{"meta":{"query_hash":"06bf393297d5","filters":{"venue":"Geological Magazine"},"cohort_total":165,"direct_labels_cover":0,"predictions_cover":165,"exported":165,"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/06bf393297d5","api":"https://metacan.xera.ac/api/v1/cohort?venue=Geological+Magazine"},"results":[{"id":"W1967972725","doi":"10.1017/s0016756808004901","title":"The Euphrates volcanic field, northeastern Syria: petrogenesis of Cenozoic basanites and alkali basalts","year":2008,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical 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":"Ministère de l'Agriculture, des Pêcheries et de l'Alimentation","funders":"","keywords":"Geology; Geochemistry; Basalt; Partial melting; Petrogenesis; Olivine; Lava; Fractional crystallization (geology); Plagioclase; Volcanic rock; Ultramafic rock; Mantle (geology); Volcano; Alkali basalt; Quartz; Paleontology","score_opus":0.012197779225959967,"score_gpt":0.183049709334649,"score_spread":0.17085193010868904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967972725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983546,0.00010333288,0.000014181961,0.000008579977,6.8014555e-7,0.0000030644417,0.000062537714,0.000001777064,0.0014511606],"genre_scores_gemma":[0.99931824,0.00009424305,0.000031277123,0.000003068327,0.0000014294857,0.000001689194,0.00010533141,9.687495e-7,0.00044371988],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999579,0.0000048796896,0.00000344121,0.000008219809,0.000008238283,0.00001728488],"domain_scores_gemma":[0.9999585,0.0000048888596,0.000013963158,0.000003150825,0.000010588021,0.00000892804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009746265,0.00018599081,0.00013560482,0.0010966951,0.00042214553,0.00046113218,0.00007315111,0.00008705481,0.0015427675],"category_scores_gemma":[0.000115343006,0.00012616826,0.00006276572,0.0005623866,0.00038469763,0.00015941107,0.00035883134,0.00007858643,0.00019841205],"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":[0.00037475658,0.00004889047,0.9129469,0.00011419912,0.000049043832,0.0020217844,0.0017488269,0.0007527588,0.039821874,0.001129562,0.0004480903,0.040543355],"study_design_scores_gemma":[0.0000050827302,0.000019021043,0.9981698,0.0000076528195,0.0000044825947,0.0002453099,0.0002725165,0.00015958403,0.0004251238,0.000016595419,0.0006738223,0.0000010755969],"about_ca_topic_score_codex":0.021030204,"about_ca_topic_score_gemma":0.0710464,"teacher_disagreement_score":0.021030204,"about_ca_system_score_codex":0.00067996926,"about_ca_system_score_gemma":0.0005652396,"threshold_uncertainty_score":0.04181564},"labels":[],"label_agreement":null},{"id":"W1976418321","doi":"10.1017/s001675681000083x","title":"Geochemical implications of gabbro from the slow-spreading Northern Central Indian Ocean Ridge, Indian Ocean","year":2010,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical 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":"University of British Columbia","funders":"","keywords":"Gabbro; Geology; Basalt; Geochemistry; Olivine; Plagioclase; Norite; Petrology; Paleontology","score_opus":0.008841770262929972,"score_gpt":0.19351789545474815,"score_spread":0.18467612519181817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976418321","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978992,0.00045760119,0.00003225221,0.000057500605,0.0000047619583,0.0000041098046,0.00021445843,0.000010730736,0.0013193815],"genre_scores_gemma":[0.9990025,0.0002490177,0.00012581616,0.00002874288,0.0000038145643,0.0000022625472,0.0002947619,0.0000052694827,0.00028770894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998915,0.000007699467,0.000010669046,0.000034951543,0.000021907668,0.0000331406],"domain_scores_gemma":[0.99977,0.000018875735,0.00006497015,0.000018391727,0.000085621825,0.000042260952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019413594,0.00033571944,0.00019857271,0.0016688466,0.000872782,0.00091884116,0.00036545325,0.00025538696,0.0007918793],"category_scores_gemma":[0.0003980438,0.00019267891,0.00023945137,0.0010215056,0.0004605291,0.0003163374,0.00055375585,0.000238974,0.00014162659],"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":[0.00018692587,0.000033652897,0.8473695,0.00012635185,0.000082433995,0.001093552,0.0018582593,0.00023268492,0.13416514,0.00012248497,0.00012559163,0.014603461],"study_design_scores_gemma":[0.0000013500728,0.000009975365,0.9976266,0.0000074964473,0.000012506828,0.00011075085,0.0005770865,0.00006176535,0.0011261547,0.000010814966,0.00045243048,0.0000031705983],"about_ca_topic_score_codex":0.17231633,"about_ca_topic_score_gemma":0.30386764,"teacher_disagreement_score":0.17231633,"about_ca_system_score_codex":0.0010542399,"about_ca_system_score_gemma":0.00077919156,"threshold_uncertainty_score":0.34262663},"labels":[],"label_agreement":null},{"id":"W1978081540","doi":"10.1017/s0016756811001026","title":"Intra-basaltic soil formation, sedimentary reworking and eodiagenetic K-enrichment in the Middle to Upper Ordovician Dunn Point Formation of eastern Canada: a rare window into early Palaeozoic surface and near-surface conditions","year":2011,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Saint Mary's University","funders":"","keywords":"Geology; Geochemistry; Ordovician; Basalt; Soil water; Soil horizon; Soil science","score_opus":0.018714221351396235,"score_gpt":0.19188786326894477,"score_spread":0.17317364191754853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978081540","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980622,0.00024397162,0.000024261259,0.000015576934,0.0000017919889,0.0000039053725,0.00034906404,0.0000055701994,0.0012935974],"genre_scores_gemma":[0.9991074,0.0000955337,0.000030426445,0.000004560697,7.296739e-7,0.0000010683758,0.00024468382,0.0000024578724,0.0005130836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998288,0.00000437028,0.0000074247296,0.000035779958,0.000030716532,0.00009291349],"domain_scores_gemma":[0.99971503,0.000012563285,0.0000311472,0.000010210821,0.00013480695,0.00009630065],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010384203,0.00024541744,0.00021593872,0.0022603688,0.0017103009,0.0012966847,0.0005095658,0.00027470285,0.0018175374],"category_scores_gemma":[0.00029718791,0.0001880108,0.00017987838,0.0020852815,0.00094962545,0.00024702906,0.000522823,0.00019370051,0.00022008385],"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":[0.00012049501,0.000021516058,0.9744873,0.000039682815,0.000047034937,0.0005423442,0.0021888898,0.0002564583,0.010642789,0.00035513044,0.00026409343,0.011034355],"study_design_scores_gemma":[8.20083e-7,0.000003770605,0.99866056,0.000005192593,0.0000034624122,0.00003757974,0.00064815657,0.000059262467,0.00011391591,0.000008274144,0.00045638776,0.0000025853967],"about_ca_topic_score_codex":0.9535799,"about_ca_topic_score_gemma":0.9847413,"teacher_disagreement_score":0.046420097,"about_ca_system_score_codex":0.007867709,"about_ca_system_score_gemma":0.005983032,"threshold_uncertainty_score":0.09338689},"labels":[],"label_agreement":null},{"id":"W1986466812","doi":"10.1017/s0016756801255599","title":"B<scp>RADLEY</scp>, R. S. 1999. <i>Paleoclimatology. Reconstructing Climates of the Quaternary</i>, 2nd ed. International Geophysics Series, Volume 64. xv+613 pp. San Diego, London, Boston, New York, Sydney, Tokyo, Toronto: Academic Press. Price £44.95 (hard covers). ISBN 0 12 124010 X.","year":2001,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geology and Paleoclimatology Research","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":"Volume (thermodynamics); Series (stratigraphy); Paleoclimatology; Quaternary; Geology; Environmental ethics; History; Archaeology; Oceanography; Philosophy; Climate change; Paleontology","score_opus":0.024290594989192872,"score_gpt":0.2370043360780197,"score_spread":0.21271374108882685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986466812","genre_codex":"other","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00097086676,0.41925648,0.0041512605,0.05524005,0.028065713,0.000092810136,0.013780999,0.0017719377,0.47666988],"genre_scores_gemma":[0.0059005828,0.24740338,0.0039260047,0.0052909576,0.0048144455,0.000075958356,0.006742045,0.0009956292,0.724851],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995035,0.00004343013,0.00004011956,0.00007919944,0.0002958932,0.000037845948],"domain_scores_gemma":[0.99847025,0.00031808633,0.00011690945,0.00007690051,0.00082403794,0.00019385904],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000570553,0.0016454135,0.0010348324,0.0035191302,0.0011270951,0.0035934777,0.0009971054,0.0015479818,0.33543006],"category_scores_gemma":[0.0025077583,0.0007944313,0.0005447096,0.006737082,0.0008043158,0.0039489837,0.0011809889,0.0027961046,0.29784277],"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":[0.000009758664,0.0000032577077,0.000078999175,0.00015147091,0.000003530069,0.000021837814,0.000028636608,0.00002583724,0.00013627994,0.00061008934,0.94490516,0.054025203],"study_design_scores_gemma":[0.0000029671405,0.000006427674,0.0009898734,0.0002218783,0.0000040353107,0.000076347664,0.00005898177,0.000025061898,0.00009263741,0.0008838676,0.99763215,0.0000057512825],"about_ca_topic_score_codex":0.031941034,"about_ca_topic_score_gemma":0.08119522,"teacher_disagreement_score":0.33543006,"about_ca_system_score_codex":0.001793465,"about_ca_system_score_gemma":0.0015988499,"threshold_uncertainty_score":0.94792837},"labels":[],"label_agreement":null},{"id":"W1989178395","doi":"10.1017/s0016756801005957","title":"Late Cenozoic, post-collisional Aegean igneous rocks: Nd, Pb and Sr isotopic constraints on petrogenetic and tectonic models","year":2001,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":101,"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; Saint Mary's University","funders":"","keywords":"Geology; Geochemistry; Igneous rock; Basalt; Continental crust; Subduction; Zircon; Terrigenous sediment; Partial melting; Mantle (geology); Oceanic crust; Sedimentary rock; Paleontology; Tectonics","score_opus":0.012455208332061003,"score_gpt":0.1921407049263912,"score_spread":0.1796854965943302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989178395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946913,0.00048245868,0.0009895719,0.000029820278,0.0000030708497,0.000004002085,0.00044510313,0.00003239298,0.003322276],"genre_scores_gemma":[0.9976292,0.00026422128,0.00084299996,0.000004687542,0.000001290464,0.0000027513256,0.00053304416,0.0000068991894,0.00071488076],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999695,0.00000520578,0.0000030776175,0.000010515142,0.0000062260474,0.0000054579004],"domain_scores_gemma":[0.99994993,0.000009420486,0.000011834951,0.000009359513,0.000014925452,0.0000045826523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017329412,0.00024095626,0.00009555295,0.00043050904,0.00013796713,0.00035521554,0.00020846885,0.00012764812,0.0011889832],"category_scores_gemma":[0.00022186886,0.000086438304,0.00015846583,0.00030851568,0.00020620746,0.0002456307,0.00014454323,0.00010369766,0.00025034734],"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":[0.0005283177,0.000028322478,0.8009752,0.00014454723,0.00012565644,0.00049904233,0.0006462817,0.0132329585,0.12099759,0.0032592074,0.00030437976,0.059258427],"study_design_scores_gemma":[0.000030607433,0.00009718612,0.943066,0.000031997093,0.0000670795,0.0006068777,0.00040525783,0.02119802,0.022200555,0.0016598576,0.010621792,0.0000147328665],"about_ca_topic_score_codex":0.013401635,"about_ca_topic_score_gemma":0.021961886,"teacher_disagreement_score":0.013401635,"about_ca_system_score_codex":0.00086713285,"about_ca_system_score_gemma":0.00026746112,"threshold_uncertainty_score":0.02664727},"labels":[],"label_agreement":null},{"id":"W1997554288","doi":"10.1017/s0016756812000751","title":"History of faulting on the Doruneh Fault System: implications for the kinematic changes of the Central Iranian Microplate","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"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":"","keywords":"Geology; Clockwise; Fault (geology); Paleontology; Seismology; Kinematics; Fold (higher-order function); Rotation (mathematics); Geometry","score_opus":0.035051918193407555,"score_gpt":0.20825782642081295,"score_spread":0.1732059082274054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997554288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994068,0.001489015,0.0005178968,0.00018224724,0.000020578802,0.0000084698895,0.00021412011,0.000022173248,0.0034774342],"genre_scores_gemma":[0.99907076,0.00041736703,0.00017277726,0.00001472713,0.000018442777,0.000002523685,0.000113839196,0.0000030779318,0.00018640334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998795,0.000014349658,0.000012126858,0.000042256313,0.000023551253,0.000028156452],"domain_scores_gemma":[0.9997271,0.000025603367,0.00011032627,0.000020563115,0.00008821633,0.00002817018],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052912784,0.0003284452,0.0002482914,0.0021308265,0.000778195,0.0008793234,0.00037300857,0.00042880565,0.0023343007],"category_scores_gemma":[0.0006389889,0.00015132333,0.0002730768,0.001799089,0.00094706035,0.0007304689,0.00053727,0.00030856096,0.00028362256],"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":[0.0002566492,0.000048604972,0.909495,0.00020426315,0.00014305387,0.0010740659,0.0028509998,0.003641968,0.0336017,0.0027032022,0.0003920981,0.04558852],"study_design_scores_gemma":[0.0000081881335,0.000054710952,0.99301636,0.000039326926,0.000037186328,0.0003780885,0.001075918,0.0011187713,0.0011764665,0.00051158667,0.002567852,0.000015520325],"about_ca_topic_score_codex":0.012293217,"about_ca_topic_score_gemma":0.0111655835,"teacher_disagreement_score":0.012293217,"about_ca_system_score_codex":0.0011146001,"about_ca_system_score_gemma":0.00051666267,"threshold_uncertainty_score":0.024443328},"labels":[],"label_agreement":null},{"id":"W1998147849","doi":"10.1017/s0016756810000129","title":"A basal bird from the Campanian (Late Cretaceous) of Dinosaur Provincial Park (Alberta, Canada)","year":2010,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Evolutionary Biology","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":"","keywords":"Cretaceous; Geology; Paleontology; Geography","score_opus":0.007803245089498598,"score_gpt":0.18452572025691116,"score_spread":0.17672247516741257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998147849","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9861562,0.0005000258,0.00022073486,0.00014158293,0.000026263295,0.00003551709,0.0005472013,0.00001866096,0.012353808],"genre_scores_gemma":[0.9934128,0.00030717734,0.00093291025,0.00007784657,0.000008021652,0.000005657992,0.0004824814,0.0000055568125,0.004767553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999231,0.0000024039207,0.0000021982628,0.000015572334,0.00003249632,0.000024239662],"domain_scores_gemma":[0.99987936,0.000008406015,0.000013507343,0.0000067195288,0.000044309152,0.000047745783],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007742669,0.0002015394,0.00016243364,0.0010270464,0.0026087898,0.000624617,0.000343916,0.00020083443,0.003247184],"category_scores_gemma":[0.00017406253,0.000119436285,0.00009240386,0.0011811627,0.0010048097,0.0000919731,0.00037538994,0.00035271473,0.00037805774],"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":[0.0010946365,0.00013119254,0.71746033,0.0004661269,0.000097445685,0.016302215,0.018173084,0.00046042446,0.058672577,0.0021385287,0.0065331724,0.17847025],"study_design_scores_gemma":[0.000011932013,0.00006254361,0.9758807,0.00005758266,0.000024094594,0.0040244497,0.0059380145,0.00012326712,0.00089957815,0.00007635873,0.012890927,0.000010511462],"about_ca_topic_score_codex":0.84536666,"about_ca_topic_score_gemma":0.97152215,"teacher_disagreement_score":0.15463334,"about_ca_system_score_codex":0.002334937,"about_ca_system_score_gemma":0.002963839,"threshold_uncertainty_score":0.31108797},"labels":[],"label_agreement":null},{"id":"W2009060439","doi":"10.1017/s0016756807003615","title":"T. Märss M. V. H. Wilson &amp; R. Thorsteinsson 2006. Silurian and Lower Devonian thelodonts and putative chondrichthyans from the Canadian Artic Archipelago. Special Papers in Palaeontology no. 75. 144 pp. London: The Palaeontological Association. Price £54.00 (paperback). ISBN 0 901702 99 4; ISSN 0038-6804.","year":2007,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Evolutionary Biology","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":"Devonian; Archipelago; Paleontology; Late Devonian extinction; Geology; Oceanography; Carboniferous","score_opus":0.010563399908607893,"score_gpt":0.20954727916094834,"score_spread":0.19898387925234046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009060439","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":[0.0071119973,0.55679744,0.0030484325,0.040533848,0.021367105,0.00012580295,0.004866246,0.0010302323,0.3651189],"genre_scores_gemma":[0.018199744,0.17904413,0.0025240602,0.0019480817,0.002062602,0.000024474155,0.002464577,0.0002733073,0.79345906],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.999752,0.000012610205,0.000010310325,0.00003369398,0.00016365004,0.000027722048],"domain_scores_gemma":[0.9995579,0.00004939395,0.000048362654,0.00001265499,0.00019308586,0.0001386111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039460984,0.0010185557,0.0005441552,0.0020152645,0.0013998275,0.0017659324,0.0007726899,0.0008554429,0.1607449],"category_scores_gemma":[0.0007744392,0.0005331572,0.00036291825,0.0031125972,0.001058703,0.0012676097,0.0006959514,0.0012207696,0.053465735],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048344536,0.0000061415776,0.0004225675,0.00027651366,0.000008500334,0.00008541928,0.00016648631,0.00005712748,0.0005724507,0.00048742554,0.8422325,0.15563644],"study_design_scores_gemma":[0.000007528819,0.000018644172,0.0069030705,0.00028248693,0.00001378799,0.00023225423,0.00033851754,0.00004760966,0.00021406467,0.00044421098,0.9914818,0.000016098284],"about_ca_topic_score_codex":0.24225754,"about_ca_topic_score_gemma":0.6064048,"teacher_disagreement_score":0.75774246,"about_ca_system_score_codex":0.0028293314,"about_ca_system_score_gemma":0.0023113955,"threshold_uncertainty_score":0.53774524},"labels":[],"label_agreement":null},{"id":"W2015735647","doi":"10.1017/s0016756805000555","title":"Fossils and matgrounds from the Neoproterozoic Longmyndian Supergroup, Shropshire, UK","year":2005,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","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":"Memorial University of Newfoundland","funders":"","keywords":"Supergroup; Trace fossil; Paleontology; Geology; Phanerozoic; Assemblage (archaeology); Structural basin; Cenozoic","score_opus":0.014794571042426907,"score_gpt":0.2082424031091291,"score_spread":0.19344783206670219,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015735647","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9647857,0.0050632493,0.0004271787,0.00013862168,0.00005018414,0.000046479672,0.006036567,0.000051501418,0.0234006],"genre_scores_gemma":[0.9668003,0.0042547174,0.00098415,0.000100978104,0.000029636618,0.00003613071,0.005510807,0.000046106892,0.022237262],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998628,0.000009183172,0.000020577365,0.000031929623,0.000050391114,0.000025094805],"domain_scores_gemma":[0.9996012,0.00005173433,0.00015212267,0.000052088206,0.00007466986,0.00006814444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015821686,0.00027299923,0.00018992429,0.0026901658,0.0009745386,0.0004755999,0.00040251922,0.00018449548,0.013069383],"category_scores_gemma":[0.00050581584,0.0001964226,0.000106223655,0.0032325615,0.0007780307,0.00058266555,0.0007987379,0.00025390476,0.0016469652],"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":[0.0009512333,0.000055976834,0.44431248,0.002092942,0.00016218316,0.009181593,0.039396096,0.00050731376,0.074366994,0.0020518666,0.017790904,0.40913045],"study_design_scores_gemma":[0.0000063250677,0.000056233817,0.9552551,0.00011280111,0.000019878855,0.0015606725,0.0023533828,0.000038794806,0.000845264,0.00006987994,0.039672513,0.000009129421],"about_ca_topic_score_codex":0.08573752,"about_ca_topic_score_gemma":0.3880061,"teacher_disagreement_score":0.08573752,"about_ca_system_score_codex":0.0011275175,"about_ca_system_score_gemma":0.00040406195,"threshold_uncertainty_score":0.17047697},"labels":[],"label_agreement":null},{"id":"W2016565796","doi":"10.1017/s0016756811001130","title":"The Grenville–Sveconorwegian orogen in the high Arctic","year":2012,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":91,"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":"Geology; Terrane; Arctic; Paleozoic; Paleontology; Provenance; Lithosphere; Earth science; Oceanography; Tectonics","score_opus":0.013559051932792292,"score_gpt":0.1941264757563325,"score_spread":0.18056742382354019,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016565796","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9703826,0.0042728907,0.00045448105,0.00030290242,0.00010876435,0.000027070206,0.0017469258,0.00004984888,0.022654563],"genre_scores_gemma":[0.99316543,0.0012539726,0.00055216986,0.000056675264,0.000015559737,0.000007464526,0.0012783789,0.000032095664,0.00363839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993461,0.000071161674,0.000047103673,0.0001641451,0.0001273343,0.00024421024],"domain_scores_gemma":[0.99964976,0.000032607157,0.00013104979,0.000022601982,0.00010055634,0.00006336247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008306179,0.0006091046,0.00038607116,0.0022849175,0.0011159941,0.001637563,0.00048802086,0.0003436394,0.0022003946],"category_scores_gemma":[0.00059300236,0.00019275169,0.000289079,0.0021626975,0.00081277813,0.00033175555,0.0011240756,0.00032771612,0.000560006],"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":[0.001133244,0.00007347824,0.81320214,0.00079541263,0.00054742175,0.006764332,0.016046805,0.0011964751,0.030032324,0.006178882,0.0035277228,0.12050185],"study_design_scores_gemma":[0.000016986065,0.00005565353,0.96474206,0.0003551884,0.000088583394,0.0009925697,0.005689885,0.00028579013,0.0014702402,0.00026257287,0.026017776,0.000022641856],"about_ca_topic_score_codex":0.4539068,"about_ca_topic_score_gemma":0.7204989,"teacher_disagreement_score":0.4539068,"about_ca_system_score_codex":0.0025980081,"about_ca_system_score_gemma":0.0034359023,"threshold_uncertainty_score":0.90252954},"labels":[],"label_agreement":null},{"id":"W2017401753","doi":"10.1017/s0016756808005438","title":"Pliocene dinoflagellate cyst stratigraphy, palaeoecology and sequence stratigraphy of the Tunnel-Canal Dock, Belgium","year":2008,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geology and Paleoclimatology Research","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":"Brock University","funders":"","keywords":"Geology; Sequence stratigraphy; Paleontology; Sedimentary depositional environment; Stratigraphy; Transgressive; Sequence (biology); Fluvial; Tectonics; Structural basin","score_opus":0.03307981919496475,"score_gpt":0.2289057665218863,"score_spread":0.19582594732692155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017401753","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946786,0.0004087454,0.00024188083,0.000018214809,0.0000039137058,0.000004103825,0.0011547669,0.00003796495,0.0034516703],"genre_scores_gemma":[0.9961195,0.00017067883,0.0003061888,0.0000040734226,0.0000015607424,0.0000035817654,0.0010917134,0.000029638724,0.0022731659],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998728,0.000010639858,0.000005496457,0.000042308773,0.000031005107,0.0000378136],"domain_scores_gemma":[0.9999149,0.000006714182,0.000025368749,0.000005842825,0.000023007578,0.000024197474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009863435,0.00017116271,0.00015732956,0.0011222048,0.0003652681,0.00097401364,0.00015629978,0.00016009898,0.0027498233],"category_scores_gemma":[0.00020611449,0.0001650557,0.00021233637,0.00096265733,0.0002588466,0.00019131288,0.00032956278,0.0001480831,0.00058176747],"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":[0.0005216798,0.000042569067,0.85472876,0.00015764718,0.00018411234,0.0009007197,0.004656293,0.004992758,0.03585552,0.0011895846,0.0025335522,0.094236836],"study_design_scores_gemma":[0.0000033741576,0.000009673289,0.992366,0.000009899106,0.0000047752906,0.00014391984,0.00034941005,0.00033215704,0.00046102647,0.000021447748,0.006294863,0.0000033975807],"about_ca_topic_score_codex":0.21488182,"about_ca_topic_score_gemma":0.36766624,"teacher_disagreement_score":0.21488182,"about_ca_system_score_codex":0.0014426565,"about_ca_system_score_gemma":0.00064574,"threshold_uncertainty_score":0.4272622},"labels":[],"label_agreement":null},{"id":"W2023345113","doi":"10.1017/s0016756800464411","title":"Z<scp>IMMER</scp>, C. 1998. <i>At the Water's Edge. Macroevolution and the Transformation of Life</i>. ix+290 pp. New York, London, Toronto, Sydney, Singapore: The Free Press; distributed in the UK by Simon &amp; Schuster. Price £17.99, US $25.00, Can. $35.00 (hard covers). ISBN 0 684 83490 1.","year":2000,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Economic Theory and Policy","field":"Economics, Econometrics and Finance","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":"Transformation (genetics); Macroevolution; Enhanced Data Rates for GSM Evolution; Biology; Engineering; Telecommunications","score_opus":0.017295198272835946,"score_gpt":0.19930545934550314,"score_spread":0.1820102610726672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023345113","genre_codex":"other","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":[0.0015108305,0.3877832,0.004752971,0.060552016,0.009650455,0.000089277375,0.012905853,0.001578232,0.5211772],"genre_scores_gemma":[0.01254217,0.23181143,0.0031413536,0.0033355353,0.0023646015,0.00008157303,0.004935741,0.0007792588,0.7410083],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99966776,0.000031180058,0.000022736123,0.00004476298,0.00019919555,0.00003425302],"domain_scores_gemma":[0.9991524,0.00022427904,0.00008848504,0.000050553703,0.00035970184,0.0001245713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037754377,0.0013144129,0.0008642742,0.00257873,0.0009809074,0.0031589018,0.00082886143,0.0013360998,0.28458226],"category_scores_gemma":[0.0019935786,0.00067721517,0.00036652546,0.006273094,0.0011145603,0.00405742,0.0012201722,0.001997321,0.14689013],"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":[0.000012866357,0.000003385167,0.00011424258,0.0001929294,0.000004396594,0.000036372567,0.00009013378,0.00007191562,0.00013321583,0.0037657225,0.93048626,0.0650885],"study_design_scores_gemma":[0.0000041719254,0.000006329976,0.0012442674,0.00032086347,0.000005219828,0.00006355875,0.00012228322,0.000046819,0.00011454517,0.0032539458,0.9948101,0.000007876242],"about_ca_topic_score_codex":0.030114602,"about_ca_topic_score_gemma":0.06536915,"teacher_disagreement_score":0.28458226,"about_ca_system_score_codex":0.0021667155,"about_ca_system_score_gemma":0.0016981589,"threshold_uncertainty_score":0.9520225},"labels":[],"label_agreement":null},{"id":"W2025363919","doi":"10.1017/s001675681300023x","title":"A new species of <i>Largocephalosaurus</i> (Diapsida: Saurosphargidae), with implications for the morphological diversity and phylogeny of the group","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":51,"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 Museum of Nature","funders":"","keywords":"Anatomy; Biology; Skull; Dorsum; Quadrate bone; Sister group; Phylogenetics; Clade","score_opus":0.0197778083303474,"score_gpt":0.19220785934849843,"score_spread":0.17243005101815104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025363919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911718,0.00090362475,0.0018482052,0.000096450174,0.000056476063,0.00007146307,0.0001621269,0.000038746562,0.0056511406],"genre_scores_gemma":[0.9934075,0.0003577926,0.0038344401,0.00015978128,0.000038233688,0.00005741324,0.00033956827,0.000005523533,0.0017998116],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99992466,0.000008516931,0.0000131559045,0.000030935767,0.000015745902,0.000007003907],"domain_scores_gemma":[0.99990845,0.000010130798,0.00003615227,0.000012443732,0.000015037502,0.000017834907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000112070265,0.00030390028,0.0001743331,0.00069345045,0.0009625019,0.00035516324,0.000392345,0.00060883764,0.0019361352],"category_scores_gemma":[0.00019351573,0.00018537557,0.00023971155,0.0003850253,0.00068834855,0.0007321938,0.0008290329,0.0003360709,0.00034163732],"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":[0.00058327464,0.00014030492,0.32313693,0.001070224,0.00024823984,0.013025796,0.009180738,0.0006522396,0.45384368,0.0019794793,0.0017111764,0.19442791],"study_design_scores_gemma":[0.0000670562,0.00084315444,0.9321703,0.00021038373,0.0001924619,0.019797875,0.0031828466,0.0010106338,0.0068217753,0.0006288348,0.035012282,0.00006235673],"about_ca_topic_score_codex":0.00154255,"about_ca_topic_score_gemma":0.0041664816,"teacher_disagreement_score":0.0019361352,"about_ca_system_score_codex":0.00019646267,"about_ca_system_score_gemma":0.00017266868,"threshold_uncertainty_score":0.0064769983},"labels":[],"label_agreement":null},{"id":"W2026624969","doi":"10.1017/s001675681100015x","title":"Petrogenesis of Cenozoic mafic–ultramafic alkaline lavas from the Tigris volcanic field, NE Syria","year":2011,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"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 de l'Agriculture, des Pêcheries et de l'Alimentation","funders":"","keywords":"Geology; Geochemistry; Partial melting; Ultramafic rock; Basalt; Mafic; Petrogenesis; Olivine; Volcanic rock; Fractional crystallization (geology); Mantle (geology); Incompatible element; Lava; Mantle plume; Asthenosphere; Volcano; Petrology; Lithosphere; Tectonics; Paleontology","score_opus":0.023421333641516537,"score_gpt":0.18993903372866783,"score_spread":0.16651770008715128,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026624969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99792176,0.00005682495,0.00002494102,0.000005105931,9.1138713e-7,0.0000043058044,0.00012707777,0.0000034772668,0.0018555941],"genre_scores_gemma":[0.9986975,0.00006875883,0.000063918575,0.0000022830668,0.0000012216018,0.0000017153344,0.00021780274,0.0000028395916,0.0009439839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995863,0.0000033956087,0.000002744045,0.000009761616,0.000010572898,0.000014817328],"domain_scores_gemma":[0.9999552,0.0000050913604,0.000012423445,0.0000053962845,0.000013113328,0.000008775037],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008536221,0.00028280602,0.0001199468,0.001601902,0.0004960955,0.0005087919,0.00013292413,0.00016330939,0.0010908279],"category_scores_gemma":[0.00014455288,0.00019081336,0.00017496408,0.00057743036,0.00031680698,0.00009322448,0.00033899833,0.000125161,0.00032366012],"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":[0.00053098507,0.00006961808,0.8116096,0.00010317635,0.00010162093,0.0047116685,0.0025730676,0.0029443423,0.1444151,0.0007740983,0.0004242878,0.03174239],"study_design_scores_gemma":[0.0000037383927,0.00002469804,0.99649954,0.0000053030662,0.0000074107056,0.00030861647,0.00016474997,0.00046130928,0.0017566344,0.000010505931,0.0007555774,0.0000018083048],"about_ca_topic_score_codex":0.047341943,"about_ca_topic_score_gemma":0.10932434,"teacher_disagreement_score":0.047341943,"about_ca_system_score_codex":0.0009298624,"about_ca_system_score_gemma":0.0005010436,"threshold_uncertainty_score":0.09413278},"labels":[],"label_agreement":null},{"id":"W2029330373","doi":"10.1017/s0016756813001155","title":"Multidisciplinary studies of global Carboniferous stage boundaries: towards a better definition and global correlations: an introduction","year":2014,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":false,"ca_institutions":"Geological Survey of Canada","funders":"National Key Research and Development Program of China; State Key Laboratory of Geological Processes and Mineral Resources","keywords":"Tournaisian; Geology; Gondwana; Paleontology; Viséan; Carboniferous; Supercontinent; Permian; Pennsylvanian; Paleozoic; Craton; Tectonics","score_opus":0.03349095700314972,"score_gpt":0.2751441997347999,"score_spread":0.2416532427316502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029330373","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.43747848,0.4156213,0.06718145,0.015934573,0.0010130109,0.00027348334,0.009241395,0.00036862993,0.05288771],"genre_scores_gemma":[0.8533695,0.07539164,0.05971558,0.0014155866,0.0019914007,0.0003163632,0.002831917,0.00012185169,0.0048463433],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992793,0.0002940248,0.00006573889,0.00021821642,0.00007878592,0.000063954954],"domain_scores_gemma":[0.9964269,0.0017336747,0.00069270015,0.00034651975,0.00054156827,0.0002587089],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023245541,0.0006716506,0.00067588664,0.0093425345,0.0006993138,0.003228388,0.00073367875,0.00062463846,0.0035503188],"category_scores_gemma":[0.0030899136,0.0003134144,0.0007953221,0.016162962,0.0013148304,0.0031962895,0.003179641,0.0009449625,0.0003811738],"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":[0.00007427342,0.00009461136,0.60678977,0.0020137497,0.0007323005,0.00022046945,0.004868604,0.0014752185,0.001679585,0.044393472,0.0073856683,0.3302723],"study_design_scores_gemma":[0.000007744403,0.00016179288,0.86568975,0.001779991,0.00025373176,0.00051189255,0.008428602,0.0030675442,0.00050492265,0.03797122,0.08155928,0.00006367903],"about_ca_topic_score_codex":0.00596515,"about_ca_topic_score_gemma":0.010501248,"teacher_disagreement_score":0.0093425345,"about_ca_system_score_codex":0.0010895794,"about_ca_system_score_gemma":0.0009387625,"threshold_uncertainty_score":0.012293577},"labels":[],"label_agreement":null},{"id":"W2032542353","doi":"10.1017/s0016756812000131","title":"A deep subaqueous fan depositional model for the Palaeoarchaean (3.46 Ga) Marble Bar Cherts, Warrawoona Group, Western Australia","year":2012,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological formations and processes","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":"MaRS","funders":"","keywords":"Geology; Sedimentary depositional environment; Breccia; Turbidity current; Facies; Sedimentary rock; Geochemistry; Group (periodic table); Geomorphology; Paleontology; Structural basin","score_opus":0.05060567134077915,"score_gpt":0.25564147660814035,"score_spread":0.2050358052673612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032542353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98214704,0.00011781009,0.006801887,0.000313309,0.000013893081,0.00004871805,0.000544553,0.000076170254,0.009936579],"genre_scores_gemma":[0.9925568,0.00008699856,0.0028318944,0.000031175045,0.000006590181,0.000045418114,0.00023393484,0.000039795952,0.0041673556],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99994874,0.000012645471,0.000002970946,0.000016539489,0.000007287852,0.00001177802],"domain_scores_gemma":[0.99991035,0.00001077471,0.000010333044,0.0000076003494,0.000027005568,0.000033828765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015474227,0.0003545756,0.00024900236,0.0005412228,0.00060646376,0.00093007635,0.00099443,0.0006872041,0.003521263],"category_scores_gemma":[0.00041261045,0.00038321855,0.00049353327,0.00040278904,0.0006045529,0.00035679425,0.0006104844,0.0003435631,0.00051114534],"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":[0.000075902426,0.00008316812,0.0501822,0.000037439255,0.0000751572,0.00053305796,0.0005522888,0.9314513,0.0034484374,0.0070607867,0.00088831264,0.0056117848],"study_design_scores_gemma":[0.000042790216,0.00003256848,0.025887912,0.000011974981,0.00002142505,0.00007318208,0.00021405722,0.9703831,0.00010421288,0.001591399,0.0016209885,0.000016390508],"about_ca_topic_score_codex":0.2646485,"about_ca_topic_score_gemma":0.19291942,"teacher_disagreement_score":0.2646485,"about_ca_system_score_codex":0.0025939113,"about_ca_system_score_gemma":0.0014968906,"threshold_uncertainty_score":0.52621615},"labels":[],"label_agreement":null},{"id":"W2043923063","doi":"10.1017/s0016756807003780","title":"Last Interglacial (Eemian) hydrographic conditions in the southwestern Baltic Sea based on dinoflagellate cysts from Ristinge Klint, Denmark","year":2007,"lang":"en","type":"article","venue":"Geological Magazine","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":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Brock University","funders":"","keywords":"Eemian; Interglacial; Oceanography; Geology; Hydrography; Pleistocene; Paleontology; Physical geography; Geography","score_opus":0.019667163993314255,"score_gpt":0.2563242972655086,"score_spread":0.23665713327219434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043923063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986401,0.00016298129,0.000028096112,0.000006856947,0.0000033350848,0.0000035701873,0.00061185576,0.000003803084,0.00053930795],"genre_scores_gemma":[0.9979449,0.0001224946,0.00012453721,0.00000874286,0.000002382477,0.000007226454,0.0013603575,0.0000027038177,0.00042655526],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982613,0.0000140623315,0.000025482372,0.000052726435,0.00003452875,0.000047074016],"domain_scores_gemma":[0.9996518,0.00002792365,0.000110500965,0.000019419645,0.00007713401,0.00011326079],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002817669,0.00022452809,0.00021331852,0.0013120064,0.00040949427,0.0006903129,0.0002721048,0.0002513329,0.0009881769],"category_scores_gemma":[0.0003428818,0.00022157795,0.0002190359,0.0007973292,0.00028390423,0.0002697645,0.0006043988,0.00013632773,0.00026400443],"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":[0.00004400966,0.00001899952,0.9927394,0.000025786496,0.000036954396,0.00030050118,0.00079147506,0.00009601352,0.0020749655,0.000032760297,0.00018735391,0.0036517999],"study_design_scores_gemma":[0.000001793867,0.000011853227,0.99876523,0.000007128651,0.0000070402393,0.00008378918,0.000318747,0.000060204726,0.00010313678,0.0000041108847,0.0006354034,0.0000015857158],"about_ca_topic_score_codex":0.06911119,"about_ca_topic_score_gemma":0.16192673,"teacher_disagreement_score":0.06911119,"about_ca_system_score_codex":0.0007817075,"about_ca_system_score_gemma":0.00059046724,"threshold_uncertainty_score":0.13741785},"labels":[],"label_agreement":null},{"id":"W2046148520","doi":"10.1017/s0016756800003769","title":"Superposed Neoproterozoic and Silurian magmatic arcs in central Cape Breton Island, Canada: geochemical and geochronological constraints","year":2000,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Saint Mary's University; McGill University; St. Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Zircon; Diorite; Geochemistry; Gabbro; Hornblende; Pluton; Volcanic rock; Geochronology; Plateau (mathematics); Rift; Igneous rock; Biotite; Paleontology; Volcano; Quartz; Tectonics","score_opus":0.005405461547439181,"score_gpt":0.16214921474731403,"score_spread":0.15674375319987485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046148520","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99185234,0.00066177413,0.00006622911,0.00010001815,0.0000040237796,0.000016242206,0.0013991899,0.000018739433,0.0058814217],"genre_scores_gemma":[0.99599224,0.00032191884,0.00020131569,0.000031372037,0.0000022933773,0.000007537306,0.0008981059,0.000010968829,0.002534291],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985087,0.0000051531033,0.0000070464744,0.000036584788,0.000038105416,0.000062207546],"domain_scores_gemma":[0.99942774,0.000031459902,0.000083636725,0.000013912347,0.0003026166,0.00014059122],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001490579,0.0002459051,0.0002424253,0.00257744,0.0018274795,0.0017207757,0.0006754591,0.00031096695,0.004511594],"category_scores_gemma":[0.0006232347,0.0002937672,0.00018924604,0.0031227458,0.0007554283,0.0003074501,0.00077453064,0.00024530725,0.00033620597],"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":[0.00013604925,0.000028684288,0.9643364,0.00011456046,0.000072859555,0.00046626138,0.003434321,0.0008654722,0.0073396526,0.0007936545,0.0013141056,0.021097882],"study_design_scores_gemma":[0.0000039511956,0.000002998004,0.9966714,0.000022268028,0.000009105808,0.000038146693,0.0010046386,0.0002856727,0.00013433579,0.000023615019,0.0017987621,0.0000049470987],"about_ca_topic_score_codex":0.9932327,"about_ca_topic_score_gemma":0.9984591,"teacher_disagreement_score":0.02003999,"about_ca_system_score_codex":0.02003999,"about_ca_system_score_gemma":0.012496723,"threshold_uncertainty_score":0.145401},"labels":[],"label_agreement":null},{"id":"W2054513775","doi":"10.1017/s001675681200091x","title":"Gross morphology and microstructure of type locality ossicles of<i>Psephophorus polygonus</i>Meyer, 1847 (Testudines, Dermochelyidae)","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Turtle Biology and Conservation","field":"Environmental Science","cited_by":16,"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":"Ministero dell’Istruzione, dell’Università e della Ricerca; Ministère de la Santé et des Services sociaux; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Ossicles; Anatomy; Biology; Gross morphology; Type locality; Morphology (biology); Carapace; Paleontology; Geology; Taxonomy (biology); Zoology; Middle ear","score_opus":0.009952556834929295,"score_gpt":0.21167855404848238,"score_spread":0.20172599721355308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054513775","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899846,0.00008276057,0.00009086584,0.00000213696,0.0000012345231,0.0000039841507,0.0001917037,0.0000042747206,0.00062460144],"genre_scores_gemma":[0.9990613,0.000040139228,0.0002120065,0.0000034447642,0.0000015101349,0.0000045264633,0.00022491784,0.0000036163085,0.00044847524],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991965,0.0000061914434,0.000006543685,0.000032840813,0.000019202884,0.000015565762],"domain_scores_gemma":[0.9997633,0.000021930675,0.000114416434,0.000019682502,0.000034439174,0.000046239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007536052,0.00018596617,0.000110728426,0.0012275407,0.00028940107,0.0003119186,0.00015867251,0.0001714422,0.0013038955],"category_scores_gemma":[0.00017910173,0.00014338354,0.00015210263,0.00040002548,0.00051084824,0.00022514677,0.00038963134,0.00015259291,0.00032804714],"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":[0.00048862805,0.0000453145,0.5502102,0.00013803986,0.000106249936,0.0010494506,0.0012905878,0.00030651529,0.4275014,0.00019227099,0.00013558997,0.018535847],"study_design_scores_gemma":[9.146556e-7,0.00004894594,0.9972441,0.0000024304113,0.0000062466156,0.0003308384,0.00016825482,0.00003325372,0.001844386,0.000009811292,0.00030878256,0.0000021107364],"about_ca_topic_score_codex":0.0027176747,"about_ca_topic_score_gemma":0.004654913,"teacher_disagreement_score":0.0027176747,"about_ca_system_score_codex":0.00020299916,"about_ca_system_score_gemma":0.00008227185,"threshold_uncertainty_score":0.0054036975},"labels":[],"label_agreement":null},{"id":"W2062209960","doi":"10.1017/s0016756805000440","title":"Crustal xenoliths in Triassic lamprophyre dykes in western Morocco: tectonic implications for the Rheic Ocean suture","year":2005,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":51,"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; University of Toronto; Saint Mary's University","funders":"","keywords":"Geology; Terrane; Geochemistry; Zircon; Craton; Granulite; Metamorphism; Fibrous joint; Mafic; Archean; Geochronology; Massif; Petrology; Paleontology; Facies; Tectonics","score_opus":0.0192546753091476,"score_gpt":0.23406114403395928,"score_spread":0.21480646872481168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062209960","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99878544,0.00041817123,0.000019473333,0.000047231537,0.0000026015725,0.0000015110633,0.0000561829,0.0000018991083,0.0006675462],"genre_scores_gemma":[0.9995956,0.0001243707,0.000030555097,0.000008901338,0.000002239582,7.734159e-7,0.00004676082,0.000001073634,0.00018974597],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988496,0.000011000007,0.000007071536,0.000024636345,0.000012952032,0.0000593336],"domain_scores_gemma":[0.9998815,0.000010102652,0.000057291672,0.000007365392,0.000022120623,0.000021465863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023372253,0.00023353832,0.00016880511,0.0013772905,0.000819159,0.0005738318,0.00021098825,0.00023433527,0.001979289],"category_scores_gemma":[0.000284094,0.0001729643,0.00017170918,0.00077245093,0.00045996904,0.0002452965,0.0006623637,0.00013123886,0.00024594192],"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":[0.00013481536,0.000017497114,0.9571501,0.000045674977,0.0000617583,0.0017642741,0.0039205346,0.00020711875,0.014865827,0.00047563636,0.00019135632,0.021165492],"study_design_scores_gemma":[0.0000016187184,0.0000073249257,0.9982895,0.000009853776,0.000007684909,0.0001591903,0.00067345664,0.000062996034,0.00019768692,0.000012535853,0.00057647214,0.0000017541905],"about_ca_topic_score_codex":0.14406823,"about_ca_topic_score_gemma":0.3106258,"teacher_disagreement_score":0.14406823,"about_ca_system_score_codex":0.001674939,"about_ca_system_score_gemma":0.0006148035,"threshold_uncertainty_score":0.28645933},"labels":[],"label_agreement":null},{"id":"W2072375335","doi":"10.1017/s0016756807003597","title":"A new lower Cambrian eodiscoid trilobite fauna from Swedish Lapland and its implications for intercontinental