{"meta":{"query_hash":"0a8cfa3962ba","filters":{"venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh"},"cohort_total":37,"direct_labels_cover":0,"predictions_cover":37,"exported":37,"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/0a8cfa3962ba","api":"https://metacan.xera.ac/api/v1/cohort?venue=Earth+and+Environmental+Science+Transactions+of+the+Royal+Society+of+Edinburgh"},"results":[{"id":"W1964563643","doi":"10.1017/s1755691011011030","title":"Early Carboniferous minor intrusions of the Clyde Plateau: new data from the Cumbrae islands","year":2011,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":"Western University","funders":"","keywords":"Geology; Carboniferous; Lava; Paleontology; Basalt; Flood basalt; Trachyte; Lineament; Geochemistry; Volcanic rock; Volcano; Tectonics; Volcanism; Structural basin","score_opus":0.01855202507157584,"score_gpt":0.17611376792335443,"score_spread":0.1575617428517786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964563643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967332,0.00034080676,0.00003398757,0.000022048092,0.000004372974,0.000024329884,0.0012259616,0.0000060780985,0.0016091273],"genre_scores_gemma":[0.9938712,0.00022967253,0.00025827825,0.000035774647,0.000013391168,0.000028822213,0.0046245465,0.00001201476,0.00092622405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996941,0.000022654258,0.000024879746,0.00007900857,0.00008418548,0.00009521723],"domain_scores_gemma":[0.99884135,0.00009698566,0.00017192963,0.00014751895,0.00048201752,0.0002601949],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035288036,0.00030050575,0.0004094406,0.0025073418,0.00091875717,0.00092625414,0.0006107125,0.00043911987,0.0016860708],"category_scores_gemma":[0.00076717616,0.00023299185,0.00025064757,0.0017142033,0.0005246416,0.0003801057,0.0012223311,0.00047568994,0.00049761625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015313082,0.0000870995,0.98085463,0.000109298104,0.00006841697,0.0007861321,0.0032350007,0.0000683599,0.005140893,0.000044407443,0.0007764923,0.008676139],"study_design_scores_gemma":[0.0000019874844,0.000009646481,0.9983234,0.000010491686,0.000004765073,0.0000996036,0.0004678415,0.00001997349,0.00005645418,0.0000016283063,0.0010022912,0.000001920514],"about_ca_topic_score_codex":0.24748062,"about_ca_topic_score_gemma":0.51571923,"teacher_disagreement_score":0.24748062,"about_ca_system_score_codex":0.0011039939,"about_ca_system_score_gemma":0.00066316273,"threshold_uncertainty_score":0.49208027},"labels":[],"label_agreement":null},{"id":"W2025078594","doi":"10.1017/s1755691009016065","title":"Causes of compositional diversity in a lobe of the Half Dome granodiorite, Tuolumne Batholith, Central Sierra Nevada, California","year":2009,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Akademie Věd České Republiky; University of Southern California","keywords":"Leucogranite; Batholith; Geology; Diorite; Geochemistry; Dome (geology); Magma; Fractional crystallization (geology); Mineralogy; Paleontology; Zircon; Metamorphic rock; Gneiss; Volcano; Tectonics","score_opus":0.007051263944898744,"score_gpt":0.16950778550767287,"score_spread":0.16245652156277413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025078594","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989103,0.00015941894,0.00003554228,0.000016080485,0.0000010588716,0.0000026635491,0.00012214812,0.000009159572,0.0007436534],"genre_scores_gemma":[0.9995535,0.000042882068,0.000050869257,0.00000807233,9.7136e-7,0.0000019275217,0.0001413895,0.0000031207649,0.0001972009],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998871,0.0000055715786,0.0000064610613,0.000043921515,0.000026038027,0.000030988907],"domain_scores_gemma":[0.99977547,0.000026288206,0.000044654375,0.00001772149,0.000081621845,0.000054234326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015001681,0.00011858992,0.00025188373,0.0009606727,0.00084499177,0.00087016507,0.00045743494,0.00025455412,0.0007876333],"category_scores_gemma":[0.00036287916,0.00014372508,0.000118251606,0.0005907547,0.000637894,0.00020093078,0.0005791793,0.00012243116,0.00011432738],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015519062,0.000018844199,0.9563554,0.000063143976,0.000058694102,0.00045545248,0.0019577767,0.0003252527,0.031672187,0.00016892502,0.00021485389,0.008554215],"study_design_scores_gemma":[0.0000021307085,0.000006522238,0.99816906,0.000004997822,0.000005598811,0.00009384273,0.00060328376,0.00009696642,0.0004036942,0.000019323166,0.00059250504,0.0000020536777],"about_ca_topic_score_codex":0.15113048,"about_ca_topic_score_gemma":0.31515202,"teacher_disagreement_score":0.15113048,"about_ca_system_score_codex":0.0011867998,"about_ca_system_score_gemma":0.0005634081,"threshold_uncertainty_score":0.30050164},"labels":[],"label_agreement":null},{"id":"W2053181574","doi":"10.1017/s1755691007006123","title":"The