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016503035,0.00031269988,0.00023993402,0.0007893641,0.00014722694,0.0009144873,0.0002153256,0.000339415,0.000691001],"category_scores_gemma":[0.00013672662,0.00008284664,0.00017837468,0.0013323392,0.00022391879,0.00037455204,0.00032672472,0.00021072528,0.0002915404],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045087739,0.00005887707,0.085939966,0.0064105275,0.000931487,0.0006122495,0.0003590771,0.015326831,0.31074435,0.022706604,0.0081498,0.54830927],"study_design_scores_gemma":[0.00004831119,0.0009357927,0.5165202,0.000986816,0.0010492703,0.0011959979,0.00057520217,0.0053216484,0.052194353,0.017519023,0.4035701,0.00008333616],"about_ca_topic_score_codex":0.0108535,"about_ca_topic_score_gemma":0.007312415,"teacher_disagreement_score":0.0108535,"about_ca_system_score_codex":0.0008984755,"about_ca_system_score_gemma":0.000579535,"threshold_uncertainty_score":0.021580637},"labels":[],"label_agreement":null},{"id":"W4411236617","doi":"10.1029/2024gb008467","title":"Natural Nanoparticles and Colloids in Forested Streams Across Europe: Seasonal Patterns and Impact of Soil Groups","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Heavy metals in environment","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Deutsche Forschungsgemeinschaft","keywords":"STREAMS; Environmental science; Natural (archaeology); Weather patterns; Colloid; Physical geography; Hydrology (agriculture); Ecology; Earth science; Geology; Climate change; Oceanography; Geography; Chemistry; Biology; Geotechnical engineering; Paleontology","score_opus":0.006167024093500139,"score_gpt":0.264753569532962,"score_spread":0.25858654543946186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411236617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99950457,0.00013407462,0.000055004235,0.0000044230896,9.97732e-7,0.0000020314287,0.00015703849,0.0000023545015,0.00013952078],"genre_scores_gemma":[0.99930835,0.00009677483,0.00013644145,0.0000074521117,0.0000025128113,0.0000037547586,0.00029379813,0.0000025613701,0.00014835417],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997061,0.000042953165,0.000029612553,0.00013428529,0.000038756207,0.000048384038],"domain_scores_gemma":[0.99950063,0.00010835475,0.00017008919,0.000025867314,0.000124808,0.00007027604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041087304,0.00015880678,0.0003001212,0.0011785183,0.00028927528,0.000861334,0.00023409586,0.00036490615,0.0006081127],"category_scores_gemma":[0.00056021346,0.00014597624,0.00023388548,0.00121599,0.00031179638,0.00030304244,0.00045140268,0.000111959715,0.000100593454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022584164,0.000047423026,0.9862417,0.000048960977,0.0001130506,0.00014531333,0.00042977196,0.00026336368,0.005494527,0.000043576703,0.000076248936,0.006870196],"study_design_scores_gemma":[0.0000023359064,0.000015385214,0.999288,0.000004073217,0.000009193601,0.000035028494,0.000184002,0.00012495984,0.00019348528,0.000011418479,0.00012991721,0.0000020850573],"about_ca_topic_score_codex":0.0113440575,"about_ca_topic_score_gemma":0.015735455,"teacher_disagreement_score":0.0113440575,"about_ca_system_score_codex":0.00044520316,"about_ca_system_score_gemma":0.00021124973,"threshold_uncertainty_score":0.022556007},"labels":[],"label_agreement":null},{"id":"W4411236740","doi":"10.1029/2024gb008460","title":"Permafrost, Peatland, and Cropland Regions Are Key to Reconciling North American Carbon Sink Estimates","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Canadian Forest Service","funders":"National Aeronautics and Space Administration","keywords":"Peat; Permafrost; Carbon sink; Sink (geography); Physical geography; Environmental science; Carbon fibers; Carbon cycle; Hydrology (agriculture); Geology; Earth science; Soil science; Climate change; Oceanography; Ecosystem; Geography; Ecology; Archaeology; Cartography","score_opus":0.007630096884277737,"score_gpt":0.2346225802604782,"score_spread":0.22699248337620045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411236740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9867466,0.00051127205,0.007916528,0.00095313095,0.000032313357,0.0000106569005,0.0005194121,0.0002861264,0.0030240577],"genre_scores_gemma":[0.9952467,0.00009878772,0.0041148616,0.000070915135,0.0000121588,0.0000052391388,0.0002903613,0.000038931765,0.00012213837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994777,0.00014891461,0.000035986166,0.00017907677,0.00009742839,0.000060870072],"domain_scores_gemma":[0.9991026,0.00020589614,0