correlation","year":2007,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":23,"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":"Trilobite; Fauna; Baltica; Paleontology; Geology; Ecology; Biology; Ordovician","score_opus":0.018644383978581532,"score_gpt":0.2434405693302125,"score_spread":0.22479618535163096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072375335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985928,0.00019583329,0.00004100784,0.000027953212,0.0000029805387,0.0000026541788,0.0000579713,0.0000030783965,0.001075783],"genre_scores_gemma":[0.99901605,0.00016683173,0.00012014216,0.000020636036,0.0000039829297,0.000004545275,0.0002601146,0.0000018496588,0.00040587928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998759,0.000014761901,0.000015248486,0.000028697832,0.000026027605,0.00003937521],"domain_scores_gemma":[0.99976474,0.000040890875,0.00006428045,0.000015119803,0.00006688995,0.000048130616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019799286,0.00020330636,0.00016493532,0.0016376371,0.00089298346,0.0011004317,0.0002164456,0.00021263541,0.0021194597],"category_scores_gemma":[0.00032697432,0.00010473626,0.00009073315,0.0009829276,0.00057578465,0.00022599092,0.0005624013,0.00021218053,0.00022473262],"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":[0.00017447142,0.0000504351,0.9287856,0.000098413104,0.00003680913,0.0009275803,0.009229045,0.00008391901,0.014247036,0.00021317972,0.00031504506,0.045838397],"study_design_scores_gemma":[0.0000040475916,0.00003804158,0.99274945,0.000045178294,0.000009569212,0.00065856765,0.0031925146,0.00008600152,0.0002502459,0.00005238355,0.002910024,0.0000039911265],"about_ca_topic_score_codex":0.025218584,"about_ca_topic_score_gemma":0.06556863,"teacher_disagreement_score":0.025218584,"about_ca_system_score_codex":0.00070007937,"about_ca_system_score_gemma":0.00042890353,"threshold_uncertainty_score":0.0501436},"labels":[],"label_agreement":null},{"id":"W2074881970","doi":"10.1017/s0016756803007830","title":"Changes in organic matter production and accumulation as a mechanism for isotopic evolution in the Mesoproterozoic ocean","year":2003,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":69,"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":"Biosphere; Isotopes of carbon; Total organic carbon; Organic matter; Geology; δ13C; Arctic; Paleontology; Earth science; Precambrian; Anoxic waters; Oceanography; Ecology; Stable isotope ratio; Chemistry; Environmental chemistry; Biology","score_opus":0.024870114142202727,"score_gpt":0.24269474012655376,"score_spread":0.21782462598435104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074881970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971112,0.0010231903,0.00051881257,0.00015211538,0.000008404323,0.0000036733666,0.00010096192,0.000016749815,0.0010648106],"genre_scores_gemma":[0.9982905,0.00076815207,0.00043225515,0.000030127921,0.000009700369,0.0000027528238,0.000074996075,0.0000039853503,0.0003875272],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995196,0.000008955029,0.0000045067122,0.000011237994,0.000011474286,0.000011894005],"domain_scores_gemma":[0.99989986,0.000016514283,0.000033760087,0.00001013534,0.00002063508,0.000019141196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028999877,0.0002189883,0.00012721603,0.00060024566,0.00038267096,0.00062393246,0.000188464,0.00019888481,0.00041373298],"category_scores_gemma":[0.00029185132,0.00028613274,0.00012657954,0.00045243726,0.00060065114,0.00041573503,0.00025461236,0.000205343,0.000085237196],"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":[0.00044910383,0.00003583058,0.729739,0.00009334072,0.000082636085,0.0004343734,0.00066907855,0.0016042984,0.22375111,0.002308103,0.0003583292,0.040474806],"study_design_scores_gemma":[0.000008618592,0.000047074074,0.9895927,0.000010072638,0.000035724228,0.00013070845,0.00024114581,0.0014078794,0.006552876,0.00066759984,0.0012975789,0.000008161989],"about_ca_topic_score_codex":0.009898321,"about_ca_topic_score_gemma":0.018514603,"teacher_disagreement_score":0.009898321,"about_ca_system_score_codex":0.00090077956,"about_ca_system_score_gemma":0.00029987725,"threshold_uncertainty_score":0.019681454},"labels":[],"label_agreement":null},{"id":"W2075593710","doi":"10.1017/s0016756811000665","title":"An evaluation of crustal assimilation within the Late Devonian South Mountain Batholith, SW Nova Scotia","year":2012,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Saint Mary's University","funders":"","keywords":"Zircon; Geology; Batholith; Geochemistry; Leucogranite; Pluton; Biotite; Terrane; Crust; Petrology; Quartz; Metamorphic rock; Paleontology; Gneiss; Tectonics","score_opus":0.03805778895657201,"score_gpt":0.25591905403003024,"score_spread":0.2178612650734582,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075593710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980399,0.00014978007,0.000047548034,0.000011892338,0.0000018679688,0.0000074942973,0.0007217379,0.0000046645473,0.0010151328],"genre_scores_gemma":[0.9988789,0.00008509059,0.00007546931,0.000005424564,8.838517e-7,0.0000034761138,0.00048649765,0.0000028992904,0.00046139938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998945,0.000008598261,0.000009478575,0.000026872782,0.000024146773,0.00003624459],"domain_scores_gemma":[0.9995989,0.000031519532,0.000079588164,0.000020622612,0.00018253495,0.00008677818],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001942426,0.00031555453,0.00016157415,0.0016549219,0.00064649555,0.0006647989,0.0002457462,0.00014547906,0.001157008],"category_scores_gemma":[0.0005971006,0.00017552721,0.0002712498,0.0013102706,0.0003495669,0.00015391069,0.00044785172,0.00010183909,0.0002832205],"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":[0.000093972834,0.000005858651,0.9884497,0.00004188501,0.000052093288,0.00028245797,0.0007699235,0.0004395925,0.00427907,0.000043480934,0.00017254737,0.005369399],"study_design_scores_gemma":[8.6233126e-7,0.000004156877,0.99937516,0.0000050301182,0.000004143859,0.00002325404,0.00019813531,0.0001271966,0.00008738861,0.000002400597,0.00017123047,9.997915e-7],"about_ca_topic_score_codex":0.8199831,"about_ca_topic_score_gemma":0.9071705,"teacher_disagreement_score":0.18001688,"about_ca_system_score_codex":0.002293971,"about_ca_system_score_gemma":0.0013328501,"threshold_uncertainty_score":0.362154},"labels":[],"label_agreement":null},{"id":"W2083605325","doi":"10.1017/s0016756810000324","title":"Long-lived granite-related molybdenite mineralization at Connemara, western Irish Caledonides","year":2010,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Geochemistry; Molybdenite; Mineralization (soil science); Zircon; Magmatism; Orogeny; Geochronology; Tectonics; Hydrothermal circulation; Fluid inclusions; Paleontology","score_opus":0.012909034158802355,"score_gpt":0.20913952998249227,"score_spread":0.19623049582368993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083605325","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99325126,0.00021229505,0.00008811297,0.00006708576,0.000009150898,0.00000896665,0.00058133877,0.000020794512,0.005760933],"genre_scores_gemma":[0.9950023,0.00008965124,0.00022462913,0.000046587866,0.0000033258716,0.000010133942,0.00059609447,0.000016389416,0.00401091],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997118,0.000019948864,0.00001352284,0.00011194349,0.000049330705,0.00009345044],"domain_scores_gemma":[0.999663,0.000018345443,0.00009171619,0.000033150754,0.00012191325,0.000071847986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003066299,0.00024007338,0.00024239134,0.0011070711,0.00079043634,0.0010444168,0.00039829034,0.00031235843,0.0016637335],"category_scores_gemma":[0.0003837561,0.00028637532,0.00027315025,0.00087043206,0.00078319805,0.00036523593,0.0011908687,0.00034204323,0.0004916431],"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":[0.00087929185,0.00006155787,0.9155738,0.0001642724,0.00014936361,0.0021589997,0.0046022087,0.00075760996,0.034108646,0.0004097992,0.0020795297,0.039054874],"study_design_scores_gemma":[0.0000042843935,0.000021134509,0.9964694,0.000010306376,0.000004532373,0.00009023157,0.0005481438,0.000031395117,0.00033191164,0.0000081328935,0.0024763097,0.0000043400005],"about_ca_topic_score_codex":0.1966845,"about_ca_topic_score_gemma":0.61243874,"teacher_disagreement_score":0.1966845,"about_ca_system_score_codex":0.0030658117,"about_ca_system_score_gemma":0.0014543239,"threshold_uncertainty_score":0.3910793},"labels":[],"label_agreement":null},{"id":"W2093614839","doi":"10.1017/s0016756812000878","title":"Structural controls in the western offshore Midland Valley of Scotland: implications for Late Palaeozoic regional tectonics","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"Western University","funders":"","keywords":"Geology; Transpression; Massif; Paleontology; Sinistral and dextral; Paleogene; Devonian; Paleozoic; Echelon formation; Seismology; Fault (geology); Fold (higher-order function); Orogeny; Strike-slip tectonics; Tectonics; Structural basin","score_opus":0.02539130023639902,"score_gpt":0.2303668096520283,"score_spread":0.20497550941562928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093614839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99611676,0.0006168582,0.00013902067,0.0001739342,0.0000063298753,0.000006976283,0.00018017054,0.000011844082,0.00274814],"genre_scores_gemma":[0.9994486,0.0001338784,0.0000551811,0.000015088046,0.0000055458095,0.000001514211,0.00007552129,0.0000015464072,0.00026301437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998337,0.000019699533,0.000012482606,0.00003867575,0.00002585344,0.00006954408],"domain_scores_gemma":[0.9996075,0.00003895098,0.00016429517,0.000017416733,0.00010425653,0.00006753375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025456503,0.00018640928,0.0002046495,0.0018890891,0.000597298,0.0014500646,0.00036421698,0.00019695896,0.0027782063],"category_scores_gemma":[0.0005924208,0.00015716733,0.0001714587,0.001768627,0.0011982272,0.00047777005,0.00059169455,0.00019315866,0.00019840126],"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":[0.0002568578,0.000052623716,0.9251849,0.00022348971,0.00008768332,0.0016297785,0.0046516773,0.0018416339,0.014977241,0.0036140685,0.0005870944,0.046892878],"study_design_scores_gemma":[0.0000054107236,0.000027892647,0.9976767,0.000015430336,0.0000047291383,0.00007421254,0.0007605824,0.00018845368,0.00009119936,0.00020128071,0.00094898336,0.0000052570717],"about_ca_topic_score_codex":0.112348646,"about_ca_topic_score_gemma":0.2170101,"teacher_disagreement_score":0.112348646,"about_ca_system_score_codex":0.0017606432,"about_ca_system_score_gemma":0.0008044135,"threshold_uncertainty_score":0.22338939},"labels":[],"label_agreement":null},{"id":"W2096014506","doi":"10.1017/s0016756811000823","title":"The Northeast Arran Trough, the Corrie conundrum and the Highland Boundary Fault in the Firth of Clyde, SW Scotland","year":2011,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Trough (economics); Fault (geology); Paleontology; Sinistral and dextral; Fault scarp; Paleogene; Sedimentary rock; Tournaisian; Transform fault; Fault trace; Carboniferous; Structural basin","score_opus":0.015507793426892338,"score_gpt":0.18459810069567345,"score_spread":0.1690903072687811,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096014506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99446857,0.00034194064,0.00006334985,0.0000885437,0.000009895804,0.00001838715,0.00022017212,0.00001378582,0.0047753244],"genre_scores_gemma":[0.996777,0.00013555556,0.00021400042,0.00003609157,0.000006442574,0.000011173462,0.00028999354,0.0000044304124,0.0025254472],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972945,0.00002076199,0.000015240525,0.000053140306,0.00007200821,0.000109424334],"domain_scores_gemma":[0.9996526,0.00003319755,0.00010709445,0.000015520165,0.00011204719,0.000079537655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019664485,0.00018131988,0.00024765212,0.0010694655,0.001182678,0.00086094125,0.00037922003,0.00023014261,0.003372177],"category_scores_gemma":[0.00046752184,0.00018310451,0.00016437248,0.0008983664,0.00071462843,0.00025624695,0.0007429244,0.00019037646,0.00036105252],"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":[0.00044022303,0.00010736062,0.86965024,0.0004841442,0.00008494245,0.0073511982,0.009889742,0.00037875707,0.033956345,0.0013009114,0.0029707644,0.07338537],"study_design_scores_gemma":[0.0000068482314,0.00005867944,0.99250895,0.000026071917,0.000004276801,0.00036173838,0.0025388023,0.000052528874,0.00014797338,0.000019825484,0.0042684423,0.000005779568],"about_ca_topic_score_codex":0.28582954,"about_ca_topic_score_gemma":0.663941,"teacher_disagreement_score":0.28582954,"about_ca_system_score_codex":0.0011999639,"about_ca_system_score_gemma":0.0015100014,"threshold_uncertainty_score":0.56833166},"labels":[],"label_agreement":null},{"id":"W2096868193","doi":"10.1017/s0016756802006283","title":"The Blackstones Bank igneous complex: geochemistry and crustal context of a submerged Tertiary igneous centre in the Scottish Hebrides","year":2002,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"McMaster University","funders":"","keywords":"Geology; Proterozoic; Igneous rock; Basement; Geochemistry; Archean; Context (archaeology); Fibrous joint; Continental crust; Precambrian; Crust; Paleontology; Archaeology; Tectonics","score_opus":0.014275493537869575,"score_gpt":0.18512649616451515,"score_spread":0.17085100262664557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096868193","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980878,0.00021868787,0.000014553414,0.000052131007,0.0000019564823,0.0000027253986,0.00014706099,0.0000028981963,0.0014722608],"genre_scores_gemma":[0.998418,0.00022872238,0.000043923952,0.00003243299,0.0000063089124,0.0000022726797,0.00019234621,0.0000032735825,0.0010727422],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999051,0.000008071952,0.0000046095784,0.000026871963,0.00002763016,0.000027649665],"domain_scores_gemma":[0.99982697,0.0000129657155,0.00004956388,0.000006665324,0.00004480372,0.00005900334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011741216,0.00024099578,0.00021207535,0.001966304,0.0010085473,0.0010782327,0.00029743224,0.00020508099,0.003407313],"category_scores_gemma":[0.00038585055,0.0002076725,0.00010429028,0.001533579,0.0009973234,0.00035587992,0.0007239328,0.00017594478,0.0002636887],"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":[0.00013479903,0.000039638064,0.9514848,0.00008050885,0.000109427514,0.0033769174,0.008165208,0.00026453784,0.0106428545,0.00042886383,0.001105457,0.024166975],"study_design_scores_gemma":[0.0000021425915,0.000008553676,0.99834394,0.000006296628,0.0000048562,0.00012095742,0.0006951968,0.000029048748,0.00012448974,0.000017761937,0.00064382533,0.0000029437942],"about_ca_topic_score_codex":0.49678776,"about_ca_topic_score_gemma":0.7084175,"teacher_disagreement_score":0.49678776,"about_ca_system_score_codex":0.0021756452,"about_ca_system_score_gemma":0.00084474176,"threshold_uncertainty_score":0.98779225},"labels":[],"label_agreement":null},{"id":"W2099666261","doi":"10.1017/s0016756809006438","title":"Late Miocene magmatic activity in the Attic-Cycladic Belt of the Aegean (Lavrion, SE Attica, Greece): implications for the geodynamic evolution and timing of ore deposition","year":2009,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"Saint Mary's University","funders":"Eidgenössische Technische Hochschule Zürich; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Geology; Zircon; Granulite; Geochemistry; Metamorphism; Metamorphic rock; Igneous rock; Protolith; Facies; Petrology; Paleontology","score_opus":0.021003940995940086,"score_gpt":0.23688535680948167,"score_spread":0.2158814158135416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099666261","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982443,0.00041667666,0.000057592566,0.000026039985,0.0000020898633,0.0000033521037,0.00012460416,0.0000046929063,0.001120601],"genre_scores_gemma":[0.9994393,0.0001822543,0.00006870695,0.000005226363,0.0000023963614,0.0000013758273,0.00009811781,0.0000017321092,0.00020088335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994886,0.000006607287,0.00000626259,0.000022256232,0.00000622532,0.000009739064],"domain_scores_gemma":[0.9999305,0.0000064667047,0.00003153113,0.000004323121,0.000016327835,0.000010763137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018941195,0.00021543281,0.00014697012,0.001046155,0.00019286879,0.0005491237,0.00015695645,0.00022829088,0.0015217041],"category_scores_gemma":[0.00016903706,0.000118719574,0.0001292779,0.0006093462,0.0003687478,0.0002772707,0.0002584173,0.000094851464,0.00025289512],"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":[0.00019103213,0.000022791524,0.94445205,0.000089034795,0.0000785497,0.00047838147,0.00078839465,0.0005006887,0.039328407,0.00027541703,0.000098306875,0.013696883],"study_design_scores_gemma":[0.0000024380363,0.000018152305,0.9986551,0.0000050601325,0.0000074802315,0.000112731555,0.00022113929,0.00010622974,0.0004803428,0.000021021246,0.00036887263,0.0000014187048],"about_ca_topic_score_codex":0.016900187,"about_ca_topic_score_gemma":0.021872029,"teacher_disagreement_score":0.016900187,"about_ca_system_score_codex":0.0007069292,"about_ca_system_score_gemma":0.00026083246,"threshold_uncertainty_score":0.03360361},"labels":[],"label_agreement":null},{"id":"W2099792230","doi":"10.1017/s0016756803007283","title":"Brittle fault evolution of the Montréal area (St Lawrence Lowlands, Canada): rift-related structural inheritance and tectonism approached by palaeostress analysis","year":2003,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Montreal Police Service; Geological Survey of Canada; Centre de Géomatique du Québec; Institut National de la Recherche Scientifique","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Foreland basin; Ordovician; Paleozoic; Transtension; Tectonics; Seismology; Paleontology; Rift; Fault (geology); Inversion (geology); Strain partitioning","score_opus":0.005165619429293267,"score_gpt":0.15501119755773118,"score_spread":0.1498455781284379,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099792230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99230367,0.00070605805,0.00023443389,0.00009919117,0.0000036809556,0.000029700564,0.0022571404,0.00003860002,0.004327438],"genre_scores_gemma":[0.996888,0.0002308579,0.00037383882,0.000013513609,0.0000018368598,0.000006913262,0.0007853744,0.000009036815,0.0016905856],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999846,0.0000073256983,0.0000052386918,0.000039407758,0.000052649142,0.00004927488],"domain_scores_gemma":[0.99957484,0.000017919232,0.000077272605,0.000012906419,0.0002485132,0.00006851388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014795396,0.00031099515,0.00020290239,0.0030966145,0.0009951399,0.0013235196,0.00073590066,0.00028840208,0.0027229],"category_scores_gemma":[0.0005357305,0.00022641558,0.00020075365,0.004140988,0.00072046544,0.00025443838,0.00041494297,0.00020184266,0.00031327162],"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":[0.00013546398,0.00003822121,0.9368501,0.00011187866,0.00015478116,0.00055726717,0.0014907107,0.0057261004,0.011213849,0.0010195433,0.0018930006,0.040809147],"study_design_scores_gemma":[0.0000030304823,0.0000075456514,0.9967565,0.000008075384,0.000011669716,0.00003085414,0.00019493498,0.0014491415,0.00019206623,0.0000226881,0.001314824,0.000008649482],"about_ca_topic_score_codex":0.99197394,"about_ca_topic_score_gemma":0.9967878,"teacher_disagreement_score":0.022189226,"about_ca_system_score_codex":0.022189226,"about_ca_system_score_gemma":0.0075642755,"threshold_uncertainty_score":0.16099489},"labels":[],"label_agreement":null},{"id":"W2102581872","doi":"10.1017/s0016756800004702","title":"Late Ordovician to earliest Silurian graptolite and brachiopod biozonation from the Yangtze region, South China, with a global correlation","year":2000,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":230,"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":"Ordovician; Paleontology; Geology; Fauna; Peninsula; Arctic; Biostratigraphy; Ecological succession; Geography; Archaeology; Oceanography; Ecology","score_opus":0.008573318418791517,"score_gpt":0.19059293225451937,"score_spread":0.18201961383572784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102581872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991148,0.0001810433,0.000022135768,0.000024443598,0.0000018424751,0.0000038648063,0.00020509104,0.000003570638,0.00044322695],"genre_scores_gemma":[0.99891233,0.00017917392,0.000051676696,0.000012818795,0.0000027545648,0.0000057235457,0.0005199694,0.0000011789012,0.00031439736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999343,0.000004638085,0.000007331217,0.000022911508,0.0000129159,0.000017859844],"domain_scores_gemma":[0.99989057,0.000007714254,0.000037230217,0.0000063241014,0.000023002587,0.000035240962],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013982061,0.0003391713,0.000116513555,0.0020554173,0.0005602166,0.00039886122,0.00015433408,0.00010303991,0.0012228366],"category_scores_gemma":[0.00019006323,0.00015140993,0.00014938973,0.0018437157,0.00035559756,0.00018183338,0.00047709534,0.00011517057,0.00007455239],"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":[0.00002441808,0.0000060710604,0.98618513,0.00006275547,0.000044865952,0.00023432961,0.0017039723,0.000112978494,0.002793763,0.00010048764,0.00021946426,0.008511806],"study_design_scores_gemma":[0.0000011793159,0.0000035556905,0.9994048,0.0000028334002,0.0000042515603,0.000036755453,0.0002507653,0.000023730921,0.000031560718,0.000009273057,0.00023026444,0.0000010962681],"about_ca_topic_score_codex":0.09301266,"about_ca_topic_score_gemma":0.26445705,"teacher_disagreement_score":0.09301266,"about_ca_system_score_codex":0.000648482,"about_ca_system_score_gemma":0.0010697035,"threshold_uncertainty_score":0.18494254},"labels":[],"label_agreement":null},{"id":"W2105640096","doi":"10.1017/s0016756802006830","title":"Bio-signatures in metabasaltic glass of a Caledonian ophiolite, West Norway","year":2002,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":25,"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":"","keywords":"Ophiolite; Pillow lava; Geology; Geochemistry; Metamorphism; Oceanic crust; Organic matter; Greenschist; Basalt; Mineralogy; Volcanic rock; Volcano; Chemistry; Paleontology; Subduction","score_opus":0.026285568233079742,"score_gpt":0.2383800626391015,"score_spread":0.21209449440602177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105640096","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994886,0.000067067806,0.000045213597,0.0000039471274,0.0000014974863,0.0000024523772,0.00011192575,0.0000030474228,0.00027614686],"genre_scores_gemma":[0.999203,0.0000593822,0.000096675714,0.0000046015384,0.000001050866,0.0000020491127,0.00017940579,0.0000031239845,0.00045059918],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999341,0.0000030135661,0.0000051404463,0.000025304671,0.000014004226,0.000018572287],"domain_scores_gemma":[0.9999263,0.000009230107,0.00001661963,0.0000049331666,0.000024234263,0.000018777539],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006609316,0.00025570224,0.00012224847,0.00082998927,0.00036605875,0.00049678615,0.00015648842,0.00023344906,0.0006141985],"category_scores_gemma":[0.00017644794,0.0001665662,0.00008626554,0.00032710744,0.0006308516,0.00012676665,0.00029559195,0.00008558563,0.00011570267],"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":[0.00044501497,0.00002509011,0.33235782,0.00008487705,0.000037416146,0.0011813915,0.0019420927,0.0004655185,0.65612,0.00009062843,0.00006388138,0.007186275],"study_design_scores_gemma":[0.0000070439914,0.000068931164,0.989808,0.000006207308,0.000013884306,0.00025286188,0.00057999545,0.00035602594,0.008248497,0.000021531685,0.00063209113,0.000004949742],"about_ca_topic_score_codex":0.085259706,"about_ca_topic_score_gemma":0.10877082,"teacher_disagreement_score":0.085259706,"about_ca_system_score_codex":0.0006427425,"about_ca_system_score_gemma":0.000328793,"threshold_uncertainty_score":0.16952688},"labels":[],"label_agreement":null},{"id":"W2110788983","doi":"10.1017/s001675680700386x","title":"The ontogeny and systematics of the otarionine trilobite<i>Otarionella</i>from the Devonian of the Montagne Noire, France and the Maider, Morocco","year":2007,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Trilobite; Ontogeny; Devonian; Biology; Systematics; Juvenile; Tribe; Paleontology; Genus; Zoology; Taxonomy (biology); Ecology; Ordovician","score_opus":0.007524989702317087,"score_gpt":0.18723948596054846,"score_spread":0.17971449625823138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110788983","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99749374,0.00047020693,0.0000881087,0.000018107763,0.0000024029976,0.000009155221,0.00007326277,0.000006861406,0.0018382093],"genre_scores_gemma":[0.9991308,0.00013886989,0.0002020408,0.000013273677,0.000004035884,0.0000054026755,0.00009587172,0.0000043209743,0.00040545853],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977404,0.000020863314,0.000014730247,0.000089211804,0.000040506235,0.000060557057],"domain_scores_gemma":[0.9997527,0.000026554293,0.00010458817,0.000013421967,0.00006503373,0.000037621234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019295487,0.0003048036,0.00025228172,0.0022231606,0.0012040879,0.00064110226,0.00042374013,0.00037428146,0.0020960376],"category_scores_gemma":[0.00028958326,0.00015189218,0.00017662351,0.00090601697,0.000868141,0.00029933796,0.000759605,0.00021056601,0.00037021431],"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":[0.0003838228,0.00007906594,0.74059576,0.0002777958,0.00010268982,0.0014935589,0.011597117,0.00040424892,0.15418789,0.0006685121,0.00034048333,0.089869045],"study_design_scores_gemma":[0.0000023495509,0.000058135167,0.99443674,0.00001964021,0.000008593102,0.00058650057,0.0007498738,0.00008777973,0.00046033438,0.000018213887,0.00356662,0.0000052916644],"about_ca_topic_score_codex":0.02571633,"about_ca_topic_score_gemma":0.06780139,"teacher_disagreement_score":0.02571633,"about_ca_system_score_codex":0.0011780171,"about_ca_system_score_gemma":0.00046386512,"threshold_uncertainty_score":0.051133275},"labels":[],"label_agreement":null},{"id":"W2112120044","doi":"10.1017/s001675680400041x","title":"Petrology and potential tectonic significance of a K-bentonite in a Taconian shale basin (eastern Ontario, Canada), northern Appalachians","year":2005,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Geological Survey of Canada; Carleton University","funders":"","keywords":"Geology; Ordovician; Oil shale; Illite; Paleontology; Onlap; Geochemistry; Carbonate; Diamictite; Structural basin; Clay minerals; Clastic rock; Facies","score_opus":0.005549643517307448,"score_gpt":0.16557859117043564,"score_spread":0.1600289476531282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112120044","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981844,0.000100837795,0.000021135376,0.000022611313,7.2223406e-7,0.000004647872,0.00020985617,0.0000025856507,0.0014532029],"genre_scores_gemma":[0.9990669,0.0000832523,0.000043941563,0.000005387934,8.00841e-7,0.000001637998,0.00016742486,0.0000013911032,0.000629185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999897,0.00000497732,0.000006195095,0.000023373355,0.00003383922,0.000034617024],"domain_scores_gemma":[0.9997342,0.000015691805,0.000048843733,0.0000071289414,0.00012984997,0.00006418943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008457748,0.00018994746,0.00010885123,0.0012009415,0.0013599305,0.0008569354,0.000363151,0.00019548598,0.0010364762],"category_scores_gemma":[0.00039548622,0.00018861788,0.00010093725,0.0011905807,0.0007915598,0.00017979041,0.00042541025,0.00013641486,0.00013608656],"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":[0.00006616144,0.000013035268,0.98139405,0.000034640718,0.0000301694,0.0005912735,0.0023329742,0.0004056,0.0076880553,0.00016689583,0.00021886405,0.0070583043],"study_design_scores_gemma":[8.9547643e-7,0.0000030567646,0.9989126,0.0000041953026,0.0000032580513,0.000043824675,0.00054821034,0.00011413182,0.00005309521,0.0000063061534,0.00030855736,0.0000018667586],"about_ca_topic_score_codex":0.96044576,"about_ca_topic_score_gemma":0.99254346,"teacher_disagreement_score":0.03955424,"about_ca_system_score_codex":0.0057801837,"about_ca_system_score_gemma":0.0042049424,"threshold_uncertainty_score":0.07957429},"labels":[],"label_agreement":null},{"id":"W2113963001","doi":"10.1017/s0016756809990240","title":"The postcranial skeleton of<i>Monolophosaurus jiangi</i>(Dinosauria: Theropoda) from the Middle Jurassic of Xinjiang, China, and a review of Middle Jurassic Chinese theropods","year":2009,"lang":"en","type":"review","venue":"Geological Magazine","topic":"Paleontology and Evolutionary Biology","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":"University of Alberta","funders":"","keywords":"Postcrania; Theropoda; Paleontology; Geology; Cretaceous; Taxon","score_opus":0.027372701116083982,"score_gpt":0.2540998108466441,"score_spread":0.22672710973056015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113963001","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":[0.6203655,0.3670072,0.0013373339,0.00046536193,0.00018131333,0.000087167566,0.0028235803,0.00004492911,0.007687635],"genre_scores_gemma":[0.73487866,0.25585046,0.0019669512,0.00034224812,0.00024296304,0.00011234545,0.0026491212,0.000020910826,0.003936454],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99976796,0.000019434761,0.00005898399,0.00006738779,0.00006765671,0.000018592309],"domain_scores_gemma":[0.9998136,0.000036618196,0.00007658762,0.000008926761,0.000049466038,0.000014787103],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037131057,0.00048543685,0.00031926326,0.0046301335,0.0005447382,0.0003413157,0.00048001026,0.00030859833,0.0016290218],"category_scores_gemma":[0.00042213788,0.000223798,0.00029743623,0.0027074998,0.0005897946,0.0004457314,0.0004025263,0.00014106995,0.00023544295],"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":[0.00015105847,0.000022659557,0.4257621,0.01220986,0.0005217726,0.0026414488,0.003919913,0.00037563682,0.013978444,0.00048615006,0.003652559,0.5362784],"study_design_scores_gemma":[0.000003914679,0.00006446615,0.96059793,0.0008497635,0.0002823739,0.0037756877,0.00074275275,0.00007774618,0.0006596777,0.00008835746,0.03284115,0.000016138052],"about_ca_topic_score_codex":0.013649598,"about_ca_topic_score_gemma":0.03847794,"teacher_disagreement_score":0.013649598,"about_ca_system_score_codex":0.0003659666,"about_ca_system_score_gemma":0.0006931238,"threshold_uncertainty_score":0.02714026},"labels":[],"label_agreement":null},{"id":"W2115931436","doi":"10.1017/s0016756806002469","title":"First record of the Hirnantian (Upper Ordovician) δ<sup>13</sup>C excursion in the North American Midcontinent and its regional implications","year":2006,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":131,"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":"Ordovician; Geology; Paleontology; Excursion; Glacial period; Arctic; Diamictite; Gondwana; Structural basin; Clastic rock; Oceanography","score_opus":0.015633050808984104,"score_gpt":0.2109196193949239,"score_spread":0.1952865685859398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115931436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878241,0.0016610646,0.00032339868,0.00013490547,0.000017031765,0.000008066717,0.0008476937,0.00003230533,0.009151417],"genre_scores_gemma":[0.99701476,0.00054751337,0.0006677715,0.000065167435,0.000021594611,0.000006311989,0.00064016867,0.000009201617,0.0010274935],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999684,0.000003597289,0.000002416905,0.000009808436,0.000007751353,0.0000080955915],"domain_scores_gemma":[0.99966764,0.000030455527,0.000068390844,0.000032022734,0.0001575903,0.000043998185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015576046,0.00010604129,0.000083701874,0.0006409706,0.00045632484,0.0004133695,0.00016533496,0.0001240239,0.0020104924],"category_scores_gemma":[0.00027017298,0.00008392606,0.00005097118,0.00094649027,0.00044776572,0.00018320282,0.00034532364,0.00020905303,0.00022183437],"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":[0.00022529498,0.000039057424,0.85496116,0.00016927566,0.00006922391,0.00049972004,0.002903256,0.0002707655,0.014832639,0.00056196935,0.003431227,0.1220364],"study_design_scores_gemma":[0.0000011343207,0.00000863356,0.99397707,0.000009526207,0.0000074281425,0.0000570046,0.00022314137,0.000032720753,0.00032489642,0.000028845934,0.0053279814,0.0000017104568],"about_ca_topic_score_codex":0.044162765,"about_ca_topic_score_gemma":0.16053106,"teacher_disagreement_score":0.044162765,"about_ca_system_score_codex":0.00035328214,"about_ca_system_score_gemma":0.00050887605,"threshold_uncertainty_score":0.08781141},"labels":[],"label_agreement":null},{"id":"W2116221932","doi":"10.1017/s0016756814000016","title":"Record of climatic fluctuations and high pH weathering conditions in a thick Ordovician palaeosol developed in rhyolite of the Dunn Point Formation, Arisaig, Nova Scotia, Canada","year":2014,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geochemistry and Elemental Analysis","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":"Saint Mary's University","funders":"","keywords":"Rhyolite; Pedogenesis; Weathering; Geology; Paleosol; Ordovician; Soil horizon; Geochemistry; Basalt; Calcite; Volcanic rock; Volcano; Paleontology; Soil water; Soil science","score_opus":0.010000051300910046,"score_gpt":0.19635912181357912,"score_spread":0.18635907051266906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116221932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985753,0.00009091844,0.000024640449,0.000010229085,0.0000013795852,0.0000074050186,0.0006478751,0.0000036223344,0.0006385105],"genre_scores_gemma":[0.9992749,0.00004720532,0.000038993207,0.0000060637603,0.0000010673592,0.000002656942,0.00038055872,0.0000014399768,0.00024705435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991083,0.0000051975676,0.0000070513333,0.000021375627,0.000020152522,0.00003540887],"domain_scores_gemma":[0.99970394,0.00001967107,0.0000583201,0.000012548275,0.00011191091,0.00009367116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000114475835,0.00020326547,0.00021044338,0.0014864187,0.000822857,0.0006260128,0.00036980974,0.00021537406,0.00069736387],"category_scores_gemma":[0.00022892473,0.00016837798,0.00013306578,0.0014080644,0.0005459077,0.00014107976,0.00038726896,0.00015993405,0.00019313967],"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":[0.000058735037,0.000014690243,0.99039286,0.000028055905,0.00002882328,0.00037786723,0.00095059426,0.00010309125,0.0058162273,0.000036755624,0.00014133743,0.002050931],"study_design_scores_gemma":[8.230332e-7,0.0000039370907,0.99940693,0.0000026688665,0.0000022205818,0.000029258044,0.00032179538,0.00003214716,0.000056512217,0.0000015327049,0.00014108351,0.0000011372034],"about_ca_topic_score_codex":0.8298401,"about_ca_topic_score_gemma":0.94113505,"teacher_disagreement_score":0.17015988,"about_ca_system_score_codex":0.0024757537,"about_ca_system_score_gemma":0.0014893678,"threshold_uncertainty_score":0.3423239},"labels":[],"label_agreement":null},{"id":"W2118709509","doi":"10.1017/s0016756815000436","title":"Mercury anomalies associated with three extinction events (Capitanian Crisis, Latest Permian Extinction and the Smithian/Spathian Extinction) in NW Pangea","year":2015,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":208,"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; Geological Survey of Canada","funders":"Research Executive Agency; FP7 People: Marie-Curie Actions; Natural Environment Research Council; Sight Research UK","keywords":"Extinction event; Permian; Early Triassic; Extinction (optical mineralogy); Permian–Triassic extinction event; Mercury (programming language); Geology; Paleontology","score_opus":0.02517212638518119,"score_gpt":0.23626262426886685,"score_spread":0.21109049788368567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118709509","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99938846,0.000039079845,0.000023242244,0.000008812705,7.388209e-7,0.0000018294801,0.000113660564,0.0000056830336,0.0004185382],"genre_scores_gemma":[0.9994105,0.00005387893,0.00010259882,0.000005930632,0.0000023322905,0.0000028812167,0.00027175806,0.0000026082278,0.0001474782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999516,0.0000039515326,0.000004703242,0.000016549098,0.000011265847,0.000011900627],"domain_scores_gemma":[0.9998592,0.000016958667,0.00005438524,0.000009275478,0.000035489564,0.000024638366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001702215,0.00018139994,0.00016154765,0.0014959346,0.00045938228,0.00038393782,0.00020269086,0.00023653035,0.00079585006],"category_scores_gemma":[0.00030682786,0.00016088694,0.00013184584,0.0010311955,0.0004975788,0.00026869436,0.00059340405,0.00018459473,0.00008243959],"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":[0.00013251563,0.000024321653,0.9729285,0.000032981497,0.0000749244,0.00043180393,0.0011869944,0.00048817508,0.014834354,0.00009011049,0.00013281673,0.009642565],"study_design_scores_gemma":[0.0000010217767,0.000010249891,0.99934286,0.0000011898697,0.000004581906,0.00004525415,0.0000826222,0.00008578798,0.00025231304,0.000009115364,0.00016394588,9.725882e-7],"about_ca_topic_score_codex":0.03102382,"about_ca_topic_score_gemma":0.06003218,"teacher_disagreement_score":0.03102382,"about_ca_system_score_codex":0.0006114018,"about_ca_system_score_gemma":0.00030457496,"threshold_uncertainty_score":0.061686516},"labels":[],"label_agreement":null},{"id":"W2121038255","doi":"10.1017/s0016756809990252","title":"Vestiges of lost tectonic units in conglomerate pebbles? A test in Permian sequences of the Southalpine Orobic Alps","year":2009,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"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 New Brunswick","funders":"","keywords":"Permian; Geology; Metamorphic rock; Greenschist; Basement; Conglomerate; Geochemistry; Facies; Metamorphic facies; Paleozoic; Paleontology; Petrology; Structural basin; Sedimentary rock; Archaeology; Geography","score_opus":0.016650198324224662,"score_gpt":0.20365660764119423,"score_spread":0.18700640931696957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121038255","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99900633,0.00007961323,0.0001234068,0.000007268038,7.945144e-7,0.0000026422838,0.00006683372,0.0000039422102,0.0007092089],"genre_scores_gemma":[0.9997936,0.000014061901,0.00005575259,0.000002141359,0.0000014214334,0.0000012369712,0.0000628191,0.0000018240429,0.00006706351],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996043,0.00007527037,0.000037225876,0.00015713522,0.000059662452,0.00006650161],"domain_scores_gemma":[0.99865144,0.00044134073,0.00041407195,0.000091426904,0.00019842264,0.00020334206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005556094,0.00022118154,0.0002531313,0.0031614031,0.00067763904,0.0012929616,0.0004521432,0.00040851053,0.002954572],"category_scores_gemma":[0.0020125639,0.00014283226,0.00025446844,0.0014025904,0.0013219249,0.0006466222,0.0007997703,0.00023496864,0.00040378436],"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":[0.0006742984,0.000026806176,0.9732756,0.000037206788,0.0001084875,0.00048245458,0.0011323452,0.0004586882,0.014787409,0.00019856331,0.000027994745,0.008790103],"study_design_scores_gemma":[0.0000026701846,0.000047879752,0.9982798,0.0000044885046,0.000009302216,0.00015318746,0.00050529616,0.0004623684,0.00038547826,0.000031148316,0.000115427254,0.0000029908185],"about_ca_topic_score_codex":0.013947701,"about_ca_topic_score_gemma":0.017096965,"teacher_disagreement_score":0.013947701,"about_ca_system_score_codex":0.00052677246,"about_ca_system_score_gemma":0.00023229736,"threshold_uncertainty_score":0.027733028},"labels":[],"label_agreement":null},{"id":"W2121807415","doi":"10.1017/s0016756808005815","title":"A modern assessment of Ordovician chitinozoans from the Shelve and Caradoc areas, Shropshire, and their significance for correlation","year":2008,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Marine Biology and Ecology Research","field":"Earth and Planetary Sciences","cited_by":25,"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; Landesverteidigungsakademie; Petrobras; Fonds Wetenschappelijk Onderzoek; University of Oxford; Vlaamse regering; Tallinna Tehnikaülikool; Universiteit Gent; University of Alberta","keywords":"Biozone; Ordovician; Geology; Paleontology; Section (typography); Fauna; Lithostratigraphy; Biostratigraphy; Ecology; Biology","score_opus":0.027163311279220316,"score_gpt":0.24386972035559246,"score_spread":0.21670640907637215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121807415","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938777,0.0012282948,0.00009570669,0.000036539703,0.000008524526,0.000009709668,0.00034549565,0.000006179444,0.004391841],"genre_scores_gemma":[0.9987801,0.00027704673,0.00013875298,0.000008135583,0.0000050979975,0.000004559555,0.00036428467,0.0000020105892,0.00042000867],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99953437,0.000058671332,0.000040335486,0.0001327136,0.00012982551,0.00010393808],"domain_scores_gemma":[0.9987244,0.00013451792,0.00029921337,0.0001194571,0.0005150573,0.00020740238],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054542086,0.00024980158,0.0002279092,0.00457858,0.00090288307,0.0011734527,0.0003672988,0.00014060167,0.0024404097],"category_scores_gemma":[0.0012120273,0.00015006117,0.00010913196,0.0030814854,0.0009233386,0.0003819908,0.0010198535,0.00024587134,0.00023556936],"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":[0.000046432087,0.0000062375734,0.97689587,0.00005438436,0.00003700417,0.00018237243,0.001660109,0.0000685807,0.0017365759,0.00016305002,0.00019050777,0.018958928],"study_design_scores_gemma":[5.57841e-7,0.00000972641,0.9978567,0.000010643426,0.000004284789,0.00007197538,0.00091497233,0.00003461036,0.000063038424,0.000013099168,0.0010185904,0.0000017040721],"about_ca_topic_score_codex":0.18345596,"about_ca_topic_score_gemma":0.52699006,"teacher_disagreement_score":0.18345596,"about_ca_system_score_codex":0.0016234793,"about_ca_system_score_gemma":0.0007324126,"threshold_uncertainty_score":0.3647762},"labels":[],"label_agreement":null},{"id":"W2124046098","doi":"10.1017/s0016756813001015","title":"The St Lawrence Platform and Appalachian deformation front in the St Lawrence Estuary and adjacent areas (Quebec, Canada): structural complexity revealed by magnetic and seismic imaging","year":2014,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Foreland basin; Seismology; Tectonics; Front (military); Ordovician; Structural complexity; Paleontology; Oceanography","score_opus":0.00893783644430936,"score_gpt":0.17850977318967098,"score_spread":0.1695719367453616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124046098","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911964,0.0003594258,0.00013615515,0.00013287851,0.000003990355,0.000023752755,0.0021535275,0.0000120638115,0.0059816726],"genre_scores_gemma":[0.9966151,0.0002065751,0.00025657276,0.000030776882,0.0000026517282,0.0000082837,0.0009389871,0.000003661182,0.0019374295],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982315,0.0000087538865,0.000006070247,0.000028583354,0.00006232131,0.0000711191],"domain_scores_gemma":[0.999553,0.000030427593,0.00005196037,0.000012189571,0.00028737978,0.000065000844],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014092863,0.00021008273,0.00020216027,0.002217493,0.0014853574,0.0013920353,0.0003294032,0.0002730562,0.0024068228],"category_scores_gemma":[0.0003978807,0.00015175437,0.00014611705,0.0035857826,0.00074463047,0.00030567922,0.00046550002,0.00024689626,0.0002683518],"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":[0.00013119525,0.000031367155,0.9552637,0.00006622296,0.00007262509,0.00067229546,0.0023877511,0.0007122314,0.006716454,0.0003257984,0.0021518173,0.031468548],"study_design_scores_gemma":[0.0000015033584,0.0000033095705,0.99767035,0.000010097812,0.0000045786155,0.0000420593,0.000971439,0.00026845155,0.000073126335,0.00001192982,0.0009390526,0.0000040514215],"about_ca_topic_score_codex":0.9896861,"about_ca_topic_score_gemma":0.9975412,"teacher_disagreement_score":0.010313928,"about_ca_system_score_codex":0.007527555,"about_ca_system_score_gemma":0.0071755606,"threshold_uncertainty_score":0.05461651},"labels":[],"label_agreement":null},{"id":"W2124599718","doi":"10.1017/s0016756809990033","title":"A fistful of shells: amplifying sclerochronological and palaeoclimate signals from molluscan death assemblages","year":2009,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Tree-ring climate 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":"University of Calgary","funders":"","keywords":"Dendrochronology; Chronology; Dendroclimatology; Series (stratigraphy); Context (archaeology); Geology; Paleontology; Physical geography; Geography","score_opus":0.03546406473718947,"score_gpt":0.2514111100867941,"score_spread":0.21594704534960465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124599718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907706,0.00019057681,0.0076471195,0.000041110154,0.0000109493085,0.0000150829055,0.0002251024,0.00010329929,0.0009960914],"genre_scores_gemma":[0.9937028,0.000082071165,0.0054886164,0.000013694583,0.000015981865,0.000010825922,0.00036571428,0.000030044,0.00029027383],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995919,0.00012085974,0.00002377374,0.00011602003,0.00009963786,0.000047830115],"domain_scores_gemma":[0.99823546,0.0007572214,0.00035770106,0.00018975035,0.00034121692,0.00011864516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012093073,0.00029668145,0.00030527645,0.0015423856,0.00034260817,0.0008599168,0.00024040665,0.00029580394,0.0010689471],"category_scores_gemma":[0.0041785873,0.00018512933,0.0002437429,0.00091934996,0.00039959783,0.0005736869,0.0008933124,0.0003461361,0.00027375665],"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":[0.0009321346,0.00008919973,0.65193254,0.0003545007,0.0003491552,0.0004412746,0.002014591,0.007005152,0.15184201,0.00052727974,0.0008523468,0.18365978],"study_design_scores_gemma":[0.0000054827005,0.00010628893,0.97219735,0.00002491205,0.00007861868,0.00013825155,0.00046391328,0.016491376,0.0089228805,0.00027975056,0.0012663876,0.000024716486],"about_ca_topic_score_codex":0.0029611024,"about_ca_topic_score_gemma":0.008980962,"teacher_disagreement_score":0.0029611024,"about_ca_system_score_codex":0.00021096651,"about_ca_system_score_gemma":0.00022293163,"threshold_uncertainty_score":0.006395459},"labels":[],"label_agreement":null},{"id":"W2125058223","doi":"10.1017/s0016756804009215","title":"Evolution