Cambrian Fauna of the Leny Limestone, Perthshire, Scotland","year":2008,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":22,"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 Glasgow","keywords":"Geology; Paleontology; Ordovician; Fauna; Biostratigraphy; Terrane; Laurentia; Pennsylvanian; Structural basin; Tectonics; Ecology","score_opus":0.007830678845705414,"score_gpt":0.17803191355708392,"score_spread":0.17020123471137852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053181574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9829928,0.002291537,0.000054049775,0.00028856736,0.000011888942,0.000036304264,0.0007023681,0.000027398748,0.013595132],"genre_scores_gemma":[0.9893462,0.0011292008,0.00015090157,0.00010616502,0.000024190622,0.000027065613,0.0006319294,0.000009055467,0.008575286],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998385,0.000015174527,0.000012399706,0.00003065836,0.000054843127,0.000048405396],"domain_scores_gemma":[0.9997514,0.000028743285,0.00008745393,0.000011890054,0.00005143344,0.000068987734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001439426,0.00024027858,0.00017808561,0.0017067597,0.0010800528,0.00088210445,0.00040120233,0.00015687851,0.007955708],"category_scores_gemma":[0.00041471006,0.00018171898,0.00008724438,0.0015425605,0.00084137026,0.0004347341,0.00095769437,0.00012590806,0.00061536365],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003330464,0.000077782766,0.65968204,0.0010730828,0.00024689437,0.009302084,0.041185677,0.0005235644,0.019504467,0.0022127894,0.011651626,0.25420687],"study_design_scores_gemma":[0.000007368825,0.00004318291,0.977539,0.000064105014,0.000009400213,0.00046271743,0.0037822793,0.000046077344,0.00012689379,0.00004534196,0.01786848,0.0000050852727],"about_ca_topic_score_codex":0.24429467,"about_ca_topic_score_gemma":0.57081723,"teacher_disagreement_score":0.24429467,"about_ca_system_score_codex":0.0019426766,"about_ca_system_score_gemma":0.0007652536,"threshold_uncertainty_score":0.48574543},"labels":[],"label_agreement":null},{"id":"W2072664224","doi":"10.1017/s0263593300001115","title":"Source and redox controls on metallogenic variations in intrusion-related ore systems, Tombstone-Tungsten Belt, Yukon Territory, Canada","year":2004,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University","funders":"U.S. Geological Survey","keywords":"Geochemistry; Geology; Mafic; Zircon; Felsic; Metallogeny; Petrology","score_opus":0.0035470418736403223,"score_gpt":0.15450847282535654,"score_spread":0.1509614309517162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072664224","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965712,0.00027239136,0.00006910218,0.000052987532,0.0000026092969,0.000012259616,0.001651689,0.0000089500845,0.0013587951],"genre_scores_gemma":[0.9961486,0.00024154002,0.00018353923,0.000023049633,7.361399e-7,0.000007538741,0.0016679179,0.000008913245,0.0017181856],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998234,0.000008563869,0.000012383638,0.000042026317,0.000045770787,0.00006789166],"domain_scores_gemma":[0.99947804,0.000018271376,0.00005663672,0.000012018678,0.00035210754,0.00008305883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013846756,0.00028151827,0.0002870984,0.001470077,0.0016611542,0.0010839956,0.00047804406,0.00022725669,0.001440582],"category_scores_gemma":[0.00036704764,0.0001819508,0.00023744958,0.00339301,0.0005725823,0.0002436985,0.0005841155,0.00020833492,0.00018431456],"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":[0.00033295993,0.000046594912,0.9663462,0.00007757599,0.00011078682,0.00031107166,0.0026233024,0.00032792435,0.018854326,0.00050361874,0.000650171,0.009815469],"study_design_scores_gemma":[0.0000036543427,0.0000071951586,0.9975368,0.000007734518,0.0000092681175,0.000034820485,0.0013010275,0.000092774426,0.00032283895,0.000016662148,0.00066301,0.0000042399442],"about_ca_topic_score_codex":0.98432124,"about_ca_topic_score_gemma":0.9945702,"teacher_disagreement_score":0.015678763,"about_ca_system_score_codex":0.012017724,"about_ca_system_score_gemma":0.011164015,"threshold_uncertainty_score":0.0871951},"labels":[],"label_agreement":null},{"id":"W2080058784","doi":"10.1017/s1755691010009047","title":"Fluid inclusions in Irish granite quartz: monitors of fluids trapped in the onshore Irish Massif","year":2010,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Geochemistry; Fluid inclusions; Quartz; Massif; Orogeny; Sedimentary rock; Igneous rock; Petrology; Structural