.00016755641,0.00015828045,0.00030375982,0.00006202207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019392337,0.00046912872,0.00037254943,0.000864764,0.0005136756,0.0015366591,0.00050722156,0.00048706212,0.0007838663],"category_scores_gemma":[0.0030150684,0.0002267578,0.0002986914,0.0008826472,0.00040172145,0.001413921,0.0008278957,0.00041474582,0.0001268271],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016693177,0.00006543485,0.87024325,0.00014057655,0.0004955492,0.0002157083,0.00090085104,0.038448628,0.015456107,0.002802193,0.0019589257,0.06910585],"study_design_scores_gemma":[0.000034699486,0.00003361849,0.81181186,0.00020117151,0.00027958307,0.000115986615,0.0027293782,0.1618327,0.007819688,0.0067053554,0.008356211,0.00007977728],"about_ca_topic_score_codex":0.029954039,"about_ca_topic_score_gemma":0.055781424,"teacher_disagreement_score":0.970046,"about_ca_system_score_codex":0.0005871623,"about_ca_system_score_gemma":0.0009477973,"threshold_uncertainty_score":0.059559405},"labels":[],"label_agreement":null},{"id":"W4411505001","doi":"10.1029/2025gb008558","title":"Seasonal Influence on Subsurface Rates of Microbial Sulfate Reduction and Sulfur Isotope Fractionation in Coastal Sediments","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Environment Research Council; Leverhulme Trust","keywords":"Sulfate; Sulfur cycle; Sulfur; Pyrite; Biogeochemical cycle; Environmental chemistry; Isotope fractionation; Sediment; Geochemical cycle; Geology; Fractionation; Chemistry; Mineralogy","score_opus":0.010920520766333118,"score_gpt":0.267047977726955,"score_spread":0.2561274569606219,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411505001","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996362,0.000014719595,0.00006337781,0.0000046747623,7.1379395e-7,8.740592e-7,0.00014521556,0.000007136493,0.00012709716],"genre_scores_gemma":[0.99966085,0.000018952784,0.000085305306,0.0000021874132,8.430535e-7,0.0000016135958,0.00013788596,0.0000038554817,0.00008859687],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999941,0.00000984601,0.000007417727,0.000019312109,0.00001272176,0.000009706284],"domain_scores_gemma":[0.99962056,0.0000973383,0.000103211125,0.000030343177,0.000090506044,0.000057928286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019933056,0.00022315835,0.00018070269,0.0004192994,0.00015704989,0.00036014942,0.00016214765,0.00020625723,0.0005082948],"category_scores_gemma":[0.00053063774,0.00019498279,0.0002094365,0.0003265528,0.00018896961,0.00018597592,0.00022334012,0.00012582332,0.00012501715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006573601,0.00005270471,0.7638493,0.000046631216,0.000093290764,0.00022906395,0.00025496873,0.0038745375,0.22438662,0.000095506555,0.00010360566,0.0063563534],"study_design_scores_gemma":[0.000005758457,0.00008362919,0.9879909,0.0000028342213,0.000014450964,0.00004641487,0.00008777496,0.003127651,0.0084342435,0.000028390026,0.0001716457,0.00000635713],"about_ca_topic_score_codex":0.009382998,"about_ca_topic_score_gemma":0.008927363,"teacher_disagreement_score":0.009382998,"about_ca_system_score_codex":0.0003645136,"about_ca_system_score_gemma":0.00014512493,"threshold_uncertainty_score":0.01865673},"labels":[],"label_agreement":null},{"id":"W4411505139","doi":"10.1029/2025gb008545","title":"Long‐Term and Seasonal Drivers of Organic Matter in the Clearwater Tapajós River and Implications for the Amazon River Basin","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dissolved organic carbon; Amazon rainforest; Tributary; Environmental science; Carbon cycle; Total organic carbon; Hydrology (agriculture); Drainage basin; Organic matter; Environmental chemistry; Ecosystem; Geology; Chemistry; Geography; Ecology","score_opus":0.006656780648527082,"score_gpt":0.2116973178890123,"score_spread":0.2050405372404852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411505139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99883145,0.00014670323,0.000085655076,0.00016718887,0.000003800321,0.0000035646108,0.00039940563,0.000006465883,0.00035576778],"genre_scores_gemma":[0.9995852,0.000063864754,0.000055009616,0.000021968775,0.0000049463297,0.000003709544,0.0001629135,0.000002479559,0.00009990761],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999001,0.000013568848,0.000009437506,0.00003502335,0.000016513735,0.000025298095],"domain_scores_gemma":[0.9996722,0.000052662836,0.00013321696,0.000012446832,0.00007394142,0.000055662626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019981731,0.00013806096,0.00014335825,0.0004345582