of boninites and island-arc tholeiites in the Pindos Ophiolite, Greece","year":2004,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Saint Mary's University","funders":"","keywords":"Geology; Geochemistry; Ophiolite; Mantle (geology); Mantle wedge; Basalt; Rift; Peridotite; Igneous rock; Subduction; Petrology; Paleontology; Tectonics","score_opus":0.010723861576484724,"score_gpt":0.19549675513938775,"score_spread":0.18477289356290302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125058223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992275,0.000117493786,0.000021297696,0.0000064489464,9.1178805e-7,0.0000020982197,0.000031429037,0.0000026486748,0.000590052],"genre_scores_gemma":[0.9994752,0.00008338082,0.000055203833,0.0000042225593,8.053233e-7,0.0000019196334,0.000084327,0.000003016116,0.0002918924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986696,0.000012845027,0.000013978721,0.000047373993,0.000026646932,0.00003215552],"domain_scores_gemma":[0.99985135,0.00001509322,0.000055098826,0.000007951065,0.000036089918,0.000034383524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000177979,0.00036420813,0.00023345147,0.0026908617,0.00041594854,0.00088619365,0.00026785745,0.00035711192,0.00089881674],"category_scores_gemma":[0.00037621858,0.0002745816,0.00020759588,0.0008551585,0.0006880449,0.00032582824,0.00068828,0.00013866059,0.000230786],"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":[0.00045234637,0.00003925309,0.8271021,0.00011187957,0.00014730828,0.0012975164,0.003013466,0.0012098792,0.144809,0.0007002898,0.000076123426,0.021040754],"study_design_scores_gemma":[0.0000040030145,0.000054665106,0.9953003,0.000009409173,0.000011070148,0.0006048006,0.00087841507,0.0002368153,0.0018433003,0.00006838347,0.0009821653,0.0000066789653],"about_ca_topic_score_codex":0.014591009,"about_ca_topic_score_gemma":0.021546103,"teacher_disagreement_score":0.014591009,"about_ca_system_score_codex":0.00091263634,"about_ca_system_score_gemma":0.000318136,"threshold_uncertainty_score":0.029012144},"labels":[],"label_agreement":null},{"id":"W2126969471","doi":"10.1017/s0016756809006013","title":"Epeirogenic transgression near a triple junction: the oldest (latest early–middle Cambrian) marine onlap of cratonic New York and Quebec","year":2009,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","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":"Geology; Marine transgression; Onlap; Paleontology; Craton; Proterozoic; Trilobite; Sedimentary rock; Siliciclastic; Laurentia; Paleozoic; Unconformity; Structural basin; Sedimentary depositional environment; Ordovician; Tectonics","score_opus":0.02327482808244594,"score_gpt":0.20307088325742348,"score_spread":0.17979605517497754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126969471","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99111956,0.0002588641,0.00009135462,0.0002187687,0.000007787598,0.000011949294,0.0004288135,0.0000115941175,0.007851279],"genre_scores_gemma":[0.9964395,0.00009870268,0.000110411966,0.000041898864,0.0000020052464,0.0000040456207,0.0002332945,0.0000038523044,0.0030662066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998325,0.0000093465505,0.00000554539,0.000038622406,0.000037038102,0.000076785356],"domain_scores_gemma":[0.99939215,0.000036544858,0.000083516345,0.000020998197,0.00030537063,0.0001613833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017144285,0.0001707775,0.00015575763,0.0010653386,0.0020443012,0.0012367795,0.00051034207,0.00026092623,0.005616443],"category_scores_gemma":[0.00057972857,0.00013956233,0.00012770887,0.0009991123,0.000796913,0.0003628188,0.0007032198,0.0004653925,0.00024342425],"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":[0.00010743827,0.00002698697,0.95394427,0.000039466024,0.0000427047,0.00085805607,0.005421385,0.00023801399,0.008873436,0.0014846226,0.0019683095,0.026995163],"study_design_scores_gemma":[0.000003170055,0.000011030569,0.99186665,0.000018763772,0.000006502025,0.00011333402,0.0026966147,0.0002357358,0.00029290438,0.000030937532,0.0047189584,0.0000054638617],"about_ca_topic_score_codex":0.97812396,"about_ca_topic_score_gemma":0.9952284,"teacher_disagreement_score":0.021876037,"about_ca_system_score_codex":0.014011133,"about_ca_system_score_gemma":0.006747313,"threshold_uncertainty_score":0.101658344},"labels":[],"label_agreement":null},{"id":"W2128239025","doi":"10.1017/s0016756812001070","title":"An evolutionary and developmental perspective on the loss of regionalization in the limbs of derived ichthyosaurs","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Congenital limb and hand anomalies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":27,"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":"Uppsala Universitet; Natural Sciences and Engineering Research Council of Canada; University of Cambridge; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Heterochrony; Biology; Anatomy; Ossification; Phalanx; Axial skeleton; Convergent evolution; Skeleton (computer programming); Ontogeny; Evolutionary biology; Phylogenetics","score_opus":0.01235678720094805,"score_gpt":0.23180859145221125,"score_spread":0.2194518042512632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128239025","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977597,0.00030190876,0.0004042892,0.000018727547,0.0000011466728,0.0000044951985,0.00007613543,0.0000053931935,0.00142811],"genre_scores_gemma":[0.9982759,0.00033881492,0.00051072513,0.000017719125,0.0000049844616,0.0000065661884,0.00014548449,0.000004647048,0.00069522863],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99986935,0.00002007496,0.000012475101,0.000045399403,0.000029322851,0.000023291937],"domain_scores_gemma":[0.99976474,0.00003061791,0.00009074243,0.000022930048,0.000055030567,0.000035979203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019917934,0.00024005439,0.00023762508,0.0011618055,0.0004741141,0.0005467633,0.0003878427,0.00038134825,0.001667064],"category_scores_gemma":[0.00027879703,0.00015432718,0.00018701529,0.0006871694,0.00088744506,0.000312679,0.00065844797,0.00029194678,0.00026014601],"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":[0.00025230652,0.000024154448,0.23483312,0.00015511428,0.00009562987,0.0010188648,0.001961526,0.00053320004,0.7401258,0.00068219926,0.000064103864,0.020253979],"study_design_scores_gemma":[0.0000012486149,0.000059305108,0.9959805,0.000006722184,0.000009522495,0.00039325084,0.00035070963,0.00012634779,0.0025993683,0.00005992612,0.00040924508,0.0000037394504],"about_ca_topic_score_codex":0.002917489,"about_ca_topic_score_gemma":0.0052259555,"teacher_disagreement_score":0.002917489,"about_ca_system_score_codex":0.00031040565,"about_ca_system_score_gemma":0.00022939469,"threshold_uncertainty_score":0.0058009624},"labels":[],"label_agreement":null},{"id":"W2131967920","doi":"10.1017/s0016756802007227","title":"Taxonomic and biostratigraphical significance of the Tremadoc graptolite fauna from northern Yukon Territory, Canada","year":2003,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Biozone; Fauna; Paleontology; Geology; Genus; Paleocurrent; Biostratigraphy; Ecology; Biology; Clastic rock; Sedimentary rock","score_opus":0.009898087991688334,"score_gpt":0.17277611743175703,"score_spread":0.16287802944006868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131967920","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975727,0.00029584143,0.00003400738,0.000033023785,0.000002292924,0.000007216199,0.00033348546,0.0000045812726,0.0017168728],"genre_scores_gemma":[0.998599,0.00028640212,0.00017397563,0.00001622747,9.1124144e-7,0.0000041739554,0.0004295813,0.0000018556009,0.00048786227],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998585,0.000009712197,0.000010516022,0.000031309763,0.000043847016,0.000046055695],"domain_scores_gemma":[0.9997178,0.000017263847,0.00003880407,0.0000077312725,0.00013343601,0.00008484128],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010805213,0.00015854201,0.00013933083,0.0013288194,0.0014245143,0.0005819951,0.000337795,0.00015342174,0.0011439044],"category_scores_gemma":[0.0004415691,0.00011590144,0.00010648014,0.0016061576,0.00046801966,0.00015549587,0.0005135767,0.00015338283,0.000100998586],"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":[0.000059257654,0.000012090042,0.97087103,0.00007879616,0.000032192213,0.00034514864,0.0018747912,0.00019559755,0.0052755843,0.00017761951,0.00036150267,0.020716356],"study_design_scores_gemma":[0.0000014671133,0.000012759983,0.9968731,0.000018430941,0.00000699661,0.00014390607,0.001576343,0.00011976058,0.000100039375,0.000009792539,0.0011334973,0.000003929529],"about_ca_topic_score_codex":0.9333557,"about_ca_topic_score_gemma":0.97953266,"teacher_disagreement_score":0.06664431,"about_ca_system_score_codex":0.004507819,"about_ca_system_score_gemma":0.005299685,"threshold_uncertainty_score":0.13407356},"labels":[],"label_agreement":null},{"id":"W2132096271","doi":"10.1017/s0016756803008070","title":"An application of Nd isotope mapping in structural geology: delineating an allochthonous Grenvillian terrane at North Bay, Ontario","year":2003,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"University of Toronto; McMaster University","funders":"","keywords":"Terrane; Geology; Gneiss; Bay; Geochemistry; Metamorphic rock; Paleontology; Tectonics; Oceanography","score_opus":0.015803366864723774,"score_gpt":0.2107717998477493,"score_spread":0.19496843298302552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132096271","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896882,0.0004265842,0.0007404134,0.00011986697,0.0000039313773,0.000027741282,0.0007387358,0.000018660066,0.00823596],"genre_scores_gemma":[0.99445033,0.00037544654,0.001680582,0.000023958844,0.0000017624703,0.000009054904,0.00042652863,0.0000062011154,0.0030261395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987304,0.0000056109848,0.000004180971,0.000028363303,0.000056545257,0.00003226375],"domain_scores_gemma":[0.9998423,0.000016026654,0.000023412724,0.000009562271,0.00008240438,0.000026410436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010438988,0.00017085487,0.00009514208,0.00089417037,0.001433167,0.00067772594,0.00036833654,0.00020784543,0.0010472464],"category_scores_gemma":[0.00033823538,0.00012152451,0.00011871822,0.0011076723,0.0005542799,0.00011879204,0.00041615654,0.00016403178,0.00016095539],"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":[0.0002135369,0.000022797849,0.8328919,0.00015998223,0.00004313093,0.0009781091,0.005738973,0.0013927635,0.06955674,0.0005112577,0.0010814947,0.08740941],"study_design_scores_gemma":[0.000006656321,0.000020331856,0.9895864,0.000013003009,0.000013214391,0.00020194758,0.0013706556,0.0004965734,0.0022449968,0.00006719781,0.005972199,0.000006768898],"about_ca_topic_score_codex":0.96511394,"about_ca_topic_score_gemma":0.99289894,"teacher_disagreement_score":0.034886062,"about_ca_system_score_codex":0.007953698,"about_ca_system_score_gemma":0.0036832376,"threshold_uncertainty_score":0.07018298},"labels":[],"label_agreement":null},{"id":"W2135753979","doi":"10.1017/s0016756814000508","title":"Effects of fluid flow, cooling and deformation as recorded by<sup>40</sup>Ar/<sup>39</sup>Ar, Rb–Sr and zircon fission track ages in very low- to low-grade metamorphic rocks in Avalonian SE Cape Breton Island (Nova Scotia, Canada)","year":2014,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"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; Acadia University","funders":"","keywords":"Zircon; Terrane; Geology; Metamorphism; Metamorphic rock; Isochron dating; Geochemistry; Gondwana; Paleontology; Isochron; Tectonics","score_opus":0.005711973940559368,"score_gpt":0.18349430700756658,"score_spread":0.17778233306700722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135753979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99939716,0.000033923992,0.000023114064,0.000004901218,7.063641e-7,0.0000024339636,0.00014858288,0.000003520129,0.00038560253],"genre_scores_gemma":[0.9990546,0.000028854929,0.00004960775,0.0000042172173,5.615877e-7,0.000002661773,0.00022683176,0.0000033103813,0.00062928715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990594,0.000006045387,0.000005860508,0.000025860387,0.00002971339,0.000026578276],"domain_scores_gemma":[0.99984574,0.000029256435,0.00002753304,0.000007218088,0.000057254885,0.00003299629],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014059416,0.00017090913,0.00012715344,0.00037550463,0.000418736,0.0005067282,0.0002476155,0.00015345319,0.0010470429],"category_scores_gemma":[0.00025074484,0.00018257138,0.00010623956,0.00030699084,0.0005078553,0.000111523164,0.00021065598,0.00015937428,0.00018160831],"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":[0.0007359621,0.000033652683,0.6167922,0.00005571253,0.000053795407,0.00041592488,0.0008070581,0.0017604384,0.3715032,0.00010053736,0.0003127794,0.007428734],"study_design_scores_gemma":[0.0000030985964,0.000019977722,0.9961504,0.0000018225302,0.000004202689,0.000024424284,0.0001328823,0.00030758177,0.003133405,0.0000036857223,0.0002166836,0.0000017913746],"about_ca_topic_score_codex":0.5565248,"about_ca_topic_score_gemma":0.6467937,"teacher_disagreement_score":0.4434752,"about_ca_system_score_codex":0.0024694954,"about_ca_system_score_gemma":0.0012505072,"threshold_uncertainty_score":0.89217377},"labels":[],"label_agreement":null},{"id":"W2136562697","doi":"10.1017/s0016756806002081","title":"Geochemical characteristics of the Cretaceous ophiolitic rocks of Ikaria island, Greece","year":2006,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Saint Mary's University","funders":"","keywords":"Geology; Metamorphism; Plutonism; Geochemistry; Radiometric dating; Blueschist; Basalt; Nappe; Protolith; Petrology; Paleontology; Subduction; Eclogite; Pluton; Tectonics","score_opus":0.006712165427283442,"score_gpt":0.1735662125731272,"score_spread":0.16685404714584376,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136562697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99861526,0.000078396464,0.000016981208,0.000008426067,8.8848054e-7,0.0000037480236,0.0001881658,0.0000035890107,0.0010846156],"genre_scores_gemma":[0.9993455,0.0000653781,0.000043917364,0.000005076304,0.0000013592713,0.000002797683,0.00028193352,0.00000190633,0.0002522348],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999012,0.0000059492613,0.000017307026,0.000030841104,0.00002557249,0.000019070927],"domain_scores_gemma":[0.9998653,0.000015281019,0.000051076488,0.000011252333,0.000031177144,0.000025850113],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007076231,0.00022276887,0.00016643491,0.0025241552,0.00025513288,0.000412625,0.00018967074,0.00020335134,0.0012012664],"category_scores_gemma":[0.00027206278,0.00012348991,0.000120482364,0.0011565909,0.0004178215,0.00023532624,0.00037274268,0.00008399652,0.00027724795],"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":[0.00012562773,0.000038536324,0.934887,0.000096533906,0.00008007454,0.0010160859,0.0011498679,0.0004216142,0.050642464,0.00010982187,0.00015365216,0.011278701],"study_design_scores_gemma":[0.0000034544196,0.00002242266,0.9980775,0.000004262085,0.000007737722,0.00034540394,0.00047488534,0.000071338276,0.00057607575,0.000015624903,0.00039870315,0.0000026170019],"about_ca_topic_score_codex":0.014551557,"about_ca_topic_score_gemma":0.022422228,"teacher_disagreement_score":0.014551557,"about_ca_system_score_codex":0.00039844908,"about_ca_system_score_gemma":0.00025942377,"threshold_uncertainty_score":0.028933704},"labels":[],"label_agreement":null},{"id":"W2136703616","doi":"10.1017/s001675680400038x","title":"Diachronous supracrustal extension in an intraplate setting and the origin of the Connecticut Valley–Gaspé and Merrimack troughs, northern Appalachians","year":2005,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Institut National de la Recherche Scientifique; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Vedecká Grantová Agentúra MŠVVaŠ SR a SAV","keywords":"Geology; Laurentia; Devonian; Intraplate earthquake; Ordovician; Unconformity; Basement; Geochemistry; Paleontology; Sedimentary rock; Tectonics","score_opus":0.009931095880196146,"score_gpt":0.2050349706448725,"score_spread":0.19510387476467636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136703616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974699,0.00021625937,0.00002305746,0.000040084353,0.0000018456111,0.000004003738,0.00008903634,0.0000054002153,0.0021503132],"genre_scores_gemma":[0.99917185,0.00010578819,0.00005676768,0.000012645749,0.0000026025045,0.0000045344223,0.000120139244,0.0000023236155,0.000523381],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998648,0.000014135943,0.000006287616,0.000057474037,0.000020490224,0.000036698413],"domain_scores_gemma":[0.99973685,0.000029626457,0.00007292137,0.00001594207,0.000066087,0.00007851783],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017207288,0.00025917531,0.0001381696,0.002110211,0.0010604801,0.0013124138,0.00048025194,0.00031087475,0.0021333566],"category_scores_gemma":[0.0004543744,0.00024360069,0.000095500574,0.0020759276,0.0010405489,0.00038060208,0.0006088943,0.0002708376,0.000174718],"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":[0.00011278837,0.000033648103,0.97144777,0.000047248046,0.000035764493,0.0011596204,0.004050301,0.0003398782,0.007566468,0.00084289623,0.0004203158,0.013943381],"study_design_scores_gemma":[0.000001630218,0.0000051942584,0.9984875,0.000014352618,0.0000027952383,0.000087071996,0.00082623237,0.000055735432,0.000065287095,0.000019711093,0.0004325737,0.000001894382],"about_ca_topic_score_codex":0.32390273,"about_ca_topic_score_gemma":0.6677794,"teacher_disagreement_score":0.6760973,"about_ca_system_score_codex":0.0017079122,"about_ca_system_score_gemma":0.0009650623,"threshold_uncertainty_score":0.6440348},"labels":[],"label_agreement":null},{"id":"W2137954146","doi":"10.1017/s0016756811000938","title":"Nd–Sr–Pb isotopic composition and mantle sources of Triassic rift units in the Serbo-Macedonian and the western Rhodope massifs (Bulgaria–Greece)","year":2011,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Massif; Geology; Geochemistry; Protolith; Rift; Mantle (geology); Mafic; Basalt; Petrology; Paleontology; Tectonics; Metamorphic rock","score_opus":0.030816379227181348,"score_gpt":0.19844138839358094,"score_spread":0.1676250091663996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137954146","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996251,0.00007672719,0.000011347523,0.0000032525743,2.5811806e-7,8.032908e-7,0.000056521316,0.0000012483578,0.00022472435],"genre_scores_gemma":[0.9997373,0.000039771006,0.000024106212,0.0000022874588,4.6924393e-7,9.748353e-7,0.00009659521,8.5867356e-7,0.00009760577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992776,0.000007339214,0.000008782297,0.000023667517,0.0000117034715,0.00002068022],"domain_scores_gemma":[0.99992144,0.000007729736,0.00003138995,0.000008672066,0.000017675246,0.0000131706365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013029906,0.00018343741,0.00018072524,0.0020860676,0.00021893003,0.00038711634,0.00019207451,0.00014472404,0.00074136426],"category_scores_gemma":[0.00018179334,0.00014570897,0.00011299061,0.0007740953,0.00041018074,0.00019832976,0.0003780743,0.000081786864,0.00016192239],"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":[0.0001635516,0.000014139147,0.9629175,0.000031031712,0.000068073,0.00027552326,0.0009856573,0.0002544157,0.02563645,0.0000884593,0.00004804649,0.0095169945],"study_design_scores_gemma":[0.00000174011,0.000010600546,0.99916506,0.000002927707,0.0000050853387,0.00008164042,0.00018769894,0.00004922024,0.00039762477,0.0000066668467,0.000090856556,8.136394e-7],"about_ca_topic_score_codex":0.024096915,"about_ca_topic_score_gemma":0.03130353,"teacher_disagreement_score":0.024096915,"about_ca_system_score_codex":0.00053971726,"about_ca_system_score_gemma":0.0001802207,"threshold_uncertainty_score":0.047913313},"labels":[],"label_agreement":null},{"id":"W2139830071","doi":"10.1017/s0016756810001007","title":"Stratigraphy and geochemistry of the Early Carboniferous Clyde Plateau Lavas in south Bute, Midland Valley of Scotland","year":2010,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Eli Lilly and Company","keywords":"Geology; Basalt; Geochemistry; Augite; Phenocryst; Trachyte; Volcanic rock; Lava; Feldspar; Volcano; Paleontology; Plagioclase; Quartz","score_opus":0.006596746400546185,"score_gpt":0.17315165796806914,"score_spread":0.16655491156752295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139830071","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99816823,0.00026392465,0.000039198538,0.000029459594,0.0000029961507,0.000008479259,0.00051980285,0.0000062698277,0.0009615959],"genre_scores_gemma":[0.9985813,0.00011405677,0.00006116266,0.000017297454,0.0000053502545,0.0000070092947,0.000555531,0.0000021572046,0.0006561852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979204,0.00001258248,0.000012209881,0.00003698408,0.000059325823,0.00008691098],"domain_scores_gemma":[0.999617,0.000034482895,0.00012682326,0.000013306111,0.00012090624,0.00008748197],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012644178,0.00018288534,0.00022173623,0.0018229202,0.0007357653,0.0008830315,0.00026352383,0.00019861759,0.0014913512],"category_scores_gemma":[0.0003867919,0.00016607251,0.00015557595,0.0011979282,0.00047090993,0.00023660209,0.0004179191,0.00011669212,0.0002822471],"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":[0.000093329334,0.000031575964,0.9742106,0.00010284062,0.000047131758,0.0006599011,0.0024633978,0.000119979144,0.008361135,0.00012963774,0.0005427715,0.01323768],"study_design_scores_gemma":[0.0000025826093,0.000019948706,0.9987167,0.0000065242543,0.000002579594,0.000050434068,0.00033400868,0.000027098304,0.000073121824,0.0000039390648,0.0007612551,0.0000018075264],"about_ca_topic_score_codex":0.23907979,"about_ca_topic_score_gemma":0.42949554,"teacher_disagreement_score":0.23907979,"about_ca_system_score_codex":0.0013406995,"about_ca_system_score_gemma":0.00059260515,"threshold_uncertainty_score":0.47537637},"labels":[],"label_agreement":null},{"id":"W2140569261","doi":"10.1017/s0016756808005785","title":"A new mantle xenolith locality from Simien shield volcano, NW Ethiopia","year":2008,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"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":"Xenolith; Geology; Olivine; Geochemistry; Mantle (geology); Basalt; Trace element; Spinel; Volcano; Partial melting; Recrystallization (geology); Petrology; Paleontology","score_opus":0.024093520951642074,"score_gpt":0.20573687221671974,"score_spread":0.18164335126507766,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140569261","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968611,0.00031897114,0.00030507112,0.000023199194,0.000009896878,0.000010573439,0.00021085542,0.000008166158,0.00225211],"genre_scores_gemma":[0.9979346,0.00021900072,0.0004169051,0.000023436343,0.000008046277,0.00000403369,0.00027624736,0.0000033452238,0.0011143422],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994504,0.0000036370575,0.000003862643,0.000017971966,0.000010763007,0.000018775223],"domain_scores_gemma":[0.99994826,0.000007996781,0.000010054594,0.0000065978634,0.000011293272,0.000015807329],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007147822,0.00030810887,0.00016973884,0.0014407041,0.0008712408,0.00055137684,0.00025772123,0.0001678386,0.0016956216],"category_scores_gemma":[0.00010539711,0.00022319579,0.00014671276,0.000635946,0.00036520668,0.00018765405,0.00054841937,0.00017417608,0.00029769068],"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":[0.0005699018,0.0000985633,0.6499186,0.00037040724,0.00014988829,0.023856485,0.018112332,0.00036883226,0.25382206,0.0013214856,0.0006458378,0.050765567],"study_design_scores_gemma":[0.000019460107,0.00019243053,0.9226951,0.00009253508,0.00009035411,0.023297654,0.0122569855,0.00032826597,0.022104027,0.00021049152,0.018690882,0.000021858732],"about_ca_topic_score_codex":0.0062639248,"about_ca_topic_score_gemma":0.016258087,"teacher_disagreement_score":0.0062639248,"about_ca_system_score_codex":0.00031909344,"about_ca_system_score_gemma":0.00031157324,"threshold_uncertainty_score":0.012454927},"labels":[],"label_agreement":null},{"id":"W2141135506","doi":"10.1017/s0016756808004913","title":"The SPICE carbon isotope excursion in Siberia: a combined study of the upper Middle Cambrian–lowermost Ordovician Kulyumbe River section, northwestern Siberian Platform","year":2008,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":122,"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; University of Ottawa","funders":"","keywords":"Geology; Excursion; Ordovician; Paleontology; Biozone; Laurentia; Horizon; Chemostratigraphy; Global Boundary Stratotype Section and Point; Trilobite; Isotopes of carbon; Stage (stratigraphy); Biostratigraphy; Total organic carbon; Geometry","score_opus":0.02095008348739851,"score_gpt":0.20658064577790958,"score_spread":0.18563056229051106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141135506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991948,0.00019715025,0.00003458364,0.000008834523,0.0000014290936,0.0000023531861,0.00016127621,0.0000026105138,0.00039699892],"genre_scores_gemma":[0.99913955,0.00012316575,0.00006533559,0.0000139198255,0.0000031001803,0.000004465145,0.0004535392,0.0000024792337,0.00019448913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987864,0.000018018634,0.000014457352,0.000031694613,0.000022967812,0.000034210127],"domain_scores_gemma":[0.99983406,0.000020252235,0.000037006383,0.000017031047,0.000044096123,0.00004761026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003512465,0.0003740901,0.00049509876,0.002252038,0.0010053641,0.0007915907,0.000297371,0.00032166587,0.0012121467],"category_scores_gemma":[0.00031023464,0.00020232014,0.0003620609,0.00234598,0.0003879424,0.00029956634,0.0008520965,0.00016079893,0.00026475126],"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":[0.00011324442,0.000025414047,0.9835105,0.000034813096,0.00011992783,0.00042489285,0.0011811638,0.00016088386,0.0065887445,0.00003202102,0.000066544846,0.007741845],"study_design_scores_gemma":[0.0000010629658,0.00001012494,0.99934834,0.0000030519275,0.00000963509,0.000053604315,0.00025327396,0.00008107297,0.00009795499,0.000004680521,0.00013599444,0.0000010928054],"about_ca_topic_score_codex":0.07256035,"about_ca_topic_score_gemma":0.102381155,"teacher_disagreement_score":0.07256035,"about_ca_system_score_codex":0.00073578,"about_ca_system_score_gemma":0.0007147616,"threshold_uncertainty_score":0.14427596},"labels":[],"label_agreement":null},{"id":"W2142155761","doi":"10.1017/s0016756805000543","title":"Late Cambrian ptychaspidid trilobites from western Utah: implications for trilobite systematics and biostratigraphy","year":2005,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":"","keywords":"Trilobite; Biostratigraphy; Paleontology; Taxon; Fauna; Systematics; Geology; Geography; Ecology; Biology; Taxonomy (biology); Ordovician","score_opus":0.02892151364032609,"score_gpt":0.24747153727543786,"score_spread":0.21855002363511178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142155761","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99738127,0.0004614131,0.000084910775,0.000105187624,0.000003907825,0.000006143804,0.0000856329,0.000007934357,0.0018636126],"genre_scores_gemma":[0.9988794,0.0003408285,0.00019895703,0.000039775052,0.000005672506,0.000007691694,0.00021971288,0.0000029973219,0.0003049495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999248,0.000012353138,0.000008548465,0.000017767901,0.000016892194,0.000019577936],"domain_scores_gemma":[0.999788,0.000026768608,0.000049645252,0.000014073924,0.00007575782,0.00004564733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019214778,0.00016687746,0.0001754412,0.0016351647,0.0011557918,0.0007608214,0.0004006105,0.0002897172,0.0016849859],"category_scores_gemma":[0.00052589475,0.000116890136,0.00007580385,0.00173876,0.00064670236,0.0005202063,0.00084626646,0.00022223426,0.00019786436],"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":[0.00015263962,0.00003566786,0.9150195,0.000106974556,0.000031904085,0.0006310792,0.011243355,0.00026715893,0.012042951,0.00040970207,0.0006333628,0.059425652],"study_design_scores_gemma":[0.0000019472216,0.000014413618,0.9963636,0.000029870667,0.0000072303633,0.00011961082,0.0019376455,0.00017180796,0.00016173729,0.000062903586,0.0011265641,0.0000027400945],"about_ca_topic_score_codex":0.095212296,"about_ca_topic_score_gemma":0.22748408,"teacher_disagreement_score":0.095212296,"about_ca_system_score_codex":0.000969207,"about_ca_system_score_gemma":0.00069015037,"threshold_uncertainty_score":0.18931615},"labels":[],"label_agreement":null},{"id":"W2143093330","doi":"10.1017/s0016756814000168","title":"Geology and geochemistry of the Baijiantan–Baikouquan ophiolitic mélanges: implications for geological evolution of west Junggar, Xinjiang, NW China","year":2014,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"Peking University; Université Laval","keywords":"Geology; Isochron; Ophiolite; Geochemistry; Basalt; Subduction; Ordovician; Mantle (geology); Metamorphic rock; Mid-ocean ridge; Zircon; Partial melting; Metamorphism; Rare-earth element; Paleontology; Tectonics; Rare earth; Earth science","score_opus":0.010780300728594896,"score_gpt":0.20789126296517532,"score_spread":0.19711096223658042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143093330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995055,0.000104386054,0.0000219991,0.000009918136,5.9351083e-7,0.0000016470791,0.000058873433,0.0000013737235,0.0002956563],"genre_scores_gemma":[0.99958843,0.00007286717,0.00004863814,0.000005392916,9.329634e-7,0.0000017597542,0.00009921953,8.9388186e-7,0.00018188315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999404,0.0000049759597,0.000006225534,0.000019444828,0.000013219714,0.000015711377],"domain_scores_gemma":[0.99990094,0.0000074131167,0.000039338807,0.0000074792,0.00002030674,0.00002455834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001328884,0.000258094,0.00015763425,0.0016275514,0.00055242155,0.00053808634,0.00016184259,0.00013766764,0.0005758993],"category_scores_gemma":[0.000118802134,0.00017190905,0.00013145655,0.0014931052,0.00046099376,0.00020664404,0.00034770113,0.00011278565,0.000057242538],"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":[0.000053571104,0.000011609422,0.96921074,0.00004280705,0.000051162973,0.00019924935,0.0011926462,0.00021861898,0.022020513,0.00011263526,0.000036616555,0.0068499283],"study_design_scores_gemma":[0.0000010836088,0.0000045742095,0.9993248,0.0000017162187,0.000004707274,0.000027180691,0.00024451708,0.0000500437,0.00018008165,0.000009824396,0.00015030708,0.0000010924045],"about_ca_topic_score_codex":0.06599171,"about_ca_topic_score_gemma":0.1352123,"teacher_disagreement_score":0.06599171,"about_ca_system_score_codex":0.00088456424,"about_ca_system_score_gemma":0.00057485,"threshold_uncertainty_score":0.13121516},"labels":[],"label_agreement":null},{"id":"W2144240006","doi":"10.1017/s0016756804009951","title":"Petrology and geochronology of Mesoproterozoic mafic–intermediate plutonic rocks from Mitwaba (D. R. Congo): implications for the evolution of the Kibaran belt in central Africa","year":2005,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","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":"Memorial University of Newfoundland","funders":"","keywords":"Mafic; Geochemistry; Geology; Zircon; Felsic; Partial melting; Pluton; Igneous rock; Metamorphism; Continental arc; Mantle wedge; Petrology; Underplating; Gabbro; Petrogenesis; Continental crust; Porphyritic; Crust; Mantle (geology); Volcanic rock; Subduction","score_opus":0.010543153460903027,"score_gpt":0.19716628116877896,"score_spread":0.18662312770787592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144240006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99737775,0.00045643287,0.00009507065,0.000025518122,0.0000017376964,0.000006615909,0.00035553658,0.000007364303,0.0016739145],"genre_scores_gemma":[0.9990121,0.00015634562,0.00015964574,0.000006746543,0.000001912992,0.000006067128,0.00019412783,0.0000048511615,0.0004582007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992824,0.000008429699,0.000008105323,0.000021640928,0.000011071314,0.000022499185],"domain_scores_gemma":[0.99987745,0.00001371367,0.00005366999,0.000010020972,0.00002712972,0.00001804248],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013867514,0.00034288052,0.00014083178,0.0021291147,0.00071314466,0.0007350179,0.0002237406,0.00022512466,0.0016864545],"category_scores_gemma":[0.0002838479,0.00032425896,0.00011182485,0.0015976683,0.0003305987,0.0003405902,0.00024774682,0.00013660634,0.00027008101],"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":[0.00033304142,0.000040468025,0.81304115,0.00022820484,0.000085122956,0.0018477641,0.004863472,0.0011187446,0.1496505,0.0005450156,0.00030261424,0.027943922],"study_design_scores_gemma":[0.0000035467424,0.000011552926,0.9962339,0.000018738428,0.00001969365,0.00027554628,0.00042585857,0.00015056257,0.0015462097,0.000013500493,0.001296898,0.000004068812],"about_ca_topic_score_codex":0.108348794,"about_ca_topic_score_gemma":0.2787478,"teacher_disagreement_score":0.108348794,"about_ca_system_score_codex":0.0016978815,"about_ca_system_score_gemma":0.0003337608,"threshold_uncertainty_score":0.21543628},"labels":[],"label_agreement":null},{"id":"W2144553566","doi":"10.1017/s0016756813000356","title":"<i>Diandongosaurus acutidentatus</i>Shang, Wu &amp; Li, 2011 (Diapsida: Sauropterygia) and the relationships of Chinese eosauropterygians","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":24,"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 Museum of Nature","funders":"National Science Council","keywords":"Cladogram; Skull; Pelvic girdle; Anatomy; Taxon; Biology; Phylogenetic tree; Clade; Evolutionary biology; Paleontology","score_opus":0.01756933316885398,"score_gpt":0.2103784198954283,"score_spread":0.19280908672657432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144553566","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908193,0.0004423026,0.00037349318,0.000056495883,0.000011453124,0.000010270216,0.00009805802,0.000016948748,0.008171791],"genre_scores_gemma":[0.9975848,0.00023852842,0.0005467153,0.000034680746,0.000008921553,0.0000128784395,0.00023398492,0.0000030558067,0.001336408],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994385,0.000007341138,0.000009057007,0.000018180343,0.00001420932,0.000007395414],"domain_scores_gemma":[0.9999256,0.000006562985,0.000032519714,0.000009422351,0.00001250004,0.000013357779],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000096971875,0.00015919445,0.00012042551,0.0011781467,0.0006563419,0.00022121571,0.00024348739,0.00021145266,0.0026791976],"category_scores_gemma":[0.00013492366,0.00006537312,0.00012524743,0.0010198574,0.00066206494,0.00023788848,0.0006710888,0.00017871433,0.00037925382],"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":[0.000301632,0.000059895945,0.662184,0.00045190123,0.00012067991,0.0025529221,0.005481136,0.0004213589,0.12715337,0.0017394655,0.0011484398,0.1983852],"study_design_scores_gemma":[0.0000064458345,0.00004866817,0.98578507,0.00003315521,0.000032192867,0.0019172451,0.0011949864,0.00030093384,0.001431972,0.00026657878,0.008971758,0.00001096555],"about_ca_topic_score_codex":0.0043073115,"about_ca_topic_score_gemma":0.01080126,"teacher_disagreement_score":0.0043073115,"about_ca_system_score_codex":0.0002615983,"about_ca_system_score_gemma":0.00026626175,"threshold_uncertainty_score":0.00896281},"labels":[],"label_agreement":null},{"id":"W2147617970","doi":"10.1017/s001675680100509x","title":"Burrowing below the basal Cambrian GSSP, Fortune Head, Newfoundland","year":2001,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":158,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Global Boundary Stratotype Section and Point; Stratotype; Geology; Paleontology; Proterozoic; Head (geology); Section (typography); Stage (stratigraphy); Period (music); Range (aeronautics)","score_opus":0.027414873373522206,"score_gpt":0.24137423114280146,"score_spread":0.21395935776927927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147617970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831141,0.00056480546,0.000121480014,0.00041044145,0.000011078516,0.0000120730965,0.002242868,0.000022291373,0.013500772],"genre_scores_gemma":[0.9760324,0.0006492337,0.00038994735,0.00008692749,0.000004156831,0.000007471799,0.001154552,0.000007166876,0.021668166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999503,0.000002341265,0.000001509868,0.00001177128,0.00000777322,0.000026258575],"domain_scores_gemma":[0.99986136,0.0000098971905,0.000029748613,0.000008546644,0.00005495721,0.000035448204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000072254064,0.00011276737,0.00006217263,0.00061066507,0.0015985651,0.0004492771,0.00022057943,0.00010297076,0.005177067],"category_scores_gemma":[0.00020413306,0.00011197188,0.00004974754,0.0007802916,0.00045219946,0.00027441987,0.00047778327,0.00019297823,0.00049370807],"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":[0.00022830522,0.0000328341,0.836798,0.00009669162,0.00002516345,0.0015701599,0.008680534,0.00034791345,0.008194401,0.0008178034,0.016875314,0.12633292],"study_design_scores_gemma":[0.0000011494001,0.000008359811,0.9908564,0.000015349748,0.0000026345908,0.00012201823,0.001812517,0.000027953607,0.00023346594,0.000019103141,0.0068990095,0.0000019945282],"about_ca_topic_score_codex":0.9187236,"about_ca_topic_score_gemma":0.9915051,"teacher_disagreement_score":0.08127642,"about_ca_system_score_codex":0.0037823676,"about_ca_system_score_gemma":0.0021711758,"threshold_uncertainty_score":0.16351008},"labels":[],"label_agreement":null},{"id":"W2149319683","doi":"10.1017/s0016756810000476","title":"Petrogenetic and tectonic inferences from the study of the Mt Cer pluton (West Serbia)","year":2010,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"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":"Università degli Studi di Perugia; European Commission; Aristotle University of Thessaloniki; University of Bristol; Ministero dell’Istruzione, dell’Università e della Ricerca; University of Alberta","keywords":"Quartz monzonite; Pluton; Geology; Geochemistry; Mafic; Fractional crystallization (geology); Partial melting; Quartz; Petrology; Mantle (geology); Tectonics; Seismology; Paleontology","score_opus":0.013485444373661313,"score_gpt":0.1978828485448325,"score_spread":0.1843974041711712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149319683","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99094665,0.0017463851,0.00022792126,0.000033427623,0.000012752789,0.000023731985,0.0003605631,0.0000148738745,0.006633678],"genre_scores_gemma":[0.9985116,0.0003758874,0.00027584538,0.00000826832,0.0000032608054,0.0000052613213,0.0002905522,0.00000544855,0.000523931],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999033,0.0000210196,0.000008644626,0.000027473614,0.0000121026305,0.000027346283],"domain_scores_gemma":[0.99989057,0.000011694525,0.00004458441,0.000012287835,0.00002489211,0.000015925314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033312946,0.0004374918,0.00034024913,0.0019839024,0.0004858618,0.00068979396,0.00021100977,0.00017746589,0.0015970386],"category_scores_gemma":[0.00038616685,0.00024482873,0.00019720852,0.0010383788,0.00046456917,0.00018568391,0.00054558855,0.00024770264,0.00030294797],"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":[0.0014257407,0.00016975154,0.8001393,0.000855541,0.00024119359,0.008209979,0.0068734433,0.0062221256,0.06546064,0.0042347307,0.0016699057,0.10449757],"study_design_scores_gemma":[0.000020504347,0.000102559,0.9900748,0.00011781503,0.000026779768,0.00071032176,0.0009226473,0.0005916363,0.0009359885,0.00006398086,0.0064282417,0.000004725107],"about_ca_topic_score_codex":0.02389762,"about_ca_topic_score_gemma":0.046358544,"teacher_disagreement_score":0.02389762,"about_ca_system_score_codex":0.00068270747,"about_ca_system_score_gemma":0.000415555,"threshold_uncertainty_score":0.04751706},"labels":[],"label_agreement":null},{"id":"W2151874497","doi":"10.1017/s0016756813000976","title":"Zircon U–Pb ages, major and trace elements, and Hf isotope characteristics of the Tiantangzhai granites in the North Dabie orogen, Central China: tectonic implications","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"University of Windsor","funders":"","keywords":"Zircon; Protolith; Geology; Geochemistry; Partial melting; Subduction; Crust; Geochronology; Plagioclase; Cretaceous; Magmatism; Tectonics; Quartz; Paleontology","score_opus":0.00785625481314045,"score_gpt":0.180377765874111,"score_spread":0.17252151106097055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151874497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993777,0.00013576078,0.00003621902,0.000008533545,8.405447e-7,0.0000024220585,0.00010394588,0.0000032137532,0.00033126303],"genre_scores_gemma":[0.99938536,0.000099073826,0.00006257989,0.0000046613213,0.0000013411604,0.000002383769,0.00013863278,0.000002208991,0.00030377368],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992836,0.0000038542485,0.000007105373,0.000024085723,0.00001617909,0.000020279],"domain_scores_gemma":[0.99991274,0.0000065694135,0.00003070631,0.0000075079597,0.000024364981,0.000018160299],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018648875,0.00031138674,0.00023829711,0.0017362301,0.0005124645,0.0006109477,0.0002552801,0.00021460539,0.0006983991],"category_scores_gemma":[0.00012864081,0.00024073353,0.00019880327,0.0014764175,0.00044184682,0.00020038454,0.0003532934,0.0001351963,0.000081731516],"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":[0.00024939654,0.000023612378,0.9312385,0.00007147095,0.00010639833,0.00035178082,0.0012948224,0.0006821071,0.05232231,0.00019146164,0.00008835322,0.013379768],"study_design_scores_gemma":[0.000004371233,0.000010212147,0.9986755,0.0000020455366,0.000013931166,0.00004435083,0.00021238693,0.00014085002,0.0005740869,0.000014605879,0.00030501813,0.0000025650534],"about_ca_topic_score_codex":0.10153669,"about_ca_topic_score_gemma":0.16965362,"teacher_disagreement_score":0.10153669,"about_ca_system_score_codex":0.0011602184,"about_ca_system_score_gemma":0.0005932961,"threshold_uncertainty_score":0.20189136},"labels":[],"label_agreement":null},{"id":"W2153494502","doi":"10.1017/s0016756803268837","title":"M<scp>ARGULIS</scp>, L. &amp; D<scp>OLAN</scp>, M. F. 2002. <i>Early Life. Evolution on the Precambrian Earth</i>, 2nd ed. xxiv + 168 pp. Sudbury, Boston, Toronto, London, Singpore: Jones &amp; Bartlett. Price £21.99 (paperback). ISBN 0 7637 1463 1","year":2003,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":"Precambrian; Geology; Paleontology","score_opus":0.01619904451704283,"score_gpt":0.20999805402131316,"score_spread":0.19379900950427034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153494502","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.002105992,0.44397652,0.003512386,0.029096426,0.022257583,0.00007069898,0.011432028,0.0017969331,0.48575145],"genre_scores_gemma":[0.0070525333,0.14547701,0.0018040508,0.002088461,0.0035951713,0.00004744273,0.0029362221,0.00047710494,0.83652216],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99981755,0.0000138281375,0.00001415343,0.000034982437,0.00010445739,0.000015031389],"domain_scores_gemma":[0.99944764,0.00017194345,0.00006318247,0.000036661386,0.00020399423,0.00007659522],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002565814,0.0010532908,0.0007109871,0.0020119145,0.0007425698,0.0018767162,0.0007346373,0.0008159851,0.3585631],"category_scores_gemma":[0.0012789725,0.0005575832,0.0003194651,0.0048937513,0.0004265379,0.0021941857,0.0009181205,0.0011180536,0.1978553],"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":[0.000013545264,0.0000026881396,0.00007641745,0.00022892866,0.0000032856155,0.000037781712,0.000061027007,0.000038793085,0.0002213092,0.0007324197,0.8870864,0.11149737],"study_design_scores_gemma":[0.000002239725,0.000004727663,0.0011107103,0.00021023145,0.000003987764,0.00009685972,0.00006968352,0.00002449789,0.00010393602,0.00047711298,0.99789256,0.0000034812495],"about_ca_topic_score_codex":0.015558029,"about_ca_topic_score_gemma":0.053579994,"teacher_disagreement_score":0.3585631,"about_ca_system_score_codex":0.0010129726,"about_ca_system_score_gemma":0.00063411274,"threshold_uncertainty_score":0.9149319},"labels":[],"label_agreement":null},{"id":"W2154183595","doi":"10.1017/s0016756811000926","title":"The origin and significance of pedogenic dolomite from the Upper Permian of the South Urals of Russia","year":2011,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":39,"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":"Dolomite; Permian; Geology; Pedogenesis; Petrography; Geochemistry; Diagenesis; Paleontology; Calcite; Authigenic; Carbonate; Paleosol; Paleozoic; Extinction event; Structural basin; Soil water","score_opus":0.035580399488376734,"score_gpt":0.21650469633972388,"score_spread":0.18092429685134714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154183595","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990727,0.00022905294,0.000052204694,0.0000052421938,0.0000012434119,0.0000017638015,0.00007436629,0.0000024249102,0.00056104705],"genre_scores_gemma":[0.9995528,0.00011954034,0.000060198035,0.0000016750932,0.0000012086929,9.638618e-7,0.00008573517,0.0000017912813,0.00017605643],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998759,0.000011461002,0.00001283586,0.00003182258,0.000034715045,0.00003318265],"domain_scores_gemma":[0.9998814,0.000015233119,0.00003862112,0.000007633345,0.00003754858,0.00001959586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013072866,0.00022559287,0.00024441406,0.002357022,0.00068130455,0.000716889,0.00021409687,0.00013826833,0.00067627645],"category_scores_gemma":[0.0002096021,0.00015992337,0.00013636063,0.001165091,0.00054884795,0.00020513478,0.00042162978,0.00009707467,0.00013640523],"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":[0.00011607657,0.00001754392,0.93342245,0.000108386535,0.000052645744,0.0008494134,0.0018502113,0.00020699321,0.046644974,0.00018983465,0.00004069739,0.016500633],"study_design_scores_gemma":[8.174462e-7,0.000010182237,0.9976069,0.0000062544086,0.0000068029594,0.00022904146,0.00049595896,0.00007676363,0.0010098636,0.000018806948,0.00053715473,0.0000014601294],"about_ca_topic_score_codex":0.034217644,"about_ca_topic_score_gemma":0.05861636,"teacher_disagreement_score":0.034217644,"about_ca_system_score_codex":0.00041785516,"about_ca_system_score_gemma":0.0004632717,"threshold_uncertainty_score":0.06803697},"labels":[],"label_agreement":null},{"id":"W2156032427","doi":"10.1017/s0016756813000204","title":"A