basin; Geomorphology; Paleontology","score_opus":0.007333152807650519,"score_gpt":0.19255190778999873,"score_spread":0.18521875498234822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080058784","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979138,0.000050489733,0.00014909891,0.000010231212,0.0000032074086,0.00001357401,0.00066902157,0.000036516176,0.0011541916],"genre_scores_gemma":[0.9970318,0.00006141485,0.0010575155,0.000016080121,0.000005768728,0.000020333247,0.00089661544,0.000015579133,0.00089487963],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981767,0.0000100922425,0.000010330845,0.000054538486,0.00005936877,0.000048014743],"domain_scores_gemma":[0.999843,0.000011567698,0.000046525663,0.000007923105,0.00006154251,0.00002955445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016980276,0.00030782816,0.00020268466,0.0012467823,0.00049546134,0.00053154916,0.00031476098,0.00033316883,0.0007006991],"category_scores_gemma":[0.00020011628,0.00015306463,0.00019649528,0.0008758907,0.00026806592,0.00023496662,0.0006126515,0.00019591869,0.00033481763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006163239,0.00009324887,0.8544596,0.000059929258,0.00005743269,0.00048645644,0.001417138,0.00046603565,0.12432917,0.000047618007,0.00044085263,0.017526254],"study_design_scores_gemma":[0.000008841805,0.00007549447,0.99103034,0.0000108615395,0.000015295009,0.00015822865,0.00065705803,0.00057478476,0.0059385444,0.000009316221,0.0015119881,0.000009233906],"about_ca_topic_score_codex":0.034287687,"about_ca_topic_score_gemma":0.07391717,"teacher_disagreement_score":0.034287687,"about_ca_system_score_codex":0.0006159692,"about_ca_system_score_gemma":0.00037258852,"threshold_uncertainty_score":0.06817621},"labels":[],"label_agreement":null},{"id":"W2080223678","doi":"10.1017/s175569101300039x","title":"Herpetofaunas from the “overburden” (Quaternary) of western Canada","year":2012,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Evolution and Paleontology 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":true,"ca_institutions":"Royal Tyrrell Museum; Royal Alberta Museum","funders":"University of Texas at Austin","keywords":"Quaternary; Cave; Glacial period; Geology; Taxon; Ecology; Paleontology; Geography; Archaeology; Biology","score_opus":0.0081221699002774,"score_gpt":0.17896726432233404,"score_spread":0.17084509442205664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080223678","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99811196,0.00020057047,0.00003818886,0.00002683227,0.0000031564725,0.000007860399,0.00074101496,0.000003839839,0.00086647976],"genre_scores_gemma":[0.99803776,0.00022063742,0.0001167561,0.000028895109,0.0000026484847,0.000005724973,0.000858984,0.0000026249058,0.00072595343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99969614,0.000014297379,0.0000179266,0.00005247129,0.00008998881,0.00012930686],"domain_scores_gemma":[0.99924207,0.000030132145,0.000097418895,0.000022307095,0.00043227413,0.00017584534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027763125,0.00028167397,0.00022439026,0.001888129,0.0032485593,0.00082401955,0.0004266892,0.00020575926,0.0013890655],"category_scores_gemma":[0.0007146499,0.0001622649,0.00014597333,0.0032714026,0.0007351306,0.00025003558,0.0006291338,0.00026457387,0.00018852492],"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":[0.000105003885,0.000019923851,0.97683525,0.000042945365,0.000028212753,0.00025614284,0.0064890264,0.00015887701,0.0016608563,0.00015205472,0.0009114578,0.013340145],"study_design_scores_gemma":[0.0000017351472,0.00001199726,0.9956962,0.000013324995,0.000010175886,0.00008403364,0.002519148,0.000112538386,0.00012382446,0.000015799485,0.0014074208,0.0000038151816],"about_ca_topic_score_codex":0.9868752,"about_ca_topic_score_gemma":0.9974274,"teacher_disagreement_score":0.013124824,"about_ca_system_score_codex":0.0090125725,"about_ca_system_score_gemma":0.006976555,"threshold_uncertainty_score":0.06539106},"labels":[],"label_agreement":null},{"id":"W2092725842","doi":"10.1017/s1755691011010048","title":"The Early Carboniferous volcanic outliers of Little Cumbrae and south Bute: implications for westward attenuation of the Clyde Lava Plateau","year":2011,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; British Geological Survey; University of Edinburgh","keywords":"Volcanic plateau; Geology; Plateau (mathematics); Escarpment; Lava; Carboniferous; Volcanic rock; Pyroclastic rock; Volcano; Sedimentary rock; Firth; Paleontology; Lava field; Trachyte; Geochemistry; Geomorphology; Structural