,0.00031601542,0.0005732725,0.00021479596,0.00023515668,0.0011073791],"category_scores_gemma":[0.00051546365,0.000104161474,0.00022307325,0.0007392414,0.00029356618,0.00049109047,0.00037065858,0.00022700267,0.0000699301],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039511873,0.000028695295,0.98874855,0.00003462994,0.00004687683,0.00018558702,0.00034803577,0.00020884466,0.0059329546,0.00015100441,0.00022189712,0.0040532257],"study_design_scores_gemma":[0.000001336491,0.000004296471,0.99860114,0.000004757026,0.000008260786,0.000029661122,0.0003478858,0.0006083929,0.00010165655,0.000042288386,0.00024731853,0.000003000007],"about_ca_topic_score_codex":0.060718726,"about_ca_topic_score_gemma":0.08094306,"teacher_disagreement_score":0.060718726,"about_ca_system_score_codex":0.0006700445,"about_ca_system_score_gemma":0.00052255596,"threshold_uncertainty_score":0.12073058},"labels":[],"label_agreement":null},{"id":"W4411747298","doi":"10.1029/2024gb008396","title":"Wave Glider‐Based Measurements and Corrections of Near‐Surface <i>p</i> CO <sub>2</sub> Gradients in the Coastal Ocean","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Canada First Research Excellence Fund; Ocean Frontier Institute; Mitacs","keywords":"Glider; Geology; Oceanography; Remote sensing; Marine engineering","score_opus":0.015182903738386813,"score_gpt":0.21834124601913923,"score_spread":0.2031583422807524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411747298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98726046,0.000023717395,0.01014681,0.00004830188,0.000017675431,0.00003124838,0.0004278422,0.00035372298,0.0016902618],"genre_scores_gemma":[0.98603445,0.00003147596,0.012818919,0.00002236181,0.000005207522,0.000020061521,0.0004118228,0.00004178107,0.0006139982],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999243,0.000009861106,0.0000030893434,0.000019697034,0.000028484576,0.000014522228],"domain_scores_gemma":[0.9998443,0.000025046045,0.000025604319,0.000023398352,0.00007048643,0.000011153764],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015353136,0.000272488,0.00016071215,0.00032395584,0.00020923669,0.00034444922,0.00028716933,0.00017675475,0.0008104403],"category_scores_gemma":[0.0005657457,0.00014032629,0.00012499568,0.00040452793,0.00014150888,0.0001972217,0.0002737214,0.00025239118,0.00033946423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040795005,0.0001462055,0.5348983,0.00008959345,0.00006978836,0.00021919052,0.0004986487,0.035300657,0.23947264,0.00032842287,0.0030232156,0.18554534],"study_design_scores_gemma":[0.00004772066,0.00017620572,0.8072921,0.000022636905,0.000031597792,0.00009701889,0.0002928785,0.15485147,0.034428786,0.00013440789,0.0025930235,0.000032200725],"about_ca_topic_score_codex":0.052835938,"about_ca_topic_score_gemma":0.117319174,"teacher_disagreement_score":0.052835938,"about_ca_system_score_codex":0.0004021345,"about_ca_system_score_gemma":0.00071961805,"threshold_uncertainty_score":0.10505682},"labels":[],"label_agreement":null},{"id":"W4412639480","doi":"10.1029/2025gb008639","title":"Changes in the Composition of Nitrogen Yields in Large Arctic Rivers Linked to Temperature and Precipitation","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Science Foundation","keywords":"Precipitation; Nitrogen; Environmental science; Arctic; Composition (language); Oceanography; The arctic; Atmospheric sciences; Chemistry; Geology; Geography; Meteorology","score_opus":0.01388601990486718,"score_gpt":0.24888323023832457,"score_spread":0.23499721033345738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412639480","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986135,0.00006628925,0.00056749507,0.000013801465,0.0000027959218,0.0000012366522,0.000381157,0.000013119334,0.00034071633],"genre_scores_gemma":[0.9992725,0.00003099959,0.00022556004,0.0000037950874,0.0000019070635,0.0000022269653,0.0003282862,0.0000028184304,0.00013199316],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998615,0.00004171867,0.000009030723,0.000047521564,0.000020349848,0.000019871373],"domain_scores_gemma":[0.9995253,0.00016669153,0.00013421725,0.000035479097,0.000102533806,0.000035786772],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004946183,0.00016620732,0.00013593119,0.00041016602,0.00018225604,0.00036648262,0.00011219194,0.000108016386,0.00036734468],"category_scores_gemma":[0.0007795636,0.00009692843,0.00029555275,0.0005569203,0.00017361615,0.00012560013,0.00022852585,0.0001313468,0.00006602412],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000076555894,0.000