starfish bed in the Middle Miocene Grand Bay Formation of Carriacou, The Grenadines (West Indies)","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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 New Brunswick","funders":"","keywords":"Geology; Paleontology; Starfish; Bay; Late Miocene; Taxon; Oceanography; Structural basin","score_opus":0.030015554430661683,"score_gpt":0.21091306468811807,"score_spread":0.1808975102574564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156032427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984831,0.00014256577,0.00003234827,0.00004034797,0.0000047542594,0.000012273734,0.00023745571,0.0000049946525,0.0010420576],"genre_scores_gemma":[0.99823844,0.00011622028,0.00016581539,0.000023289876,0.0000037827956,0.000011858007,0.0003876791,0.0000020649484,0.0010508258],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989843,0.000008495317,0.0000070468695,0.000032357413,0.00002183815,0.00003184707],"domain_scores_gemma":[0.99984574,0.000011878278,0.000048241043,0.000007806788,0.000035134715,0.000051057177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012854443,0.00025687218,0.0001641144,0.0016884009,0.0011828176,0.00058172416,0.00043353476,0.0003637147,0.0033410392],"category_scores_gemma":[0.00030628397,0.00022962228,0.00015116672,0.0011141708,0.00053252996,0.0003089289,0.00063993473,0.00016934308,0.0004610232],"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":[0.00011467528,0.0000360913,0.96598154,0.00010621175,0.000035271827,0.002712956,0.005733879,0.00006490705,0.012541519,0.00009438042,0.0005454792,0.012033062],"study_design_scores_gemma":[0.0000025587299,0.000026281075,0.99644727,0.000020285599,0.000005027459,0.00029952612,0.002049422,0.000046094734,0.00008338404,0.00000362633,0.0010139542,0.0000026077487],"about_ca_topic_score_codex":0.38662812,"about_ca_topic_score_gemma":0.763285,"teacher_disagreement_score":0.38662812,"about_ca_system_score_codex":0.0012496075,"about_ca_system_score_gemma":0.0008753656,"threshold_uncertainty_score":0.7687554},"labels":[],"label_agreement":null},{"id":"W2161212486","doi":"10.1017/s0016756803007854","title":"Palaeobiogeographic implications of Middle Permian brachiopods from Johore (Peninsular Malaysia)","year":2003,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geophysical Studies","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":"Fauna; Terrane; Paleontology; Permian; Geology; Crinoid; Taxon; Ecology; Biology; Tectonics; Structural basin","score_opus":0.023692988722338063,"score_gpt":0.20542378333796357,"score_spread":0.18173079461562552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161212486","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99937254,0.000046487807,0.000012453311,0.000011093944,0.0000010367456,0.0000010867675,0.00005439725,0.0000011314881,0.00049977243],"genre_scores_gemma":[0.9997081,0.00004130951,0.000044176853,0.0000054280113,9.982949e-7,0.0000012143948,0.00007914618,6.69067e-7,0.00011898768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999255,0.000012166919,0.000008106476,0.00002322271,0.000010510028,0.00002049018],"domain_scores_gemma":[0.9998485,0.000018759307,0.00005705674,0.0000072641405,0.000020222458,0.00004812914],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016370976,0.00015848698,0.00008451507,0.0008051555,0.0003665352,0.0005059504,0.00015534529,0.00013121948,0.0012997369],"category_scores_gemma":[0.00024327134,0.00017126133,0.00010924137,0.0005407254,0.00029352336,0.00024901875,0.000363553,0.00014767953,0.00018811015],"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":[0.00005676529,0.000021414879,0.9842159,0.00003205921,0.00003484996,0.00019959385,0.0021407015,0.00008874874,0.0036577014,0.00006791668,0.000086875785,0.009397526],"study_design_scores_gemma":[7.385451e-7,0.000009089177,0.99872106,0.0000069293433,0.0000037216205,0.00011779282,0.00075037807,0.00004558888,0.00008790101,0.0000062215554,0.0002489466,0.000001585874],"about_ca_topic_score_codex":0.022916256,"about_ca_topic_score_gemma":0.070240036,"teacher_disagreement_score":0.022916256,"about_ca_system_score_codex":0.0003941602,"about_ca_system_score_gemma":0.00034779447,"threshold_uncertainty_score":0.045565724},"labels":[],"label_agreement":null},{"id":"W2162999453","doi":"10.1017/s0016756806002020","title":"Ammonoid stratigraphy and sedimentary evolution across the Permian–Triassic boundary in East Greenland","year":2006,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","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":"","keywords":"Permian; Global Boundary Stratotype Section and Point; Geology; Paleontology; Stratotype; Stratigraphy; Early Triassic; Biostratigraphy; Boreal; Sedimentary rock; Marine transgression; Structural basin; Stage (stratigraphy); Tectonics","score_opus":0.010857270880866925,"score_gpt":0.2140535980841004,"score_spread":0.20319632720323347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162999453","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999585,0.000048596245,0.000013426679,0.000014022545,6.938456e-7,7.2694564e-7,0.00008809787,0.0000028282307,0.00024667234],"genre_scores_gemma":[0.9995523,0.00003364234,0.000031393058,0.0000078705925,7.995654e-7,8.583272e-7,0.00019466654,0.0000016378034,0.00017688505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999434,0.0000059173603,0.0000042093316,0.00001681236,0.000009636368,0.000020032401],"domain_scores_gemma":[0.9998822,0.000009893491,0.000040234325,0.000007715162,0.000025026986,0.00003485339],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012603564,0.00013173248,0.00011200135,0.001306065,0.0003130629,0.00035536342,0.00019752825,0.00014960955,0.0007479488],"category_scores_gemma":[0.00018244835,0.000089335794,0.00009983526,0.0010322547,0.00038025065,0.0002378613,0.0003419316,0.000119852135,0.00013678127],"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":[0.000055817312,0.000015335685,0.98730785,0.00000931059,0.000032045788,0.00018476603,0.0010730368,0.00019046794,0.0041908226,0.00015703411,0.00017067544,0.0066127772],"study_design_scores_gemma":[5.308229e-7,0.000002799035,0.99962914,0.0000016918448,0.0000012088879,0.00001737035,0.00014974413,0.00005422122,0.000029746838,0.000011998836,0.00010096872,6.151473e-7],"about_ca_topic_score_codex":0.12845059,"about_ca_topic_score_gemma":0.32444486,"teacher_disagreement_score":0.12845059,"about_ca_system_score_codex":0.00092830794,"about_ca_system_score_gemma":0.00044233294,"threshold_uncertainty_score":0.25540584},"labels":[],"label_agreement":null},{"id":"W2163240516","doi":"10.1017/s0016756807003949","title":"The Miocene igneous rocks in the Basal Unit of Lavrion (SE Attica, Greece): petrology and geodynamic implications","year":2007,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"Saint Mary's University","funders":"","keywords":"Geology; Igneous rock; Geochemistry; Quartz monzonite; Pluton; Mafic; Zircon; Petrology; Petrogenesis; Metamorphic rock; Mantle (geology); Tectonics; Paleontology","score_opus":0.01668922059795774,"score_gpt":0.23339685472383404,"score_spread":0.2167076341258763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163240516","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993877,0.0006644522,0.00010616503,0.000054998167,0.0000028133547,0.000009182276,0.00013925004,0.000016878406,0.0051292786],"genre_scores_gemma":[0.99908626,0.000177628,0.00007029462,0.0000048635984,0.0000023037398,0.0000017567228,0.000082302344,0.000004360363,0.0005702219],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999013,0.0000115471985,0.0000083340465,0.000036874357,0.00002092591,0.000021008233],"domain_scores_gemma":[0.99993515,0.0000070209603,0.000023076429,0.000007724757,0.000014513386,0.0000124447415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011757965,0.0002638474,0.00017893786,0.002215928,0.0003722615,0.00078850216,0.00032800838,0.0002734134,0.0019423567],"category_scores_gemma":[0.00023507686,0.00020159091,0.0001392307,0.0009958403,0.0006171801,0.00025076326,0.0005829478,0.00014300301,0.0005139011],"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":[0.00027515626,0.0000727857,0.82996523,0.00039798662,0.00018470353,0.0028036325,0.0039179977,0.0037715232,0.075357676,0.0019506674,0.000415207,0.08088744],"study_design_scores_gemma":[0.00000776984,0.000031719886,0.99495983,0.000028131382,0.0000095468995,0.0006165558,0.0005499129,0.0005801111,0.00077630364,0.00015338232,0.0022822034,0.0000046436903],"about_ca_topic_score_codex":0.019417806,"about_ca_topic_score_gemma":0.020594392,"teacher_disagreement_score":0.019417806,"about_ca_system_score_codex":0.0008692035,"about_ca_system_score_gemma":0.0003769964,"threshold_uncertainty_score":0.038609564},"labels":[],"label_agreement":null},{"id":"W2166594312","doi":"10.1017/s0016756808005323","title":"Travertine deposits from along the South Tibetan Fault System near Nyalam, Tibet","year":2008,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geology and Paleoclimatology Research","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":"Queen's University","funders":"","keywords":"Geology; Fluvial; Tufa; Alluvial fan; Geochemistry; Plateau (mathematics); Deposition (geology); Alluvium; Geomorphology; River terraces; Spring (device); Sedimentary depositional environment; Fault (geology); Tectonics; Hot spring; Quaternary; Paleontology; Sediment; Sedimentary rock; Structural basin; Carbonate","score_opus":0.025338163381224965,"score_gpt":0.21462356785915265,"score_spread":0.1892854044779277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166594312","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984168,0.00008783544,0.000038914677,0.000006455893,0.0000012159335,0.0000055506666,0.00024429816,0.0000033745857,0.0011955894],"genre_scores_gemma":[0.99812967,0.000058433197,0.00010925037,0.000003947723,0.0000022656252,0.000004150896,0.00065335195,0.0000011371828,0.001037837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999635,0.0000035752628,0.0000041060784,0.0000105992885,0.000010046552,0.000008237151],"domain_scores_gemma":[0.9999213,0.0000068668437,0.00002559555,0.0000047647322,0.000025665799,0.000015777627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000082732084,0.00015022366,0.000100653895,0.0011942749,0.00055968,0.00042474267,0.00016687762,0.00009936323,0.0012770456],"category_scores_gemma":[0.00013496664,0.00007537001,0.000070082904,0.0012559042,0.00023775065,0.00012189402,0.00021338381,0.00007781595,0.00014100969],"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":[0.00022809507,0.00004747954,0.9080633,0.00013452362,0.00006194792,0.0022837794,0.0040494394,0.0005958853,0.058814872,0.00021615307,0.00035250888,0.025152046],"study_design_scores_gemma":[0.0000032502548,0.000019888057,0.9982609,0.0000070869387,0.0000049444902,0.00020171383,0.0005425506,0.00011785246,0.00028816954,0.000011231386,0.00054054626,0.0000019731453],"about_ca_topic_score_codex":0.05175029,"about_ca_topic_score_gemma":0.17921588,"teacher_disagreement_score":0.05175029,"about_ca_system_score_codex":0.0004063226,"about_ca_system_score_gemma":0.0003401257,"threshold_uncertainty_score":0.10289818},"labels":[],"label_agreement":null},{"id":"W2167862332","doi":"10.1017/s0016756811000598","title":"Tribes Hill–Rochdale formations in east Laurentia: proxies for Early Ordovician (Tremadocian) eustasy on a tropical passive margin (New York and west Vermont)","year":2011,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":25,"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":"Laurentia; Geology; Marine transgression; Paleontology; Ordovician; Craton; Unconformity; Baltica; Sedimentary depositional environment; Structural basin; Tectonics","score_opus":0.03617807248766902,"score_gpt":0.21385631350263357,"score_spread":0.17767824101496454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167862332","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99833137,0.000130429,0.000013403448,0.0000286156,0.000002044381,0.000004447001,0.00039703297,0.000003945875,0.0010887075],"genre_scores_gemma":[0.99890435,0.00007815315,0.000059304926,0.00000909323,0.0000030977897,0.000004393816,0.000410691,0.0000019720294,0.0005289994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987626,0.000012150934,0.0000091089205,0.00003587867,0.000024405674,0.000042215655],"domain_scores_gemma":[0.99958843,0.000032484575,0.00017140247,0.000020066393,0.00006882529,0.0001187662],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020985208,0.00016942674,0.00016261433,0.0015440331,0.00057949626,0.0010063421,0.0003566082,0.0001438685,0.0018655892],"category_scores_gemma":[0.00050753716,0.00013135982,0.000113041155,0.0010755048,0.00032531735,0.0003269385,0.00062394823,0.00017022215,0.0002488989],"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":[0.000024977699,0.000016548152,0.9918853,0.000019656723,0.000024150344,0.0001212396,0.0009753277,0.00012132078,0.0018042746,0.000096131385,0.00037054883,0.004540469],"study_design_scores_gemma":[0.0000014147175,0.0000029345208,0.9989569,0.000006916176,0.0000028144573,0.000024915491,0.0003852846,0.00009223248,0.00006055299,0.0000052100645,0.00045980915,0.0000010859021],"about_ca_topic_score_codex":0.45826977,"about_ca_topic_score_gemma":0.81310767,"teacher_disagreement_score":0.45826977,"about_ca_system_score_codex":0.0018437075,"about_ca_system_score_gemma":0.00077054574,"threshold_uncertainty_score":0.9112047},"labels":[],"label_agreement":null},{"id":"W2203477797","doi":"10.1017/s0016756815000552","title":"Palynofloral patterns of terrestrial ecosystem change during the end-Triassic event – a review","year":2015,"lang":"en","type":"review","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":"Macrofossil; Extinction event; Geology; Arctic; Terrestrial ecosystem; Ecology; Structural basin; Extinction (optical mineralogy); Biological dispersal; Ecosystem; Oceanography; Paleontology; Population; Holocene; Biology","score_opus":0.0948649039214319,"score_gpt":0.3044466952998876,"score_spread":0.2095817913784557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2203477797","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":[0.00083495176,0.99855644,0.000053790962,0.000112583984,0.000068790505,0.0000027219962,0.00007043592,0.0000033672584,0.00029685698],"genre_scores_gemma":[0.0037925537,0.9957072,0.000096015174,0.00008561588,0.00010241721,0.000003670812,0.00007965436,0.0000012397517,0.00013154946],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997539,0.000021548403,0.00007252534,0.0000904823,0.000046286965,0.000015302854],"domain_scores_gemma":[0.9990578,0.00045680447,0.000261729,0.000021069753,0.00016032334,0.000042238906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005080345,0.0006869291,0.00082826824,0.004392124,0.00027129918,0.0010804567,0.00066924107,0.00056639715,0.0019309656],"category_scores_gemma":[0.0013258127,0.0002832645,0.00057987194,0.0045345426,0.00041007085,0.001568486,0.00050940627,0.0005419757,0.00042258966],"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":[0.00014575777,0.00006178326,0.008271576,0.084918156,0.00047155216,0.00044721132,0.0006400865,0.00050624553,0.0013612199,0.0015152798,0.019428791,0.8822322],"study_design_scores_gemma":[0.000015483603,0.00029723332,0.07072313,0.06643652,0.0019251765,0.0058387187,0.0011143597,0.00019442555,0.000955916,0.0017629822,0.85065764,0.00007839733],"about_ca_topic_score_codex":0.0040892465,"about_ca_topic_score_gemma":0.0051199966,"teacher_disagreement_score":0.004392124,"about_ca_system_score_codex":0.00057969487,"about_ca_system_score_gemma":0.0012160977,"threshold_uncertainty_score":0.008130848},"labels":[],"label_agreement":null},{"id":"W2213096039","doi":"10.1017/s0016756815000588","title":"Ultra-shallow-marine anoxia in an Early Triassic shallow-marine clastic ramp (Spitsbergen) and the suppression of benthic radiation","year":2015,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":112,"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; Geological Survey of Canada","funders":"Research Executive Agency; Norsk Polarinstitutt; FP7 People: Marie-Curie Actions; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Paleontology; Early Triassic; Facies; Anoxic waters; Benthic zone; Clastic rock; Sedimentary rock; Seafloor spreading; Bioturbation; Oceanography; Sediment; Structural basin; Permian","score_opus":0.023749042736581148,"score_gpt":0.23642762848186477,"score_spread":0.21267858574528362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2213096039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994573,0.00003976946,0.0000137810475,0.000004273818,0.0000010699309,5.6929264e-7,0.000053143576,0.0000020270268,0.00042809607],"genre_scores_gemma":[0.99965405,0.000025602718,0.000020787884,0.000002810824,8.9200057e-7,9.08913e-7,0.00009536844,8.8308025e-7,0.00019878405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999441,0.000003158951,0.0000038136398,0.000018150167,0.00000949066,0.000021193324],"domain_scores_gemma":[0.99990356,0.0000063835055,0.00003277211,0.0000047024155,0.000013446441,0.00003905247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000094337665,0.00014820402,0.00013457982,0.0007613926,0.0003660549,0.000355701,0.00018802748,0.00015477635,0.0015046326],"category_scores_gemma":[0.00019403157,0.000107051485,0.00011060126,0.0004322712,0.0003526626,0.00016314782,0.0003567143,0.000103100945,0.0001923474],"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":[0.00016944262,0.000021891407,0.96140414,0.000026266533,0.000032862456,0.00071414176,0.001028319,0.0001666571,0.028620932,0.00016749252,0.00012024221,0.007527753],"study_design_scores_gemma":[7.1347824e-7,0.000017691027,0.99926835,0.0000017022261,0.0000029094438,0.00008578846,0.0001646338,0.000038462298,0.00025724797,0.000017021619,0.0001447993,6.61439e-7],"about_ca_topic_score_codex":0.014338768,"about_ca_topic_score_gemma":0.04309848,"teacher_disagreement_score":0.014338768,"about_ca_system_score_codex":0.00048783363,"about_ca_system_score_gemma":0.00028736924,"threshold_uncertainty_score":0.02851063},"labels":[],"label_agreement":null},{"id":"W2215140130","doi":"10.1017/s0016756815000746","title":"<i>Melvillipteris quadriseriata</i>gen. et sp. nov., a new plant assigned to Rhacophytales from the Upper Devonian (Famennian) of Arctic Canada","year":2015,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological 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":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Appendage; Sporangium; Devonian; Biology; Paleontology; Whorl (mollusc)","score_opus":0.029329343189461444,"score_gpt":0.19490590529344648,"score_spread":0.16557656210398503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2215140130","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9696425,0.003412199,0.0027192542,0.00034315718,0.00013490295,0.00016724097,0.0028214555,0.00018897626,0.020570332],"genre_scores_gemma":[0.9840528,0.0013512444,0.0045343284,0.00026910056,0.00004297581,0.000030118681,0.004046989,0.000028113245,0.0056443703],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998746,0.0000065849563,0.00001054453,0.00004381721,0.00003201675,0.000032432145],"domain_scores_gemma":[0.9998275,0.000017672286,0.000032190208,0.000015728057,0.00006075269,0.00004612671],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000135031,0.00040796533,0.00028556204,0.0010481047,0.0016225993,0.0007792447,0.0005300208,0.0003742281,0.0011669185],"category_scores_gemma":[0.00014551125,0.00011458998,0.00019259185,0.000817752,0.00047150187,0.00032970766,0.000420369,0.00048071338,0.0005426484],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082197646,0.00017760381,0.23322168,0.0007437906,0.00013997927,0.008172153,0.007039288,0.0014398118,0.42925203,0.001049239,0.003932865,0.31400958],"study_design_scores_gemma":[0.00002948686,0.00021350417,0.8755229,0.0001220006,0.00011379376,0.005727815,0.0034768048,0.0008251601,0.00598443,0.00016506098,0.10776604,0.00005308977],"about_ca_topic_score_codex":0.25599095,"about_ca_topic_score_gemma":0.51089984,"teacher_disagreement_score":0.744009,"about_ca_system_score_codex":0.0018029518,"about_ca_system_score_gemma":0.0013008423,"threshold_uncertainty_score":0.50900185},"labels":[],"label_agreement":null},{"id":"W2228520680","doi":"10.1017/s0016756815000990","title":"The Chondritic Moon: a solution to the <sup>142</sup>Nd conundrum and implications for terrestrial mantle evolution","year":2016,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","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":"McMaster University","funders":"","keywords":"Chondrite; Enstatite; Geology; Mantle (geology); Meteorite; Astrobiology; Geochemistry; Crust; Physics","score_opus":0.01802411735686705,"score_gpt":0.21976876366766865,"score_spread":0.2017446463108016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2228520680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4331202,0.31717643,0.034784444,0.14887206,0.0030652129,0.000046449455,0.0004889177,0.00060806534,0.061838243],"genre_scores_gemma":[0.9095584,0.04949952,0.007770862,0.008334084,0.0028248318,0.000022890674,0.0002818762,0.000118972945,0.021588523],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9998448,0.000026304828,0.000014462324,0.000042055643,0.000040217932,0.000032190273],"domain_scores_gemma":[0.9995308,0.00012461538,0.000082572355,0.000037994963,0.00014454548,0.00007950627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011091147,0.00039719,0.00040514892,0.00074917835,0.0006743701,0.002240122,0.0009272772,0.0017462922,0.0033669376],"category_scores_gemma":[0.00070994167,0.0002083089,0.00022986784,0.00054947997,0.0035188708,0.002718492,0.0013726393,0.0013145794,0.0007308438],"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":[0.000764366,0.00010805931,0.054959208,0.0023867642,0.00013265232,0.008801705,0.0031981776,0.0017858163,0.18687364,0.21917206,0.024081882,0.4977358],"study_design_scores_gemma":[0.000039656818,0.00055192603,0.08234902,0.00067681225,0.00012066737,0.01052269,0.008066209,0.004260551,0.042593215,0.27562493,0.57504725,0.0001470455],"about_ca_topic_score_codex":0.0010292169,"about_ca_topic_score_gemma":0.0015350006,"teacher_disagreement_score":0.0033669376,"about_ca_system_score_codex":0.000833683,"about_ca_system_score_gemma":0.00058861525,"threshold_uncertainty_score":0.011263549},"labels":[],"label_agreement":null},{"id":"W2263574146","doi":"10.1017/s0016756815001120","title":"Emplacement age and isotopic composition of the Prairie Lake carbonatite complex, Northwestern Ontario, Canada","year":2016,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Lakehead University","funders":"","keywords":"Carbonatite; Magmatism; Baddeleyite; Geochemistry; Geology; Rift; Mantle (geology); Mantle plume; Magma; Zircon; Paleontology; Lithosphere; Tectonics; Volcano","score_opus":0.013450186384515882,"score_gpt":0.18124345972695613,"score_spread":0.16779327334244024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2263574146","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879624,0.00077852077,0.00015167655,0.00016702426,0.000007917039,0.000028283328,0.003935729,0.000025661286,0.006942961],"genre_scores_gemma":[0.9899025,0.00038659267,0.0003978964,0.000033222845,0.0000032433045,0.000013087206,0.0015242298,0.000009958501,0.0077293613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997241,0.000006801286,0.000010999946,0.000059496742,0.0001382647,0.000060438815],"domain_scores_gemma":[0.99899095,0.00002252606,0.00010096567,0.000017133014,0.0007381127,0.00013031508],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018018359,0.00020562121,0.00015030059,0.0021156017,0.0024948926,0.00075080997,0.00062189257,0.00022921171,0.0022629523],"category_scores_gemma":[0.00041207566,0.00019568029,0.00012624216,0.0024891687,0.0004682446,0.00021712726,0.00034977772,0.00018665615,0.00030943],"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":[0.00016678552,0.000029801955,0.9538493,0.00012183591,0.00008302262,0.00032667603,0.0037113589,0.00033953742,0.017235868,0.00036831194,0.0030052129,0.02076236],"study_design_scores_gemma":[0.000003153505,0.0000053389476,0.99459594,0.0000076844635,0.000007114935,0.000038647446,0.00064235466,0.00011002202,0.00040093448,0.000009735988,0.0041747503,0.0000043330806],"about_ca_topic_score_codex":0.9922007,"about_ca_topic_score_gemma":0.998162,"teacher_disagreement_score":0.018599464,"about_ca_system_score_codex":0.018599464,"about_ca_system_score_gemma":0.010162638,"threshold_uncertainty_score":0.1349492},"labels":[],"label_agreement":null},{"id":"W2279123631","doi":"10.1017/s0016756815000874","title":"Testing a back-arc ‘aulacogen’ model for the Central Metasedimentary Belt of the Grenville Province","year":2015,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"McMaster University","funders":"","keywords":"Geology; Rift; Batholith; Crust; Pluton; Basement; Geochemistry; Geophysics; Seismology; Tectonics; Geography","score_opus":0.052818667274749626,"score_gpt":0.21581025615148158,"score_spread":0.16299158887673196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2279123631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99100995,0.00005688801,0.0025530267,0.00017467163,0.000013579067,0.00005763906,0.0003715817,0.00012213342,0.005640455],"genre_scores_gemma":[0.99757296,0.000016705282,0.0013389402,0.000042702723,0.0000031519562,0.000010278957,0.00038776844,0.000042786163,0.0005846065],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988826,0.00032077497,0.000053713884,0.00038198908,0.00019848597,0.00016248335],"domain_scores_gemma":[0.99846905,0.0004588981,0.00024890824,0.00022176624,0.00044298233,0.0001584035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013999589,0.0004897154,0.00035576272,0.0010899974,0.0006591455,0.0023415133,0.0019567227,0.00070953346,0.0040713362],"category_scores_gemma":[0.003830596,0.00034492108,0.00076880195,0.00058402197,0.0007989925,0.0007971784,0.0008735067,0.00035216688,0.0007643255],"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":[0.0013521292,0.00032712962,0.8290529,0.00012231158,0.0005392028,0.00078439224,0.0010294537,0.118203044,0.01966281,0.004941557,0.000935503,0.023049569],"study_design_scores_gemma":[0.00034191308,0.00052563014,0.3905746,0.00006199612,0.00020250985,0.00030131036,0.0021679238,0.58926886,0.0077043553,0.0021642074,0.006610615,0.00007597793],"about_ca_topic_score_codex":0.3389611,"about_ca_topic_score_gemma":0.2506785,"teacher_disagreement_score":0.3389611,"about_ca_system_score_codex":0.0059164623,"about_ca_system_score_gemma":0.0022296868,"threshold_uncertainty_score":0.67397624},"labels":[],"label_agreement":null},{"id":"W2281805343","doi":"10.1017/s0016756815000448","title":"U–Pb geochronology of the Eocene Kærven intrusive complex, East Greenland: constraints on the Iceland hotspot track during the rift-to-drift transition","year":2015,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geochronology; Geology; Rift; Hotspot (geology); Paleontology; Seismology; Tectonics","score_opus":0.02842564511421502,"score_gpt":0.2064594000313492,"score_spread":0.17803375491713416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2281805343","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99813217,0.000093442846,0.00003791782,0.000010316458,0.0000015975967,0.0000031101843,0.00022090526,0.00000694298,0.001493614],"genre_scores_gemma":[0.9986148,0.00005854423,0.00008253705,0.000009004578,0.0000015177498,0.0000025568092,0.0004717452,0.0000070411666,0.0007522689],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998882,0.000007140641,0.000008358771,0.00003741161,0.000024426967,0.000034415298],"domain_scores_gemma":[0.99986386,0.000013084,0.00003967061,0.0000095812275,0.000047791324,0.000025913363],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021357188,0.00025139307,0.0001624406,0.0009445817,0.00044794244,0.0007381063,0.00029655025,0.00023248127,0.0010831212],"category_scores_gemma":[0.00023029232,0.00018046987,0.00011292491,0.0006842584,0.0004209898,0.00030193877,0.00057927374,0.0001176032,0.00024015398],"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":[0.00025286648,0.00003240888,0.9512012,0.00004839739,0.00006467737,0.0003884395,0.001965847,0.0011429489,0.02777477,0.0003431959,0.0004889061,0.016296327],"study_design_scores_gemma":[0.000001596555,0.0000071338686,0.9985474,0.0000054073125,0.0000037552788,0.000022931326,0.00018943043,0.00018460989,0.00041571527,0.0000073308156,0.0006134661,0.0000012236217],"about_ca_topic_score_codex":0.13703296,"about_ca_topic_score_gemma":0.36665517,"teacher_disagreement_score":0.13703296,"about_ca_system_score_codex":0.0016869763,"about_ca_system_score_gemma":0.00048576292,"threshold_uncertainty_score":0.27247065},"labels":[],"label_agreement":null},{"id":"W2317648447","doi":"10.1017/s0016756813000125","title":"A Middle Jurassic (Bajocian) ophthalmosaurid (Reptilia, Ichthyosauria) from the Tuxedni Formation, Alaska and the early diversification of the clade","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Evolutionary Biology","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":"Natural Sciences and Engineering Research Council of Canada; Alexander von Humboldt-Stiftung","keywords":"Paleontology; Geology; Cretaceous; Ammonoidea; Cenomanian; Terrane; Extinction event; Mesozoic; Clade; Biological dispersal; Tectonics; Biology; Phylogenetics; Structural basin","score_opus":0.018073675220109026,"score_gpt":0.18441906311378048,"score_spread":0.16634538789367145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317648447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99681705,0.00044903776,0.00011919453,0.000020467198,0.000010691688,0.0000050033145,0.00011834061,0.0000057421407,0.002454571],"genre_scores_gemma":[0.99833184,0.00032910134,0.00030078026,0.0000132337,0.0000074360523,0.000005093513,0.0002361948,0.0000028783265,0.00077362393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999145,0.000007622796,0.000010166118,0.000028105016,0.000023249091,0.000016348844],"domain_scores_gemma":[0.9998227,0.00002106695,0.000062237596,0.000014566315,0.00004409175,0.00003537578],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017018076,0.00017081821,0.00013038468,0.0015143004,0.0013382796,0.0008545109,0.0002012076,0.00023450668,0.0026365924],"category_scores_gemma":[0.00034111858,0.0001228175,0.00009980518,0.0010311145,0.00065220834,0.00026379808,0.0007320927,0.00023773135,0.00030067598],"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":[0.00022626239,0.000049574675,0.8743966,0.00018485427,0.000059080612,0.0021672314,0.01345354,0.0002484011,0.060224824,0.0004686855,0.00033669363,0.048184257],"study_design_scores_gemma":[0.0000018283862,0.000024637024,0.99379504,0.000036735466,0.000015169718,0.0005711623,0.0021599992,0.00004717161,0.0005666656,0.000040381663,0.0027376916,0.000003457459],"about_ca_topic_score_codex":0.031172575,"about_ca_topic_score_gemma":0.086311355,"teacher_disagreement_score":0.031172575,"about_ca_system_score_codex":0.0005660054,"about_ca_system_score_gemma":0.00046726392,"threshold_uncertainty_score":0.061982274},"labels":[],"label_agreement":null},{"id":"W2320024490","doi":"10.1017/s0016756815000114","title":"Nd isotope mapping of the Allochthon Boundary Thrust on the shores of Georgian Bay, Ontario: significance for Grenvillian crustal structure and evolution","year":2015,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"McMaster University","funders":"","keywords":"Geology; Allochthon; Gneiss; Outcrop; Orogeny; Eclogite; Paleontology; Tectonics; Crust; Geochemistry; Seismology; Nappe; Subduction; Metamorphic rock","score_opus":0.02369920048451422,"score_gpt":0.19817464321241948,"score_spread":0.17447544272790527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2320024490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935842,0.00021480805,0.0002431549,0.000071693255,0.0000035090588,0.000008762692,0.0007123251,0.000018840397,0.0051425723],"genre_scores_gemma":[0.99682164,0.0001295464,0.0005201639,0.000019240944,0.0000012873256,0.000004428321,0.00043079487,0.0000072974476,0.00206546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994314,0.0000024751066,0.0000022495108,0.000017798247,0.000022629001,0.000011683835],"domain_scores_gemma":[0.9998528,0.000008088497,0.000026746407,0.0000064592373,0.00007969049,0.000026214806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000085157655,0.00016833111,0.0000948911,0.00062111986,0.00078296824,0.00053441746,0.00025299785,0.00014925403,0.0010072126],"category_scores_gemma":[0.00019375815,0.000117808275,0.00011509416,0.00058263255,0.00034288477,0.00011831295,0.00036250934,0.00011497876,0.00024160545],"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":[0.00008692858,0.0000069536586,0.9351103,0.000063120715,0.00003054782,0.00018758727,0.0016776621,0.00041063526,0.047971297,0.00013310711,0.00043677745,0.013885029],"study_design_scores_gemma":[0.0000017729427,0.0000072562716,0.99738234,0.000006338063,0.0000055851333,0.00002552827,0.00042341507,0.00019338999,0.0007389235,0.000012080963,0.0012009599,0.0000023474643],"about_ca_topic_score_codex":0.86946726,"about_ca_topic_score_gemma":0.97501624,"teacher_disagreement_score":0.13053274,"about_ca_system_score_codex":0.004369033,"about_ca_system_score_gemma":0.0026623153,"threshold_uncertainty_score":0.26260293},"labels":[],"label_agreement":null},{"id":"W2322914709","doi":"10.1017/s001675681400079x","title":"Late Cambrian (middle Furongian) shallow-marine dysoxic mudstone with calcrete and brachiopod–olenid–<i>Lotagnostus</i>faunas in Avalonian Cape Breton Island, Nova Scotia","year":2015,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":"","keywords":"Trilobite; Baltica; Geology; Conglomerate; Paleontology; Marine transgression; Laurentia; Subaerial; Macrofossil; Ordovician; Sedimentary rock; Holocene","score_opus":0.022012061390404812,"score_gpt":0.21336963431580583,"score_spread":0.191357572925401,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2322914709","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979526,0.000203236,0.000020487014,0.000028914916,0.0000032926666,0.0000124475055,0.00033817635,0.0000042544166,0.0014364889],"genre_scores_gemma":[0.9985007,0.00014357005,0.000062685045,0.000025186575,0.0000025575703,0.0000065680615,0.00033102976,0.0000014092411,0.00092628185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994123,0.000003765272,0.000005028889,0.000015838408,0.00001402436,0.00002006029],"domain_scores_gemma":[0.99973446,0.000021401002,0.00006930407,0.000010392434,0.00007865098,0.00008577407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000108491346,0.00016720877,0.00010886909,0.0009958782,0.0006166297,0.00040113082,0.0002104203,0.00014154233,0.001886787],"category_scores_gemma":[0.0002626154,0.00013621637,0.000080820995,0.0007528741,0.0005173479,0.00014983983,0.00030452156,0.00012802577,0.0002427806],"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":[0.00007523331,0.0000164284,0.97886014,0.00008011027,0.000029511366,0.0006663907,0.0019344277,0.000112509966,0.009278582,0.00009673728,0.00047492926,0.008375],"study_design_scores_gemma":[0.000002296183,0.0000059655717,0.9990736,0.000008018725,0.0000016524061,0.000043413853,0.00032953155,0.000022579781,0.000046021298,0.0000037244185,0.00046234348,7.480245e-7],"about_ca_topic_score_codex":0.6605976,"about_ca_topic_score_gemma":0.89128387,"teacher_disagreement_score":0.33940238,"about_ca_system_score_codex":0.0020059883,"about_ca_system_score_gemma":0.001246851,"threshold_uncertainty_score":0.6828023},"labels":[],"label_agreement":null},{"id":"W2323729515","doi":"10.1017/s0016756813000228","title":"Reconstructing the Avalonia palaeocontinent in the Cambrian: A 519 Ma caliche in South Wales and transcontinental middle Terreneuvian sandstones","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":34,"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":"Geology; Paleozoic; Paleontology; Bay; Sedimentary depositional environment; Craton; Structural basin; Marine transgression; Oceanography; Tectonics","score_opus":0.02214570319766697,"score_gpt":0.2038288879077761,"score_spread":0.18168318471010914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2323729515","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951827,0.00018824467,0.00011132523,0.00007659506,0.0000046531813,0.000011672777,0.00015233431,0.0000079321635,0.0042645927],"genre_scores_gemma":[0.9989599,0.00006460221,0.00011063932,0.000015178046,0.0000025760423,0.000004224425,0.00013793416,0.0000047667927,0.00070018583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989974,0.000011822028,0.0000069781568,0.000025079009,0.000024637202,0.000031670836],"domain_scores_gemma":[0.999806,0.000030003128,0.000036548834,0.000018409904,0.000073239,0.000035807818],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028296246,0.0001946427,0.00018363043,0.0021500846,0.00091309246,0.0010402452,0.000425183,0.00051270024,0.0029702643],"category_scores_gemma":[0.0006930177,0.00023831552,0.00022657646,0.0014225107,0.00069473474,0.00035822074,0.0010702565,0.0002880237,0.0005715003],"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":[0.00021429227,0.000056564953,0.93316805,0.00012168528,0.00008500164,0.0021565736,0.007058116,0.0018388936,0.02120182,0.0015927879,0.0008679582,0.03163831],"study_design_scores_gemma":[0.0000040834957,0.000011441213,0.9960452,0.000021697244,0.000006399292,0.00009635309,0.0011209366,0.000693156,0.00017774838,0.00007869812,0.0017401129,0.00000423203],"about_ca_topic_score_codex":0.20954233,"about_ca_topic_score_gemma":0.41241166,"teacher_disagreement_score":0.20954233,"about_ca_system_score_codex":0.002200606,"about_ca_system_score_gemma":0.0008039116,"threshold_uncertainty_score":0.41664535},"labels":[],"label_agreement":null},{"id":"W2332187196","doi":"10.1017/s0016756813000538","title":"Geochronology, geochemistry and petrogenesis of the late Palaeoproterozoic A-type granites from the Dunhuang block, SE Tarim Craton, China: implications for the break-up of the Columbia supercontinent","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":54,"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":"Zircon; Geology; Craton; Geochemistry; Petrogenesis; Supercontinent; Geochronology; Amphibole; Mantle (geology); Petrology; Tectonics; Quartz; Paleontology","score_opus":0.01157491906534208,"score_gpt":0.19209191988367053,"score_spread":0.18051700081832844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2332187196","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994087,0.00004289463,0.000029147977,0.00000480852,4.913018e-7,0.0000038782696,0.00006393555,0.000003569846,0.0004426212],"genre_scores_gemma":[0.9995054,0.00003557217,0.000075964126,0.0000022518354,5.293378e-7,0.0000027470735,0.0000859887,0.0000019928002,0.00028967217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999546,0.0000016390783,0.0000034659533,0.0000140709,0.000013151995,0.000013115096],"domain_scores_gemma":[0.99988186,0.0000083264795,0.000031102172,0.000009349864,0.00004255771,0.00002683838],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008575007,0.00026332116,0.00013221535,0.0016453962,0.0007940022,0.00057813304,0.00024223168,0.000157963,0.0007950724],"category_scores_gemma":[0.00016527381,0.0001744342,0.00015060372,0.001083564,0.0005190282,0.00010708191,0.0003839691,0.00015207652,0.00010709436],"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":[0.000302526,0.000028577986,0.8580887,0.000060468396,0.000045539546,0.0006235617,0.0014798328,0.0004950241,0.12712148,0.00020415343,0.00007046458,0.011479636],"study_design_scores_gemma":[0.0000033764748,0.000013208193,0.99813664,0.0000026325167,0.000004863199,0.00007057471,0.0002501504,0.00012832615,0.0011429528,0.00000867217,0.00023669696,0.0000019819288],"about_ca_topic_score_codex":0.16163698,"about_ca_topic_score_gemma":0.28548157,"teacher_disagreement_score":0.16163698,"about_ca_system_score_codex":0.0012297794,"about_ca_system_score_gemma":0.0007625089,"threshold_uncertainty_score":0.3213923},"labels":[],"label_agreement":null},{"id":"W2333945315","doi":"10.1017/s001675681300071x","title":"Late Visean – early Serpukhovian conodont succession at the Naqing (Nashui) section in Guizhou, South China","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":"Geological Survey of Canada","funders":"","keywords":"Conodont; Viséan; Geology; Paleontology; Section (typography); Ecological succession; Biostratigraphy; Global Boundary Stratotype Section and Point; Stratotype; Carboniferous; Stage (stratigraphy); Structural basin; Biology; Ecology","score_opus":0.011508373283076651,"score_gpt":0.20423306493652885,"score_spread":0.19272469165345218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2333945315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996,0.000051203966,0.000030462414,0.000007150841,5.068987e-7,0.0000016268984,0.00004205774,0.0000022700992,0.00026474902],"genre_scores_gemma":[0.99964654,0.000028989145,0.00005725396,0.000002455749,4.8457383e-7,0.0000021059693,0.00006803519,7.768136e-7,0.00019342404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999114,0.000009833858,0.000008085271,0.000029050274,0.000018124181,0.000023516073],"domain_scores_gemma":[0.9998677,0.000017766752,0.000039380888,0.0000079085885,0.000032098673,0.0000352027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000213324,0.00018078747,0.0001606066,0.0014999034,0.0006964228,0.00035015258,0.00023687679,0.00013004335,0.0007849023],"category_scores_gemma":[0.00022707628,0.00012987049,0.00013101505,0.0010772111,0.00041693187,0.00018713016,0.0004000779,0.0000739026,0.000045709865],"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":[0.000067793655,0.000010212546,0.97142655,0.000040415365,0.00003436841,0.00037841743,0.0020823204,0.00029806237,0.013576466,0.00024323985,0.000079316895,0.011762805],"study_design_scores_gemma":[0.0000011798622,0.000007783113,0.99914145,0.000002167745,0.0000037622744,0.000042206157,0.000288443,0.00012220284,0.00014767941,0.000014071249,0.00022740339,0.0000016833155],"about_ca_topic_score_codex":0.10847705,"about_ca_topic_score_gemma":0.27592832,"teacher_disagreement_score":0.10847705,"about_ca_system_score_codex":0.0012419974,"about_ca_system_score_gemma":0.0008610061,"threshold_uncertainty_score":0.21569133},"labels":[],"label_agreement":null},{"id":"W2343195526","doi":"10.1017/s0016756816000224","title":"Acritarchs from the Hanford Brook Formation, New Brunswick, Canada: new biochronological constraints on the<i>Protolenus elegans</i>Zone and the Cambrian Series 2–3 transition","year":2016,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Acadia University","funders":"","keywords":"Acritarch; Paleontology; Geology","score_opus":0.013421519966823087,"score_gpt":0.18280401822840567,"score_spread":0.16938249826158258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2343195526","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99103457,0.00071724737,0.00015381444,0.00007650273,0.0000075210755,0.00003059571,0.00065036403,0.00001224388,0.00731721],"genre_scores_gemma":[0.99689627,0.0002926985,0.00044074998,0.000056374873,0.000003882109,0.00001374946,0.000584096,0.000008667211,0.0017034287],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972326,0.000013083807,0.0000149263815,0.00006930151,0.00008803682,0.00009139149],"domain_scores_gemma":[0.99945265,0.000034604345,0.00009147635,0.000027706243,0.00031109122,0.00008241933],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028205503,0.0002905836,0.00024035877,0.002747532,0.0024923056,0.0015153021,0.00068799406,0.0002744709,0.0029981935],"category_scores_gemma":[0.00044051427,0.00027277987,0.00013991517,0.0025160785,0.001121981,0.00036209854,0.00091615255,0.00041962328,0.0003850229],"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":[0.0001208553,0.000029002918,0.9380822,0.00012584952,0.000043666485,0.00068636914,0.007989914,0.00029355,0.027982743,0.00055336946,0.00092556677,0.023166876],"study_design_scores_gemma":[0.0000026575246,0.000009672328,0.9935003,0.000026252927,0.000005971367,0.00007679092,0.0024132582,0.00009826158,0.0003774616,0.00002992137,0.0034530747,0.0000063480607],"about_ca_topic_score_codex":0.93781734,"about_ca_topic_score_gemma":0.9906488,"teacher_disagreement_score":0.062182665,"about_ca_system_score_codex":0.009319927,"about_ca_system_score_gemma":0.00551559,"threshold_uncertainty_score":0.12509769},"labels":[],"label_agreement":null},{"id":"W2354628995","doi":"10.1017/s0016756816000236","title":"Rediagnosis and redescription of <i>Mosasaurus hoffmannii</i> (Squamata: Mosasauridae) and an assessment of species assigned to the genus <i>Mosasaurus</i>","year":2016,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Evolutionary Biology","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":"University of Alberta","funders":"","keywords":"Anatomy; Quadrate bone; Biology; Holotype; Type species; Genus; Rostrum; Premaxilla; Taxonomy (biology); Squamata; Arthropod