basin","score_opus":0.011227376762611192,"score_gpt":0.17495283976644538,"score_spread":0.1637254630038342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092725842","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972364,0.00010330439,0.000074677715,0.00023369069,0.0000030866354,0.0000053915473,0.00009683074,0.0000050917247,0.0022414685],"genre_scores_gemma":[0.99951124,0.000020603427,0.00004431477,0.00001771189,0.00000373638,0.0000022184067,0.00007641965,0.0000023260723,0.0003214909],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997738,0.00004059284,0.000014008672,0.00005141924,0.000042002677,0.00007818486],"domain_scores_gemma":[0.9987484,0.00023599293,0.00034476418,0.00007209159,0.00034875932,0.0002499972],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034409392,0.00011727822,0.00028267395,0.0008639301,0.0012189413,0.001669266,0.00048062057,0.00040591398,0.0031255423],"category_scores_gemma":[0.002090609,0.00009886345,0.00011496648,0.0006265109,0.0011333044,0.00053324923,0.00079314876,0.0002921372,0.0001854562],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010706531,0.000014502682,0.98890334,0.000014926702,0.000008938252,0.00045750279,0.00093270146,0.00015200338,0.0026573006,0.0004220827,0.00021889449,0.006110745],"study_design_scores_gemma":[0.0000035902767,0.000016088634,0.99671507,0.000011715773,0.0000026036926,0.00009549701,0.0016262151,0.0002581025,0.0003076954,0.00009405996,0.0008655213,0.0000037923303],"about_ca_topic_score_codex":0.10275107,"about_ca_topic_score_gemma":0.17693545,"teacher_disagreement_score":0.10275107,"about_ca_system_score_codex":0.001286594,"about_ca_system_score_gemma":0.0006184419,"threshold_uncertainty_score":0.204306},"labels":[],"label_agreement":null},{"id":"W2105719044","doi":"10.1017/s0263593300001085","title":"Late Archaean Kenogamissi complex, Abitibi Subprovince, Ontario, Canada: doming, folding and deformation-assisted melt remobilisation during syntectonic batholith emplacement","year":2004,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Batholith; Geology; Archean; Geochemistry; Pluton; Greenstone belt; Doming; Crust; Petrology; Metamorphism; Tectonics; Seismology","score_opus":0.006873512288796493,"score_gpt":0.16222282291550738,"score_spread":0.1553493106267109,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105719044","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99631435,0.00019181175,0.00006700064,0.00003703333,0.0000012435636,0.000010455587,0.0004942867,0.000007113233,0.0028767649],"genre_scores_gemma":[0.9969844,0.00016908773,0.00017486142,0.000016088667,8.224519e-7,0.000008413197,0.0003512599,0.000006664387,0.0022882838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998455,0.0000047557232,0.0000049298756,0.00003661793,0.000046780984,0.000061441155],"domain_scores_gemma":[0.9997489,0.0000132410005,0.000037052665,0.000010616495,0.00014274978,0.00004745069],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013695966,0.00023307251,0.00020373095,0.0011762483,0.003099265,0.00094739924,0.00044840257,0.0002593392,0.0021570267],"category_scores_gemma":[0.00040352924,0.00025154342,0.00014205479,0.0017408405,0.0011314987,0.0002413025,0.00076381076,0.00021820543,0.0002591395],"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":[0.00022240837,0.000019222312,0.9229203,0.00012580522,0.00004916484,0.0010242953,0.023095513,0.00047873388,0.027187822,0.0004432237,0.0009474832,0.023485985],"study_design_scores_gemma":[0.0000013259861,0.00000548418,0.9936779,0.000010802396,0.00000621356,0.000061720326,0.003636825,0.00009533412,0.0003843871,0.000014661584,0.0021006027,0.000004675],"about_ca_topic_score_codex":0.97793007,"about_ca_topic_score_gemma":0.9954448,"teacher_disagreement_score":0.022069931,"about_ca_system_score_codex":0.014405356,"about_ca_system_score_gemma":0.008514616,"threshold_uncertainty_score":0.10451865},"labels":[],"label_agreement":null},{"id":"W2119956527","doi":"10.1017/s1755691009016028","title":"Anisotropy of magnetic susceptibility fabrics in syntectonic plutons as tectonic strain markers: the example of the Canso pluton, Meguma Terrane, Nova Scotia","year":2009,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Pluton; Terrane; Geology; Geochemistry; Shear zone; Lineation; Petrology; Devonian; Shearing (physics); Tectonics; Seismology; Geotechnical engineering","score_opus":0.007911634116860076,"score_gpt":0.18393758317273476,"score_spread":0.17602594905587468,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119956527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99574775,0.00018815066,0.00004765108,0.0000349724,0.0000028883696,0.000012248225,0.0005297929,0.000007649145,0.0034289202],"genre_scores_gemma":[0.99890363,0.000086648535,0.00009079615,0.000007817094,0.0000015413381,0.000003021304,0.00021020995,0.0000037578798,0.00069254206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988484,0.000010171848,0.0000063256334,0.000033408614,0.00002783913,0.00003735943],"domain_scores_gemma":[0.99950075,0.00005681984,0.00008999988,0.0000319384,0.00023728098,0.000083323175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015773452,0.00023033931,0.00013673079,0.0020941384,0.0007378535,0.000779759,0.00024726518,0.00018360085,0.0011600151],"category_scores_gemma":[0.0005850022,0.00016312682,0.00011764695,0.0018083086,0.0007216997,0.00013417326,0.0004284818,0.00018141775,0.00024783067],"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":[0.00030746395,0.000017902334,0.954891,0.000089158275,0.00007645387,0.0012621839,0.0026058452,0.00069847953,0.02850331,0.00021629922,0.00051522034,0.010816633],"study_design_scores_gemma":[0.000002233692,0.0000037025054,0.999153,0.000004960249,0.000003530655,0.0000418299,0.00028825685,0.00008444458,0.0001557123,0.0000070363,0.00025344914,0.0000018257691],"about_ca_topic_score_codex":0.8296945,"about_ca_topic_score_gemma":0.9417206,"teacher_disagreement_score":0.17030549,"about_ca_system_score_codex":0.0030946147,"about_ca_system_score_gemma":0.0013220872,"threshold_uncertainty_score":0.34261686},"labels":[],"label_agreement":null},{"id":"W2120606565","doi":"10.1017/s0263593300007392","title":"Bimodal