014092652,0.98717785,0.000011643509,0.00014730255,0.000041166993,0.00009911699,0.004333249,0.0043933536,0.00014310873,0.000096880336,0.003465754],"study_design_scores_gemma":[9.454568e-7,0.000009766971,0.9942399,0.0000019750673,0.000016019198,0.000026929845,0.00006665341,0.0050366116,0.00031884742,0.00010370897,0.00017548796,0.0000031390143],"about_ca_topic_score_codex":0.033301514,"about_ca_topic_score_gemma":0.042892873,"teacher_disagreement_score":0.033301514,"about_ca_system_score_codex":0.00036567645,"about_ca_system_score_gemma":0.00029662432,"threshold_uncertainty_score":0.06621534},"labels":[],"label_agreement":null},{"id":"W4412734253","doi":"10.1029/2024gb008218","title":"New Deoxygenation Threshold for N<sub>2</sub> and N<sub>2</sub>O Production in Coastal Waters and Sediments","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Université du Québec à Rimouski","funders":"Fonds de recherche du Québec – Nature et technologies; Ministère des Transports; Natural Sciences and Engineering Research Council of Canada; Marine Environmental Observation Prediction and Response Network","keywords":"Deoxygenation; Environmental science; Sediment; Production (economics); Oceanography; Geology; Hydrology (agriculture); Geomorphology; Chemistry","score_opus":0.0074555737461810805,"score_gpt":0.20750469763008994,"score_spread":0.20004912388390886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412734253","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988803,0.00011007808,0.00036572447,0.000018816361,0.000001562892,0.0000027234455,0.00010851182,0.000020766367,0.0004914309],"genre_scores_gemma":[0.9995845,0.000023337212,0.00021605272,0.000010503918,9.862396e-7,0.0000026524858,0.00008440574,0.0000021491753,0.00007549325],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994576,0.0000031760478,0.0000033183746,0.000027524398,0.0000084745025,0.000011721353],"domain_scores_gemma":[0.99989855,0.000014195349,0.000037488433,0.0000059659897,0.000023015848,0.00002066885],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010281554,0.00015074726,0.00012740128,0.00036280134,0.00020660362,0.00037808044,0.00023225551,0.00024534235,0.0003856713],"category_scores_gemma":[0.00014584756,0.00014479969,0.00010592405,0.00014308307,0.00026958657,0.00027683488,0.00032072884,0.00023574934,0.00006673338],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026822055,0.000046291105,0.46394882,0.0000630382,0.00003133252,0.00016461892,0.0003436267,0.0011639019,0.5265498,0.0004739709,0.00016728562,0.006779078],"study_design_scores_gemma":[0.0000057577477,0.00008362168,0.9528346,0.000012136514,0.000012859475,0.0000634885,0.00035457287,0.0049924334,0.04036873,0.00029350905,0.0009651696,0.000013080842],"about_ca_topic_score_codex":0.012266751,"about_ca_topic_score_gemma":0.017697453,"teacher_disagreement_score":0.012266751,"about_ca_system_score_codex":0.00066118874,"about_ca_system_score_gemma":0.0002855879,"threshold_uncertainty_score":0.024390697},"labels":[],"label_agreement":null},{"id":"W4412956863","doi":"10.1029/2025gb008518","title":"Seasonal and Diurnal Patterns of Methane Emissions From a Northern Pristine Peatland in the Last Decade","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Peat; Methane; Environmental science; Atmospheric methane; Ombrotrophic; Methane emissions; Physical geography; Atmospheric sciences; Climatology; Bog; Geography; Geology; Ecology; Archaeology","score_opus":0.007050048317779135,"score_gpt":0.24181428695282775,"score_spread":0.2347642386350486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412956863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995913,0.000017547443,0.0000880445,0.000004305065,0.000001115536,8.276215e-7,0.00018980958,0.000011690088,0.000095474476],"genre_scores_gemma":[0.99935645,0.000017344626,0.00014981211,0.0000019910767,0.000001182094,0.0000024700098,0.0003735766,0.0000024540532,0.000094737414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999652,0.0000050565613,0.0000030923588,0.00001236065,0.0000061887613,0.0000080619575],"domain_scores_gemma":[0.9999279,0.000019166542,0.000016085418,0.000007864777,0.000017145978,0.000011843893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018117178,0.00022694381,0.00014796539,0.00030123806,0.00015756332,0.00024706038,0.00013804845,0.00023544562,0.000281434],"category_scores_gemma":[0.00019237383,0.00009743301,0.00026039217,0.00023111983,0.00012225955,0.00018675407,0.00014415523,0.00009747148,0.0000635277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004963172,0.00013815974,0.87606555,0.000108671215,0.00019258015,0.000549761,0.0004557987,0.05513515,0.05278736,0.00012830734,0.0003843939,0.013558044],"study_design_scores_gemma":[0.000006465742,0.000046792276,0.9525565,0.000007787757,0.000037150196,0.00008613134,0.00016523145,0.04234039,0.0041889744,0.000041990268,0.0005101499,0.000012388011],"about_ca_topic_score_codex":0.017522302,"about_ca_topic_score_gemma":0.027105978,"teacher_disagreement_score":0.017522302,"about_ca_system_score_codex":0.00033936324,"about_ca_system_score_gemma":0.00015941272,"threshold_uncertainty_score":0.034840643},"labels":[],"label_agreement":null},{"id":"W4413170854","doi":"10.1029/2025gb008608","title":"Dissolved