mouthparts; Zoology; Maxilla","score_opus":0.022414711383847652,"score_gpt":0.25781111982343335,"score_spread":0.2353964084395857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2354628995","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95436686,0.0038879714,0.0040947963,0.00036492918,0.00040158234,0.00015654814,0.00040035753,0.00017279931,0.036154065],"genre_scores_gemma":[0.9911691,0.0009632908,0.0047669574,0.00019554637,0.000090388996,0.00004087207,0.00038378136,0.000015557946,0.0023746304],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9998555,0.000032571126,0.00003012449,0.000030803567,0.000038984657,0.000011942001],"domain_scores_gemma":[0.99983275,0.000021701851,0.00006309125,0.000020701793,0.0000429893,0.000018706418],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038739396,0.00032275572,0.00016748067,0.0013184851,0.00087741436,0.00044353734,0.000625162,0.00044226655,0.0026451177],"category_scores_gemma":[0.00037463667,0.00015638773,0.00027474447,0.00060222065,0.0015784686,0.0005570586,0.0008699194,0.0004487855,0.0007980065],"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":[0.00069161487,0.00019598352,0.3058229,0.0019273697,0.00025567238,0.009297342,0.023997875,0.001115342,0.15744261,0.0112819,0.0052113384,0.48275995],"study_design_scores_gemma":[0.000033665245,0.0011574018,0.8459215,0.00086535723,0.00020784047,0.023604272,0.009679904,0.0015657265,0.009331542,0.0019443178,0.10560252,0.00008599116],"about_ca_topic_score_codex":0.0029615401,"about_ca_topic_score_gemma":0.006901292,"teacher_disagreement_score":0.0029615401,"about_ca_system_score_codex":0.00033550232,"about_ca_system_score_gemma":0.00040144584,"threshold_uncertainty_score":0.008848786},"labels":[],"label_agreement":null},{"id":"W2367689278","doi":"10.1017/s001675681600025x","title":"Lateral accretion of modern unvegetated rivers: remotely sensed fluvial–aeolian morphodynamics and perspectives on the Precambrian rock record","year":2016,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological formations and processes","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":true,"ca_institutions":"Laurentian University","funders":"","keywords":"Fluvial; Geology; Sinuosity; Aeolian processes; Beach morphodynamics; Point bar; Geomorphology; Paleontology; Sediment transport; Sediment","score_opus":0.022163096561395913,"score_gpt":0.20447145029180805,"score_spread":0.18230835373041213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2367689278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988456,0.0001953631,0.000036467092,0.000012367137,8.0644634e-7,0.0000015342913,0.0002492102,0.0000038250278,0.00065480237],"genre_scores_gemma":[0.9995735,0.00007626977,0.00008860256,0.0000024719466,0.0000022166798,0.000001698879,0.00018312995,0.000001839105,0.00007022997],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992526,0.000010643268,0.000009223674,0.000027786227,0.000011462377,0.000015746466],"domain_scores_gemma":[0.999764,0.000037335725,0.00010864294,0.000030812153,0.000041926545,0.000017173832],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019544423,0.00013618026,0.00017139643,0.0015133562,0.00023804346,0.0004725235,0.00018095665,0.00016213731,0.0012213035],"category_scores_gemma":[0.0005949668,0.00012295131,0.00013116682,0.0011029788,0.00042658712,0.00029101636,0.00039039968,0.00012963788,0.00015916092],"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":[0.000078268895,0.000010082175,0.97909045,0.000057050165,0.000049473903,0.0001364452,0.0016409879,0.00023487244,0.0048924433,0.0001549513,0.00009759989,0.013557351],"study_design_scores_gemma":[5.076656e-7,0.0000031284683,0.9995765,0.000004330845,0.0000026179946,0.000035469617,0.000103468235,0.000064999826,0.00003610196,0.0000065163154,0.00016536306,0.0000010569537],"about_ca_topic_score_codex":0.023223612,"about_ca_topic_score_gemma":0.05200344,"teacher_disagreement_score":0.023223612,"about_ca_system_score_codex":0.00031756752,"about_ca_system_score_gemma":0.00009032723,"threshold_uncertainty_score":0.04617685},"labels":[],"label_agreement":null},{"id":"W2464531492","doi":"10.1017/s0016756816000455","title":"The first ophthalmosaurid ichthyosaur from the Upper Jurassic of the Umbrian–Marchean Apennines (Marche, Central Italy)","year":2016,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Evolutionary Biology","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":"University of Alberta","funders":"","keywords":"Paleontology; Geology; Humerus; Biological dispersal; Taxon","score_opus":0.014676350946813004,"score_gpt":0.20352527041164492,"score_spread":0.18884891946483193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2464531492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99474156,0.0008021523,0.00021433632,0.00006735919,0.000026606534,0.000031189425,0.00017009265,0.000021919399,0.0039249],"genre_scores_gemma":[0.99736327,0.00041372367,0.0005803371,0.000053324802,0.000036395446,0.000020544569,0.00027993193,0.0000066785396,0.001245749],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997706,0.000023022169,0.00002199545,0.00007915422,0.000048695045,0.00005641204],"domain_scores_gemma":[0.99982953,0.000017488534,0.00005932454,0.000026616677,0.000026486117,0.00004055974],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017704656,0.0007040489,0.00044678999,0.0018303894,0.0014757673,0.0007843329,0.000510681,0.00060686294,0.002772985],"category_scores_gemma":[0.0005329207,0.00026603034,0.00035365194,0.0011947408,0.0015090556,0.0003868225,0.0020325496,0.00043392074,0.0005388144],"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":[0.0009252853,0.0001205917,0.7295532,0.0004652169,0.00030132735,0.016450766,0.01986747,0.00032559605,0.07716372,0.0006176824,0.0015139624,0.15269516],"study_design_scores_gemma":[0.000013059461,0.00022215876,0.9805767,0.000058280697,0.000050598795,0.004932139,0.0015202559,0.00010073689,0.00066857965,0.00008586141,0.011756061,0.000015749427],"about_ca_topic_score_codex":0.010868397,"about_ca_topic_score_gemma":0.024581145,"teacher_disagreement_score":0.010868397,"about_ca_system_score_codex":0.0005701388,"about_ca_system_score_gemma":0.00041508288,"threshold_uncertainty_score":0.02161026},"labels":[],"label_agreement":null},{"id":"W2466821217","doi":"10.1017/s0016756816000376","title":"U–Pb geochronology of bentonites from the Upper Cretaceous Kanguk Formation, Sverdrup Basin, Arctic Canada: constraints on sedimentation rates, biostratigraphic correlations and the late magmatic history of the High Arctic Large Igneous Province","year":2016,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":37,"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; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochronology; Cretaceous; Arctic; Cenomanian; Paleontology; Sverdrup; Zircon; Volcanic ash; Volcano; Geochemistry; Oceanography","score_opus":0.009407643212429958,"score_gpt":0.17378794033999873,"score_spread":0.16438029712756877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2466821217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99822336,0.00011819876,0.00009256051,0.0000060847074,0.0000011345694,0.000002815514,0.00057040626,0.000012337012,0.00097306824],"genre_scores_gemma":[0.9979102,0.000091197995,0.00023204094,0.000003290207,6.5710947e-7,0.00000285017,0.00091368594,0.000007706394,0.000838299],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999175,0.0000034171198,0.0000061832047,0.000024049747,0.000024163153,0.000024667075],"domain_scores_gemma":[0.9998548,0.000009344139,0.00001996664,0.00000863918,0.0000829266,0.000024239394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013520622,0.00021705565,0.00014476392,0.0014398942,0.00076235016,0.00064992736,0.00026125758,0.00012071823,0.0007726258],"category_scores_gemma":[0.00025458154,0.00020589116,0.00016795995,0.0012451689,0.00027352732,0.00016007532,0.000356996,0.00010049172,0.00016091057],"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":[0.0001683438,0.000013128476,0.9430256,0.000050763843,0.00006875714,0.00021079551,0.0022702543,0.0008736594,0.03198167,0.00022303888,0.00023217734,0.020881882],"study_design_scores_gemma":[0.0000012863538,0.0000063088355,0.9981698,0.000004444607,0.0000076990755,0.000029280436,0.00022394845,0.00019808195,0.0007630476,0.0000073292877,0.0005867788,0.0000020630368],"about_ca_topic_score_codex":0.7604331,"about_ca_topic_score_gemma":0.9112264,"teacher_disagreement_score":0.23956692,"about_ca_system_score_codex":0.0020132822,"about_ca_system_score_gemma":0.0018181733,"threshold_uncertainty_score":0.48195553},"labels":[],"label_agreement":null},{"id":"W2475360221","doi":"10.1017/s0016756816000571","title":"The agnostoid arthropod <i>Lotagnostus</i> Whitehouse, 1936 (late Cambrian; Furongian) from Avalonian Cape Breton Island (Nova Scotia, Canada) and its significance for international correlation","year":2016,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"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":"Terrane; Paleontology; Conodont; Cape; Geology; Type species; Genus; Ordovician; Nova scotia; Geography; Ecology; Oceanography; Archaeology; Biostratigraphy; Biology; Tectonics","score_opus":0.010569253847875574,"score_gpt":0.19929663975043646,"score_spread":0.18872738590256088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2475360221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928039,0.0008598373,0.00011861754,0.000079109144,0.000018408069,0.000019070938,0.0010225213,0.0000068263325,0.00507172],"genre_scores_gemma":[0.9968929,0.0002776474,0.00020732929,0.000040922656,0.000006088814,0.000010108851,0.0012499837,0.0000033381104,0.0013116209],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998229,0.000014165767,0.000010601336,0.0000482335,0.000050004368,0.000053995987],"domain_scores_gemma":[0.99942905,0.00005114265,0.00014398858,0.00003527744,0.0002448805,0.00009561806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001788901,0.00021153354,0.00014744244,0.0019189086,0.0010256105,0.00060755655,0.00042377747,0.00012503062,0.0025164962],"category_scores_gemma":[0.0004287151,0.00012352101,0.000101168516,0.0017894275,0.00078056974,0.0002627619,0.0005181293,0.00025126344,0.00031069937],"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":[0.00008884196,0.00001211565,0.96880263,0.0000627951,0.000041475272,0.00028513058,0.0026058895,0.00005932787,0.00494012,0.00015451152,0.0011496823,0.02179735],"study_design_scores_gemma":[0.0000011012835,0.0000040454092,0.9972154,0.000014859248,0.000003144058,0.000060905313,0.00067535695,0.000022710497,0.00006269972,0.000007098093,0.0019309458,0.0000017380763],"about_ca_topic_score_codex":0.7533162,"about_ca_topic_score_gemma":0.92690283,"teacher_disagreement_score":0.24668378,"about_ca_system_score_codex":0.0031770065,"about_ca_system_score_gemma":0.0020732551,"threshold_uncertainty_score":0.49627304},"labels":[],"label_agreement":null},{"id":"W2536110350","doi":"10.1017/s0016756816000704","title":"<i>Watsonella crosbyi</i>from the lower Cambrian (Terreneuvian, Stage 2) Normanville Group in South Australia","year":2016,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":"","keywords":"Paleontology; Geology; Fauna; Stage (stratigraphy); Taxon; Group (periodic table); Sinistral and dextral; Range (aeronautics); Structural basin; Ecology; Biology","score_opus":0.030004419190651593,"score_gpt":0.23299011810804102,"score_spread":0.20298569891738943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2536110350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980082,0.00012119785,0.00006027929,0.000029557637,0.0000016909776,0.000011812781,0.00011577779,0.0000037521486,0.0016477415],"genre_scores_gemma":[0.9983328,0.0000957031,0.00031991457,0.000025743628,0.0000018609926,0.000010405731,0.00024016957,0.000002211936,0.0009712913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990845,0.0000084979865,0.0000075650382,0.000024919089,0.000027293456,0.000023333756],"domain_scores_gemma":[0.9998079,0.00001700272,0.000066803324,0.000009823663,0.000054501346,0.000044123786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011394677,0.00014264879,0.00012086162,0.0014020349,0.0008765812,0.00037803632,0.00028896713,0.00020114469,0.0020878532],"category_scores_gemma":[0.00028577936,0.00013591861,0.00010162983,0.0008076706,0.0003854026,0.00029799907,0.00063926936,0.00016343166,0.00024788384],"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":[0.000109021435,0.000032766497,0.9200204,0.00013760233,0.000037912563,0.0008831011,0.008250285,0.00016260747,0.03171097,0.00015363889,0.0006824756,0.03781913],"study_design_scores_gemma":[9.078888e-7,0.000015522788,0.9977118,0.000008902425,0.0000031775103,0.00009906027,0.0007768763,0.00007112223,0.00024727674,0.000010054825,0.0010537236,0.0000015746086],"about_ca_topic_score_codex":0.2325318,"about_ca_topic_score_gemma":0.5363401,"teacher_disagreement_score":0.2325318,"about_ca_system_score_codex":0.0009248697,"about_ca_system_score_gemma":0.00063204445,"threshold_uncertainty_score":0.46235663},"labels":[],"label_agreement":null},{"id":"W2568646821","doi":"10.1017/s0016756816001126","title":"Sequence stratigraphy, basin morphology and sea-level history for the Permian Kapp Starostin Formation of Svalbard, Norway","year":2017,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":true,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"Research Executive Agency; Norsk Polarinstitutt; FP7 People: Marie-Curie Actions; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Paleontology; Permian; Marine transgression; Facies; Transgressive; Sequence stratigraphy; Sea level; Sedimentary depositional environment; Sequence (biology); Unconformity; Structural basin; Paleozoic; Oceanography","score_opus":0.07850371034356902,"score_gpt":0.2604603939175492,"score_spread":0.1819566835739802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2568646821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985671,0.00012514304,0.00006126389,0.000006586288,0.0000034299214,0.0000027318504,0.0005404481,0.0000074034256,0.00068582676],"genre_scores_gemma":[0.9983804,0.00006513837,0.00015279624,0.000004549961,0.000002201506,0.0000046934883,0.00086372165,0.000005286208,0.00052130874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987876,0.000010440387,0.0000129275795,0.000043757344,0.000020000889,0.000034108423],"domain_scores_gemma":[0.9998741,0.000019270932,0.00004166282,0.000008847699,0.000020330066,0.000035665853],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018660934,0.00017177386,0.00017606527,0.001015701,0.00034860044,0.00050772075,0.00028229796,0.00016932936,0.0014132533],"category_scores_gemma":[0.00021065435,0.0001557162,0.00023145016,0.00046048078,0.00046918285,0.0002087919,0.00044776595,0.000110779016,0.0003788229],"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":[0.00012301872,0.000029191877,0.9734832,0.00006522505,0.00007859934,0.00057630416,0.0013990168,0.000749352,0.0039001084,0.00021846687,0.0004939793,0.018883528],"study_design_scores_gemma":[0.00000219165,0.000021837774,0.9978655,0.000011544388,0.0000088319375,0.00014278038,0.00050741306,0.00022054317,0.00015867173,0.000020794036,0.0010369362,0.0000028768338],"about_ca_topic_score_codex":0.0700949,"about_ca_topic_score_gemma":0.16522847,"teacher_disagreement_score":0.0700949,"about_ca_system_score_codex":0.0006572614,"about_ca_system_score_gemma":0.0005349026,"threshold_uncertainty_score":0.13937378},"labels":[],"label_agreement":null},{"id":"W2591599990","doi":"10.1017/s0016756817000085","title":"A Tonian age for the Visingsö Group in Sweden constrained by detrital zircon dating and biochronology: implications for evolutionary events","year":2017,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":"","keywords":"Geology; Zircon; Sedimentary depositional environment; Paleontology; Group (periodic table); Radiometric dating; Range (aeronautics); Chronostratigraphy; Geochronology; Laurentia; Ordovician; Sedimentary rock; Structural basin","score_opus":0.03667466797453645,"score_gpt":0.28642797687882116,"score_spread":0.2497533089042847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2591599990","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962645,0.0003909144,0.00012766011,0.000039196337,0.000011687026,0.0000033308274,0.000083786,0.000008821174,0.003070171],"genre_scores_gemma":[0.9985178,0.00028508995,0.00024795608,0.000018543045,0.00000848646,0.000004781224,0.00019370602,0.000008027642,0.00071571366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997069,0.000024745043,0.000019610328,0.00009770328,0.00004088013,0.000110060384],"domain_scores_gemma":[0.9997174,0.000032088345,0.00009436228,0.00002017766,0.00007504321,0.00006084897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042900312,0.0005498354,0.00038750787,0.0017898951,0.0013303454,0.0018374282,0.0004856611,0.0004271822,0.0012860837],"category_scores_gemma":[0.00050804147,0.00022153466,0.00030668484,0.00094575965,0.0009369222,0.0005123009,0.0013277568,0.00027695365,0.0005549576],"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":[0.00048477217,0.000043002223,0.93402517,0.000096354546,0.000110993125,0.0009304922,0.0069092517,0.00040467203,0.015366293,0.0015114296,0.00031245142,0.039805233],"study_design_scores_gemma":[0.000011001402,0.00009392241,0.98414373,0.000059683294,0.000051655774,0.0005226959,0.007124504,0.00021270153,0.0010346201,0.00046197063,0.0062677735,0.00001573046],"about_ca_topic_score_codex":0.021855759,"about_ca_topic_score_gemma":0.043391887,"teacher_disagreement_score":0.021855759,"about_ca_system_score_codex":0.000856757,"about_ca_system_score_gemma":0.0007873012,"threshold_uncertainty_score":0.04345709},"labels":[],"label_agreement":null},{"id":"W2595597031","doi":"10.1017/s001675681700005x","title":"A revised model for the crustal structure of the SW Grenville Province, Ontario, Canada","year":2017,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"McMaster University","funders":"","keywords":"Allochthon; Geology; Nappe; Terrane; Orogeny; Tectonics; Eclogite; Paleontology; Seismology; Geochemistry; Geomorphology; Subduction","score_opus":0.014399158813228152,"score_gpt":0.18721148284679873,"score_spread":0.17281232403357058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2595597031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.542037,0.0035396535,0.15164547,0.00628276,0.0004406439,0.0005005472,0.037016265,0.0022195976,0.25631803],"genre_scores_gemma":[0.9321361,0.0009531018,0.025076384,0.00015350993,0.000024511655,0.00012930397,0.0032699432,0.00015295902,0.03810408],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998578,0.000017807815,0.000007074271,0.000046787627,0.00003562349,0.000034970537],"domain_scores_gemma":[0.9997305,0.000018611445,0.000016277263,0.000015856302,0.000183827,0.000034880857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002415541,0.0004968783,0.000259907,0.0009444939,0.001150847,0.0020165124,0.0021077883,0.0005961282,0.0089302445],"category_scores_gemma":[0.00084112416,0.00039526288,0.0004911197,0.0012000204,0.00083701103,0.00064583664,0.0005120187,0.0004740802,0.0011577846],"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":[0.000072229945,0.00003092501,0.04657971,0.00012590892,0.000106046784,0.00037057334,0.0006949258,0.8462629,0.003189755,0.052043866,0.017922916,0.03260038],"study_design_scores_gemma":[0.00010378143,0.000030515146,0.03984278,0.00013124432,0.0000729819,0.00015119043,0.0008203776,0.8584278,0.00042068175,0.01324287,0.08667546,0.000080230806],"about_ca_topic_score_codex":0.98095244,"about_ca_topic_score_gemma":0.97727406,"teacher_disagreement_score":0.019468855,"about_ca_system_score_codex":0.019468855,"about_ca_system_score_gemma":0.015673216,"threshold_uncertainty_score":0.1412571},"labels":[],"label_agreement":null},{"id":"W2606827335","doi":"10.1017/s0016756817000292","title":"Zircon U–Pb ages and Hf isotope compositions of the Chencai migmatite, central Zhejiang Province, South China: constraints on the early Palaeozoic orogeny","year":2017,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"University of Waterloo","funders":"","keywords":"Orogeny; Geology; Anatexis; Zircon; Paleozoic; Archean; Migmatite; Terrane; Geochemistry; Metamorphism; Crust; Protolith; Paleontology; Metamorphic rock; Tectonics; Gneiss; Partial melting","score_opus":0.013128654670352836,"score_gpt":0.19264573160480603,"score_spread":0.17951707693445318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2606827335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994748,0.00009214259,0.00005260486,0.00000801698,6.768416e-7,0.0000024928277,0.000099461475,0.0000031230975,0.00026669234],"genre_scores_gemma":[0.9995882,0.000042235704,0.000054357435,0.0000037018192,0.0000011035986,0.0000015245805,0.00014360092,0.0000011356809,0.0001642259],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988294,0.0000073327,0.000014561859,0.00003949274,0.00002797996,0.000027655804],"domain_scores_gemma":[0.99983895,0.000018045605,0.00005184197,0.000013029484,0.00004731253,0.000030741256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021926929,0.0003041867,0.00022510234,0.0020065783,0.00064069516,0.000531994,0.00029467407,0.00022572304,0.0004828794],"category_scores_gemma":[0.00022705442,0.00020533477,0.00019892179,0.0014207291,0.00042138025,0.00015875742,0.00034797005,0.000095323965,0.000058848906],"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":[0.0002564961,0.000013678599,0.9106914,0.00006680294,0.00007407327,0.00035184907,0.00097244856,0.00073966576,0.07632052,0.00025168454,0.00006573816,0.010195612],"study_design_scores_gemma":[0.00000486733,0.000014902596,0.9985044,0.0000023903806,0.000010202581,0.00003307374,0.00010049765,0.00023464816,0.00088857475,0.0000127398425,0.00019139994,0.0000023084135],"about_ca_topic_score_codex":0.091741025,"about_ca_topic_score_gemma":0.1644729,"teacher_disagreement_score":0.091741025,"about_ca_system_score_codex":0.0012069553,"about_ca_system_score_gemma":0.00068047363,"threshold_uncertainty_score":0.18241405},"labels":[],"label_agreement":null},{"id":"W2619164023","doi":"10.1017/s0016756817000383","title":"Deciphering the geology of some Darriwilian–Sandbian (Ordovician) ‘ghost’ formations in the UK and North America using olistoliths in marine debris flows","year":2017,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":"Conodont; Geology; Ordovician; Paleozoic; Paleontology; Sedimentary depositional environment; Dolomitization; Dolostone; Sedimentary rock; Ladinian; Biostratigraphy; Carbonate rock; Facies","score_opus":0.02936675769111582,"score_gpt":0.24637578420771605,"score_spread":0.21700902651660023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2619164023","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99911124,0.00012065529,0.00003079829,0.000011409982,0.0000012817477,0.0000020797916,0.00007497096,0.0000023544305,0.00064515485],"genre_scores_gemma":[0.99944705,0.000085357686,0.00008463207,0.000005883651,0.0000015564156,0.0000017492575,0.0001536286,0.0000017428234,0.00021842233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988806,0.00001257318,0.000011048466,0.000024842366,0.000021997972,0.00004137444],"domain_scores_gemma":[0.9997311,0.000035341858,0.00010337297,0.00002122068,0.00005585341,0.0000530363],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020818063,0.00013322652,0.0001480385,0.0022411037,0.00064802886,0.0008093224,0.00019539932,0.0001857689,0.0014526665],"category_scores_gemma":[0.0003994276,0.00017200546,0.00010477312,0.0013404984,0.00059604895,0.00039845117,0.00074685167,0.00013543888,0.00020171973],"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":[0.000036229987,0.0000071883196,0.9834509,0.000036318514,0.000016996353,0.00024592166,0.0038971326,0.000059167272,0.0031384255,0.00009529641,0.00018369354,0.008832733],"study_design_scores_gemma":[6.3505234e-7,0.000004387301,0.9980598,0.000008960932,0.000002409101,0.0000526629,0.0013194606,0.0000400503,0.00005004035,0.000006194508,0.0004544533,8.569361e-7],"about_ca_topic_score_codex":0.09592045,"about_ca_topic_score_gemma":0.33896482,"teacher_disagreement_score":0.09592045,"about_ca_system_score_codex":0.00048497273,"about_ca_system_score_gemma":0.00039985182,"threshold_uncertainty_score":0.19072425},"labels":[],"label_agreement":null},{"id":"W2791026833","doi":"10.1017/s001675681800002x","title":"Carbon-isotope stratigraphy of the uppermost Cambrian in eastern Laurentia: implications for global correlation","year":2018,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":25,"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":"","keywords":"Global Boundary Stratotype Section and Point; Excursion; Geology; Paleontology; Chemostratigraphy; Stratigraphy; Ordovician; Laurentia; Isotopes of carbon; Biostratigraphy; Isotope; Physics","score_opus":0.01973118060031185,"score_gpt":0.2464964110279192,"score_spread":0.22676523042760735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791026833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958752,0.00068943243,0.00008386275,0.00012286466,0.0000053430826,0.0000062512972,0.00051323784,0.0000109654375,0.002692921],"genre_scores_gemma":[0.99929345,0.00013835086,0.00010243341,0.000025972286,0.0000049932028,0.0000026267503,0.00021267732,0.0000026339117,0.0002167498],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998332,0.000015772655,0.0000123727095,0.000054801323,0.000024876352,0.000058923408],"domain_scores_gemma":[0.9996125,0.000048766113,0.00012412715,0.00002342552,0.00014486659,0.000046291807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029555644,0.00026566052,0.00030197736,0.0018354171,0.00049398956,0.0008924123,0.00032800584,0.00017129006,0.0010760142],"category_scores_gemma":[0.00066362397,0.00009057314,0.00018033931,0.0018178774,0.00043295723,0.0003671502,0.00045268293,0.00014356742,0.00016636144],"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":[0.000044322987,0.000010451913,0.980485,0.00006260995,0.00009093567,0.0002891115,0.0005218556,0.0004574991,0.0052157748,0.000105396924,0.00020461247,0.012512334],"study_design_scores_gemma":[7.118529e-7,0.0000032969563,0.9990784,0.000012259051,0.000006302901,0.000016365218,0.00023816623,0.00016935078,0.000095699615,0.00001053962,0.00036674834,0.000002250474],"about_ca_topic_score_codex":0.39764902,"about_ca_topic_score_gemma":0.6580305,"teacher_disagreement_score":0.39764902,"about_ca_system_score_codex":0.0024061564,"about_ca_system_score_gemma":0.0011464925,"threshold_uncertainty_score":0.7906689},"labels":[],"label_agreement":null},{"id":"W2796023638","doi":"10.1017/s0016756818000195","title":"Nd and Pb isotope mapping of crustal domains within the Makkovik Province, Labrador","year":2018,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"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 Newfoundland and Labrador; Western University; McMaster University","funders":"","keywords":"Geology; Subduction; Orogeny; Accretion (finance); Archean; Island arc; Continental crust; Continental margin; Geochemistry; Crust; Foreland basin; Earth science; Tectonics; Paleontology","score_opus":0.012807833899015622,"score_gpt":0.19611043326270647,"score_spread":0.18330259936369084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2796023638","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962819,0.00038861384,0.00019210593,0.00001323106,0.00000149885,0.0000064632513,0.00092506345,0.000028938837,0.0021621224],"genre_scores_gemma":[0.99855083,0.00006865583,0.00021900183,0.0000046418736,8.1971143e-7,0.0000039908136,0.00060074526,0.0000074479467,0.0005437057],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999149,0.0000041896637,0.0000060592474,0.000027781409,0.000016295115,0.000030733918],"domain_scores_gemma":[0.9999355,0.0000046774203,0.000023294322,0.0000055849036,0.000020455203,0.000010475389],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009996414,0.00020378303,0.00017295177,0.0018779186,0.00039474774,0.0007094364,0.00036548896,0.0001565756,0.000948296],"category_scores_gemma":[0.000128027,0.00015612104,0.00019863444,0.0011072541,0.00024996215,0.00013897536,0.00036922458,0.00010878732,0.00025101608],"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":[0.00057239056,0.000034398436,0.8225491,0.00015938473,0.00017652159,0.0006867681,0.001077907,0.0023617833,0.13077207,0.00045626663,0.00046906015,0.04068437],"study_design_scores_gemma":[0.000005660192,0.000014571337,0.9957704,0.0000129481805,0.00001580844,0.000070786584,0.00022705778,0.0003763431,0.0022824316,0.0000146219245,0.0012053228,0.000003907695],"about_ca_topic_score_codex":0.13424197,"about_ca_topic_score_gemma":0.19735208,"teacher_disagreement_score":0.86575806,"about_ca_system_score_codex":0.0011691226,"about_ca_system_score_gemma":0.00058908836,"threshold_uncertainty_score":0.26692116},"labels":[],"label_agreement":null},{"id":"W2886510746","doi":"10.1017/s0016756818000547","title":"The Kinzers Formation (Pennsylvania, USA): the most diverse assemblage of Cambrian Stage 4 radiodonts","year":2018,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","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":"Lagerstätte; Laurentia; Ordovician; Taxon; Stage (stratigraphy); Paleontology; Genus; Appendage; Biology; Ecology; Geology","score_opus":0.02360692766563411,"score_gpt":0.2362928939350545,"score_spread":0.2126859662694204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886510746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99873227,0.00012643615,0.00004291071,0.0000154132,0.0000011086936,0.0000047779204,0.000121620295,0.0000042681563,0.0009513129],"genre_scores_gemma":[0.9991567,0.00007916697,0.00017868904,0.000012004769,0.0000013745059,0.0000031971265,0.00023565459,0.000001177514,0.00033190058],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999368,0.000005754616,0.0000041423295,0.000024410409,0.000015851621,0.000013038641],"domain_scores_gemma":[0.9999062,0.00001151923,0.000032624514,0.0000064856436,0.000022506736,0.000020612159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000074550684,0.00012373156,0.00010221678,0.00060292706,0.00043908303,0.00026261614,0.00016435572,0.00011271114,0.0017275739],"category_scores_gemma":[0.00015141643,0.00008754256,0.000043893815,0.00043244945,0.00027814074,0.00028076826,0.00053128327,0.00011231622,0.00016424387],"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":[0.00006949528,0.000015116952,0.9613784,0.000053484775,0.000022869255,0.0005119725,0.0030498884,0.00007190049,0.011519312,0.00010586976,0.00040013078,0.022801572],"study_design_scores_gemma":[0.0000016034986,0.000018248975,0.99700063,0.000008352567,0.0000047177023,0.00016833187,0.0012567014,0.000045471388,0.0002560686,0.000014519051,0.0012235728,0.0000016589272],"about_ca_topic_score_codex":0.03966344,"about_ca_topic_score_gemma":0.17170292,"teacher_disagreement_score":0.03966344,"about_ca_system_score_codex":0.00029672388,"about_ca_system_score_gemma":0.0002796449,"threshold_uncertainty_score":0.07886511},"labels":[],"label_agreement":null},{"id":"W2888719028","doi":"10.1017/s0016756818000535","title":"Reconstruction of the Cryogenian palaeogeography in the Yangtze Domain: constraints from detrital age patterns","year":2018,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"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":"","keywords":"Provenance; Geology; Palaeogeography; Zircon; Detritus; Sedimentary depositional environment; Sedimentary rock; Paleontology; Geochemistry; Structural basin","score_opus":0.011734745626030958,"score_gpt":0.18846270054685962,"score_spread":0.17672795492082866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888719028","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99918216,0.00006787057,0.00032038195,0.000018311313,8.48828e-7,0.0000018742506,0.00012250384,0.000006076025,0.00027998898],"genre_scores_gemma":[0.99952257,0.0000436826,0.00014268943,0.00000387443,0.0000011592131,0.0000022902457,0.00018943612,0.0000027639785,0.000091498885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994147,0.000013630134,0.0000033915728,0.000020447033,0.000008711862,0.00001242927],"domain_scores_gemma":[0.9998907,0.000020355837,0.000025119209,0.000012869206,0.00003419775,0.0000167105],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030904115,0.00022069702,0.00013733264,0.0016316631,0.0003489474,0.0004226344,0.00015901771,0.0001292524,0.0008671766],"category_scores_gemma":[0.00031937682,0.00015148993,0.0002035824,0.0015791203,0.00027786772,0.00021439228,0.0003832101,0.00012755019,0.0000890924],"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":[0.00009104436,0.000011896655,0.9581162,0.000037916252,0.00012253216,0.00034017014,0.0012090366,0.00372973,0.018662412,0.00064161373,0.0001708546,0.01686663],"study_design_scores_gemma":[0.000004114247,0.000009488138,0.9950206,0.0000052080727,0.000017665456,0.00006684151,0.0003711863,0.0031376276,0.0005400412,0.00012313608,0.00069885293,0.000005246228],"about_ca_topic_score_codex":0.021504821,"about_ca_topic_score_gemma":0.032443658,"teacher_disagreement_score":0.021504821,"about_ca_system_score_codex":0.00046707242,"about_ca_system_score_gemma":0.0003434961,"threshold_uncertainty_score":0.0427593},"labels":[],"label_agreement":null},{"id":"W2901718220","doi":"10.1017/s0016756818000651","title":"Pooled subsidence records from numerous wells reveal variations in pre-break-up rifting along the proximal domains of the Iberia–Newfoundland continental margins","year":2018,"lang":"en","type":"article","venue":"Geological Magazine","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"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":"Rift; Geology; Subsidence; Passive margin; Margin (machine learning); Tectonics; Continental margin; Paleontology; Seismology; Tectonic subsidence; Structural basin","score_opus":0.013531611010772817,"score_gpt":0.2216604344084095,"score_spread":0.20812882339763666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901718220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99534297,0.00024801772,0.0002128444,0.000032456366,0.0000034667069,0.0000047360727,0.0028676495,0.000032602104,0.001255399],"genre_scores_gemma":[0.99501014,0.000105684674,0.0003974373,0.000016126709,0.0000036153685,0.0000069633043,0.0036871906,0.000010019865,0.0007629467],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998227,0.000010045587,0.000010813519,0.000057039055,0.000026874875,0.00007262517],"domain_scores_gemma":[0.9994103,0.000044385364,0.0001451927,0.000075532866,0.00025201862,0.000072629555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030935332,0.00023838301,0.00022875561,0.0015010757,0.00036335894,0.0008485342,0.0002693276,0.00019016638,0.0015529654],"category_scores_gemma":[0.0005964749,0.00014245413,0.00018522576,0.0015840832,0.00034310255,0.0003033555,0.0005226317,0.0001903832,0.0002455869],"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":[0.00010157977,0.000022987053,0.973343,0.000027003889,0.00011970951,0.00011071182,0.00046354774,0.0012993279,0.0045809243,0.00009254432,0.0016158612,0.018222747],"study_design_scores_gemma":[8.311914e-7,0.0000021457029,0.9990513,0.0000047949416,0.000007320986,0.000008300924,0.00012959134,0.00022141551,0.00011859183,0.0000033619335,0.0004502159,0.0000021900462],"about_ca_topic_score_codex":0.76107085,"about_ca_topic_score_gemma":0.88447326,"teacher_disagreement_score":0.23892915,"about_ca_system_score_codex":0.002371752,"about_ca_system_score_gemma":0.0009796508,"threshold_uncertainty_score":0.48067248},"labels":[],"label_agreement":null},{"id":"W2920876457","doi":"10.1017/s0016756818000973","title":"Outcrop analysis and facies model of an Upper Permian tidally influenced fluvio-deltaic system: Northern Sydney Basin, SE Australia","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":17,"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":"","keywords":"Geology; Facies; Sedimentary depositional environment; Progradation; Paleontology; Fluvial; Sedimentary rock; Delta; Outcrop; Unconformity; Geomorphology; Subaerial; Structural basin; Sequence stratigraphy","score_opus":0.022556843359330062,"score_gpt":0.23805949153584732,"score_spread":0.21550264817651726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2920876457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99665534,0.000021385362,0.0020190545,0.00003395809,0.0000023935957,0.000011932444,0.00017697354,0.000038904676,0.0010400997],"genre_scores_gemma":[0.9979956,0.000018613038,0.000686599,0.00000561784,0.000001530904,0.000007698137,0.00014934725,0.000012791139,0.0011220861],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999486,0.000011263354,0.0000022951187,0.000015756312,0.0000087193885,0.000013424214],"domain_scores_gemma":[0.9998442,0.00004149753,0.000024066934,0.000010912335,0.000052318253,0.000026977295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021722399,0.00033283202,0.00022027154,0.00082217675,0.0003685552,0.0007007893,0.0004483205,0.00030353805,0.0021976347],"category_scores_gemma":[0.00053108705,0.00034534457,0.00053436705,0.00031971646,0.00031001525,0.00020504092,0.00027118615,0.00020396749,0.0002122975],"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":[0.0000887774,0.000046019835,0.088455014,0.000022341432,0.000078170844,0.00020259622,0.00013725835,0.9009062,0.0015032295,0.0010512844,0.00043546464,0.007073569],"study_design_scores_gemma":[0.0000042193055,0.000009659643,0.019573502,0.0000033946299,0.0000082130655,0.000012688513,0.000035802448,0.979992,0.00007287655,0.00014829346,0.0001362716,0.0000030186993],"about_ca_topic_score_codex":0.27849934,"about_ca_topic_score_gemma":0.19105306,"teacher_disagreement_score":0.27849934,"about_ca_system_score_codex":0.0016353241,"about_ca_system_score_gemma":0.0008608416,"threshold_uncertainty_score":0.5537566},"labels":[],"label_agreement":null},{"id":"W2925772392","doi":"10.1017/s0016756819000141","title":"A protracted Ediacaran–Cambrian transition: an ichnologic ecospace analysis of the Fortunian in Newfoundland, Canada","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological formations and processes","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":true,"ca_institutions":"Queen's University; University of Saskatchewan","funders":"","keywords":"Paleontology; Geology; Fauna; Ecosystem; Ecology; Peninsula; Biology","score_opus":0.009524488662398476,"score_gpt":0.194091197475626,"score_spread":0.18456670881322754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2925772392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99648714,0.00022559642,0.000067194844,0.00012253773,0.0000018919541,0.000009128519,0.0012295651,0.0000040125306,0.0018529866],"genre_scores_gemma":[0.99760395,0.0002058983,0.00017311526,0.000033857443,0.0000011509877,0.0000047137733,0.0010120665,0.0000045645997,0.0009606102],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998605,0.000007608462,0.0000052992777,0.000019590314,0.000023725901,0.00008334068],"domain_scores_gemma":[0.9996704,0.000027779064,0.000047630754,0.000012270153,0.00013335579,0.00010858791],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014377908,0.0001850524,0.0001983222,0.0017609769,0.002022803,0.0017391674,0.0005920598,0.00021284695,0.0020142233],"category_scores_gemma":[0.00035752507,0.00014345438,0.00024050089,0.004370998,0.0009253527,0.00040626875,0.0008990801,0.00035828017,0.0001488118],"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":[0.000097495016,0.00004181962,0.96495837,0.000047505942,0.000070922026,0.0008536033,0.008677359,0.00093614135,0.0017197138,0.0011164686,0.0020417247,0.019438898],"study_design_scores_gemma":[9.038052e-7,0.000004747204,0.9904603,0.000012844064,0.000007718327,0.00004380686,0.0073162033,0.0003246355,0.00007353795,0.000030630075,0.0017193693,0.000005353115],"about_ca_topic_score_codex":0.99165136,"about_ca_topic_score_gemma":0.9974107,"teacher_disagreement_score":0.02086902,"about_ca_system_score_codex":0.02086902,"about_ca_system_score_gemma":0.0112124,"threshold_uncertainty_score":0.151416},"labels":[],"label_agreement":null},{"id":"W2935959749","doi":"10.1017/s0016756817000656","title":"<i>Treptichnus pedum</i>and the Ediacaran–Cambrian boundary: significance and caveats","year":2017,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological formations and processes","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":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Facies; Trace fossil; Paleontology; Intertidal zone; Ordovician; Ichnology; Confusion; Oceanography; Structural basin","score_opus":0.014954158337891198,"score_gpt":0.22118206038591387,"score_spread":0.20622790204802266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2935959749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.61959565,0.08305062,0.009018905,0.120581925,0.013767265,0.0001967293,0.0047256635,0.00070769613,0.14835548],"genre_scores_gemma":[0.967452,0.0057662018,0.0034003954,0.0077679325,0.0055717253,0.00011976619,0.0009788385,0.000109909815,0.008833212],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991762,0.0003519569,0.00008724182,0.0001647977,0.0001293037,0.00009045598],"domain_scores_gemma":[0.989312,0.0070200227,0.0010342168,0.00073295983,0.0015084499,0.00039243736],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0032186941,0.0007041714,0.00076327665,0.003905493,0.0030642673,0.0035573435,0.004715262,0.0021002777,0.013776772],"category_scores_gemma":[0.013545739,0.00018415716,0.0004697055,0.0052524894,0.0035761222,0.0034888561,0.002452258,0.0019744497,0.0016948654],"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":[0.0025799964,0.00026341935,0.31794286,0.0068535954,0.0007279043,0.018891811,0.028480897,0.003447174,0.0047927396,0.10465679,0.21022113,0.3011418],"study_design_scores_gemma":[0.00014223227,0.0005092183,0.50460434,0.007253351,0.00038643976,0.0051253447,0.05277523,0.007938649,0.003139783,0.0874007,0.33041245,0.00031218116],"about_ca_topic_score_codex":0.04530936,"about_ca_topic_score_gemma":0.06690659,"teacher_disagreement_score":0.04530936,"about_ca_system_score_codex":0.0015434067,"about_ca_system_score_gemma":0.001083402,"threshold_uncertainty_score":0.09009129},"labels":[],"label_agreement":null},{"id":"W2947433921","doi":"10.1017/s0016756819000402","title":"Mud deposition and diagenesis within an Early Palaeozoic clinothem: Power Steps Formation, Newfoundland, Canada","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological formations and processes","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":true,"ca_institutions":"Memorial University of Newfoundland; University of Calgary","funders":"Society for Sedimentary Geology","keywords":"Geology; Illite; Mafic; Diagenesis; Petrography; Provenance; Chlorite; Geochemistry; Cove; Facies; Authigenic; Clay minerals; Mineralogy; Geomorphology; Quartz; Paleontology","score_opus":0.01081565858211704,"score_gpt":0.19198608178508775,"score_spread":0.18117042320297072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2947433921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9830351,0.00088560855,0.00018066472,0.0003583012,0.000008780657,0.000042946063,0.003390219,0.000038044913,0.012060315],"genre_scores_gemma":[0.99282515,0.000510616,0.0003516389,0.00006268199,0.000002572337,0.000011031841,0.00084712694,0.000013192156,0.005375849],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997297,0.00000903615,0.000011116191,0.000063683234,0.000073369105,0.000113023474],"domain_scores_gemma":[0.99932814,0.000030293539,0.00010153565,0.00001990302,0.00039194417,0.00012831551],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017643649,0.00028363962,0.00018329543,0.002111626,0.0027538012,0.0013252528,0.00057501654,0.00021346277,0.00465496],"category_scores_gemma":[0.0004963836,0.0002577394,0.00015726266,0.0023730216,0.00129166,0.00034697267,0.00069175643,0.00033260396,0.00037205004],"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":[0.00013135196,0.00003161458,0.9483784,0.000121719706,0.00008020537,0.0007754117,0.0041509448,0.0006137589,0.006945448,0.00090160046,0.0033978736,0.034471694],"study_design_scores_gemma":[0.0000026137748,0.000006773489,0.9941221,0.000025468493,0.000007700488,0.00006597632,0.0016376019,0.00010249219,0.0002767949,0.000018767203,0.0037275697,0.0000061436863],"about_ca_topic_score_codex":0.9954644,"about_ca_topic_score_gemma":0.99913555,"teacher_disagreement_score":0.031455413,"about_ca_system_score_codex":0.031455413,"about_ca_system_score_gemma":0.018396618,"threshold_uncertainty_score":0.22822607},"labels":[],"label_agreement":null},{"id":"W2950590923","doi":"10.1017/s0016756819000414","title":"Mixed local and ultra-distal volcanic ash deposition within the Upper Cretaceous Kanguk Formation, Sverdrup Basin, Canadian Arctic Islands","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"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":"Geology; Zircon; Rhyolite; Sverdrup; Geochemistry; Arctic; Volcanic ash; Cretaceous; Volcanic rock; Volcano; Outcrop; Paleontology; Oceanography","score_opus":0.006833799314628522,"score_gpt":0.1672621818993759,"score_spread":0.16042838258474737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2950590923","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99702966,0.00038333022,0.00006846637,0.000018409415,0.0000023521527,0.0000072634316,0.0006454392,0.000009761468,0.0018352998],"genre_scores_gemma":[0.99861944,0.00014359313,0.00016597014,0.000006312244,8.868834e-7,0.0000035759301,0.000427097,0.0000037460848,0.0006293745],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997526,0.000009669674,0.000013435335,0.000062032006,0.00006467623,0.00009754147],"domain_scores_gemma":[0.9997414,0.000011856983,0.000041656178,0.0000107140995,0.00013292933,0.00006148704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021390611,0.0002904969,0.00023773636,0.001971724,0.0016636422,0.00079431554,0.0004758516,0.00015296949,0.0011021895],"category_scores_gemma":[0.0003275109,0.00018619541,0.0002155787,0.0018017148,0.00057832483,0.0002200568,0.0005323977,0.00012655095,0.000116541334],"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":[0.000093080685,0.000013505774,0.95841986,0.00009451071,0.00013551688,0.00041766302,0.0032196234,0.0004109702,0.022068245,0.0003439038,0.0003907983,0.014392442],"study_design_scores_gemma":[8.3823727e-7,0.0000039100332,0.998357,0.000007795922,0.000009093172,0.00003954541,0.0007190706,0.00008055939,0.00022692318,0.0000069192906,0.0005453386,0.000003057449],"about_ca_topic_score_codex":0.9536404,"about_ca_topic_score_gemma":0.9897406,"teacher_disagreement_score":0.0463596,"about_ca_system_score_codex":0.006271094,"about_ca_system_score_gemma":0.005282216,"threshold_uncertainty_score":0.093265176},"labels":[],"label_agreement":null},{"id":"W2953103793","doi":"10.1017/s0016756819000517","title":"Three-dimensional visualization of top-down superimposed thrust sheets in the SW Grenville Province, Ontario","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"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":"Geology; Visualization; Tectonics; Thrust; Rift; Seismology; Front (military); Trajectory; Allochthon; Boundary (topology); Nappe; Computer