magmatism as a consequence of the post-collisional readjustment of the thickened Variscan continental lithosphere (Aiguilles Rouges-Mont Blanc Massifs, Western Alps)","year":2000,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Ontario Museum","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Geology; Geochemistry; Subduction; Pluton; Continental crust; Magmatism; Mantle (geology); Underplating; Lithosphere; Continental collision; Mafic; Petrology; Tectonics; Paleontology","score_opus":0.0041783233639750795,"score_gpt":0.17162396748104977,"score_spread":0.1674456441170747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120606565","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984884,0.00013287547,0.000107052605,0.000027884957,0.0000024235455,0.000004140928,0.00022150064,0.00003851112,0.0009772208],"genre_scores_gemma":[0.99917346,0.000023440121,0.000050989674,0.000006066626,0.0000023663074,0.000001563078,0.00016775793,0.0000039566225,0.00057033915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999267,0.0000060482976,0.0000024755427,0.000030835217,0.000013571409,0.00002037714],"domain_scores_gemma":[0.9999368,0.000007326923,0.000024463545,0.0000082393035,0.000008341244,0.000014782665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011539031,0.000180733,0.000122605,0.00053336506,0.00032891365,0.0005063144,0.00018251673,0.000260737,0.0027644169],"category_scores_gemma":[0.00016888142,0.0001326524,0.00009637194,0.000511256,0.0005672665,0.00012684766,0.0003042676,0.00018560232,0.00024542704],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007513528,0.00004179127,0.76874286,0.00008336892,0.00007678986,0.002418614,0.0012202368,0.0015287253,0.20053677,0.0008041405,0.0005720206,0.023223344],"study_design_scores_gemma":[0.0000045312117,0.00002221262,0.99691725,0.0000019853042,0.0000046307505,0.00038675746,0.000058646543,0.00017962245,0.001432047,0.000041602612,0.00094848615,0.000002303406],"about_ca_topic_score_codex":0.02667667,"about_ca_topic_score_gemma":0.05086078,"teacher_disagreement_score":0.02667667,"about_ca_system_score_codex":0.0009779101,"about_ca_system_score_gemma":0.00031817515,"threshold_uncertainty_score":0.05304277},"labels":[],"label_agreement":null},{"id":"W2124722446","doi":"10.1017/s1755691007078449","title":"Cryptic speciation in the Recent thecideide brachiopod <i>Thecidellina</i> in the Atlantic and the Caribbean","year":2007,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Marine Biology and Ecology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Deutsche Forschungsgemeinschaft; European Commission","keywords":"Allopatric speciation; Cape verde; Biological dispersal; Biology; Species complex; Genetic algorithm; Genus; Paleontology; Ridge; Dorsum; Biogeography; Taxonomy (biology); Cape; Ecology; Zoology; Geography; Anatomy; Archaeology","score_opus":0.008085660386563057,"score_gpt":0.2040434057113073,"score_spread":0.19595774532474425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124722446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940653,0.0006100733,0.00016565832,0.00012186185,0.000009809713,0.000008818892,0.000032511514,0.0000054989678,0.004980518],"genre_scores_gemma":[0.9992686,0.0002362582,0.00017044944,0.000044619697,0.0000037949133,0.0000035920882,0.000047278503,0.0000021251449,0.00022320657],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999759,0.000024937899,0.000016541208,0.000078840276,0.000044575994,0.00007612193],"domain_scores_gemma":[0.99959534,0.000032012416,0.000104658015,0.000022327562,0.00016162253,0.0000841595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003477749,0.00022741948,0.00031906943,0.0007858112,0.0016353342,0.001466663,0.00047024226,0.00055924326,0.0017368648],"category_scores_gemma":[0.0011002482,0.00014018547,0.0001830174,0.0008439553,0.0009225638,0.0003665948,0.00096450024,0.00045097497,0.00012846098],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011294782,0.000069391994,0.7239821,0.0003788221,0.00018669968,0.0043756966,0.009687635,0.00064136996,0.17069364,0.0061254515,0.0006843475,0.082045436],"study_design_scores_gemma":[0.00003507522,0.00010237376,0.9798982,0.00009650438,0.00007541998,0.0016574415,0.005076222,0.0004786578,0.0013898221,0.00039940144,0.010752477,0.00003829081],"about_ca_topic_score_codex":0.110772096,"about_ca_topic_score_gemma":0.19982447,"teacher_disagreement_score":0.110772096,"about_ca_system_score_codex":0.0019306072,"about_ca_system_score_gemma":0.0010334157,"threshold_uncertainty_score":0.22025466},"labels":[],"label_agreement":null},{"id":"W2149787909","doi":"10.1017/s0263593300001188","title":"On <i>Cephalaspis magnifica</i> Traquair, 1893, from the Middle Devonian of Scotland, and the relationships of the last osteostracans","year":2004,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":"Devonian; Paleontology; Taxon; Holotype; Geology; Late Devonian extinction; Genus; Zoology; Geography; Biology; Carboniferous; Structural basin","score_opus":0.01074727077459793,"score_gpt":0.16898051768023248,"score_spread":0.15823324690563456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149787909","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9313262,0.024913032,0.0011473519,0.0009618438,0.00039931363,0.0001301891,0.00077248976,0.00008427465,0.0402653],"genre_scores_gemma":[0.98387235,0.006739145,0.0012533464,0.00052798586,0.0002598105,0.000049779064,0.0015680912,0.000010669971,0.0057188114],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99979645,0.000031203585,0.000016253998,0.000047732716,0.00005904432,0.0000493739],"domain_scores_gemma":[0.99970335,0.00003817486,0.00012952948,0.000020348587,0.00007954534,0.000029049435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020056365,0.00058385386,0.00031066235,0.0024015766,0.0016206076,0.00060785166,0.0015452891,0.0006091653,0.0034458812],"category_scores_gemma":[0.00040994206,0.00022635775,0.0003362773,0.0019408052,0.0016168031,0.0007093945,0.0010624491,0.0007745144,0.0016096131],"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":[0.000466983,0.0001248622,0.1638933,0.0011450654,0.00014201476,0.01013873,0.01027819,0.00064490904,0.027177794,0.0022031376,0.008214663,0.7755704],"study_design_scores_gemma":[0.000015666354,0.0002933904,0.9187078,0.00030749515,0.000048866234,0.010344346,0.0031113774,0.00028766718,0.0006361599,0.00026225412,0.0659498,0.00003504025],"about_ca_topic_score_codex":0.07062277,"about_ca_topic_score_gemma":0.18582809,"teacher_disagreement_score":0.07062277,"about_ca_system_score_codex":0.0011580597,"about_ca_system_score_gemma":0.0005920053,"threshold_uncertainty_score":0.14042342},"labels":[],"label_agreement":null},{"id":"W2164786600","doi":"10.1017/s1755691007080383","title":"Diversity analysis of the Early Ordovician <i>Sinorthis</i> Fauna (Brachiopoda) from the Meitan Formation of Zunyi, northern Guizhou, South China","year":2007,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Science and Technology of the People's Republic of China","keywords":"Biozone; Ordovician; Fauna; Paleontology; Geology; Conodont; Ecology; Biostratigraphy; Biology","score_opus":0.0063521066132463085,"score_gpt":0.17338116362619127,"score_spread":0.16702905701294496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164786600","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99969184,0.000045495748,0.000021139498,0.0000057834513,5.0488893e-7,0.0000017778735,0.00008310529,0.000002000843,0.00014839978],"genre_scores_gemma":[0.99955124,0.00003229827,0.00004417691,0.0000039058764,0.0000010546986,0.0000033939953,0.0002400086,6.316962e-7,0.00012320369],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999027,0.000009734902,0.000011950027,0.000028425617,0.000020807793,0.000026359037],"domain_scores_gemma":[0.99980336,0.000020004645,0.000057838955,0.000012087579,0.000050438553,0.00005636355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018376057,0.00023745274,0.0001358875,0.0020468477,0.0005199433,0.00029816988,0.00018471692,0.00013395758,0.0008130574],"category_scores_gemma":[0.00022920799,0.000109996596,0.00017879544,0.0013589815,0.00032034316,0.0001393105,0.0003035693,0.000086006476,0.00007203625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025642772,0.000007189947,0.9873447,0.000024122257,0.000043170556,0.00010317277,0.0009243472,0.0001065502,0.004856977,0.000044114688,0.00009673864,0.006423355],"study_design_scores_gemma":[8.6586476e-7,0.0000046705563,0.99965346,0.0000011190685,0.0000034093046,0.000014628437,0.00011133257,0.000051135456,0.00004994733,0.000002862453,0.000105789535,7.4992977e-7],"about_ca_topic_score_codex":0.083404474,"about_ca_topic_score_gemma":0.19469917,"teacher_disagreement_score":0.083404474,"about_ca_system_score_codex":0.00074500806,"about_ca_system_score_gemma":0.0004936551,"threshold_uncertainty_score":0.165838},"labels":[],"label_agreement":null},{"id":"W2170913211","doi":"10.1017/s1755691009007038","title":"Geochemical investigation of an unusual alteration profile developed at the base of a Carboniferous lava flow, Isle of Bute, Scotland","year":2008,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Lava; Igneous