Oxygen Variability on the Canadian Pacific Shelf: Trends, Drivers, and Projections in the Context of Emerging Hypoxia in Queen Charlotte Sound","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Fisheries and Oceans Canada; Tula Foundation; University of British Columbia","funders":"Tula Foundation","keywords":"Oceanography; Hypoxia (environmental); Queen (butterfly); Sound (geography); Context (archaeology); Pacific ocean; Environmental science; Geography; Geology; Oxygen; Archaeology; Biology; Ecology; Chemistry","score_opus":0.009623278523020314,"score_gpt":0.21457015185124018,"score_spread":0.20494687332821987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413170854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99010426,0.0003592668,0.00018778913,0.0006391419,0.000016412556,0.000016404294,0.007098279,0.000022043781,0.001556362],"genre_scores_gemma":[0.99602425,0.00024996593,0.00020707278,0.00005334837,0.000006282075,0.000009872033,0.002898757,0.0000037627137,0.0005466292],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973017,0.0000134364445,0.000014220475,0.00005565545,0.0001050255,0.00008157597],"domain_scores_gemma":[0.99827206,0.000060675764,0.00020232913,0.000031306685,0.0011246754,0.00030893463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044696254,0.00041579435,0.00020559886,0.0013836892,0.001135635,0.0012489639,0.00080457266,0.00046683496,0.0009821085],"category_scores_gemma":[0.0011107526,0.0002271161,0.000503739,0.0025680403,0.00040688523,0.00040476635,0.0007951304,0.00055974856,0.00013738411],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032663007,0.0000137661855,0.9937172,0.000024531284,0.00004951601,0.00005722442,0.00023899197,0.0008403893,0.0003730967,0.00009231992,0.0011939039,0.0033663579],"study_design_scores_gemma":[0.000002459043,0.0000062447725,0.9960756,0.000011853797,0.00001588072,0.000012047266,0.00055643026,0.0024550548,0.000047265206,0.000022493308,0.00078709977,0.0000074537843],"about_ca_topic_score_codex":0.9896437,"about_ca_topic_score_gemma":0.9932981,"teacher_disagreement_score":0.015559254,"about_ca_system_score_codex":0.015559254,"about_ca_system_score_gemma":0.016015645,"threshold_uncertainty_score":0.11289084},"labels":[],"label_agreement":null},{"id":"W4413623734","doi":"10.1029/2025gb008534","title":"Climate Change and Urbanization Decouple Dissolved Organic Carbon Quantity and Composition in Streams","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"STREAMS; Dissolved organic carbon; Environmental science; Urbanization; Climate change; Total organic carbon; Composition (language); Carbon fibers; Carbon cycle; Environmental chemistry; Hydrology (agriculture); Oceanography; Ecosystem; Chemistry; Ecology; Geology","score_opus":0.00920782826882777,"score_gpt":0.21214347527246802,"score_spread":0.20293564700364025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413623734","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993118,0.000042988628,0.00017618648,0.000012470499,0.000001396962,0.0000017923138,0.00020368195,0.0000053179006,0.0002443365],"genre_scores_gemma":[0.9996643,0.000032713844,0.000085749634,0.0000039193374,0.0000019993156,0.0000018449323,0.00015128776,0.0000019373967,0.00005627075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990404,0.000030432675,0.0000076004603,0.000028209717,0.000012377009,0.000017325356],"domain_scores_gemma":[0.99972826,0.00009531869,0.00006654019,0.000021102238,0.00005389231,0.000034923018],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026592053,0.00012358345,0.00016484698,0.00045027566,0.00022255107,0.00056738814,0.00010188183,0.00016733876,0.0006723871],"category_scores_gemma":[0.0005397859,0.00009119149,0.0002360253,0.00072859845,0.00020399586,0.00041010484,0.00026166215,0.00013917084,0.00007181745],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001258654,0.00004503792,0.9801174,0.000022095739,0.000074743504,0.000062731444,0.0001639149,0.0026859015,0.01054238,0.00019052779,0.000108952445,0.0058605312],"study_design_scores_gemma":[0.0000021543435,0.000016401587,0.9942761,0.0000034661996,0.00001945442,0.000019992955,0.0001761078,0.0044093262,0.0006934555,0.0001152793,0.0002644319,0.0000037637512],"about_ca_topic_score_codex":0.006944328,"about_ca_topic_score_gemma":0.012041719,"teacher_disagreement_score":0.006944328,"about_ca_system_score_codex":0.0003596859,"about_ca_system_score_gemma":0.00029805247,"threshold_uncertainty_score":0.013807833},"labels":[],"label_agreement":null},{"id":"W4414847284","doi":"10.1029/2024gb008446","title":"Global “Climate Opportunity Benefit” of Forest Regeneration: Meta‐Analysis Shows Warming From Soil CH <sub>4</sub> and N <sub>2</sub> O Is Small Relative to Agriculture","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Biome; Ecosystem; Greenhouse gas; Biomass (ecology); Temperate climate; Global warming; Climate change; Agriculture; Greenhouse effect; Forest ecology","score_opus":0.01248816636582728,"score_gpt":0.21868691025172657,"score_spread":0.2061987438858993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414847284","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.30662334,0.67271274,0.007993659,0.002735683,0.0007799395,0.00016545613,0.0065077734,0.00053876115,0.001942637],"genre_scores_gemma":[0.97404456,0.021568203,0.0016553584,0.0008170972,0.00017076076,0.000068986876,0.0013118162,0.000102645754,0.00026056537],"study_design_codex":"meta_analysis","study_design_gemma":"meta_analysis","domain_scores_codex":[0.99481225,0.0030265898,0.0004967736,0.0012437132,0.0002336722,0.00018702548],"domain_scores_gemma":[0.98768395,0.009480811,0.0009826202,0.0011437562,0.00032832084,0.00038058832],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.012288632,0.0025477393,0.006574098,0.0028478953,0.00048594098,0.002883593,0.0020974712,0.0018766463,0.003352776],"category_scores_gemma":[0.013889475,0.0010571313,0.03224388,0.0030125366,0.0008856159,0.0012136336,0.0015694668,0.0017737554,0.0003260703],"study_design_candidate":"meta_analysis","study_design_consensus":"meta_analysis","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0034533022,0.000032745273,0.02562075,0.012160377,0.9455527,0.00018532202,0.000058537036,0.0032066111,0.0021068954,0.0002002145,0.00072719227,0.0066952882],"study_design_scores_gemma":[0.0005190436,0.00036877266,0.035439868,0.00086226227,0.95753545,0.0001256874,0.00007819021,0.0019717861,0.0007158286,0.00068971637,0.0016437992,0.000049629016],"about_ca_topic_score_codex":0.0056997645,"about_ca_topic_score_gemma":0.006842494,"teacher_disagreement_score":0.012288632,"about_ca_system_score_codex":0.0007766241,"about_ca_system_score_gemma":0.0008894543,"threshold_uncertainty_score":0.06498927},"labels":[],"label_agreement":null},{"id":"W4415245531","doi":"10.1029/2025gb008520","title":"Temporal Decoupling Between Total Organic Carbon and Iron in Lakes Linked to Interannual Changes in Precipitation","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Carl Tryggers Stiftelse för Vetenskaplig Forskning; Academy of Finland; Svenska Forskningsrådet Formas","keywords":"Total organic carbon; Sulfur; Decoupling (probability); Deposition (geology); Precipitation; Context (archaeology); Carbon fibers; Dissolved organic carbon","score_opus":0.00783424643262183,"score_gpt":0.22650088958845152,"score_spread":0.21866664315582968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415245531","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995246,0.000040085793,0.000121197976,0.000013459816,0.0000010039101,0.0000013153242,0.00018530109,0.000004316601,0.00010877044],"genre_scores_gemma":[0.99968827,0.000012815167,0.000078093144,0.0000042047077,0.0000012437096,0.0000028272448,0.00017607544,0.0000010568218,0.000035537516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987864,0.000024518922,0.000009276985,0.00004139899,0.000018853621,0.000027334165],"domain_scores_gemma":[0.9994765,0.00012103725,0.00020088145,0.000030425437,0.0001172792,0.000053967244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042095868,0.00014283089,0.00020279486,0.00074693817,0.0002460742,0.0003300649,0.00018887108,0.00019877825,0.0004101207],"category_scores_gemma":[0.0010013555,0.00015432834,0.00016633463,0.0008005198,0.00024178726,0.00027872418,0.00033089195,0.00013358245,0.00004435389],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014085442,0.00001940021,0.98820436,0.000017696719,0.00010274306,0.00006583625,0.00024640455,0.0012459197,0.0064903544,0.00007999409,0.0001294861,0.0032568597],"study_design_scores_gemma":[0.0000016842321,0.0000072881717,0.99753606,0.0000013179521,0.0000086752225,0.000009330207,0.00005460085,0.0021333334,0.00015974637,0.000023556431,0.000062038016,0.0000024252827],"about_ca_topic_score_codex":0.04864493,"about_ca_topic_score_gemma":0.07608393,"teacher_disagreement_score":0.04864493,"about_ca_system_score_codex":0.00057374407,"about_ca_system_score_gemma":0.0003503457,"threshold_uncertainty_score":0.09672356},"labels":[],"label_agreement":null},{"id":"W4415617120","doi":"10.1029/2025gb008540","title":"A