science; Engineering","score_opus":0.011380699208885835,"score_gpt":0.19839446559758395,"score_spread":0.1870137663886981,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2953103793","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89191747,0.0006461644,0.011258635,0.0010346817,0.000095267984,0.00016943252,0.024565287,0.0039595654,0.0663535],"genre_scores_gemma":[0.9675146,0.0006470387,0.0137529755,0.00005438481,0.000013776767,0.000045722718,0.004416837,0.0003943342,0.013160392],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999274,0.0000034939383,0.0000025938364,0.000012153188,0.00003433882,0.000020002015],"domain_scores_gemma":[0.9998652,0.000026644902,0.0000110345345,0.0000092459295,0.00005788507,0.000029860546],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009363422,0.00030520398,0.00016149558,0.0012828129,0.0005639142,0.0011923908,0.00030494077,0.00025697434,0.013713985],"category_scores_gemma":[0.00039625642,0.00017879989,0.00023582869,0.0013085391,0.0002943029,0.00026297645,0.0005427545,0.00025215474,0.000753112],"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":[0.0013194435,0.0002257263,0.2650382,0.0018626205,0.00030704585,0.0068424223,0.0417707,0.07218699,0.21764122,0.00974247,0.06973188,0.31333125],"study_design_scores_gemma":[0.00014018996,0.00008166563,0.75638515,0.00044224758,0.00013841604,0.00067587255,0.0101740705,0.062319238,0.013298603,0.0012529397,0.15487763,0.0002138751],"about_ca_topic_score_codex":0.71917266,"about_ca_topic_score_gemma":0.87230223,"teacher_disagreement_score":0.28082734,"about_ca_system_score_codex":0.0021239987,"about_ca_system_score_gemma":0.0038639563,"threshold_uncertainty_score":0.5649624},"labels":[],"label_agreement":null},{"id":"W2957895140","doi":"10.1017/s0016756819000645","title":"Deformation partitioning in mountain belts: insights from analogue modelling experiments and the Taiwan collisional orogen","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"earthquake and tectonic studies","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 Alberta","funders":"Centre National de la Recherche Scientifique","keywords":"Geology; Lithosphere; Subduction; Strain partitioning; Tectonics; Continental margin; Crust; Plate tectonics; Convergent boundary; Seismology; Passive margin; Mantle (geology); Continental crust; Mountain formation; Crustal recycling; Obduction; Underplating; Geophysics; Oceanic crust; Rift","score_opus":0.018627756194953535,"score_gpt":0.21194706570373242,"score_spread":0.1933193095087789,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2957895140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99807066,0.000028497734,0.0009073177,0.000033110136,0.0000014482283,0.00000981611,0.00014781689,0.000019132018,0.00078233547],"genre_scores_gemma":[0.99920756,0.000030039091,0.0005616547,0.0000048388442,0.0000012888142,0.000006921462,0.00010645133,0.0000047374524,0.00007642566],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984527,0.0000768341,0.000013227383,0.00003171499,0.000014154337,0.000018692368],"domain_scores_gemma":[0.99959415,0.00022733682,0.000057445992,0.00007681451,0.000022341765,0.000021995407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004748113,0.00021521313,0.00033362847,0.00044797428,0.00022289826,0.00064470386,0.0008245929,0.000552307,0.0011041148],"category_scores_gemma":[0.0012304655,0.00017951839,0.0004115365,0.0006372268,0.00063701486,0.00048080913,0.00034159125,0.00032560405,0.00006122327],"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":[0.00048628016,0.00051435636,0.07445288,0.00012402397,0.00017373115,0.00043653476,0.00078281306,0.8976787,0.014395088,0.0037021528,0.0003082248,0.0069451253],"study_design_scores_gemma":[0.00012980234,0.0003044811,0.046187557,0.000011627791,0.000054868022,0.00007200802,0.0003373796,0.94893014,0.0019435346,0.0014136595,0.0005838067,0.000031163672],"about_ca_topic_score_codex":0.01736558,"about_ca_topic_score_gemma":0.008303236,"teacher_disagreement_score":0.01736558,"about_ca_system_score_codex":0.00058562367,"about_ca_system_score_gemma":0.00018774891,"threshold_uncertainty_score":0.03452897},"labels":[],"label_agreement":null},{"id":"W2965105912","doi":"10.1017/s0016756818000511","title":"U–Pb ages and Hf isotopes of detrital zircons from pre-Devonian sequences along the southeast Yangtze: a link to the final assembly of East Gondwana","year":2018,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"University of Windsor","funders":"","keywords":"Geology; Gondwana; Provenance; Paleozoic; Detritus; Zircon; Ordovician; Devonian; Craton; Paleontology; Sedimentary rock; Geochemistry; Structural basin","score_opus":0.021160594459342246,"score_gpt":0.21853509354512882,"score_spread":0.19737449908578658,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2965105912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992743,0.000086307526,0.00008656636,0.000008714672,0.0000011533878,0.000001908355,0.00019110908,0.0000034219897,0.00034655485],"genre_scores_gemma":[0.998473,0.00010269728,0.00017700472,0.0000086904865,0.0000033945853,0.0000050077942,0.00055890204,0.000003309524,0.0006678655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999411,0.000004138561,0.0000063718726,0.000020894639,0.000012587513,0.000014901995],"domain_scores_gemma":[0.99988866,0.000011607124,0.000025882318,0.000012679126,0.000045313725,0.000015885997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018994042,0.00018552483,0.00010941872,0.0014671016,0.0003882752,0.0003485725,0.00017090733,0.00012257847,0.0015218795],"category_scores_gemma":[0.00019388362,0.00015678788,0.00013277806,0.0011367996,0.00023248036,0.00017518477,0.00040206112,0.000164819,0.00016721291],"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":[0.00009537452,0.000011706125,0.9231498,0.000024547286,0.000062756,0.00029508406,0.0014371063,0.00015369584,0.054775447,0.00017411986,0.00011345257,0.019706888],"study_design_scores_gemma":[0.0000016752609,0.000008316693,0.99804014,0.0000018379131,0.000008162137,0.00006178618,0.00011349791,0.00006579828,0.0011665404,0.00001172001,0.00051919784,0.0000012945302],"about_ca_topic_score_codex":0.016020395,"about_ca_topic_score_gemma":0.03607935,"teacher_disagreement_score":0.016020395,"about_ca_system_score_codex":0.0003460998,"about_ca_system_score_gemma":0.00023104339,"threshold_uncertainty_score":0.031854272},"labels":[],"label_agreement":null},{"id":"W2965381262","doi":"10.1017/s0016756819000694","title":"Derivation of the Early Carboniferous Wedgeport pluton by crystal fractionation of a mafic parental magma: a rare case of an A-type granite within the Meguma terrane (Nova Scotia, Canada)","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"Saint Mary's University","funders":"","keywords":"Pluton; Geology; Mafic; Silicic; Geochemistry; Terrane; Carboniferous; Zircon; Magma chamber; Devonian; Anorthosite; Magma; Basalt; Paleontology; Volcano; Structural basin; Plagioclase","score_opus":0.008240399161127046,"score_gpt":0.18747259433795777,"score_spread":0.17923219517683073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2965381262","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99439645,0.0002062688,0.0013408777,0.0000641257,0.0000072699186,0.000023171051,0.0004758973,0.00005149206,0.0034344923],"genre_scores_gemma":[0.99784887,0.00008068988,0.001008138,0.000009123002,9.770872e-7,0.000004734269,0.00021274672,0.000020335921,0.0008142957],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998934,0.0000047575704,0.00000517404,0.000040274237,0.000031962438,0.00002444476],"domain_scores_gemma":[0.9998505,0.000029329207,0.000022509153,0.000016662438,0.00005283574,0.000028127857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012884951,0.00027890338,0.00021011777,0.00057683577,0.0011963978,0.0010376811,0.0006291521,0.00036351316,0.0010208343],"category_scores_gemma":[0.0004995943,0.0001873955,0.00028336878,0.0007780805,0.0006556648,0.00012804041,0.00030359766,0.0002280918,0.00022183248],"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":[0.0004612286,0.000055761633,0.7678122,0.0003010933,0.00018740051,0.0061492887,0.00236304,0.05633905,0.122168414,0.0050506466,0.0012669184,0.037844863],"study_design_scores_gemma":[0.0000578685,0.00006128018,0.84475183,0.00008044188,0.00011229436,0.002082696,0.0019241372,0.11488908,0.014801196,0.0011819835,0.019999053,0.000058078316],"about_ca_topic_score_codex":0.86848897,"about_ca_topic_score_gemma":0.9260949,"teacher_disagreement_score":0.13151103,"about_ca_system_score_codex":0.0059602237,"about_ca_system_score_gemma":0.0049216696,"threshold_uncertainty_score":0.264571},"labels":[],"label_agreement":null},{"id":"W2966205797","doi":"10.1017/s0016756818000407","title":"Detrital zircon characterization of early Cambrian sandstones from East Avalonia and SE Ireland: implications for terrane affinities in the peri-Gondwanan Caledonides","year":2018,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"St. Francis Xavier University; University of Alberta","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Terrane; Gondwana; Zircon; Geology; Provenance; Paleontology; Ordovician; Laurentia; Geochemistry; Structural basin; Tectonics","score_opus":0.02756366392187561,"score_gpt":0.22475012977751954,"score_spread":0.19718646585564392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2966205797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99880385,0.0000660548,0.00008457663,0.0000051943093,0.0000010331984,0.0000049595983,0.00026216704,0.0000046208484,0.0007674573],"genre_scores_gemma":[0.99885285,0.00004315891,0.00018935975,0.0000071358604,0.0000010990564,0.0000053839444,0.00041751203,0.000004458112,0.0004790039],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999136,0.00000509296,0.000011803715,0.000021880673,0.000017521506,0.00003016249],"domain_scores_gemma":[0.99988055,0.000016411004,0.000023694629,0.000011888278,0.00004167581,0.000025678415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016516888,0.00021085028,0.00018907416,0.0020091361,0.0003909218,0.00060292246,0.00020729998,0.00018055162,0.0010013031],"category_scores_gemma":[0.00026154864,0.0001557266,0.00017094499,0.00094303186,0.00025226848,0.00013898079,0.0004010287,0.00012210099,0.0003505903],"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":[0.00028384343,0.000028186843,0.87750417,0.000040067236,0.000037076246,0.00046063022,0.0010715593,0.00017203482,0.10578054,0.00006344962,0.00010322174,0.014455156],"study_design_scores_gemma":[0.0000025095887,0.000024907227,0.99758613,0.0000036698032,0.0000056007466,0.00010112326,0.0003455929,0.00007273514,0.0014806539,0.0000051935804,0.000370581,0.0000013711417],"about_ca_topic_score_codex":0.03328874,"about_ca_topic_score_gemma":0.08188107,"teacher_disagreement_score":0.03328874,"about_ca_system_score_codex":0.0004270202,"about_ca_system_score_gemma":0.00020596558,"threshold_uncertainty_score":0.066189945},"labels":[],"label_agreement":null},{"id":"W2966297149","doi":"10.1017/s0016756818000638","title":"Carbon-isotope stratigraphy of the SPICE event (Upper Cambrian) in eastern Laurentia: implications for global correlation and a potential reference section","year":2018,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Excursion; Laurentia; Paleontology; Cove; Stratigraphy; Global Boundary Stratotype Section and Point; Sverdrup; Ordovician; Biostratigraphy; Geomorphology; Structural basin","score_opus":0.01715616795644455,"score_gpt":0.243240318488021,"score_spread":0.22608415053157643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2966297149","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978132,0.00031626594,0.000053166168,0.00003961448,0.0000028133968,0.00000514015,0.00038048255,0.0000072868806,0.0013819422],"genre_scores_gemma":[0.9993612,0.00009076483,0.00008212151,0.0000117675645,0.0000041791895,0.000003355896,0.0003069425,0.0000020461505,0.00013763786],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998456,0.000018940636,0.000012263447,0.000049110102,0.00002198238,0.000052065574],"domain_scores_gemma":[0.9996457,0.000049475184,0.00010786564,0.0000311973,0.00012077752,0.000044917342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003885353,0.00024681224,0.00027504223,0.0017959969,0.00039663963,0.000738252,0.00036237756,0.00017464206,0.0009121682],"category_scores_gemma":[0.00055062893,0.00008246648,0.00016862445,0.0018719719,0.0003860325,0.0002889021,0.00047644073,0.00012798891,0.00015899254],"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":[0.00005813756,0.000014966273,0.98630863,0.00003459707,0.00006076064,0.0002258645,0.00039596437,0.00028817655,0.0034803536,0.00006610933,0.00014419488,0.008922276],"study_design_scores_gemma":[8.053342e-7,0.0000044641806,0.9994344,0.0000060160746,0.0000044186177,0.0000115712655,0.00015917298,0.00011705192,0.00007320034,0.0000040647287,0.00018366567,0.0000011157844],"about_ca_topic_score_codex":0.23954245,"about_ca_topic_score_gemma":0.4444593,"teacher_disagreement_score":0.23954245,"about_ca_system_score_codex":0.0017393023,"about_ca_system_score_gemma":0.0007403821,"threshold_uncertainty_score":0.4762963},"labels":[],"label_agreement":null},{"id":"W2971062483","doi":"10.1017/s0016756819000864","title":"First occurrence of the Cambrian arthropod<i>Sidneyia</i>Walcott, 1911 outside of Laurentia","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","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":"","keywords":"Laurentia; Arthropod; Lagerstätte; Paleontology; Biological dispersal; Genus; Biota; Geology; Paleozoic; Ecology; Biology","score_opus":0.011186785837779602,"score_gpt":0.20162961783703207,"score_spread":0.19044283199925247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971062483","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98081756,0.0011330184,0.00054840156,0.00012777103,0.00004701823,0.000023328157,0.00025072167,0.00003651789,0.01701567],"genre_scores_gemma":[0.997912,0.00014666842,0.00047981372,0.000049155184,0.00001608606,0.0000048412835,0.00012411599,0.0000027662254,0.0012645382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999068,0.0000069841713,0.000004399366,0.000033346954,0.00002896963,0.000019507954],"domain_scores_gemma":[0.9997664,0.000030253055,0.00007494761,0.000022548296,0.0000644028,0.000041519474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011028868,0.00019989983,0.000108603854,0.0007341355,0.0013437035,0.00045426114,0.0002691143,0.00027981828,0.0029013199],"category_scores_gemma":[0.0002516967,0.000099728975,0.00009051857,0.00081174716,0.00063470623,0.00030399187,0.0004903215,0.0003662591,0.0003257745],"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":[0.00039356432,0.000046929956,0.63788843,0.00036144277,0.00007936862,0.007583699,0.009428011,0.00015074895,0.145151,0.0029056002,0.004573516,0.1914377],"study_design_scores_gemma":[0.000005646846,0.000096356984,0.95375204,0.00007634258,0.00002192046,0.0021200944,0.0011636612,0.00014621635,0.0044242833,0.00015193399,0.03802972,0.000011621203],"about_ca_topic_score_codex":0.021413691,"about_ca_topic_score_gemma":0.044010054,"teacher_disagreement_score":0.021413691,"about_ca_system_score_codex":0.0006943561,"about_ca_system_score_gemma":0.00039425207,"threshold_uncertainty_score":0.0425781},"labels":[],"label_agreement":null},{"id":"W2979468493","doi":"10.1017/s0016756819000803","title":"An Early Cretaceous stratigraphic marker fossil in the High Arctic: the belemnite <i>Arctoteuthis bluethgeni</i>","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":5,"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":"Cretaceous; Geology; Paleontology; Arctic; The arctic; Oceanography","score_opus":0.014508247273087352,"score_gpt":0.20444448668429646,"score_spread":0.1899362394112091,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979468493","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93476915,0.007749193,0.0019538722,0.00026313026,0.00019498484,0.000021721336,0.0008525966,0.00008929177,0.05410602],"genre_scores_gemma":[0.9893783,0.0012385681,0.003048807,0.00005802154,0.000040234336,0.000007938493,0.00069856003,0.00002045312,0.0055090664],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987483,0.000019573805,0.0000069849807,0.000035399968,0.000040755374,0.000022383489],"domain_scores_gemma":[0.9998273,0.000025617808,0.000052045903,0.000010028959,0.00005998479,0.000025044568],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031716086,0.00015215964,0.00014377169,0.0013893037,0.0010100324,0.00042781472,0.00027003366,0.00015266407,0.0020636516],"category_scores_gemma":[0.00022169459,0.00011440524,0.000060494574,0.0008658176,0.0005275091,0.00034284667,0.00045169753,0.00027163303,0.00031254638],"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":[0.00083283224,0.00011917382,0.4680634,0.00066534954,0.00010924683,0.002392409,0.012769275,0.0010870324,0.06267703,0.007253798,0.008774205,0.43525636],"study_design_scores_gemma":[0.000011484067,0.00013644516,0.8881012,0.00018499627,0.000039441507,0.0011619438,0.0016727499,0.00033315495,0.0017432257,0.0002774563,0.10632854,0.000009315561],"about_ca_topic_score_codex":0.05571148,"about_ca_topic_score_gemma":0.22953966,"teacher_disagreement_score":0.05571148,"about_ca_system_score_codex":0.00081146683,"about_ca_system_score_gemma":0.00034443097,"threshold_uncertainty_score":0.1107744},"labels":[],"label_agreement":null},{"id":"W2982606931","doi":"10.1017/s0016756819000128","title":"Origin of spherulitic and cone-in-cone concretions in Cambro-Ordovician black shales, St Lawrence Estuary, Quebec, Canada","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":true,"ca_institutions":"Fibics (Canada); McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Calcite; Geology; Carbonate; Sponge spicule; Mineralogy; Ordovician; Crystallization; Geochemistry; Paleontology; Chemistry","score_opus":0.012251698720686752,"score_gpt":0.21187572328329715,"score_spread":0.1996240245626104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982606931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99403584,0.00039194667,0.00014367081,0.00008515543,0.0000053025415,0.000031767497,0.0011842703,0.000024367419,0.0040976396],"genre_scores_gemma":[0.9973225,0.00012987095,0.00018464423,0.000023007226,0.0000016593837,0.0000062814693,0.00042261678,0.0000048905995,0.0019045132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979097,0.000008838335,0.000010075337,0.000044186247,0.00007772801,0.00006819977],"domain_scores_gemma":[0.99915564,0.00004579766,0.00013923776,0.00002148656,0.0004915849,0.00014625874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024439633,0.00026466977,0.00021129001,0.0019791564,0.0024964618,0.0011290567,0.0006862208,0.0003531651,0.0024243663],"category_scores_gemma":[0.0004938182,0.00020250175,0.00018391569,0.0021936784,0.00095144176,0.00021252148,0.00045827075,0.00020969547,0.00022273487],"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":[0.00012020662,0.00003473161,0.9683132,0.000070731905,0.00003848221,0.00068965985,0.0019923302,0.00043659256,0.010906558,0.00041445566,0.00088036683,0.016102677],"study_design_scores_gemma":[0.0000024314222,0.000008536084,0.9973031,0.000010677638,0.0000045620136,0.000053885542,0.00079353526,0.00023348044,0.00033964496,0.000017177334,0.0012262701,0.0000064581945],"about_ca_topic_score_codex":0.9863906,"about_ca_topic_score_gemma":0.9960211,"teacher_disagreement_score":0.014725376,"about_ca_system_score_codex":0.014725376,"about_ca_system_score_gemma":0.009635681,"threshold_uncertainty_score":0.10684055},"labels":[],"label_agreement":null},{"id":"W2983080473","doi":"10.1017/s0016756819000268","title":"U–Pb zircon age dating of diamond-bearing gneiss from Fjørtoft reveals repeated burial of the Baltoscandian margin during the Caledonian Orogeny","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","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":"University of British Columbia","funders":"","keywords":"Zircon; Gneiss; Geology; Allochthon; Metamorphic rock; Orogeny; Geochemistry; Nappe; Geochronology; Diachronous; Radiometric dating; Tectonics; Paleontology","score_opus":0.008337655894210339,"score_gpt":0.18150630905680146,"score_spread":0.1731686531625911,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2983080473","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99889106,0.00008387881,0.000103869,0.0000037906225,0.000001776026,0.0000021232968,0.00019224144,0.0000058309556,0.0007153738],"genre_scores_gemma":[0.9990478,0.000058320464,0.0001635262,0.000004078165,0.0000011772477,0.0000016004675,0.00023419892,0.0000037126763,0.00048538137],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99992347,0.0000035486041,0.0000053192575,0.00002752347,0.000018421622,0.000021650507],"domain_scores_gemma":[0.9999343,0.000007339934,0.000019535077,0.000007545851,0.000021579768,0.000009718697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010523622,0.00016849008,0.00016240234,0.0009957507,0.00034707287,0.0004176288,0.00015971718,0.00022819338,0.0010288645],"category_scores_gemma":[0.00016574346,0.00012791033,0.00011860404,0.0005882285,0.00041557458,0.00009498715,0.00031110455,0.00009500391,0.00024653637],"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":[0.00023901004,0.000023259765,0.77003264,0.00007819589,0.00007299551,0.0011864906,0.0021386163,0.00040322004,0.19901368,0.00015689527,0.00018629679,0.026468648],"study_design_scores_gemma":[0.0000010717793,0.000017021704,0.9976279,0.0000040680447,0.00000690768,0.00014200855,0.00016158387,0.000057132787,0.0014776682,0.000005939847,0.0004974096,0.0000013391365],"about_ca_topic_score_codex":0.036788244,"about_ca_topic_score_gemma":0.12778778,"teacher_disagreement_score":0.036788244,"about_ca_system_score_codex":0.00034367904,"about_ca_system_score_gemma":0.00018405325,"threshold_uncertainty_score":0.07314825},"labels":[],"label_agreement":null},{"id":"W2993009385","doi":"10.1017/s0016756819001328","title":"Earliest North American articulated freshwater acanthomorph fish (Teleostei: Percopsiformes) from Upper Cretaceous deposits of Alberta, Canada","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Ichthyology and Marine Biology","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":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"","keywords":"Monophyly; Sister group; Taxon; Genus; Paleontology; Cretaceous; Biology; Clade; Phylogenetic tree; Teleostei; Cladistics; Zoology; Fish <Actinopterygii>; Fishery","score_opus":0.004035339723918168,"score_gpt":0.1771193677698878,"score_spread":0.17308402804596962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2993009385","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98915,0.00078810286,0.00028157438,0.000050729104,0.000008576725,0.000030717656,0.001944435,0.000022163364,0.007723725],"genre_scores_gemma":[0.9930227,0.0004731492,0.0005818758,0.000039519222,0.000003965277,0.0000120671275,0.0014026456,0.000006647977,0.004457484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986124,0.0000039724778,0.000005880142,0.00003412403,0.00005234924,0.000042513748],"domain_scores_gemma":[0.9996854,0.000016359818,0.00004457849,0.000012902001,0.00016857634,0.00007218249],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001431064,0.000279117,0.00021097779,0.0029803808,0.002125768,0.0007154761,0.00047829046,0.00018438013,0.0035501905],"category_scores_gemma":[0.00029806813,0.00018447015,0.00015272887,0.0030574375,0.0006275633,0.00018747842,0.00042393265,0.00022023144,0.00045388888],"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":[0.00015281673,0.000027974593,0.92501736,0.00017920489,0.00006610849,0.00078995567,0.0053620785,0.00028658658,0.013474937,0.0003814097,0.0018123467,0.052449193],"study_design_scores_gemma":[0.0000019528711,0.0000052024197,0.9956806,0.000019884079,0.000011762022,0.00010603876,0.001389612,0.00006448754,0.00017402806,0.000012990448,0.0025304072,0.0000030482115],"about_ca_topic_score_codex":0.96212584,"about_ca_topic_score_gemma":0.99477816,"teacher_disagreement_score":0.037874162,"about_ca_system_score_codex":0.0065206485,"about_ca_system_score_gemma":0.0051260022,"threshold_uncertainty_score":0.076194346},"labels":[],"label_agreement":null},{"id":"W2995844133","doi":"10.1017/s0016756819001316","title":"Finding the VOICE: organic carbon isotope chemostratigraphy of Late Jurassic – Early Cretaceous Arctic Canada","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":46,"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 Calgary; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Chemostratigraphy; Cretaceous; Arctic; Geology; Paleontology; Isotopes of carbon; δ13C; Earth science; Oceanography; Total organic carbon; Stable isotope ratio; Ecology; Biology","score_opus":0.007670207000435408,"score_gpt":0.18874771462406212,"score_spread":0.1810775076236267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995844133","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903536,0.00079398457,0.0002169771,0.000150105,0.000019132856,0.000007817774,0.0012092413,0.000023971992,0.0072250664],"genre_scores_gemma":[0.99635977,0.00032755756,0.00031326278,0.0000535536,0.0000047061167,0.000002392327,0.00048587986,0.000008349365,0.0024445502],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983776,0.0000056286494,0.000005830585,0.00003623794,0.000057042038,0.00005744399],"domain_scores_gemma":[0.9995615,0.000020420892,0.000034025,0.000009269639,0.0002955178,0.00007925692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021304433,0.00020782402,0.00014731273,0.0016147647,0.0018915056,0.0011057436,0.00034525254,0.00019792774,0.0017730971],"category_scores_gemma":[0.0004295142,0.000097470365,0.00015524549,0.001639343,0.00045807727,0.00019273974,0.00037294652,0.00018770163,0.0002010565],"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":[0.00013382058,0.00001807464,0.9410726,0.000075593925,0.00009204813,0.00056313124,0.0022282726,0.00038014023,0.018284563,0.0005932587,0.0012630321,0.035295326],"study_design_scores_gemma":[0.0000018690882,0.000009233173,0.9915481,0.000017726921,0.000018257917,0.00010386934,0.0015307277,0.0001759272,0.0011678054,0.00004327689,0.005375208,0.0000080457085],"about_ca_topic_score_codex":0.94626,"about_ca_topic_score_gemma":0.98681587,"teacher_disagreement_score":0.053740025,"about_ca_system_score_codex":0.0064880755,"about_ca_system_score_gemma":0.0071618767,"threshold_uncertainty_score":0.10811299},"labels":[],"label_agreement":null},{"id":"W3007391917","doi":"10.1017/s0016756820000023","title":"Rare sapphire-bearing syenitoid pegmatites and associated granitoids of the Hamedan region, Sanandaj–Sirjan zone, Iran: analysis of petrology, lithogeochemistry and zircon geochronology / trace element geochemistry","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Zircon; Pegmatite; Geology; Geochemistry; Geochronology; Petrogenesis; Magma; Trace element; Petrology; Basalt; Volcano","score_opus":0.014161875621950785,"score_gpt":0.19242258462142564,"score_spread":0.17826070899947485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007391917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99944466,0.000086113956,0.000041742704,0.00000558606,8.681684e-7,0.0000035498997,0.00006597123,0.0000050385056,0.0003464439],"genre_scores_gemma":[0.99948174,0.000068486195,0.00011426505,0.0000033535684,0.0000018268854,0.0000016848478,0.0001188835,0.0000014603115,0.0002084114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994266,0.000002935434,0.000005584645,0.000020786332,0.000018344048,0.000009656563],"domain_scores_gemma":[0.99995506,0.0000034540758,0.000022929557,0.000003345284,0.000009568457,0.0000056783547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008544545,0.00024607513,0.00015384174,0.0015711632,0.00030135468,0.00033389448,0.0001831169,0.00016957367,0.00044802594],"category_scores_gemma":[0.00008931134,0.0001821895,0.00015665847,0.0007401074,0.0002851488,0.0001612048,0.00022976265,0.00008252847,0.0000899246],"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":[0.00029721946,0.00007030509,0.8705332,0.00014039209,0.000087778506,0.0018396962,0.0011685041,0.0006630784,0.101833224,0.00016749553,0.0001755169,0.023023639],"study_design_scores_gemma":[0.000007088988,0.000037854963,0.9959209,0.000004032329,0.000014074734,0.00058680924,0.00038114862,0.00025379512,0.002015751,0.000028299622,0.0007471276,0.0000031117313],"about_ca_topic_score_codex":0.0063369307,"about_ca_topic_score_gemma":0.01502686,"teacher_disagreement_score":0.0063369307,"about_ca_system_score_codex":0.00027799438,"about_ca_system_score_gemma":0.0002355833,"threshold_uncertainty_score":0.012600064},"labels":[],"label_agreement":null},{"id":"W3011172644","doi":"10.1017/s0016756820000096","title":"Petrogenesis of the Carboniferous Ghaleh-Dezh metagranite, Sanandaj–Sirjan zone, Iran: constraints from new zircon U–Pb and<sup>40</sup>Ar/<sup>39</sup>Ar ages and Sr–Nd isotopes","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"University of Saskatchewan","funders":"","keywords":"Geology; Zircon; Geochemistry; Petrogenesis; Protolith; Carboniferous; Isochron; Fractional crystallization (geology); Igneous rock; Mantle (geology); Paleontology","score_opus":0.019170330579084658,"score_gpt":0.18824494445714932,"score_spread":0.16907461387806466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3011172644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983298,0.0001645807,0.00008381433,0.000017282082,0.0000032345663,0.000004925431,0.00009102143,0.000009563316,0.0012958059],"genre_scores_gemma":[0.9993967,0.00009320767,0.00015772393,0.0000032298499,0.0000029429468,0.000001965339,0.000095378906,0.000003822119,0.0002450352],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99992263,0.0000044557164,0.0000051284883,0.000024534223,0.000027877219,0.000015323692],"domain_scores_gemma":[0.9999397,0.000006231666,0.000022054293,0.000005806109,0.000019900199,0.0000063399075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001773096,0.00034513522,0.00019134919,0.0016304696,0.00054286496,0.00051724707,0.000285796,0.00022988537,0.0009726065],"category_scores_gemma":[0.00016619782,0.0003012915,0.00020895021,0.0009396905,0.00055432273,0.000154666,0.00031867938,0.00016598402,0.00021449655],"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":[0.00051126874,0.00006587421,0.8430062,0.00022273352,0.000108711516,0.001822268,0.001856405,0.0029470518,0.110057004,0.0008707041,0.0003559783,0.038175818],"study_design_scores_gemma":[0.000011107298,0.00002664881,0.9957902,0.0000073900783,0.000012932876,0.00037308325,0.00033892746,0.00058272394,0.0016980364,0.000057130645,0.0010983555,0.0000034267402],"about_ca_topic_score_codex":0.020083582,"about_ca_topic_score_gemma":0.039151117,"teacher_disagreement_score":0.020083582,"about_ca_system_score_codex":0.0008010509,"about_ca_system_score_gemma":0.0005395786,"threshold_uncertainty_score":0.039933383},"labels":[],"label_agreement":null},{"id":"W3014190113","doi":"10.1017/s0016756820000175","title":"Depleted and ultradepleted basalt and picrite in the Davis Strait: Paleocene volcanism associated with a transform continental margin","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"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":"Geology; Basalt; Geochemistry; Peridotite; Asthenosphere; Mantle (geology); Underplating; Volcanic rock; Lithosphere; Volcano; Paleontology; Tectonics","score_opus":0.015068879258621905,"score_gpt":0.17910680095921314,"score_spread":0.16403792170059123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014190113","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993343,0.000056982764,0.000007334284,0.000009329936,5.977953e-7,9.311859e-7,0.00011624139,0.0000013265603,0.00047294534],"genre_scores_gemma":[0.99962914,0.000029248924,0.000014183974,0.0000035082562,7.1056957e-7,6.203357e-7,0.00015117832,5.8285207e-7,0.00017072556],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993634,0.0000036557833,0.0000050314316,0.00001509433,0.000020310208,0.000019612455],"domain_scores_gemma":[0.999881,0.00001005318,0.000031406318,0.00000764395,0.000034285757,0.00003553555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000055065535,0.00012990553,0.00011293331,0.001056334,0.00046842496,0.00054587465,0.00021983094,0.00017226297,0.00076631946],"category_scores_gemma":[0.00018580648,0.00012434636,0.00006450295,0.00069509266,0.00031192572,0.00010323838,0.00030065016,0.00010500226,0.00010335333],"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":[0.000046258567,0.0000088978795,0.98940057,0.0000134467155,0.00002320209,0.00032728945,0.00083907,0.00008887749,0.006311074,0.000061643834,0.000113637245,0.0027661126],"study_design_scores_gemma":[7.9868926e-7,0.0000050115987,0.99867237,0.000002653049,0.000004142161,0.000086219836,0.0005476446,0.000057493926,0.00026908328,0.0000047071444,0.00034893904,9.549046e-7],"about_ca_topic_score_codex":0.20394577,"about_ca_topic_score_gemma":0.49424425,"teacher_disagreement_score":0.20394577,"about_ca_system_score_codex":0.0010367784,"about_ca_system_score_gemma":0.00043796375,"threshold_uncertainty_score":0.40551734},"labels":[],"label_agreement":null},{"id":"W3019115559","doi":"10.1017/s0016756820000229","title":"Contact metamorphism of the Tethyan Sedimentary Sequence, Upper Mustang region, west-central Nepal","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Metamorphism; Geology; Pluton; Metamorphic rock; Monazite; Leucogranite; Geochemistry; Biotite; Sillimanite; Schist; Sedimentary rock; Staurolite; Petrology; Paleontology; Gneiss; Zircon; Tectonics","score_opus":0.028760387737012907,"score_gpt":0.2005973324176233,"score_spread":0.1718369446806104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3019115559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973678,0.00011121835,0.00006424467,0.000016847713,0.0000014281331,0.000009482842,0.00059975,0.000009097288,0.00182019],"genre_scores_gemma":[0.9984956,0.000074030046,0.00013084208,0.000011718662,0.0000014666086,0.000011414201,0.00082473306,0.000004226728,0.00044597808],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989486,0.000009062636,0.0000139471385,0.000035649693,0.000022347484,0.00002418467],"domain_scores_gemma":[0.9998103,0.000022206339,0.00005596693,0.000021365771,0.0000626553,0.000027423312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009739817,0.00019141908,0.00016078204,0.002066462,0.0006408393,0.0005296993,0.00024027009,0.00020159782,0.0014846871],"category_scores_gemma":[0.00043262655,0.00014530383,0.00012487036,0.0020577966,0.00035365162,0.00026740733,0.00065844104,0.00013816288,0.00029135062],"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":[0.00009796775,0.00003600006,0.94611484,0.00016298125,0.00009296193,0.0015824294,0.008019699,0.00027703776,0.018275699,0.00021255043,0.00047673075,0.024651024],"study_design_scores_gemma":[0.0000020587368,0.000009455741,0.99739635,0.000015713638,0.000009026785,0.0002306261,0.0009739998,0.00011264897,0.00034004851,0.000014387365,0.00089329906,0.0000023845082],"about_ca_topic_score_codex":0.060624056,"about_ca_topic_score_gemma":0.18496503,"teacher_disagreement_score":0.060624056,"about_ca_system_score_codex":0.0005212404,"about_ca_system_score_gemma":0.00042356362,"threshold_uncertainty_score":0.12054241},"labels":[],"label_agreement":null},{"id":"W3019892000","doi":"10.1017/s0016756820000138","title":"Structural setting of a transpressive shear zone: insights from geological mapping, quartz petrofabric and kinematic vorticity analysis in NE Sardinia (Italy)","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Geology; Shear zone; Mylonite; Metamorphic rock; Shear (geology); Quartz; Pure shear; Simple shear; Vorticity; Mineralogy; Seismology; Petrology; Paleontology; Tectonics","score_opus":0.015355404524549318,"score_gpt":0.19876489468924763,"score_spread":0.18340949016469832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3019892000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990916,0.000052440057,0.00006227798,0.000011763571,7.8543525e-7,0.000002565814,0.000107341024,0.000005984871,0.00066512724],"genre_scores_gemma":[0.9995969,0.00002960432,0.000115369636,0.0000041546914,0.0000013814787,0.000002498316,0.000111839916,0.0000025420188,0.00013563977],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987996,0.000015136695,0.0000089818295,0.000053069798,0.00001680868,0.00002610328],"domain_scores_gemma":[0.99987304,0.000016762318,0.000056983914,0.0000132479245,0.00002533935,0.00001460118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013382034,0.00023960505,0.00019442919,0.001398507,0.00030226482,0.0005700616,0.00022347091,0.00030054216,0.0010433417],"category_scores_gemma":[0.00025451407,0.00018843003,0.00014724224,0.0013496997,0.00057928305,0.00017544586,0.0004531209,0.00013785719,0.00021640246],"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":[0.00018622896,0.000073653115,0.9392087,0.00007519359,0.000067389665,0.00086167594,0.0027146423,0.0015407616,0.03354973,0.00021668182,0.0002404321,0.021264935],"study_design_scores_gemma":[0.0000017805403,0.000010558849,0.9993674,0.0000024284911,0.0000028199831,0.00003588049,0.0001536939,0.00017211157,0.00008410148,0.000006812048,0.0001612367,0.0000011824994],"about_ca_topic_score_codex":0.03868222,"about_ca_topic_score_gemma":0.064274386,"teacher_disagreement_score":0.03868222,"about_ca_system_score_codex":0.00050526654,"about_ca_system_score_gemma":0.0002531588,"threshold_uncertainty_score":0.07691413},"labels":[],"label_agreement":null},{"id":"W3020390606","doi":"10.1017/s0016756820000254","title":"A reworked isolated deposit of the Kos Plateau Tuff and its significance for dating raised marine terraces, Kos, Greece","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Saint Mary's University; Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Pyroclastic rock; Interglacial; Clastic rock; Tephra; Geomorphology; Pumice; Plateau (mathematics); Holocene; Geochemistry; Granulometry; Sea level; River terraces; Volcano; Paleontology; Glacial period; Sedimentary rock; Fluvial; Sediment; Oceanography","score_opus":0.03534063641091657,"score_gpt":0.23840008304917323,"score_spread":0.20305944663825665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3020390606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976221,0.00014504533,0.00009074679,0.0000064231117,0.0000032467597,0.000006409222,0.00009246224,0.000008065682,0.0020255456],"genre_scores_gemma":[0.99946994,0.000055971304,0.00014574853,0.0000026075372,0.0000019082227,0.00000196758,0.00011307518,0.000002761217,0.00020614693],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998946,0.00000835347,0.000012334402,0.00003604333,0.000029692292,0.000019007543],"domain_scores_gemma":[0.9998853,0.000013613948,0.000037613238,0.000019581159,0.000024500294,0.000019215797],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001602071,0.00021161744,0.00016040611,0.0018967657,0.0003546094,0.0005836547,0.00024044196,0.00023854467,0.0009633816],"category_scores_gemma":[0.00035370758,0.00015399906,0.00016694496,0.0010745648,0.0005775856,0.00022522964,0.00055182027,0.0001312997,0.00022530655],"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":[0.00014109585,0.000041039893,0.88725185,0.00015040874,0.000106031446,0.0070745633,0.0025411912,0.00076001947,0.06574769,0.0004309823,0.00016747654,0.03558768],"study_design_scores_gemma":[0.0000037072152,0.00004349189,0.99508685,0.00001954347,0.000011480535,0.001839604,0.00077089353,0.00026227694,0.0008278344,0.000033427394,0.0010979268,0.0000028782886],"about_ca_topic_score_codex":0.009374922,"about_ca_topic_score_gemma":0.0193148,"teacher_disagreement_score":0.009374922,"about_ca_system_score_codex":0.0002891661,"about_ca_system_score_gemma":0.00028835534,"threshold_uncertainty_score":0.018640697},"labels":[],"label_agreement":null},{"id":"W3088175892","doi":"10.1017/s0016756820000941","title":"Palaeobiology of the reclining rangeomorph <i>Beothukis</i> from the Ediacaran Mistaken Point Formation of southeastern Newfoundland","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":24,"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":"Morphology (biology); Fractal; Geology; Paleontology; Ontogeny; Frond; Biology; Mathematics","score_opus":0.03263640657758127,"score_gpt":0.21027319422605203,"score_spread":0.17763678764847077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088175892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975925,0.00010931526,0.00006935313,0.000022651308,0.0000018771815,0.0000048102474,0.00010641537,0.000004009235,0.0020889514],"genre_scores_gemma":[0.99898213,0.00008450626,0.00010674303,0.000012636525,0.0000010540248,0.000002432549,0.0001234131,0.000003381656,0.00068358186],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987113,0.0000071957,0.0000050527838,0.000040452873,0.000023662202,0.000052525535],"domain_scores_gemma":[0.99981815,0.000015568055,0.00006423818,0.00001300776,0.000053602103,0.000035377576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010679506,0.00020760203,0.00024447954,0.0011193649,0.001792818,0.0011367092,0.00039298154,0.00024118494,0.0025309597],"category_scores_gemma":[0.00021104437,0.00025206726,0.00013339038,0.0010871798,0.0015497546,0.00030712844,0.0006458139,0.0003708077,0.0003783972],"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":[0.00031858924,0.000049766582,0.8673284,0.00017015278,0.000083446415,0.0016328772,0.020255124,0.00035669992,0.072150126,0.0008529432,0.000577609,0.036224257],"study_design_scores_gemma":[0.000001050854,0.00001123292,0.9965366,0.000008385409,0.000006900479,0.00018891813,0.0018126379,0.000035483157,0.00021628587,0.000013693186,0.0011663621,0.0000024911853],"about_ca_topic_score_codex":0.5190194,"about_ca_topic_score_gemma":0.8540306,"teacher_disagreement_score":0.48098058,"about_ca_system_score_codex":0.0033833492,"about_ca_system_score_gemma":0.001251995,"threshold_uncertainty_score":0.96762633},"labels":[],"label_agreement":null},{"id":"W3089746995","doi":"10.1017/s0016756820000990","title":"The Mesozoic Arctic: warm, green, and highly diverse","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","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":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Content (measure theory); Mesozoic; The arctic; Arctic; Chemistry; Geology; Oceanography; Paleontology; Mathematics","score_opus":0.025640950484788767,"score_gpt":0.21381875973873687,"score_spread":0.18817780925394811,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3089746995","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4963502,0.18475497,0.0021335278,0.073291145,0.0053194254,0.000022230413,0.0021674596,0.00014823506,0.23581287],"genre_scores_gemma":[0.9080825,0.063512675,0.0018234086,0.004884336,0.0016228723,0.0000073688384,0.0004903749,0.00005960559,0.019516837],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99984336,0.000034691606,0.0000054416623,0.000025125208,0.000050825565,0.000040547577],"domain_scores_gemma":[0.99978393,0.000016034219,0.000027246318,0.000008142766,0.000047668433,0.0001169673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043708063,0.0002603599,0.00018514207,0.0009551557,0.0035434817,0.0030184786,0.00014664578,0.0002766238,0.0021402796],"category_scores_gemma":[0.00029606858,0.000107592445,0.00009642121,0.0017275253,0.0014777129,0.0008256068,0.0011410182,0.0007478548,0.00041979295],"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":[0.00041137624,0.00006452158,0.16527328,0.0010265283,0.0001632079,0.0025520665,0.059163652,0.00075490255,0.016508484,0.038210455,0.18155599,0.5343154],"study_design_scores_gemma":[0.0000038905346,0.00002629751,0.2743269,0.00025910998,0.000028537539,0.0006822328,0.015937254,0.00007130239,0.00028916274,0.004067887,0.7042918,0.00001564174],"about_ca_topic_score_codex":0.05461509,"about_ca_topic_score_gemma":0.2668694,"teacher_disagreement_score":0.05461509,"about_ca_system_score_codex":0.0012996874,"about_ca_system_score_gemma":0.0015716748,"threshold_uncertainty_score":0.10859436},"labels":[],"label_agreement":null},{"id":"W3111359541","doi":"10.1017/s0016756820001338","title":"Zircon U–Pb ages, geochemistry and Sr–Nd isotopes of the Golshekanan granitoid, Urumieh–Dokhtar magmatic arc, Iran: evidence for partial melting of juvenile crust","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"University of New Brunswick","funders":"","keywords":"Lile; Zircon; Geochemistry; Geology; Partial melting; Lithophile; Primitive mantle; Mantle (geology); Continental crust; Crust; Adakite; Quartz monzonite; Back-arc basin; Diorite; Oceanic crust; Subduction; Petrology; Pluton; Tectonics; Paleontology","score_opus":0.049161945539723875,"score_gpt":0.23501677620592634,"score_spread":0.18585483066620245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3111359541","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985347,0.0002477537,0.000054585813,0.000017661054,0.0000019393717,0.000002487625,0.00027528673,0.000010048742,0.00085560983],"genre_scores_gemma":[0.9989033,0.00009296293,0.00010943948,0.0000055467654,0.0000023415696,0.000002024057,0.00040617536,0.0000035115143,0.00047467966],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994886,0.0000027978776,0.000003937047,0.000013687549,0.000013345471,0.000017362885],"domain_scores_gemma":[0.9999609,0.0000030150443,0.0000114534205,0.000002968391,0.0000157719,0.0000059252575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010745424,0.00029129896,0.00016919138,0.0016451621,0.00054744404,0.00048500532,0.00022343193,0.00023042125,0.0010393121],"category_scores_gemma":[0.000101635254,0.00016694001,0.0001816265,0.0010420538,0.00032255027,0.00014895716,0.00030376733,0.000106959546,0.00039833935],"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":[0.00026392192,0.000040768697,0.9210952,0.00008999054,0.00008984151,0.0005319028,0.00090712484,0.0009086877,0.04420708,0.00021809668,0.0003603917,0.031287126],"study_design_scores_gemma":[0.0000034207017,0.000015437945,0.99794406,0.0000027746344,0.000006592732,0.000118273245,0.00017351483,0.000118137184,0.0006948613,0.000017505783,0.0009032914,0.000002085606],"about_ca_topic_score_codex":0.03507241,"about_ca_topic_score_gemma":0.044826306,"teacher_disagreement_score":0.03507241,"about_ca_system_score_codex":0.0007013842,"about_ca_system_score_gemma":0.0003896889,"threshold_uncertainty_score":0.06973654},"labels":[],"label_agreement":null},{"id":"W3112643670","doi":"10.1017/s0016756820001260","title":"Sedimentology and integrated chronostratigraphy of the lower Heatherdale Shale (Cambrian, stages 2–3), Stansbury Basin, South Australia","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Chronostratigraphy; Sedimentary depositional environment; Lithostratigraphy; Paleontology; Chemostratigraphy; Biostratigraphy; Sedimentology; Structural