rock; Geology; Weathering; Geochemistry; Carboniferous; Volcanic rock; Sedimentary rock; Volcano; Mafic; Rare earth; Mineralogy; Petrology; Geomorphology; Structural basin","score_opus":0.008732117997964793,"score_gpt":0.1759038978294008,"score_spread":0.167171779831436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170913211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99915457,0.000062190076,0.00007299938,0.000013034344,0.0000031297552,0.000007454718,0.00014761448,0.000004650265,0.0005344389],"genre_scores_gemma":[0.9991652,0.00006819258,0.00016118994,0.0000127881885,0.000004029827,0.0000027053663,0.0002156719,0.000003488722,0.00036678347],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998877,0.000005039585,0.000004175677,0.000019763656,0.00004224828,0.00004112674],"domain_scores_gemma":[0.9998311,0.000018191819,0.00003688753,0.0000061534292,0.00006495645,0.00004277657],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007939155,0.0002178857,0.00027325546,0.0015507716,0.0009850797,0.0008586249,0.00028475295,0.00032483976,0.00050280284],"category_scores_gemma":[0.0002175913,0.00016957884,0.00017493221,0.0010048907,0.0005330947,0.00016918364,0.00030552305,0.0002140128,0.00013712223],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050852494,0.00011712033,0.5486369,0.00012038012,0.00007747614,0.009882633,0.0031758295,0.00037483923,0.4241775,0.0001850538,0.00031411316,0.01242958],"study_design_scores_gemma":[0.0000048628403,0.00008371133,0.99250835,0.000003433723,0.000011528001,0.00067826785,0.0005828109,0.00024278993,0.0048407763,0.00001057174,0.0010286645,0.0000042636693],"about_ca_topic_score_codex":0.08355023,"about_ca_topic_score_gemma":0.122249015,"teacher_disagreement_score":0.08355023,"about_ca_system_score_codex":0.00071232213,"about_ca_system_score_gemma":0.0002907346,"threshold_uncertainty_score":0.1661278},"labels":[],"label_agreement":null},{"id":"W2574324173","doi":"10.1017/s1755691016000177","title":"Evolution of body size in anteaters and sloths (Xenarthra, Pilosa): phylogeny, metabolism, diet and substrate preferences","year":2015,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Ontario Museum; University of Toronto","funders":"","keywords":"Xenarthra; Biology; Sloth; Zoology; Phylogenetic tree; Monomorphism; Ecology; Range (aeronautics)","score_opus":0.012104561646329965,"score_gpt":0.19616704192359638,"score_spread":0.1840624802772664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2574324173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994711,0.00011811243,0.000043872853,0.000006234623,6.9068363e-7,8.5826156e-7,0.000052693435,0.0000017820773,0.0003046321],"genre_scores_gemma":[0.9997081,0.000045112003,0.00006644665,0.0000029640853,0.0000012515741,0.0000014431256,0.00006750082,0.0000011371502,0.00010600326],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998951,0.000024487174,0.000006940507,0.00003368923,0.000015048806,0.000024800216],"domain_scores_gemma":[0.99967813,0.00008352144,0.00012409862,0.000028157656,0.000024232708,0.00006191421],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017394191,0.00021633315,0.0001495726,0.0010775606,0.00035142855,0.0005131089,0.00020686226,0.00029985237,0.002460919],"category_scores_gemma":[0.00036562697,0.00015182253,0.00018268004,0.0005966463,0.0004817877,0.00022775322,0.0004177255,0.00022430813,0.00044540537],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001911174,0.000028873983,0.9680328,0.00003081465,0.000060815142,0.0001467377,0.00055755564,0.00013271296,0.022048905,0.000112805734,0.000048345322,0.008608407],"study_design_scores_gemma":[5.432136e-7,0.000023765831,0.9994766,0.0000021998496,0.0000037462908,0.00012856621,0.000117947835,0.000064245265,0.00010732362,0.000012075161,0.0000616614,0.0000012463966],"about_ca_topic_score_codex":0.0011741483,"about_ca_topic_score_gemma":0.003948378,"teacher_disagreement_score":0.002460919,"about_ca_system_score_codex":0.00016179445,"about_ca_system_score_gemma":0.000089155285,"threshold_uncertainty_score":0.008232594},"labels":[],"label_agreement":null},{"id":"W2579645759","doi":"10.1017/s175569101600013x","title":"Tooth wear and microwear of theropods from the Late Maastrichtian Marília Formation (Bauru Group), Minas Gerais State, Brazil","year":2015,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Universidade Federal do Rio de Janeiro; Conselho Nacional de Desenvolvimento Científico e Tecnológico","keywords":"Tooth