System Reanalysis of the Current Greenhouse Gases Budget of Terrestrial Ecosystems in Russia","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Ministry of Science and Higher Education of the Russian Federation; European Space Agency","keywords":"Eddy covariance; Biome; Carbon cycle; Carbon sink; Greenhouse gas; Ecosystem; Sink (geography); Flux (metallurgy); Carbon flux","score_opus":0.005536041329095026,"score_gpt":0.22043735544604082,"score_spread":0.2149013141169458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415617120","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.974423,0.0005507508,0.009208808,0.00018652558,0.00009607926,0.00002172863,0.011606189,0.0007008555,0.0032060433],"genre_scores_gemma":[0.98692733,0.0002610797,0.0051243925,0.000019831034,0.000018607585,0.00002267442,0.006944476,0.000057878417,0.000623756],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998951,0.00002278317,0.000009197809,0.000033830634,0.000025734684,0.000013410969],"domain_scores_gemma":[0.99985695,0.00002250054,0.000021646236,0.00002551645,0.00006359647,0.000009699778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031340632,0.00031215957,0.00041753444,0.00061240984,0.00019197712,0.0006114679,0.00033316377,0.00028634668,0.0006118299],"category_scores_gemma":[0.0004726584,0.000295415,0.00078626024,0.0007377941,0.00014409846,0.00043958225,0.00023781434,0.0002605362,0.00027822505],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022942822,0.00008492383,0.11545111,0.00022815853,0.0012215306,0.00019017563,0.00015167099,0.8191141,0.01812177,0.0015119483,0.0034524733,0.040242698],"study_design_scores_gemma":[0.000102907776,0.00006972292,0.29143083,0.000052285584,0.00039064736,0.00006833218,0.000120073775,0.69097203,0.004279044,0.0008628233,0.011576133,0.00007510664],"about_ca_topic_score_codex":0.063867964,"about_ca_topic_score_gemma":0.04281049,"teacher_disagreement_score":0.063867964,"about_ca_system_score_codex":0.00071553374,"about_ca_system_score_gemma":0.0010505704,"threshold_uncertainty_score":0.1269924},"labels":[],"label_agreement":null},{"id":"W4416097134","doi":"10.1029/2025gb008644","title":"Hydrology and Trophic Status Control Lake Dissolved Organic Matter Concentration and Composition at a Continental Scale","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bureau de Coopération Interuniversitaire; Toronto Metropolitan University; Université de Montréal; Université du Québec à Montréal","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Groupe de recherche interuniversitaire en limnologie","keywords":"Dissolved organic carbon; Hydrology (agriculture); Composition (language); Trophic level; Watershed; Surface water; Organic matter","score_opus":0.0026874214027455775,"score_gpt":0.1827835359061044,"score_spread":0.18009611450335883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416097134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99903595,0.00011154395,0.00013732066,0.000020133968,9.830736e-7,0.0000036138379,0.00019159849,0.000007984153,0.00049089803],"genre_scores_gemma":[0.99938715,0.0000612446,0.00013253686,0.000011220951,5.940119e-7,0.0000016540869,0.00013286792,0.0000029158066,0.00026968474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999201,0.000008191718,0.0000029296766,0.00002069466,0.000015980708,0.000031978874],"domain_scores_gemma":[0.99975675,0.000036711637,0.0000411708,0.000010650166,0.0001011634,0.00005362489],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014205331,0.0001871141,0.00016523001,0.00045709257,0.00065475935,0.0006749851,0.00023354699,0.00017193954,0.0006906096],"category_scores_gemma":[0.00040095035,0.00017196774,0.00020397606,0.0005685954,0.00040839706,0.0002930019,0.00035052933,0.0001284845,0.00007501342],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022642975,0.000024202724,0.9142346,0.000039408314,0.00018485294,0.000109681765,0.00045797334,0.0010368559,0.07477745,0.0002519299,0.0003047326,0.008351956],"study_design_scores_gemma":[0.0000013949565,0.0000066910297,0.9986008,0.000001785358,0.000015323707,0.000007939303,0.0001327573,0.00052035006,0.0004981001,0.00002842786,0.00018390878,0.0000025270724],"about_ca_topic_score_codex":0.57839894,"about_ca_topic_score_gemma":0.72646,"teacher_disagreement_score":0.57839894,"about_ca_system_score_codex":0.0021062172,"about_ca_system_score_gemma":0.0016885174,"threshold_uncertainty_score":0.8481679},"labels":[],"label_agreement":null},{"id":"W4416391719","doi":"10.1029/2025gb008676","title":"Assessing