basin; Stage (stratigraphy); Isotopes of carbon; Total organic carbon","score_opus":0.028984625610789596,"score_gpt":0.2264111275460244,"score_spread":0.1974265019352348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3112643670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99898666,0.00009123006,0.000055016484,0.000008794053,6.7346105e-7,0.000008331714,0.00025544144,0.000005133578,0.0005886344],"genre_scores_gemma":[0.9983498,0.00009028097,0.00024930135,0.000011341597,0.0000013474911,0.000009304979,0.0003813232,0.0000026470423,0.00090474734],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999248,0.000006985056,0.000007146735,0.000020501227,0.000022754206,0.000017818384],"domain_scores_gemma":[0.99975044,0.000012003359,0.00007722863,0.000014808973,0.00010398673,0.000041438238],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014719422,0.00016896325,0.00011383089,0.0016763518,0.00042909558,0.00036788685,0.00019992633,0.00013091552,0.001311854],"category_scores_gemma":[0.00025043232,0.0001780177,0.00012537469,0.001106809,0.00031143663,0.00019700029,0.00041010036,0.000114967785,0.00019252612],"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":[0.000057863683,0.000026692678,0.96520233,0.000069595786,0.000047672096,0.00024319947,0.003190789,0.00040218883,0.012719151,0.00010301986,0.00038361741,0.017553966],"study_design_scores_gemma":[4.624308e-7,0.000005336002,0.99954164,0.000003027602,0.0000017461379,0.000013312902,0.000089915884,0.000047637386,0.00009702256,0.000003214918,0.00019608349,5.5097564e-7],"about_ca_topic_score_codex":0.34125912,"about_ca_topic_score_gemma":0.6967898,"teacher_disagreement_score":0.34125912,"about_ca_system_score_codex":0.0012352925,"about_ca_system_score_gemma":0.0007470175,"threshold_uncertainty_score":0.67854553},"labels":[],"label_agreement":null},{"id":"W3115647954","doi":"10.1017/s0016756820001247","title":"Probable deinonychosaur tracks from the Upper Cretaceous Wapiti Formation (upper Campanian) of Alberta, Canada","year":2020,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Evolutionary Biology","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":true,"ca_institutions":"Royal Ontario Museum; University of Alberta","funders":"","keywords":"Cretaceous; Paleontology; Geology; Margin (machine learning)","score_opus":0.01384938692773675,"score_gpt":0.18512633430552286,"score_spread":0.17127694737778612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3115647954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98820835,0.0007497153,0.00034831002,0.00007768083,0.000017941224,0.00004997971,0.0010029328,0.000034609206,0.009510524],"genre_scores_gemma":[0.9939976,0.00056465116,0.00096795417,0.000044795666,0.000008038592,0.000015940612,0.0014913573,0.000011936144,0.002897641],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997873,0.000004684002,0.000008692892,0.000040260744,0.00009150392,0.00006757837],"domain_scores_gemma":[0.9995709,0.00002223747,0.000079466416,0.00002190547,0.00021001883,0.00009538971],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014182119,0.0003145813,0.00019723974,0.0028947515,0.0024807304,0.0008626287,0.00057345483,0.00029137367,0.0016669163],"category_scores_gemma":[0.00033907205,0.00015041472,0.00012676508,0.0027088441,0.00064690853,0.00019271972,0.0007634192,0.00027300077,0.00021630037],"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":[0.0001460917,0.000031948075,0.91945606,0.00012268903,0.000052009338,0.0020476838,0.0069970503,0.00027199512,0.014768893,0.00055333565,0.0012145768,0.054337658],"study_design_scores_gemma":[0.0000024564542,0.00001260973,0.99068284,0.00003713172,0.00001041866,0.0003681331,0.0024881936,0.000117172836,0.000397165,0.000034630415,0.0058433777,0.00000580521],"about_ca_topic_score_codex":0.86876786,"about_ca_topic_score_gemma":0.9774827,"teacher_disagreement_score":0.13123214,"about_ca_system_score_codex":0.004071988,"about_ca_system_score_gemma":0.0044501326,"threshold_uncertainty_score":0.26400995},"labels":[],"label_agreement":null},{"id":"W3129082694","doi":"10.1017/s0016756820001430","title":"New insights into the early evolution of horizontal spiral trace fossils and the age of the Brioverian series (Ediacaran–Cambrian) in Brittany, NW France","year":2021,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":12,"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":"","keywords":"Geology; Paleontology; Trace fossil; Ordovician; Radiometric dating; Siliciclastic; Conodont; Series (stratigraphy); Ecological succession; Biostratigraphy; Facies; Ecology; Structural basin; Biology","score_opus":0.007062374382117307,"score_gpt":0.19033884961158393,"score_spread":0.1832764752294666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3129082694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933723,0.00189442,0.0002233108,0.00008428485,0.000009299081,0.0000032107016,0.00027182998,0.000019979125,0.004121395],"genre_scores_gemma":[0.9987727,0.00035994148,0.0001356527,0.000015190579,0.0000057827924,0.0000013305978,0.00011938065,0.0000068493077,0.0005832142],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998728,0.000014824323,0.000009272526,0.000042039937,0.00002962509,0.00003136161],"domain_scores_gemma":[0.999765,0.000048575523,0.000071238705,0.000020389336,0.00007422879,0.000020538064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042182795,0.00035338686,0.00013932711,0.0029646885,0.00044363525,0.0009877454,0.0004239278,0.0002988908,0.0030056643],"category_scores_gemma":[0.0004424793,0.00012317873,0.00016217488,0.0014636102,0.00078387634,0.0003953277,0.0005067748,0.00018018823,0.00025423273],"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":[0.00017621837,0.000023160408,0.8905107,0.00012842957,0.0001366406,0.0008742669,0.003896347,0.0009138585,0.03436318,0.0011468105,0.00042818452,0.06740227],"study_design_scores_gemma":[0.0000016109153,0.000012113131,0.9953768,0.000020731415,0.000010723178,0.00011120559,0.00045698395,0.00018869735,0.0005456006,0.000042875457,0.0032287824,0.000003815548],"about_ca_topic_score_codex":0.07834378,"about_ca_topic_score_gemma":0.15467963,"teacher_disagreement_score":0.07834378,"about_ca_system_score_codex":0.0014094012,"about_ca_system_score_gemma":0.00038239668,"threshold_uncertainty_score":0.15577555},"labels":[],"label_agreement":null},{"id":"W3164874055","doi":"10.1017/s0016756821000388","title":"Petrogenesis of the peralkaline Flowers River Igneous Suite and its significance to the development of the southern Nain Batholith","year":2021,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"Geological Survey of Canada; Cape Breton University; University of New Brunswick","funders":"","keywords":"Peralkaline rock; Geology; Geochemistry; Igneous rock; Batholith; Charnockite; Zircon; Petrogenesis; Metasomatism; Volcanic rock; Volcano; Tectonics; Paleontology; Granulite; Facies; Basalt","score_opus":0.012645755221865783,"score_gpt":0.18781863890266162,"score_spread":0.17517288368079584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3164874055","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962121,0.00017639705,0.00007296913,0.000018949246,0.0000012893009,0.0000039227834,0.000052820895,0.0000072767425,0.003454316],"genre_scores_gemma":[0.99936,0.000047519163,0.000060973405,0.0000030582771,8.497454e-7,0.0000012670338,0.000039275776,0.0000025646732,0.00048451888],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999224,0.000011516603,0.0000052027954,0.000025814488,0.000011369912,0.000023743212],"domain_scores_gemma":[0.99994206,0.0000090764115,0.000021576601,0.0000056373547,0.000012143472,0.000009509802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014890307,0.00014303505,0.000117824,0.00074019167,0.0006165451,0.0007347503,0.0002107528,0.00015973546,0.0013679594],"category_scores_gemma":[0.00021317335,0.00014068844,0.00009548846,0.0003767408,0.00056237984,0.00021219935,0.0005544696,0.00014079902,0.00017118899],"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":[0.00026763135,0.000023629927,0.89096147,0.00010975014,0.000050956747,0.0015530544,0.003971901,0.0013639777,0.065019764,0.0015105726,0.00018405894,0.034983233],"study_design_scores_gemma":[0.0000020801838,0.000018363065,0.99640095,0.000009024547,0.000005565194,0.00021395885,0.00045040363,0.00021108091,0.0010796639,0.000032538555,0.0015732802,0.0000031184134],"about_ca_topic_score_codex":0.043216407,"about_ca_topic_score_gemma":0.10585275,"teacher_disagreement_score":0.043216407,"about_ca_system_score_codex":0.0010692395,"about_ca_system_score_gemma":0.00042498184,"threshold_uncertainty_score":0.08592969},"labels":[],"label_agreement":null},{"id":"W3183872154","doi":"10.1017/s0016756821000534","title":"Beyond ‘crumple zones’: recent advances, applications and future directions in deformable plate tectonic modelling","year":2021,"lang":"en","type":"article","venue":"Geological Magazine","topic":"earthquake and tectonic studies","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":false,"ca_institutions":"McMaster University","funders":"","keywords":"Kinematics; Deformation (meteorology); Plate tectonics; Geology; Intraplate earthquake; Work (physics); Computer science; Tectonics; Mechanical engineering; Seismology; Physics; Classical mechanics; Engineering","score_opus":0.015934686622725156,"score_gpt":0.22019541330367667,"score_spread":0.20426072668095152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3183872154","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":[0.0018174526,0.9132716,0.04006003,0.0329325,0.0035617624,0.000012278697,0.00010210562,0.00012204873,0.008120102],"genre_scores_gemma":[0.032835916,0.94001716,0.014887222,0.0033067244,0.0058516827,0.000019100953,0.00013268039,0.000091774775,0.0028577903],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993186,0.00028105912,0.000063829386,0.0001183369,0.00018534137,0.00003281916],"domain_scores_gemma":[0.994555,0.004027784,0.00032956983,0.000233238,0.000720122,0.00013424436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0036647771,0.0008209942,0.0011637677,0.0019279014,0.00040819214,0.0035999715,0.0020998889,0.003170477,0.0049913647],"category_scores_gemma":[0.0066121067,0.00037964073,0.0012605783,0.002882562,0.0031138167,0.0053407475,0.001805627,0.0037726755,0.0015630719],"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":[0.00008269455,0.000034722772,0.0011005694,0.010464852,0.00017528009,0.0004063592,0.0012947043,0.028949821,0.0013514886,0.401755,0.040545166,0.51383936],"study_design_scores_gemma":[0.000008340856,0.00005341954,0.0010382566,0.0049459236,0.000077359146,0.00041844492,0.00058786524,0.021133997,0.0006539362,0.23653433,0.7344586,0.00008954548],"about_ca_topic_score_codex":0.0044713845,"about_ca_topic_score_gemma":0.00429535,"teacher_disagreement_score":0.0049913647,"about_ca_system_score_codex":0.0014997198,"about_ca_system_score_gemma":0.0016499244,"threshold_uncertainty_score":0.019381404},"labels":[],"label_agreement":null},{"id":"W3207130350","doi":"10.1017/s0016756821000601","title":"Enrichment of heavy REE and Th in carbonatite-derived fenite breccia","year":2021,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","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":"ARC Resources (Canada)","funders":"Horizon 2020 Framework Programme; Natural Environment Research Council; Sight Research UK","keywords":"Carbonatite; Breccia; Geology; Geochemistry; Augite; Metasomatism; Zircon; Plagioclase; Mantle (geology); Quartz","score_opus":0.011588087152384177,"score_gpt":0.19579007042525984,"score_spread":0.18420198327287565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3207130350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995153,0.00006153243,0.00007096151,0.000002871377,3.770053e-7,0.000001547508,0.00007686384,0.000003071491,0.00026751345],"genre_scores_gemma":[0.9990896,0.000035168865,0.00016276054,0.0000033888903,4.2037985e-7,0.0000021308172,0.00016764148,0.0000025055547,0.0005363421],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99991465,0.000006049961,0.0000062497097,0.000030582924,0.000014735944,0.000027739596],"domain_scores_gemma":[0.99988973,0.000015046056,0.00003539604,0.000010757076,0.000033163302,0.000015895379],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000087763896,0.00017763043,0.00015662442,0.0008420661,0.00029466482,0.00038848587,0.00017801549,0.00029446906,0.0005591412],"category_scores_gemma":[0.0001761845,0.00012757596,0.000115917785,0.000310953,0.00031339048,0.00013946388,0.00019663754,0.00011446897,0.00014607901],"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":[0.00026782136,0.000012386898,0.083352864,0.000046520134,0.00002543651,0.00031045618,0.00030979252,0.0001825573,0.9131215,0.000050426097,0.000016366774,0.00230391],"study_design_scores_gemma":[0.0000045711035,0.000107653126,0.9113161,0.00000753782,0.000014948915,0.0004499501,0.0003746296,0.00056896714,0.08601359,0.00002485158,0.0011115476,0.0000057325183],"about_ca_topic_score_codex":0.009786574,"about_ca_topic_score_gemma":0.011925255,"teacher_disagreement_score":0.009786574,"about_ca_system_score_codex":0.00034676678,"about_ca_system_score_gemma":0.00010165223,"threshold_uncertainty_score":0.019459248},"labels":[],"label_agreement":null},{"id":"W3207681742","doi":"10.1017/s0016756821000698","title":"Zircon U–Pb–Hf snapshots on the crustal evolution of the Serbo-Macedonian massif: new insights from Ammouliani island (Northern Greece)","year":2021,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"Université du Québec à Montréal","funders":"","keywords":"Zircon; Massif; Geology; Geochemistry; Igneous rock; Macedonian; Basement; Crust; Petrology; Archaeology; Ancient history; Geography","score_opus":0.012008467157561131,"score_gpt":0.17688045750809314,"score_spread":0.16487199035053202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3207681742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979388,0.00027930393,0.00006460126,0.000017211805,0.000001897334,0.0000038638927,0.00029430687,0.0000062874074,0.0013936858],"genre_scores_gemma":[0.99897003,0.00015551862,0.00009970206,0.000006993884,0.0000031786608,0.0000022060208,0.0002751096,0.0000038858657,0.0004833389],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999343,0.0000045255138,0.000006063042,0.000022065557,0.000012762686,0.000020257317],"domain_scores_gemma":[0.9999378,0.0000062805716,0.000019091862,0.000007762752,0.000019426552,0.000009637095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017688861,0.00035482887,0.0002309128,0.0023816116,0.00036803505,0.0006119702,0.00026691065,0.00030036768,0.0014136288],"category_scores_gemma":[0.00020020158,0.00017429802,0.00026511122,0.0013907618,0.00044807975,0.0002126143,0.0007791125,0.00013116655,0.00032408992],"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":[0.00030223562,0.000028938086,0.90073013,0.0001631204,0.00016750915,0.0033967416,0.006843563,0.0010920963,0.052003767,0.00030811675,0.00037215915,0.034591638],"study_design_scores_gemma":[0.0000013069756,0.00001109756,0.99811506,0.000007682438,0.000007953518,0.0001424904,0.0004344945,0.00008706775,0.00035146193,0.000010959946,0.0008284947,0.0000018474532],"about_ca_topic_score_codex":0.044433407,"about_ca_topic_score_gemma":0.06960003,"teacher_disagreement_score":0.044433407,"about_ca_system_score_codex":0.00076505204,"about_ca_system_score_gemma":0.00025969994,"threshold_uncertainty_score":0.08834958},"labels":[],"label_agreement":null},{"id":"W3213102622","doi":"10.1017/s0016756821001023","title":"The Pre-Grenvillian assembly of the southeastern Laurentian margin through the U–Pb–Hf detrital zircon record of Mesoproterozoic supracrustal sequences (Central Grenville Province, Quebec, Canada)","year":2021,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Université du Québec à Montréal","funders":"","keywords":"Zircon; Geology; Laurentia; Geochemistry; Sedimentary depositional environment; Crust; Supercontinent; Rodinia; Geochronology; Precambrian; Continental crust; Magmatism; Ordovician; Paleontology; Craton; Tectonics","score_opus":0.009077346898152391,"score_gpt":0.185089503159455,"score_spread":0.1760121562613026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3213102622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99264175,0.00063972175,0.00020541764,0.00008452139,0.0000049772048,0.000013049875,0.00072750857,0.00002977916,0.005653342],"genre_scores_gemma":[0.99662435,0.00012622599,0.00022102597,0.000029445268,0.0000021633707,0.0000040388613,0.00048624811,0.000011302642,0.0024952914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980253,0.000008333397,0.000007111868,0.000063826505,0.00005495523,0.00006323547],"domain_scores_gemma":[0.99972385,0.0000137166635,0.000050781604,0.000011922473,0.00016068821,0.000039067538],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021544288,0.0002589189,0.00024019656,0.0013272144,0.0014345523,0.001182945,0.0005052198,0.00024365344,0.002324529],"category_scores_gemma":[0.00035023788,0.000120006756,0.00016071828,0.0009824436,0.0006348363,0.00022819903,0.00039594475,0.00020906203,0.0002914284],"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":[0.00020021896,0.000030736213,0.8583828,0.00011120083,0.00012440892,0.000791042,0.0040062796,0.0010437105,0.08812221,0.0007400596,0.0012053786,0.04524192],"study_design_scores_gemma":[0.0000016252219,0.000007080119,0.9960485,0.000010974512,0.0000049093187,0.000060845003,0.00035889572,0.0001395418,0.0006060922,0.000010675856,0.002746981,0.0000038289313],"about_ca_topic_score_codex":0.9449145,"about_ca_topic_score_gemma":0.9808498,"teacher_disagreement_score":0.05508548,"about_ca_system_score_codex":0.008020495,"about_ca_system_score_gemma":0.0038063002,"threshold_uncertainty_score":0.1108197},"labels":[],"label_agreement":null},{"id":"W3213877518","doi":"10.1017/s0016756821001096","title":"Late Ediacaran occurrences of the organic-walled microfossils<i>Granomarginata</i>and flask-shaped<i>Lagoenaforma collaris</i>gen. et sp. nov.","year":2021,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"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":"Ministerio de Asuntos Económicos y Transformación Digital, Gobierno de España; Norges Forskningsråd; Universidad de Extremadura; Vetenskapsrådet","keywords":"Baltica; Paleontology; Geology; Range (aeronautics); Taxon; Trilobite; Arctic; Ordovician; Biostratigraphy; Assemblage (archaeology); Peninsula; Archaeology; Geography; Oceanography","score_opus":0.012839247541755807,"score_gpt":0.21453986267706562,"score_spread":0.20170061513530982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3213877518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99405956,0.0006167645,0.0002264937,0.000017484486,0.000011233321,0.000009515991,0.0004415815,0.000021768845,0.004595614],"genre_scores_gemma":[0.99800307,0.0002964091,0.00039605147,0.000020542657,0.0000049891955,0.0000054759917,0.00058611715,0.000003883733,0.0006833592],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999391,0.0000035987175,0.0000044398494,0.000026240205,0.000008482855,0.000018178798],"domain_scores_gemma":[0.9999155,0.000009848802,0.00003801967,0.0000075572743,0.000014618869,0.000014423896],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009478257,0.00025708022,0.00013913275,0.0006726912,0.00048203825,0.0005424274,0.00022447693,0.00013179895,0.001401068],"category_scores_gemma":[0.00011509931,0.000098162476,0.00012328073,0.000873838,0.0003419438,0.00016784645,0.0004564508,0.00018162043,0.00022652937],"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":[0.0004087866,0.000041228774,0.8503453,0.00021923696,0.00012044304,0.0028634153,0.0031766065,0.00031571413,0.067253985,0.00040769455,0.00064471096,0.07420279],"study_design_scores_gemma":[0.00000950409,0.000040291787,0.9869077,0.000032492593,0.00003053209,0.0009605228,0.0009472695,0.00005915939,0.0017513344,0.000033971894,0.00922269,0.0000045464117],"about_ca_topic_score_codex":0.016109727,"about_ca_topic_score_gemma":0.044837527,"teacher_disagreement_score":0.016109727,"about_ca_system_score_codex":0.00040481825,"about_ca_system_score_gemma":0.00023897558,"threshold_uncertainty_score":0.032031953},"labels":[],"label_agreement":null},{"id":"W4200452112","doi":"10.1017/s0016756821001187","title":"Distribution and correlation of<i>Sabellidites cambriensis</i>(Annelida?) in the basal Cambrian on Baltica","year":2021,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":20,"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":"Uppsala Universitet; Norges Forskningsråd","keywords":"Acritarch; Baltica; Paleontology; Geology; Global Boundary Stratotype Section and Point; Paleozoic; Stratotype; Range (aeronautics); Ordovician; Arctic; Stage (stratigraphy); Oceanography","score_opus":0.014319159714541793,"score_gpt":0.21485638251511066,"score_spread":0.20053722280056888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200452112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99854124,0.0002562286,0.00002200296,0.000007790976,0.000001309423,0.000002523618,0.00012421545,0.0000029403238,0.0010417874],"genre_scores_gemma":[0.9994486,0.00008915444,0.00005816747,0.00000552803,0.0000011844013,0.0000026493215,0.0002176311,0.0000010423895,0.0001760193],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986637,0.000013625471,0.00000991449,0.000048258833,0.000023527575,0.00003837123],"domain_scores_gemma":[0.99975485,0.000027097874,0.0000979912,0.0000164764,0.00005475863,0.000048912283],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014894028,0.00017940922,0.00014292108,0.0020193828,0.0006352082,0.00050808024,0.00031388056,0.00027736722,0.0014318015],"category_scores_gemma":[0.0002728772,0.00015283143,0.00011326742,0.0012590003,0.000618121,0.0002308265,0.0005495266,0.00017994545,0.00026991524],"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":[0.00005757872,0.00001111815,0.97971535,0.000037774553,0.000020404717,0.0001442503,0.001630058,0.000084720836,0.01019211,0.0000703647,0.000089865396,0.0079463795],"study_design_scores_gemma":[4.9316174e-7,0.0000049454243,0.9991611,0.00000573705,0.0000016455728,0.000032991622,0.00036078267,0.000027863003,0.0000852812,0.0000043373097,0.0003139764,8.118342e-7],"about_ca_topic_score_codex":0.046779882,"about_ca_topic_score_gemma":0.1185123,"teacher_disagreement_score":0.046779882,"about_ca_system_score_codex":0.00059918594,"about_ca_system_score_gemma":0.00028677643,"threshold_uncertainty_score":0.093015134},"labels":[],"label_agreement":null},{"id":"W4200575871","doi":"10.1017/s0016756821001114","title":"Triassic trachytic volcanism in the Bangong–Nujiang Ocean: geochemical and geochronological constraints on a continental rifting event","year":2021,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"Université Laval","funders":"China Geological Survey","keywords":"Geology; Terrane; Rift; Geochemistry; Gondwana; Zircon; Continental margin; Petrogenesis; Craton; Continental crust; Supercontinent; Continental collision; Fibrous joint; Geochronology; Paleontology; Lithosphere; Mantle (geology); Tectonics","score_opus":0.014212620807407381,"score_gpt":0.21204559288285504,"score_spread":0.19783297207544767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200575871","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99881965,0.00013147664,0.00003413936,0.000009226507,0.000001500494,0.0000025934842,0.00007702609,0.0000031134962,0.00092116353],"genre_scores_gemma":[0.9996891,0.000057561843,0.00003530207,0.0000030922245,0.0000014182464,0.000001637295,0.00008853916,0.0000012796157,0.00012215688],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999136,0.000011559437,0.000011006491,0.00002487994,0.000016447286,0.000022515296],"domain_scores_gemma":[0.99976045,0.000022066051,0.000091049005,0.000016906728,0.000054100132,0.000055435445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002575672,0.00035920084,0.0002187339,0.001176937,0.0006408518,0.0008956766,0.00026494672,0.00019608988,0.0013496946],"category_scores_gemma":[0.00028607,0.00020791918,0.00014048668,0.0016295818,0.0005082011,0.00028931338,0.0005950193,0.0001416948,0.00019006668],"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":[0.00022918303,0.000026423306,0.96728534,0.000054695724,0.000038443777,0.0004231795,0.0017945115,0.0002335796,0.021730827,0.00017484362,0.000055223256,0.007953644],"study_design_scores_gemma":[0.0000025514942,0.00001676201,0.9989397,0.000005202765,0.0000072984476,0.000051965195,0.00037217574,0.00012539944,0.00022939953,0.000015509953,0.00023211181,0.0000019956117],"about_ca_topic_score_codex":0.035756536,"about_ca_topic_score_gemma":0.05608633,"teacher_disagreement_score":0.035756536,"about_ca_system_score_codex":0.0007970531,"about_ca_system_score_gemma":0.00045017074,"threshold_uncertainty_score":0.07109678},"labels":[],"label_agreement":null},{"id":"W4220945571","doi":"10.1017/s0016756822000103","title":"Variation of lacustrine carbonate deposition in the Eocene Dongying Depression and its comparison with Holocene environments","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":5,"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":"Geology; Calcite; Carbonate; Dolomite; Terrigenous sediment; Sedimentary depositional environment; Geochemistry; Deposition (geology); Sedimentary rock; Holocene; Carbonate rock; Anhydrite; Gypsum; Paleontology; Sediment; Structural basin; Chemistry","score_opus":0.016804809998037098,"score_gpt":0.21451665731963515,"score_spread":0.19771184732159805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220945571","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997383,0.000054373322,0.000015852464,0.0000033457616,3.9689047e-7,8.9052537e-7,0.000053463562,8.44718e-7,0.00013253375],"genre_scores_gemma":[0.9997317,0.00003578355,0.00003295595,0.0000018816589,7.554131e-7,0.0000015917933,0.00011149865,5.3790876e-7,0.000083364444],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999231,0.000006868435,0.0000073596457,0.000027591634,0.000012158875,0.000022904042],"domain_scores_gemma":[0.99986625,0.000012840156,0.00004738607,0.000009169526,0.000028903662,0.00003545426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012838273,0.00016202078,0.00016308887,0.00082279596,0.00038270923,0.0003321334,0.00018841334,0.00016625045,0.00061813754],"category_scores_gemma":[0.00021387673,0.00013904601,0.000140682,0.0011603141,0.00026784773,0.00015941623,0.00029422995,0.000101360485,0.00005215261],"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":[0.000047177455,0.0000071382137,0.9858289,0.000022812024,0.000055228935,0.00016809668,0.0012413108,0.000089672336,0.0081783505,0.000060270086,0.00004208903,0.004258857],"study_design_scores_gemma":[5.865291e-7,0.000004204115,0.99964464,7.967937e-7,0.0000031713298,0.00001951335,0.00014024727,0.000028510683,0.000055744284,0.0000023268954,0.00009965385,6.770793e-7],"about_ca_topic_score_codex":0.04400277,"about_ca_topic_score_gemma":0.087546125,"teacher_disagreement_score":0.04400277,"about_ca_system_score_codex":0.000549848,"about_ca_system_score_gemma":0.000287412,"threshold_uncertainty_score":0.0874933},"labels":[],"label_agreement":null},{"id":"W4237741887","doi":"10.1017/s0016756817000024","title":"GEO volume 154 issue 2 Cover and Back matter","year":2017,"lang":"en","type":"paratext","venue":"Geological Magazine","topic":"Geographic Information Systems Studies","field":"Social Sciences","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":"University of British Columbia","funders":"","keywords":"Cover (algebra); Volume (thermodynamics); Action (physics); Content (measure theory); Computer science; Environmental science; Engineering; Mathematics; Physics; Mechanical engineering","score_opus":0.024484509678357,"score_gpt":0.2954288093877595,"score_spread":0.2709442997094025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237741887","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00032414173,0.0013758802,0.00020153134,0.0053796326,0.019463552,0.000040110055,0.0030415745,0.0005882853,0.96958524],"genre_scores_gemma":[0.001093218,0.0008589838,0.00006676465,0.0011436604,0.0021362517,0.000019451718,0.0012747563,0.0003387376,0.9930682],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99939525,0.00005099088,0.00002032,0.000085003,0.00036834495,0.00007996075],"domain_scores_gemma":[0.99843043,0.00022160269,0.00005581022,0.00021923704,0.00074815383,0.0003247284],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053417304,0.00080721354,0.0008739341,0.0030806416,0.0022451945,0.00777064,0.0008560846,0.0016984686,0.8118352],"category_scores_gemma":[0.0034559073,0.00030472543,0.0004163325,0.003473238,0.0010077145,0.003681509,0.0024917722,0.0018305994,0.74696565],"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":[0.000006176387,0.0000068261093,0.000044808683,0.000051404677,8.0984586e-7,0.000012825568,0.0000143943835,0.000014294072,0.000048620772,0.0017104803,0.9835587,0.014530621],"study_design_scores_gemma":[0.0000015468389,0.000002579094,0.00013980831,0.000044086675,5.519033e-7,0.0000104188375,0.00003974851,0.000013429183,0.00002397209,0.000425798,0.99929667,0.000001245129],"about_ca_topic_score_codex":0.0045329933,"about_ca_topic_score_gemma":0.0076034945,"teacher_disagreement_score":0.8118352,"about_ca_system_score_codex":0.0018401588,"about_ca_system_score_gemma":0.0020606038,"threshold_uncertainty_score":0.26839423},"labels":[],"label_agreement":null},{"id":"W4241615317","doi":"10.1017/s0016756817000486","title":"GEO volume 154 issue 4 Cover and Back matter","year":2017,"lang":"en","type":"paratext","venue":"Geological Magazine","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","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":"University of British Columbia","funders":"","keywords":"Cover (algebra); Volume (thermodynamics); Action (physics); Content (measure theory); Environmental science; Computer science; Engineering; Physics; Mathematics; Mechanical engineering","score_opus":0.020496740025966152,"score_gpt":0.23270751338313028,"score_spread":0.21221077335716412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241615317","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003142101,0.0013253515,0.00023465432,0.0051564192,0.020291694,0.000038181384,0.0026950375,0.0005908708,0.9693535],"genre_scores_gemma":[0.00096066756,0.0008095416,0.0000691079,0.0010655216,0.0021429912,0.000017419286,0.001116908,0.00035287856,0.993465],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99940443,0.00004853782,0.000019774026,0.000080484715,0.00037057337,0.0000762525],"domain_scores_gemma":[0.99839044,0.00020841385,0.000056676185,0.00020522828,0.00080524373,0.0003340072],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00051422627,0.00082977425,0.00086256093,0.00278895,0.0022337162,0.0074231215,0.00083723554,0.0015740966,0.80761015],"category_scores_gemma":[0.0032385543,0.00030306872,0.00041471975,0.0030485187,0.0009785705,0.0036902325,0.0025442203,0.0019233833,0.7521501],"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":[0.0000062978406,0.0000074901627,0.000044655077,0.00005031783,8.644361e-7,0.000011906209,0.000013253032,0.000017202328,0.000054148353,0.0018552525,0.98249394,0.015444816],"study_design_scores_gemma":[0.0000013288419,0.0000025330464,0.00011876963,0.000042443753,5.572921e-7,0.000009896323,0.000034991615,0.000014444768,0.000027371283,0.00047303576,0.99927324,0.000001277261],"about_ca_topic_score_codex":0.0041091447,"about_ca_topic_score_gemma":0.007191871,"teacher_disagreement_score":0.19238985,"about_ca_system_score_codex":0.00177198,"about_ca_system_score_gemma":0.0020735443,"threshold_uncertainty_score":0.27442068},"labels":[],"label_agreement":null},{"id":"W4281738567","doi":"10.1017/s0016756822000371","title":"Continuous versus punctuated vein widening in the Marcellus Formation, USA: the fine line between pressure fringes and hydraulic fractures","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","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":"Shell (Canada)","funders":"","keywords":"Geology; Calcite; Hydraulic fracturing; Brittleness; Fracture (geology); Vein; Fluid pressure; Deformation (meteorology); Petrology; Geotechnical engineering; Mineralogy; Materials science; Composite material; Mechanics","score_opus":0.01617676569230063,"score_gpt":0.2311548368973584,"score_spread":0.2149780712050578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281738567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999458,0.000024912328,0.00004990024,0.000005703671,3.1875203e-7,0.000001909722,0.00003296481,0.0000030918868,0.0004232215],"genre_scores_gemma":[0.99976236,0.000010927604,0.000102552454,0.0000018781848,5.8399417e-7,0.0000010972398,0.000024914829,8.706908e-7,0.00009471283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999273,0.000005232896,0.0000040325663,0.000027227105,0.000019894393,0.000016290205],"domain_scores_gemma":[0.999826,0.000028802067,0.00006338652,0.000010885051,0.00004443026,0.000026516454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000113331604,0.000069078145,0.000108930355,0.00092339964,0.00030619345,0.000308719,0.00015711144,0.00013694765,0.00051627203],"category_scores_gemma":[0.00046937563,0.00010206424,0.00006171048,0.00043865442,0.0004619241,0.00019123226,0.0003900855,0.00012769463,0.00006352443],"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":[0.00021096815,0.000037701662,0.8940088,0.000031422423,0.000030049208,0.00054182933,0.0013735843,0.00079244556,0.07918301,0.0004608407,0.000101408645,0.023227818],"study_design_scores_gemma":[0.0000018901793,0.000023839764,0.9973199,0.0000028249317,0.0000033592069,0.00007850045,0.0002423971,0.00051962363,0.0014598459,0.000029153067,0.00031634327,0.0000023699117],"about_ca_topic_score_codex":0.030407626,"about_ca_topic_score_gemma":0.10996347,"teacher_disagreement_score":0.030407626,"about_ca_system_score_codex":0.0003589174,"about_ca_system_score_gemma":0.00028827644,"threshold_uncertainty_score":0.060461283},"labels":[],"label_agreement":null},{"id":"W4285034030","doi":"10.1017/s0016756822000449","title":"Zircon geochronology and Hf isotopic study from the Leo Pargil Dome, India: implications for the palaeogeographic reconstruction and tectonic evolution of a Himalayan gneiss dome","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"Queen's University","funders":"","keywords":"Zircon; Geology; Geochronology; Geochemistry; Provenance; Orogeny; Anatexis; Gondwana; Craton; Gneiss; Rodinia; Ordovician; Migmatite; Population; Paleontology; Crust; Tectonics; Metamorphic rock; Partial melting","score_opus":0.011041856570599395,"score_gpt":0.20085162164081322,"score_spread":0.18980976507021383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285034030","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99848264,0.000057994985,0.00009614159,0.000018271501,0.0000010441128,0.0000022455854,0.00020264335,0.000009874518,0.001129072],"genre_scores_gemma":[0.9993273,0.000039587092,0.00008998839,0.000006312455,0.0000015643221,0.0000014028058,0.00020838712,0.0000033855936,0.00032217507],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99994457,0.0000048753827,0.0000034835014,0.000017939472,0.000008714349,0.000020446181],"domain_scores_gemma":[0.99993646,0.000010301906,0.0000138491705,0.000010041098,0.000017791457,0.000011595985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000093655915,0.0001524187,0.000093902476,0.001016982,0.0005182383,0.0007012739,0.00021822355,0.00012702074,0.0009196829],"category_scores_gemma":[0.00013983528,0.00015383087,0.00011983762,0.0009544743,0.00031961224,0.00013665,0.0002727271,0.00011437186,0.00023187471],"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":[0.0001465545,0.000025680514,0.9350125,0.00004503608,0.000036579728,0.0008016289,0.0035473758,0.00047064267,0.042915817,0.00040160856,0.0001712883,0.016425213],"study_design_scores_gemma":[0.0000018633716,0.000015019743,0.99774325,0.0000031057068,0.000011115369,0.00015686749,0.00054829207,0.00016913947,0.0007754773,0.00001726406,0.00055582094,0.0000028491904],"about_ca_topic_score_codex":0.047516894,"about_ca_topic_score_gemma":0.07495923,"teacher_disagreement_score":0.047516894,"about_ca_system_score_codex":0.00056004635,"about_ca_system_score_gemma":0.00034624385,"threshold_uncertainty_score":0.094480634},"labels":[],"label_agreement":null},{"id":"W4285088045","doi":"10.1017/s0016756822000462","title":"Fractures in the Niagara Escarpment in Ontario, Canada: distribution, connectivity, and geohazard implications","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":9,"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; McMaster University","funders":"","keywords":"Escarpment; Geology; Rockfall; Bedding; Outcrop; Bed; Geomorphology; Fracture (geology); Classification of discontinuities; Subsidence; Cliff; Mining engineering; Paleontology; Landslide; Anisotropy","score_opus":0.00848450493628939,"score_gpt":0.20705637879453878,"score_spread":0.1985718738582494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285088045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941906,0.00029837247,0.00037420043,0.00012274693,0.000002555074,0.000040983614,0.0022281287,0.000016860224,0.0027256357],"genre_scores_gemma":[0.9980882,0.00016733744,0.0004255561,0.000013124542,0.0000010137118,0.000013428173,0.00037425963,0.0000029974224,0.00091395783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970585,0.000014187172,0.000011631007,0.00007424111,0.00011072077,0.0000832837],"domain_scores_gemma":[0.99919564,0.00009391649,0.00017545007,0.000034920093,0.00038649977,0.00011351343],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001545326,0.00020600583,0.00019127969,0.0016144064,0.0019319877,0.0013743535,0.0007996457,0.0004197249,0.0016154636],"category_scores_gemma":[0.0010001474,0.00021091785,0.00020461339,0.0034353475,0.0012062248,0.00025147194,0.0007412381,0.00025287413,0.00016988812],"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":[0.00007739431,0.000025930967,0.96546125,0.00012154765,0.000051853647,0.00050232065,0.0034780423,0.0032356558,0.0020190973,0.0007749149,0.0012341224,0.023017863],"study_design_scores_gemma":[0.0000025843358,0.000011340073,0.9927851,0.00003701253,0.000012583383,0.00008318429,0.0032906965,0.0021631953,0.00011822433,0.000092995375,0.0013933611,0.000009815568],"about_ca_topic_score_codex":0.9911907,"about_ca_topic_score_gemma":0.9978309,"teacher_disagreement_score":0.015579646,"about_ca_system_score_codex":0.015579646,"about_ca_system_score_gemma":0.012078682,"threshold_uncertainty_score":0.11303878},"labels":[],"label_agreement":null},{"id":"W4285988301","doi":"10.1017/s0016756822000590","title":"Zinc, sulfur and cadmium isotopes and Zn/Cd ratios as indicators of the origin of the supergiant Broken Hill Pb–Zn–Ag deposit and other Broken Hill-type deposits, New South Wales, Australia","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"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":"Queen's University; National Science Foundation","keywords":"Sphalerite; Geology; Geochemistry; Sulfur; Isotope; Pyrite; Mineralogy; Chemistry","score_opus":0.015902378052918043,"score_gpt":0.20861453062256105,"score_spread":0.192712152569643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285988301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991104,0.000045454024,0.000045282686,0.0000065797167,5.7767113e-7,0.0000035954743,0.00007024833,0.0000019920278,0.00071578444],"genre_scores_gemma":[0.99880815,0.000036894373,0.00015966904,0.0000067203873,7.3923667e-7,0.0000037837924,0.000094457704,0.0000016403121,0.00088801724],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998945,0.000012892188,0.000013684951,0.000029663786,0.000033149456,0.000016056161],"domain_scores_gemma":[0.9997367,0.000023751734,0.00007489373,0.000014904235,0.00009856357,0.000051262075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021043615,0.00016528343,0.00013643254,0.00138368,0.00046903928,0.00039045178,0.0003150435,0.00016132215,0.0010767679],"category_scores_gemma":[0.00037416586,0.00024314313,0.00012759263,0.0007070144,0.00049041474,0.00022811093,0.0005105554,0.00012354198,0.00022277822],"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":[0.00020474507,0.000016093836,0.9528935,0.00008426642,0.00007364758,0.00038975308,0.0021101783,0.00022495704,0.0355311,0.00014483293,0.00013427035,0.008192563],"study_design_scores_gemma":[0.0000012212566,0.000010347393,0.9990307,0.0000029275816,0.0000042501756,0.000058102847,0.00023798936,0.000109813634,0.0003766988,0.000009584123,0.00015739967,0.0000010080073],"about_ca_topic_score_codex":0.14585175,"about_ca_topic_score_gemma":0.33947527,"teacher_disagreement_score":0.14585175,"about_ca_system_score_codex":0.0009163102,"about_ca_system_score_gemma":0.00033288312,"threshold_uncertainty_score":0.29000556},"labels":[],"label_agreement":null},{"id":"W4291555457","doi":"10.1017/s0016756822000619","title":"Petrology and Sr–Nd isotope geochemistry of Mosonik: a polygenetic phonolitic nephelinite–phonolite volcano located in the North Tanzanian Divergence of the East African Rift","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"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","funders":"Lakehead University","keywords":"Geology; Carbonatite; Geochemistry; Fractional crystallization (geology); Phenocryst; Craton; Partial melting; Amphibole; Mantle plume; Mantle (geology); Petrology; Lithosphere; Volcanic rock; Volcano; Paleontology; Tectonics; Quartz","score_opus":0.009696814870616185,"score_gpt":0.17704742588792338,"score_spread":0.1673506110173072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4291555457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99972934,0.000024301156,0.000013224437,0.000003274711,3.352971e-7,0.0000016837005,0.000061118335,0.0000011725451,0.00016553856],"genre_scores_gemma":[0.99968565,0.000014969554,0.000045252367,0.0000031339196,6.3637566e-7,0.0000014326429,0.00008664726,0.0000012905208,0.00016094172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999583,0.0000030384663,0.000002658366,0.000013799256,0.0000060711773,0.000016150761],"domain_scores_gemma":[0.9999422,0.000006379078,0.000016150718,0.0000045518404,0.000012455372,0.000018418348],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006684376,0.00025963606,0.00014567368,0.00088541297,0.0004834722,0.00030642768,0.00018586601,0.0002561942,0.00095504324],"category_scores_gemma":[0.00014316483,0.00019684031,0.00012352265,0.0004646613,0.000394322,0.00014777532,0.00027388064,0.00012696868,0.00024063712],"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":[0.00032144797,0.000033967703,0.82652247,0.00006203237,0.000040789357,0.0028335305,0.002519727,0.0003785757,0.1613412,0.0000991008,0.00009158204,0.005755585],"study_design_scores_gemma":[0.000002218157,0.000018130637,0.9985719,0.0000019312529,0.0000050655144,0.00015642866,0.00027486493,0.000099433906,0.00072125264,0.0000041954004,0.00014278664,0.0000018732345],"about_ca_topic_score_codex":0.035702746,"about_ca_topic_score_gemma":0.07056865,"teacher_disagreement_score":0.035702746,"about_ca_system_score_codex":0.0006371323,"about_ca_system_score_gemma":0.00023316676,"threshold_uncertainty_score":0.07098985},"labels":[],"label_agreement":null},{"id":"W4292332816","doi":"10.1017/s0016756822000656","title":"Reconstruction of cyclic Mesozoic–Cenozoic stress development in SE Germany using fault-slip and stylolite inversion","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"University of Calgary","funders":"European Regional Development Fund; Bayerisches Landesamt für Umwelt; European Commission","keywords":"Stylolite; Geology; Inversion (geology); Paleontology; Tectonics; Cenozoic; Seismology; Cretaceous; Thrust fault; Permian; Slip (aerodynamics); Diagenesis; Structural basin","score_opus":0.02117211415132421,"score_gpt":0.2125334165135631,"score_spread":0.19136130236223892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292332816","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99846613,0.000043883614,0.000539104,0.000014325371,0.0000015304985,0.0000023595142,0.0004443343,0.00003859994,0.0004498044],"genre_scores_gemma":[0.9994795,0.000017572944,0.0002127713,0.0000012026703,6.089979e-7,8.150427e-7,0.00019055349,0.0000030602328,0.000094052804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993265,0.0000070024,0.0000041974886,0.00002344279,0.000009686979,0.000023121223],"domain_scores_gemma":[0.99989915,0.0000107187025,0.000034781133,0.000012485113,0.000028064384,0.0000148587405],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012777721,0.00027592762,0.00016260069,0.0012074485,0.00016471687,0.0005005601,0.00018941592,0.00027593394,0.001264287],"category_scores_gemma":[0.00032360767,0.00016461717,0.00023351602,0.0010263665,0.00023429883,0.00017469403,0.0002749169,0.00013562446,0.00022710593],"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":[0.00035805625,0.000059926773,0.82386845,0.00008654527,0.00025787178,0.00077238656,0.0006219053,0.08040976,0.052048612,0.0011199955,0.0005707752,0.039825674],"study_design_scores_gemma":[0.000012446374,0.000031574986,0.9327575,0.000018620394,0.000029731538,0.00009537866,0.00020936503,0.0637315,0.0017723689,0.00012983763,0.0011893824,0.000022197057],"about_ca_topic_score_codex":0.06552973,"about_ca_topic_score_gemma":0.09858992,"teacher_disagreement_score":0.06552973,"about_ca_system_score_codex":0.0008577785,"about_ca_system_score_gemma":0.0004597196,"threshold_uncertainty_score":0.13029659},"labels":[],"label_agreement":null},{"id":"W4292479209","doi":"10.1017/s0016756822000723","title":"Morphological variation in the rangeomorph organism <i>Fractofusus misrai</i> from the Ediacaran of Newfoundland, Canada","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","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":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Department of Fisheries and Land Resources; University of Oxford","keywords":"Taphonomy; Paleontology; Geology; Branching (polymer