Marine Snow Dynamics During the Demise of the North Atlantic Spring Bloom Using In Situ Particle Imagery","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Marine snow; Bloom; Entrainment (biomusicology); Snow; Spring bloom; Storm; Mixed layer; Deep sea; Ocean color","score_opus":0.00832977447286126,"score_gpt":0.217831464695498,"score_spread":0.20950169022263673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416391719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985,0.000029065453,0.00024790343,0.00003013482,0.000005007896,0.000006382818,0.00074677524,0.000020714242,0.0004140155],"genre_scores_gemma":[0.9983156,0.00003564107,0.00054671906,0.000011606903,0.000005281118,0.0000066270327,0.0009470709,0.0000038195135,0.00012771084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999167,0.000011223824,0.00000731144,0.000023288108,0.000023750212,0.000017801713],"domain_scores_gemma":[0.9997185,0.000059663464,0.000082437014,0.0000242563,0.00006818201,0.000046904224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033781418,0.000292008,0.00019975884,0.0006671132,0.0003095805,0.00043398282,0.00026313117,0.0003447337,0.0005126897],"category_scores_gemma":[0.0005639561,0.00015523336,0.0002814866,0.0004350614,0.00013444014,0.0003017632,0.00028272785,0.00022074375,0.00013143611],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016857279,0.00007307675,0.97588897,0.000031324736,0.00008055072,0.00015282912,0.00024148065,0.0052907127,0.009819276,0.00008226456,0.00042118208,0.007749724],"study_design_scores_gemma":[0.0000047477242,0.000021838741,0.98537457,0.000006961573,0.00001348242,0.000016246953,0.00015355842,0.013519355,0.0006290565,0.00002380743,0.00023241932,0.0000040325745],"about_ca_topic_score_codex":0.057279386,"about_ca_topic_score_gemma":0.14871338,"teacher_disagreement_score":0.057279386,"about_ca_system_score_codex":0.0006868319,"about_ca_system_score_gemma":0.00029481092,"threshold_uncertainty_score":0.11389196},"labels":[],"label_agreement":null},{"id":"W7115181701","doi":"10.1029/2025gb008643","title":"Elucidating the Role of Marine Benthic Carbon in a Changing World","year":2025,"lang":"en","type":"article","venue":"Global Biogeochemical Cycles","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Benthic zone; Biogeochemistry; Carbon cycle; Coupled model intercomparison project; Ecosystem; Earth system science; Climate change; Global change","score_opus":0.005654464355659068,"score_gpt":0.22077009510897783,"score_spread":0.21511563075331877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7115181701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9079294,0.0372671,0.013693722,0.017060256,0.00022082099,0.000033339522,0.0012834363,0.00006330961,0.022448653],"genre_scores_gemma":[0.9803462,0.013385112,0.0046415552,0.00079459575,0.00006420534,0.000008350546,0.00017319662,0.0000073712213,0.000579401],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988735,0.000034377612,0.0000064772266,0.000032986773,0.000018356875,0.000020517946],"domain_scores_gemma":[0.9996258,0.00009424653,0.00008850232,0.000032350934,0.0000968245,0.000062132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006602907,0.00025106204,0.00021415242,0.0008282133,0.000459678,0.001589614,0.0003741122,0.0005620819,0.0012300296],"category_scores_gemma":[0.00091168255,0.00011699517,0.00024133333,0.0011574251,0.00080111163,0.0019850063,0.00082165946,0.0006241817,0.0001552711],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019807552,0.00017200847,0.59045035,0.0013479633,0.0005517188,0.0007664344,0.0015411559,0.031691615,0.043720767,0.07142684,0.008202404,0.24993065],"study_design_scores_gemma":[0.000012006643,0.00020003325,0.7424392,0.00085140334,0.00024618712,0.00024456892,0.008032157,0.040893856,0.0069450494,0.13335034,0.0666995,0.00008580519],"about_ca_topic_score_codex":0.022889959,"about_ca_topic_score_gemma":0.030522399,"teacher_disagreement_score":0.022889959,"about_ca_system_score_codex":0.0011143124,"about_ca_system_score_gemma":0.0008660631,"threshold_uncertainty_score":0.04551345},"labels":[],"label_agreement":null}]}