chemistry); Sediment; Chemistry","score_opus":0.012871625010664774,"score_gpt":0.1893141767207808,"score_spread":0.17644255171011602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292479209","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99518555,0.00036721866,0.00009116079,0.00003088479,0.000004705446,0.000009636669,0.0008416748,0.00000918951,0.00345995],"genre_scores_gemma":[0.99783945,0.00018811754,0.00025925855,0.000024091032,0.0000020107927,0.000006684341,0.0005944558,0.00000659306,0.0010792138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997898,0.000008414252,0.000010748227,0.00007140297,0.00004988216,0.000069710746],"domain_scores_gemma":[0.9995436,0.000030693718,0.000108423286,0.0000232673,0.00019960702,0.000094368464],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013353418,0.00028981332,0.00026407893,0.0031332313,0.0018864117,0.0009592683,0.0005332499,0.00022008028,0.0019947384],"category_scores_gemma":[0.00029831377,0.00020158551,0.00018006629,0.0024016716,0.0012825851,0.00028351415,0.000557857,0.00028859294,0.00041143253],"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":[0.00015513336,0.000027936241,0.9406148,0.00008318734,0.000077226294,0.0005086869,0.0059927106,0.00014678921,0.017272377,0.0002633125,0.0009817327,0.03387618],"study_design_scores_gemma":[4.4598596e-7,0.0000059336094,0.9980849,0.0000065562913,0.00000428179,0.000120663026,0.0007575875,0.000017582834,0.00012484152,0.0000045424113,0.000869864,0.0000027953215],"about_ca_topic_score_codex":0.8362456,"about_ca_topic_score_gemma":0.97267616,"teacher_disagreement_score":0.1637544,"about_ca_system_score_codex":0.006148751,"about_ca_system_score_gemma":0.0019210057,"threshold_uncertainty_score":0.32943755},"labels":[],"label_agreement":null},{"id":"W4294591475","doi":"10.1017/s0016756822000553","title":"Discussion of Searle, ‘Tectonic evolution of the Caledonian orogeny in Scotland: a review based on the timing of magmatism, metamorphism and deformation’","year":2022,"lang":"en","type":"review","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"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":"Geology; Orogeny; Metamorphism; Dalradian; Baltica; Laurentia; Ordovician; Paleontology; Devonian; Obduction; Continental collision; Subduction; Tectonics; Oceanic crust","score_opus":0.03362397043641504,"score_gpt":0.24080404384822632,"score_spread":0.20718007341181127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294591475","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":[0.0006800471,0.9921808,0.0000692696,0.0046374714,0.0020189339,0.0000043985588,0.00006223658,0.0000061140786,0.0003407203],"genre_scores_gemma":[0.008743254,0.9762996,0.00016493376,0.008736115,0.0053016734,0.00001668831,0.00014710546,0.000007105388,0.00058360083],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99897873,0.0002314266,0.00023979155,0.00018016527,0.00023397869,0.00013589022],"domain_scores_gemma":[0.9964212,0.0019256376,0.00064448273,0.00007811904,0.0007420445,0.00018846313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0036702957,0.0008995707,0.002034454,0.006867787,0.0008466908,0.0022984552,0.0017810558,0.0021241563,0.0018182036],"category_scores_gemma":[0.005799078,0.00037772593,0.00098109,0.007985089,0.0020964455,0.003083931,0.001629008,0.0015797196,0.0004926534],"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":[0.00033482251,0.000097876255,0.0072274255,0.058776435,0.0005140404,0.004461172,0.003375496,0.0007198716,0.0020362127,0.015136185,0.29902053,0.6082999],"study_design_scores_gemma":[0.000019261717,0.00016506475,0.013861881,0.014646817,0.0002122811,0.002316016,0.00093005475,0.00006613192,0.0001888629,0.0009689494,0.966579,0.000045446734],"about_ca_topic_score_codex":0.01425309,"about_ca_topic_score_gemma":0.02716953,"teacher_disagreement_score":0.01425309,"about_ca_system_score_codex":0.0026764926,"about_ca_system_score_gemma":0.0033179764,"threshold_uncertainty_score":0.02834022},"labels":[],"label_agreement":null},{"id":"W4294592082","doi":"10.1017/s0016756822000838","title":"Reply to Dewey and Ryan Comment on Searle, MP (2021) ‘Tectonic evolution of the Caledonian orogeny in Scotland: a review based on the timing of magmatism, metamorphism and deformation’","year":2022,"lang":"en","type":"review","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","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":"","keywords":"Dalradian; Orogeny; Metamorphism; Laurentia; Baltica; Geology; Paleontology; Ordovician; Obduction; Stratotype; Alpine orogeny; Tectonics; Plate tectonics; Subduction","score_opus":0.033340867082808305,"score_gpt":0.2420440656162031,"score_spread":0.20870319853339478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294592082","genre_codex":"commentary","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":[0.0001128956,0.0020883128,0.00006599306,0.96925765,0.02803608,0.000004206365,0.00008106485,0.000020989228,0.00033275184],"genre_scores_gemma":[0.0016908644,0.0015496967,0.00015090789,0.9579026,0.0362767,0.0000330223,0.00004027867,0.00004927089,0.0023067885],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99295783,0.0013970593,0.00089679175,0.0019314808,0.0022163151,0.0006005],"domain_scores_gemma":[0.9584447,0.022316761,0.002868711,0.0013715377,0.010937573,0.004060654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.011102688,0.001323642,0.002198692,0.0014843732,0.0035925885,0.0042665484,0.0039796135,0.029486412,0.008029556],"category_scores_gemma":[0.053972505,0.0011285594,0.0015551249,0.0017304965,0.008141827,0.008913018,0.004644757,0.052135672,0.0067881923],"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":[0.000012933766,0.0000035057192,0.000074770745,0.000056109056,0.0000054864176,0.00010364093,0.00019629946,0.000012563985,0.000048824884,0.00067997555,0.9971512,0.00165468],"study_design_scores_gemma":[0.00003713383,0.000028790959,0.0010148233,0.0004691567,0.000017961987,0.0005694679,0.0008640039,0.00005641126,0.0002224497,0.0030610762,0.99358433,0.0000744104],"about_ca_topic_score_codex":0.0130819725,"about_ca_topic_score_gemma":0.014305932,"teacher_disagreement_score":0.029486412,"about_ca_system_score_codex":0.004058898,"about_ca_system_score_gemma":0.009515368,"threshold_uncertainty_score":0.05871737},"labels":[],"label_agreement":null},{"id":"W4301396766","doi":"10.1017/s0016756822000875","title":"A new species of the Ordovician horseshoe crab <i>Lunataspis</i>","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Subterranean biodiversity and taxonomy","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":true,"ca_institutions":"Royal Ontario Museum","funders":"National Science Foundation","keywords":"Horseshoe crab; Ordovician; Paleozoic; Biology; Horseshoe (symbol); Juvenile; Ontogeny; Living fossil; Paleontology; Morphology (biology); Zoology; Ecology","score_opus":0.031131266726031392,"score_gpt":0.17657818990786012,"score_spread":0.14544692318182872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4301396766","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9840105,0.0024897004,0.0009734236,0.00028458136,0.00013204786,0.00009365471,0.00075799465,0.00009262373,0.01116535],"genre_scores_gemma":[0.98897666,0.00074866496,0.0034007288,0.0003453991,0.00008042853,0.000037172522,0.0010531722,0.00001900311,0.00533893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997832,0.000010290774,0.000017561195,0.000074162,0.000053149346,0.00006165256],"domain_scores_gemma":[0.99950373,0.00005073988,0.000120442695,0.000052159176,0.00016886203,0.0001040805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013989463,0.0003146149,0.00035682195,0.0017344541,0.0030315279,0.0015398593,0.0007662548,0.0006303873,0.0030197145],"category_scores_gemma":[0.00035875713,0.00021756973,0.00022580118,0.0012763323,0.00145695,0.00043850305,0.00085737684,0.0005608196,0.0006793963],"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":[0.0008086597,0.0002306868,0.5433211,0.0007580466,0.0001777476,0.017557122,0.027536802,0.0007903611,0.1496517,0.0022583972,0.006138658,0.25077063],"study_design_scores_gemma":[0.000024570765,0.00024894055,0.86830276,0.00014970152,0.00006127781,0.011158678,0.006324755,0.00029166086,0.0025408817,0.00021843055,0.110613175,0.0000650895],"about_ca_topic_score_codex":0.10946752,"about_ca_topic_score_gemma":0.32951388,"teacher_disagreement_score":0.10946752,"about_ca_system_score_codex":0.0020118763,"about_ca_system_score_gemma":0.0013746468,"threshold_uncertainty_score":0.21766067},"labels":[],"label_agreement":null},{"id":"W4306681738","doi":"10.1017/s0016756822000887","title":"Winter weathering of fractured sedimentary rocks in a temperate climate: observation of freeze–thaw and thermal processes on the Niagara Escarpment, Hamilton, Ontario","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Climate change and permafrost","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":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; Mitacs; Universities Space Research Association; Geological Society of America","keywords":"Escarpment; Weathering; Geology; Lithology; Sedimentary rock; Temperate climate; Geomorphology; Geochemistry; Ecology","score_opus":0.03347094922590708,"score_gpt":0.21707523821560892,"score_spread":0.18360428898970185,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4306681738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986268,0.000052235268,0.000064252315,0.000018113591,0.0000012165012,0.000012515668,0.0003837208,0.000004779658,0.00083647284],"genre_scores_gemma":[0.99878806,0.00006342219,0.00018542538,0.000011642247,0.0000020225693,0.000012019421,0.00028175802,0.0000035650376,0.00065208203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998715,0.000008089953,0.0000057778525,0.000033391225,0.00004545777,0.000035859717],"domain_scores_gemma":[0.9996785,0.000018672808,0.00008350585,0.000014745621,0.00013232525,0.00007227146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000925588,0.00020694095,0.00023536483,0.000502005,0.0016712085,0.0006160417,0.00059148675,0.00019935603,0.0010271486],"category_scores_gemma":[0.0003478583,0.00023250077,0.00013908766,0.0009630012,0.0006261106,0.00020959631,0.0004286105,0.00021754194,0.00019485084],"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":[0.00014217122,0.000035122153,0.9732246,0.000037519963,0.00004174536,0.0003599135,0.0032852232,0.00024616485,0.016903825,0.00003901537,0.00037534724,0.005309352],"study_design_scores_gemma":[0.0000017997239,0.000007238322,0.99891293,0.0000023744715,0.000002981645,0.000017408449,0.0005550219,0.000075689495,0.00014357055,0.0000026880973,0.00027679466,0.0000015013242],"about_ca_topic_score_codex":0.9085996,"about_ca_topic_score_gemma":0.9798623,"teacher_disagreement_score":0.091400385,"about_ca_system_score_codex":0.00481743,"about_ca_system_score_gemma":0.0023040674,"threshold_uncertainty_score":0.18387729},"labels":[],"label_agreement":null},{"id":"W4311379830","doi":"10.1017/s0016756822001066","title":"Neo-Tethyan subduction triggered Eocene–Oligocene magmatism in eastern Iran","year":2022,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","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":"Carleton University","funders":"","keywords":"Geology; Geochemistry; Subduction; Volcanic rock; Felsic; Magmatism; Basalt; Igneous rock; Zircon; Petrogenesis; Andesite; Fractional crystallization (geology); Lithosphere; Partial melting; Paleontology; Volcano; Tectonics","score_opus":0.021846290303687947,"score_gpt":0.20808188405299347,"score_spread":0.1862355937493055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311379830","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99838126,0.0002057771,0.00007614444,0.0000461768,0.0000038991807,0.0000025436461,0.000051791674,0.0000073024416,0.0012250597],"genre_scores_gemma":[0.9994987,0.000119377226,0.00007326986,0.000007874008,0.000004549752,9.925047e-7,0.00006198226,0.000001448284,0.00023186792],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999522,0.0000030590415,0.0000034489576,0.00001200908,0.000013338314,0.000015876662],"domain_scores_gemma":[0.9999355,0.000003993666,0.000027435904,0.00000439875,0.000022456026,0.0000062364375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012440792,0.00015310141,0.00011575564,0.0009453673,0.00032982018,0.0002649755,0.0001881541,0.00012639633,0.00078959623],"category_scores_gemma":[0.00013148325,0.000106957516,0.000120402765,0.0007551742,0.00028007102,0.00021766499,0.00027253944,0.0001217392,0.00010523984],"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":[0.0001790179,0.000044501452,0.90913284,0.000108545886,0.00006744352,0.0015402226,0.0026892473,0.0010770246,0.031899426,0.0010046957,0.0005319492,0.05172512],"study_design_scores_gemma":[0.000003862327,0.0000144621345,0.99662066,0.0000053246413,0.000010152961,0.0002457741,0.00044854422,0.00022527747,0.00076906,0.000073384566,0.0015812957,0.0000022874062],"about_ca_topic_score_codex":0.024908507,"about_ca_topic_score_gemma":0.032995455,"teacher_disagreement_score":0.024908507,"about_ca_system_score_codex":0.0006760316,"about_ca_system_score_gemma":0.00045531808,"threshold_uncertainty_score":0.04952705},"labels":[],"label_agreement":null},{"id":"W4319038397","doi":"10.1017/s0016756822001248","title":"The megathermal ant genus <i>Gesomyrmex</i> (Formicidae: Formicinae), palaeoindicator of wide latitudinal biome homogeneity during the PETM","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Insect and Arachnid Ecology and Behavior","field":"Biochemistry, Genetics and Molecular Biology","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":"Royal Ontario Museum; University of Toronto","funders":"","keywords":"Biome; Cenozoic; Genus; Formicinae; Biodiversity; Paleontology; Ecology; Paleosol; Phanerozoic; Biology; Fossil Record; Ecosystem; Structural basin","score_opus":0.009668008623849688,"score_gpt":0.2367677521208766,"score_spread":0.2270997434970269,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319038397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963894,0.0008555284,0.00034066386,0.00004593592,0.0000064781857,0.000004369761,0.000093293216,0.000018737886,0.0022456301],"genre_scores_gemma":[0.9985898,0.00024299644,0.00048506193,0.000020306936,0.000007746412,0.0000025575157,0.00013354096,0.0000043489295,0.0005134862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999954,0.000009201921,0.000003321584,0.00001707886,0.000008361379,0.000008027773],"domain_scores_gemma":[0.9999006,0.000012251309,0.00004767613,0.000009944241,0.000014326442,0.000015186516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000092410206,0.00013798462,0.00008479487,0.00041462472,0.00033270926,0.00029678983,0.00013187462,0.00015992108,0.0009451885],"category_scores_gemma":[0.0001319472,0.00006943498,0.00008140994,0.0002192557,0.00037305482,0.00017653174,0.0003162032,0.00017117399,0.0002002795],"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":[0.00032266878,0.0000305205,0.7006791,0.00020097576,0.00007517675,0.000883919,0.0024299442,0.00045086528,0.21982943,0.00083572365,0.0007334951,0.07352824],"study_design_scores_gemma":[0.000002513031,0.00003769602,0.9891824,0.00002160823,0.000009884235,0.0017678727,0.00035679978,0.00025048267,0.0026706622,0.000069601774,0.005626862,0.000003559319],"about_ca_topic_score_codex":0.001153113,"about_ca_topic_score_gemma":0.004141983,"teacher_disagreement_score":0.001153113,"about_ca_system_score_codex":0.00020198802,"about_ca_system_score_gemma":0.00009743422,"threshold_uncertainty_score":0.0031619668},"labels":[],"label_agreement":null},{"id":"W4362576124","doi":"10.1017/s0016756822001303","title":"Petrogenesis and tectonic implications of the Early Carboniferous shoshonitic to calc-alkaline magmatic rocks of the southern Yili terrane, western Tianshan","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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 Windsor","funders":"","keywords":"Terrane; Geology; Carboniferous; Geochemistry; Subduction; Mantle (geology); Tectonics; Petrogenesis; Petrology; Paleontology; Structural basin","score_opus":0.01645206298826028,"score_gpt":0.2088406162161942,"score_spread":0.19238855322793394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362576124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99889284,0.000082979175,0.000034690966,0.0000152029725,7.187107e-7,0.0000018035159,0.00008142079,0.0000027690103,0.00088757393],"genre_scores_gemma":[0.9994085,0.00006669575,0.00003994777,0.0000030021602,0.000002050928,0.0000015521932,0.00012266758,0.0000015486328,0.00035412624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996865,0.0000022617849,0.0000025196111,0.000010279704,0.0000066979396,0.000009601312],"domain_scores_gemma":[0.9999186,0.000006205849,0.000028465945,0.0000055326714,0.000020289404,0.000020961348],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010748888,0.00017607567,0.00009451361,0.0012914139,0.00044580532,0.00041201184,0.00017173783,0.00014359741,0.0014592828],"category_scores_gemma":[0.00012647241,0.00013379024,0.00011631563,0.0008604422,0.00048485416,0.00015075531,0.00024438283,0.00012938422,0.0001568444],"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":[0.00005208632,0.000011384963,0.9646086,0.000037037833,0.000029176206,0.00040156732,0.0010406184,0.00038103733,0.025319766,0.00032979695,0.00009382281,0.0076950076],"study_design_scores_gemma":[0.0000012212768,0.0000059342683,0.99865663,0.0000023272153,0.0000059819977,0.000056814264,0.00026019418,0.00017589089,0.0004886904,0.000026284142,0.00031885467,0.0000012403697],"about_ca_topic_score_codex":0.034956902,"about_ca_topic_score_gemma":0.067979746,"teacher_disagreement_score":0.034956902,"about_ca_system_score_codex":0.00053239265,"about_ca_system_score_gemma":0.00046961557,"threshold_uncertainty_score":0.06950688},"labels":[],"label_agreement":null},{"id":"W4383263345","doi":"10.1017/s0016756823000365","title":"Constraining the evolution of shear zones in the Himalayan mid crust in Central–Western Nepal: implications for the tectonic evolution of the Himalayan metamorphic core","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","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":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Metamorphic rock; Shear zone; Metamorphic core complex; Discontinuity (linguistics); Crust; Shear (geology); Main Central Thrust; Tectonics; Monazite; Shearing (physics); Seismology; Paleontology; Geochemistry; Petrology; Extensional definition","score_opus":0.04017136012431984,"score_gpt":0.24502337567237867,"score_spread":0.20485201554805882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383263345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99620736,0.00037196354,0.00043087915,0.000080919424,0.0000023539003,0.0000063243388,0.0002813483,0.000011395529,0.0026074331],"genre_scores_gemma":[0.99893516,0.00017398756,0.00040346305,0.000021130083,0.0000037891925,0.0000034574243,0.00013827423,0.000003235478,0.00031743725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999337,0.0000107746955,0.0000062156864,0.000021736856,0.000013882377,0.00001370487],"domain_scores_gemma":[0.9998561,0.000034939312,0.00003136064,0.0000139364265,0.000044999524,0.00001854056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017289273,0.0001506148,0.00013065575,0.0014207305,0.00053259725,0.00095949863,0.00020570339,0.00018683831,0.0014540676],"category_scores_gemma":[0.00035873798,0.00014744935,0.00010470081,0.0013226414,0.000490721,0.00027199276,0.00058991683,0.00017394837,0.00018186859],"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":[0.00008686976,0.000037432623,0.89991415,0.00017088541,0.00010831519,0.0013139191,0.0039959084,0.0024979536,0.044733457,0.0010769538,0.00034787395,0.04571633],"study_design_scores_gemma":[0.0000024961507,0.000011327176,0.9954727,0.00001628263,0.000015784464,0.00016901789,0.0010233516,0.0010951143,0.0008318952,0.00018423323,0.0011726094,0.000005156842],"about_ca_topic_score_codex":0.0368336,"about_ca_topic_score_gemma":0.07223573,"teacher_disagreement_score":0.0368336,"about_ca_system_score_codex":0.00048733078,"about_ca_system_score_gemma":0.0005488341,"threshold_uncertainty_score":0.07323837},"labels":[],"label_agreement":null},{"id":"W4385580464","doi":"10.1017/s0016756823000419","title":"Metamorphic and intrusive history of the Hindu Raj region, northern Pakistan","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"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 Sciences and Engineering Research Council of Canada; University of Peshawar","keywords":"Hinduism; Geology; Metamorphism; Paleontology; Geography","score_opus":0.02063045371566339,"score_gpt":0.1940310916943647,"score_spread":0.1734006379787013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385580464","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99547005,0.00016052384,0.000066164896,0.000021040409,0.0000019197314,0.0000104380415,0.0002290545,0.0000056139465,0.004035194],"genre_scores_gemma":[0.9990922,0.00014494067,0.00012204157,0.000005991586,0.0000015037059,0.000003023506,0.00012399857,0.0000013308509,0.00050488795],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999021,0.000010844102,0.000007335723,0.000025813792,0.000026125126,0.000027708424],"domain_scores_gemma":[0.9998368,0.000023869496,0.00006223058,0.000012423904,0.000039190814,0.000025437312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012797877,0.0001483249,0.00009080794,0.0011430325,0.0010366095,0.0006184184,0.00019445646,0.00012098466,0.0022261771],"category_scores_gemma":[0.00025968906,0.00016455831,0.000062914696,0.0013873476,0.0005635778,0.00024095671,0.00048236898,0.00015124472,0.00030105517],"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":[0.00019679836,0.000049379763,0.91205823,0.00018440445,0.000043339223,0.0038412043,0.007849857,0.0005214364,0.019238511,0.00077746384,0.0003949505,0.054844357],"study_design_scores_gemma":[0.0000032918263,0.00004371765,0.9929329,0.000016533151,0.0000054290954,0.0008695459,0.003004533,0.000067480636,0.0005740686,0.000036282214,0.0024407026,0.0000054735756],"about_ca_topic_score_codex":0.05302293,"about_ca_topic_score_gemma":0.09667462,"teacher_disagreement_score":0.05302293,"about_ca_system_score_codex":0.0006970479,"about_ca_system_score_gemma":0.0006952944,"threshold_uncertainty_score":0.10542858},"labels":[],"label_agreement":null},{"id":"W4385636097","doi":"10.1017/s0016756823000407","title":"The genesis of metamorphosed Paleoproterozoic massive sulphide occurrences in central Colorado: geological, mineralogical and sulphur isotope constraints","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"U.S. Geological Survey; Society of Economic Geologists Foundation","keywords":"Geology; Geochemistry; Sphalerite; Galena; Felsic; Mafic; Cassiterite; Volcanic rock; Volcanogenic massive sulfide ore deposit; Metamorphic facies; Pyrite; Sillimanite; Biotite; Quartz; Volcano; Facies; Geomorphology; Tin","score_opus":0.02089166150388787,"score_gpt":0.2184033999195458,"score_spread":0.19751173841565792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385636097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989643,0.00012710091,0.000025759198,0.00001377655,5.5786563e-7,0.0000033962233,0.0001817207,0.0000029100236,0.0006804886],"genre_scores_gemma":[0.99932265,0.000107902895,0.00007195564,0.000006091698,0.0000011722537,0.000003462924,0.00024035337,0.0000022532688,0.000244093],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999312,0.000005355418,0.0000046591285,0.000025962729,0.000012429036,0.00002047092],"domain_scores_gemma":[0.9997086,0.000024576553,0.00007357846,0.000010765861,0.00012121347,0.00006126021],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001328979,0.0001749157,0.00016275224,0.00136147,0.001020545,0.00070043444,0.00023131075,0.00026646923,0.0010822605],"category_scores_gemma":[0.00026198567,0.00018837453,0.0000920024,0.00088514976,0.00041533675,0.00021655644,0.0004582666,0.0001313548,0.00011532617],"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":[0.000113123264,0.000018656327,0.9739671,0.000050466224,0.00004687101,0.0001930232,0.0012370555,0.0002820746,0.019417264,0.00010630333,0.00013866431,0.0044294135],"study_design_scores_gemma":[0.0000014454421,0.0000057012303,0.9986588,0.000008251435,0.0000051364464,0.0000341782,0.0003821445,0.00017066183,0.00039190412,0.000008324715,0.00033232887,0.000001119881],"about_ca_topic_score_codex":0.26094258,"about_ca_topic_score_gemma":0.57502085,"teacher_disagreement_score":0.26094258,"about_ca_system_score_codex":0.0014566892,"about_ca_system_score_gemma":0.0006863997,"threshold_uncertainty_score":0.51884747},"labels":[],"label_agreement":null},{"id":"W4386784199","doi":"10.1017/s001675682300050x","title":"The genesis of calcite and dolomite carbonatite-forming magma by liquid immiscibility: a critical appraisal","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","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":"Lakehead University; University of Toronto","funders":"University of Toronto; Lakehead University","keywords":"Carbonatite; Calcite; Geology; Dolomite; Geochemistry; Magma; Trace element; Carbonate; Silicate; Mineralogy; Volcano; Mantle (geology); Chemistry","score_opus":0.014927300306722846,"score_gpt":0.24691333560577924,"score_spread":0.2319860352990564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386784199","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":[0.002368953,0.99356407,0.00049636635,0.0013501674,0.00062005396,0.000014421836,0.000012743841,0.000007913071,0.0015652375],"genre_scores_gemma":[0.033703428,0.96029675,0.00077976054,0.0017624976,0.0025960926,0.00003626301,0.0000319653,0.000018081697,0.0007751866],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99800557,0.0006581254,0.00039391592,0.00031753106,0.000490522,0.00013431296],"domain_scores_gemma":[0.978451,0.015926274,0.0013782987,0.00035186595,0.0036405572,0.000251922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009879729,0.001373384,0.0017078324,0.004607103,0.0009030569,0.002957661,0.001838513,0.002501981,0.0012953953],"category_scores_gemma":[0.010407459,0.0005258905,0.0007509606,0.0020991666,0.008121078,0.0054434813,0.0017120171,0.0036189884,0.00058072736],"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":[0.0023391985,0.00027570286,0.0075497213,0.10841064,0.0011260998,0.008716484,0.006202123,0.0032668088,0.03402074,0.109334454,0.032729194,0.68602884],"study_design_scores_gemma":[0.000058517504,0.0018477435,0.012818948,0.025080744,0.0010557324,0.0038586177,0.003115208,0.0013204635,0.02035236,0.043323368,0.8868967,0.00027151665],"about_ca_topic_score_codex":0.0019286943,"about_ca_topic_score_gemma":0.001629882,"teacher_disagreement_score":0.009879729,"about_ca_system_score_codex":0.00358801,"about_ca_system_score_gemma":0.0023889213,"threshold_uncertainty_score":0.05224961},"labels":[],"label_agreement":null},{"id":"W4389310601","doi":"10.1017/s0016756823000729","title":"U-Pb zircon dates from North American and British Avalonia bracket the Lower–Middle Cambrian boundary interval, with evaluation of the Miaolingian Series as a global unit","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"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":"University of Cambridge; University of Cincinnati; Deutsche Forschungsgemeinschaft; Massachusetts Institute of Technology; National Science Foundation","keywords":"Geology; Laurentia; Zircon; Paleontology; Sedimentary depositional environment; Onlap; Unconformity; Diachronous; Series (stratigraphy); Ordovician; Sedimentary rock; Structural basin","score_opus":0.021397750131368333,"score_gpt":0.22141639449946224,"score_spread":0.2000186443680939,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389310601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97879773,0.00033479612,0.0003978169,0.000047217134,0.000007783145,0.000020594378,0.0016799317,0.000034178625,0.018679945],"genre_scores_gemma":[0.9926524,0.0001399298,0.0007493854,0.00003558771,0.0000034984203,0.000020035637,0.0017179862,0.000013025619,0.004668005],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990714,0.0000053369045,0.0000072077587,0.000025981,0.00002339587,0.000031022497],"domain_scores_gemma":[0.99982005,0.000013355069,0.000042198226,0.000015165812,0.000080854064,0.000028461647],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001983447,0.00025485232,0.0001304409,0.002173069,0.0008946835,0.0005970764,0.00029687415,0.0001419194,0.004318623],"category_scores_gemma":[0.00028615262,0.00012443271,0.000129521,0.0019510355,0.00039458278,0.0002893448,0.00051413855,0.00018641514,0.0007719789],"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":[0.00023025127,0.000023157292,0.89439076,0.000083172206,0.000054363434,0.00042664754,0.0029961148,0.00033182555,0.040513393,0.0008905771,0.0019537113,0.058106076],"study_design_scores_gemma":[0.000002728285,0.0000075982534,0.993933,0.000006965551,0.000006052734,0.00004858634,0.00030217227,0.000082005594,0.00063963555,0.000022926892,0.004946797,0.0000014359869],"about_ca_topic_score_codex":0.27143696,"about_ca_topic_score_gemma":0.69379514,"teacher_disagreement_score":0.27143696,"about_ca_system_score_codex":0.0016117302,"about_ca_system_score_gemma":0.0007039164,"threshold_uncertainty_score":0.53971404},"labels":[],"label_agreement":null},{"id":"W4392167885","doi":"10.1017/s0016756824000049","title":"<i>Entophysalis</i> in the Rhynie chert (Lower Devonian, Scotland): implications for cyanobacterial evolution","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"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":"Generalist and specialist species; Paleontology; Ecology; Devonian; Ecosystem; Precambrian; Geology; Assemblage (archaeology); Biology; Habitat","score_opus":0.029943970477486474,"score_gpt":0.2561755955145621,"score_spread":0.2262316250370756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392167885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987494,0.00030959892,0.000056142904,0.000051964016,0.0000028203203,0.0000039819306,0.00014085614,0.000005063179,0.0006800208],"genre_scores_gemma":[0.999569,0.000088530454,0.00006076896,0.000017413206,0.0000044971907,0.0000014016177,0.00011675571,0.0000019301308,0.00013964756],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977976,0.000017015314,0.000011093151,0.000059043392,0.000046959023,0.00008618984],"domain_scores_gemma":[0.99963474,0.000039529772,0.00013058324,0.000012412299,0.000105895655,0.000076775585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031760114,0.0002856233,0.0003852812,0.0027610445,0.001237651,0.0009882475,0.0005233889,0.00045728587,0.0016995426],"category_scores_gemma":[0.0004719086,0.00012894256,0.00018931463,0.0016679903,0.001272584,0.00039176363,0.0010008223,0.00025804824,0.0003444374],"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":[0.0002979342,0.000048418027,0.92058295,0.00015961769,0.000049157337,0.0025008349,0.006817477,0.00016648899,0.053697657,0.00034191113,0.0002383128,0.015099126],"study_design_scores_gemma":[0.0000019489717,0.000035488676,0.99708986,0.000009961624,0.000004809842,0.00027499982,0.0015232443,0.00006911745,0.00021944981,0.000022255505,0.0007439186,0.000004878443],"about_ca_topic_score_codex":0.11281302,"about_ca_topic_score_gemma":0.15473102,"teacher_disagreement_score":0.11281302,"about_ca_system_score_codex":0.0012603975,"about_ca_system_score_gemma":0.000563706,"threshold_uncertainty_score":0.22431278},"labels":[],"label_agreement":null},{"id":"W4393521002","doi":"10.1017/s0016756824000050","title":"Disruption and localization of sediment pathways by continental extension: Detrital-zircon provenance change from upper Triassic to lower Jurassic in the northern Sverdrup Basin, Nunavut","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":3,"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; Geological Survey of Canada","funders":"University of Ottawa","keywords":"Sverdrup; Geology; Provenance; Zircon; Structural basin; Sediment; Paleontology; Oceanography","score_opus":0.032538337524995624,"score_gpt":0.2201212413692522,"score_spread":0.18758290384425658,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393521002","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987207,0.00014313734,0.000038071164,0.000013901298,0.0000017612053,0.0000021573676,0.000289133,0.0000047631656,0.00078631676],"genre_scores_gemma":[0.99905914,0.00007865221,0.0000815566,0.000006446372,8.41702e-7,0.0000029190446,0.00024169424,0.000003649185,0.0005250704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998361,0.00001829494,0.000011518092,0.000070194976,0.000023865176,0.000040010924],"domain_scores_gemma":[0.9997476,0.000039972754,0.00005754781,0.000023307453,0.00009502509,0.00003665099],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035277443,0.00013996828,0.00017555649,0.001157863,0.00067107216,0.0007991395,0.0004466001,0.00016711328,0.001063365],"category_scores_gemma":[0.0005485621,0.00018694648,0.00013875529,0.00085209036,0.00061119616,0.00024355958,0.000551875,0.00015482093,0.000120171644],"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":[0.00009162133,0.000016190661,0.9725744,0.000034180146,0.00004420802,0.00022456382,0.002565984,0.0004388414,0.010212953,0.000254273,0.00020705574,0.013335652],"study_design_scores_gemma":[8.8644504e-7,0.0000054771667,0.9988391,0.000007136327,0.000005050766,0.00003370234,0.00035331424,0.00009754003,0.00028393607,0.000018651825,0.0003536453,0.0000016607394],"about_ca_topic_score_codex":0.48686787,"about_ca_topic_score_gemma":0.7606008,"teacher_disagreement_score":0.5131321,"about_ca_system_score_codex":0.0019999004,"about_ca_system_score_gemma":0.0012936422,"threshold_uncertainty_score":0.968068},"labels":[],"label_agreement":null},{"id":"W4396496018","doi":"10.1017/s0016756824000128","title":"GEO volume 160 issue 11 Cover and Front matter","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","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":"University of Calgary","funders":"","keywords":"Front cover; Cover (algebra); Front (military); Volume (thermodynamics); Geology; Physical geography; Geography; Oceanography; Engineering; Physics","score_opus":0.016049002418083172,"score_gpt":0.21140891304913745,"score_spread":0.1953599106310543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396496018","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0006776152,0.0010417082,0.000363966,0.0034754002,0.009511406,0.000059818012,0.004019227,0.0015622977,0.9792885],"genre_scores_gemma":[0.0014624911,0.0008329663,0.00015681674,0.0010653506,0.0016004196,0.000018060786,0.001953509,0.0004153497,0.99249494],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9996892,0.0000155609,0.000011168797,0.0000639035,0.0001822738,0.000037944275],"domain_scores_gemma":[0.9990017,0.00011123452,0.000030306235,0.00014710835,0.0004292329,0.00028056887],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00046172028,0.0010016604,0.0008171931,0.0020745017,0.0013249859,0.0046220664,0.00056922116,0.0018455328,0.8471089],"category_scores_gemma":[0.0014190227,0.0003644662,0.0005197607,0.0016246856,0.0007077222,0.0016356404,0.0016726283,0.001375327,0.83378553],"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":[0.000018167668,0.000021414318,0.00013335052,0.000072767005,0.0000023521752,0.000034440814,0.000008100635,0.000024454474,0.00048672204,0.00078641705,0.9680904,0.030321507],"study_design_scores_gemma":[0.0000045252723,0.000009409241,0.0005611835,0.000051248204,0.0000016812487,0.000037558046,0.000019554927,0.000036980455,0.00018249714,0.00032629675,0.9987668,0.0000023247344],"about_ca_topic_score_codex":0.0021585843,"about_ca_topic_score_gemma":0.0038661137,"teacher_disagreement_score":0.1528911,"about_ca_system_score_codex":0.00083443086,"about_ca_system_score_gemma":0.0010716303,"threshold_uncertainty_score":0.21808058},"labels":[],"label_agreement":null},{"id":"W4402728613","doi":"10.1017/s0016756824000141","title":"Geochemistry, U-Pb geochronology and Nd-Hf isotopes of leucocratic dykes in the Cape Spencer area, southern New Brunswick, Canada: insights into the Alleghanian orogeny in the northern Appalachians","year":2023,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geochemistry and Geologic Mapping","field":"Computer 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":"Geological Survey of Canada; University of New Brunswick","funders":"New Brunswick Innovation Foundation","keywords":"Geochronology; Orogeny; Geology; Cape; Geochemistry; Isotope; Archaeology; Paleontology; Geography; Tectonics; Physics","score_opus":0.014453954704054464,"score_gpt":0.20660795813881294,"score_spread":0.19215400343475847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402728613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968811,0.0002680336,0.000095284384,0.00003947223,0.000002160606,0.000015316647,0.0005628581,0.0000052254,0.0021306917],"genre_scores_gemma":[0.9976525,0.00017540395,0.0003112582,0.000022269634,0.0000010375475,0.000008588673,0.00036292034,0.000006040685,0.0014599735],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976116,0.00000997334,0.000012769717,0.00006088513,0.00007967985,0.00007547477],"domain_scores_gemma":[0.99965954,0.000017590664,0.00004939026,0.000010549524,0.00022120407,0.000041818825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018193311,0.00031381386,0.0002922208,0.0022208304,0.0020743792,0.00093257247,0.00054685294,0.00022967572,0.0010877966],"category_scores_gemma":[0.00036631653,0.00020772498,0.00015370772,0.0022620747,0.00070091814,0.00022532631,0.0004442965,0.00024027102,0.00016657858],"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":[0.00018271958,0.000022391489,0.92920685,0.00009263417,0.00009022496,0.0010842604,0.0042187897,0.00041974193,0.04838947,0.00027015898,0.00050888123,0.015513846],"study_design_scores_gemma":[0.0000027607941,0.0000066747184,0.9953212,0.000011202211,0.000011361087,0.000112000904,0.002037256,0.00015139522,0.0009856949,0.0000116349665,0.0013429725,0.0000058145183],"about_ca_topic_score_codex":0.97165924,"about_ca_topic_score_gemma":0.9930992,"teacher_disagreement_score":0.028340757,"about_ca_system_score_codex":0.008395993,"about_ca_system_score_gemma":0.0053800135,"threshold_uncertainty_score":0.060917497},"labels":[],"label_agreement":null},{"id":"W4410374874","doi":"10.1017/s001675682500007x","title":"Complementary <i>in situ</i> garnet Lu-Hf geochronology and monazite U(-Th)-Pb petrochronology: an example from the Archean Slave craton, Northwest Territories, Canada","year":2025,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"Government of Northwest Territories; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geochronology; Monazite; Archean; Geology; Geochemistry; Craton; Zircon; Paleontology; Tectonics","score_opus":0.013954652428933277,"score_gpt":0.19960985016111327,"score_spread":0.18565519773217998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410374874","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98518986,0.00040774854,0.0010232707,0.00006229818,0.00000851263,0.000022948185,0.0016639297,0.00004913344,0.011572271],"genre_scores_gemma":[0.99284923,0.0002599049,0.0014815765,0.000033871667,0.0000037424695,0.000006729799,0.0007572537,0.000027321192,0.004580333],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99982494,0.0000056792182,0.0000064670335,0.000040518033,0.00007546534,0.00004701321],"domain_scores_gemma":[0.9997962,0.0000086237915,0.00001949728,0.000012197362,0.00014206498,0.000021361275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013640615,0.00032628022,0.0002558771,0.0016335921,0.0014536115,0.00084247335,0.00045383655,0.0002265175,0.0016558842],"category_scores_gemma":[0.00021647305,0.00013442399,0.00021758633,0.0020269156,0.00059258175,0.00014457632,0.0004017337,0.00025350755,0.0002569942],"study_design_candidate":"bench_or_experimental","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":[0.00035065945,0.000053530515,0.6966831,0.00018960758,0.0001806417,0.001502682,0.0044737128,0.0019405097,0.23010994,0.0010121556,0.00145315,0.062050357],"study_design_scores_gemma":[0.000005841913,0.000024751096,0.972818,0.000020621506,0.000055380613,0.00035586674,0.0020151997,0.00068232743,0.0165093,0.00007151566,0.00742773,0.000013414295],"about_ca_topic_score_codex":0.93053424,"about_ca_topic_score_gemma":0.9843753,"teacher_disagreement_score":0.06946576,"about_ca_system_score_codex":0.004789861,"about_ca_system_score_gemma":0.0041987495,"threshold_uncertainty_score":0.13974965},"labels":[],"label_agreement":null},{"id":"W4413312437","doi":"10.1017/s0016756825100137","title":"U-Pb volcanic zircon dates from New Brunswick constrain the Middle Cambrian Drumian Stage and trans-Avalonian green–black boundary","year":2025,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"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":"Zircon; Geology; Volcano; Stage (stratigraphy); Boundary (topology); Geochemistry; Paleontology","score_opus":0.017576474657342273,"score_gpt":0.2026847656108161,"score_spread":0.18510829095347384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413312437","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9771245,0.00096785196,0.00029036956,0.00017796394,0.000015920781,0.000021990947,0.0037177068,0.00003379822,0.017649898],"genre_scores_gemma":[0.9908127,0.000497211,0.0007421607,0.0001257102,0.000005601233,0.000019262772,0.0030415591,0.000024554989,0.0047312477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998252,0.000008833835,0.000015788872,0.000048353446,0.00003827448,0.00006368325],"domain_scores_gemma":[0.9997036,0.000024297331,0.000051996158,0.000021128822,0.00015533225,0.00004370831],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028559795,0.00026849232,0.00019543676,0.0022199915,0.00092103344,0.0010413126,0.00052955217,0.0002459323,0.003970978],"category_scores_gemma":[0.00047413807,0.00019751789,0.000114338276,0.0024884904,0.00048123236,0.00032829057,0.0008371286,0.00028704669,0.0008637638],"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":[0.00027793378,0.000028426726,0.9098489,0.00008781445,0.00005857044,0.00057821424,0.0025584337,0.00048979156,0.02468429,0.00082027935,0.0025489503,0.05801839],"study_design_scores_gemma":[0.000009341517,0.0000149174,0.9871191,0.00004395562,0.000012173996,0.000070329836,0.0015113011,0.00015246891,0.0016535933,0.00007138567,0.009335565,0.000005982176],"about_ca_topic_score_codex":0.73805255,"about_ca_topic_score_gemma":0.9438938,"teacher_disagreement_score":0.26194745,"about_ca_system_score_codex":0.0037659039,"about_ca_system_score_gemma":0.0024102482,"threshold_uncertainty_score":0.52698016},"labels":[],"label_agreement":null},{"id":"W4413906112","doi":"10.1017/s0016756825100204","title":"Multi-method geochronology and isotope geochemistry of carbonatites in the Aileron Province, central Australia","year":2025,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geological and Geochemical Analysis","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":"ARC Resources (Canada)","funders":"","keywords":"Geochronology; Geology; Carbonatite; Geochemistry; Isotope geochemistry; Isotope","score_opus":0.01617186853544541,"score_gpt":0.2501682253465101,"score_spread":0.2339963568110647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413906112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99789643,0.00021352379,0.00067991455,0.000014060258,0.0000021799028,0.000008935922,0.00015028505,0.00001805624,0.0010166579],"genre_scores_gemma":[0.9975222,0.00006413963,0.0015955017,0.000006443272,0.0000018172626,0.0000064481774,0.00012586334,0.000005724603,0.00067183765],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99962854,0.000034725657,0.000026877473,0.0001289875,0.0001345623,0.000046223206],"domain_scores_gemma":[0.9992625,0.000053015992,0.00017606944,0.000058794376,0.0003943763,0.000055242534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070330256,0.0002433456,0.00016174663,0.0027225346,0.00066738925,0.000510922,0.0004509737,0.00027415183,0.0005029922],"category_scores_gemma":[0.00078582356,0.00021040405,0.00021672045,0.001190592,0.00030532127,0.0003006281,0.00064427784,0.00014343728,0.00012276281],"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":[0.00014594792,0.000036552665,0.8511096,0.00011451258,0.00016948268,0.00026725815,0.0015310483,0.0012606077,0.110233806,0.00020632011,0.00018678153,0.034738],"study_design_scores_gemma":[0.0000029417233,0.000031836615,0.99237144,0.0000089142195,0.000027269578,0.00017245149,0.00018402464,0.0017833262,0.0045292797,0.00003228586,0.00084902253,0.0000070746914],"about_ca_topic_score_codex":0.123178594,"about_ca_topic_score_gemma":0.30393752,"teacher_disagreement_score":0.123178594,"about_ca_system_score_codex":0.0014686902,"about_ca_system_score_gemma":0.00069613574,"threshold_uncertainty_score":0.24492323},"labels":[],"label_agreement":null},{"id":"W7082157756","doi":"10.1017/s0016756825100265","title":"A problematic soft-bodied fossil from the Cambrian (Miaolingian, Wuliuan) of Utah","year":2025,"lang":"en","type":"article","venue":"Geological Magazine","topic":"Geochemistry and Geologic Mapping","field":"Computer 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":"University of Toronto","funders":"U.S. Forest Service; U.S. Department of Agriculture","keywords":"Fauna; Paleozoic; Oil shale; Taphonomy; Biota; Faunal assemblage","score_opus":0.014978552275634755,"score_gpt":0.23113900524492714,"score_spread":0.2161604529692924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7082157756","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959073,0.0002131323,0.00022499023,0.00003583734,0.000009337128,0.000011988115,0.00025279622,0.000022351596,0.0033223352],"genre_scores_gemma":[0.9973558,0.00008226838,0.00072247547,0.00003376323,0.000004938198,0.000009432976,0.0003963939,0.000005710454,0.0013891367],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993336,0.0000039405927,0.0000039847964,0.000022002472,0.000023641775,0.0000131568595],"domain_scores_gemma":[0.99988127,0.000016225671,0.000027105592,0.000018461471,0.00003298431,0.000023897388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000093626004,0.00017257551,0.00016557398,0.001495535,0.0020977107,0.0003636114,0.00051369425,0.00041226504,0.0021770452],"category_scores_gemma":[0.00033483963,0.000097076336,0.00007488285,0.0013810687,0.0007655761,0.0002161847,0.00079459406,0.0002344537,0.00025659756],"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":[0.00036335216,0.00009077144,0.7599016,0.0002589779,0.00009135521,0.0074716345,0.013904403,0.00085352705,0.08499269,0.0016167589,0.0026345577,0.1278204],"study_design_scores_gemma":[0.000003997179,0.00006757577,0.9804437,0.000045997313,0.00003144268,0.0016118307,0.0017640186,0.00052595173,0.0017906788,0.0001350953,0.013569895,0.000009816725],"about_ca_topic_score_codex":0.05466756,"about_ca_topic_score_gemma":0.2769555,"teacher_disagreement_score":0.05466756,"about_ca_system_score_codex":0.00074632163,"about_ca_system_score_gemma":0.00052823464,"threshold_uncertainty_score":0.108698726},"labels":[],"label_agreement":null}]}