wear; Geology; Paleontology; Dentistry; Medicine","score_opus":0.007796824165755866,"score_gpt":0.18370587892586915,"score_spread":0.1759090547601133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2579645759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990226,0.0002456155,0.00006393925,0.000012721729,0.0000010366624,0.0000063322145,0.00010029238,0.0000028405645,0.00054456387],"genre_scores_gemma":[0.9993604,0.00011836127,0.00019153536,0.000008732928,0.0000016715524,0.0000067228398,0.00010526376,0.000002052387,0.00020537263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998282,0.000025412799,0.000014789095,0.000051177325,0.00004912077,0.0000312921],"domain_scores_gemma":[0.99981016,0.00002525595,0.00006468199,0.000017737828,0.00005754867,0.000024625035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026143173,0.00029602088,0.00035031216,0.0023252224,0.00093139807,0.00048227175,0.00033067877,0.00025781215,0.0009464425],"category_scores_gemma":[0.00061223767,0.00026287138,0.00029133313,0.001483666,0.00065075915,0.00026654114,0.00067582994,0.00011934522,0.00025406262],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053388918,0.000017045257,0.9711509,0.000059138714,0.00006922137,0.0001960774,0.0069615683,0.00005017482,0.008805024,0.00006752436,0.00007045778,0.012499439],"study_design_scores_gemma":[5.9574165e-7,0.00001355068,0.9988165,0.0000047120643,0.000005902243,0.0000759879,0.0006870957,0.000029309467,0.00008553551,0.0000084328385,0.00027082447,0.0000014761927],"about_ca_topic_score_codex":0.102336876,"about_ca_topic_score_gemma":0.3300766,"teacher_disagreement_score":0.102336876,"about_ca_system_score_codex":0.0008027584,"about_ca_system_score_gemma":0.00037232714,"threshold_uncertainty_score":0.20348245},"labels":[],"label_agreement":null},{"id":"W2762741433","doi":"10.1017/s175569100900704x","title":"<i>Dawsonia</i> Nicholson: linguliform brachiopods, crustacean tail-pieces and a problematicum rather than graptolite ovarian vesicles","year":2008,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":"Natural Environment Research Council; Sight Research UK","keywords":"Appendage; Genus; Paleontology; Biology; Ordovician; Zoology","score_opus":0.008267026055334737,"score_gpt":0.18374238346799768,"score_spread":0.17547535741266293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2762741433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.83514,0.006048712,0.0015684617,0.0015642729,0.0006700191,0.00011917005,0.0010107703,0.00018206301,0.15369649],"genre_scores_gemma":[0.9783651,0.0010123692,0.0026009688,0.00052579155,0.000086367574,0.000026277196,0.00037299623,0.000019426267,0.01699064],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.999923,0.0000065104355,0.000007646626,0.000031200125,0.000014981093,0.000016654385],"domain_scores_gemma":[0.99985766,0.000017437897,0.000040692223,0.00001145239,0.00005161581,0.000021224176],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000081260485,0.00020433051,0.000116953466,0.0007710077,0.0010522116,0.0005098209,0.00024106633,0.0003509277,0.004722258],"category_scores_gemma":[0.00020230722,0.00011390581,0.000089498826,0.00056638237,0.0007643496,0.00042366036,0.00050968165,0.00029966576,0.0007596521],"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":[0.0009094348,0.00008492274,0.27469584,0.0014060598,0.00011048921,0.0076657683,0.012658536,0.00053842313,0.12185402,0.013634524,0.035894576,0.5305474],"study_design_scores_gemma":[0.000030502732,0.0001942765,0.4512676,0.00034234152,0.00007023865,0.007404827,0.0076750075,0.00048968877,0.014543989,0.0014254751,0.5165106,0.000045438625],"about_ca_topic_score_codex":0.022224562,"about_ca_topic_score_gemma":0.0864404,"teacher_disagreement_score":0.022224562,"about_ca_system_score_codex":0.0009365072,"about_ca_system_score_gemma":0.00045161945,"threshold_uncertainty_score":0.044190407},"labels":[],"label_agreement":null},{"id":"W2782996041","doi":"10.1017/s1755691017000159","title":"The distribution of <i>Schramocaris</i> (Eumalacostraca, Crustacea) along the northwestern coast of the Rheic Ocean during the Lower Carboniferous","year":2016,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":"Natural Environment Research Council; Sight Research UK","keywords":"Telson; Carboniferous; Carapace; Malacostraca; Range (aeronautics); Genus; Geology; Paleontology; Crustacean; Oceanography; Geography; Ecology; Biology; Decapoda","score_opus":0.004037956703015615,"score_gpt":0.1681465988590404,"score_spread":0.16410864215602478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2782996041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99782515,0.00013443627,0.000022801798,0.000019935098,0.0000019096008,0.000003835336,0.00013307677,0.000004027594,0.0018549359],"genre_scores_gemma":[0.99944705,0.00006109776,0.00005929325,0.000010150808,0.000001492642,0.0000017555246,0.00015924741,0.0000013608299,0.00025858518],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985325,0.000011325881,0.000008980588,0.000033229935,0.000046500143,0.0000467134],"domain_scores_gemma":[0.99964,0.00003243706,0.00012019198,0.000012824708,0.00012895859,0.00006554623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015994455,0.00011822701,0.0001234553,0.0013320912,0.0007362394,0.00045302848,0.00025123445,0.00018057125,0.0016881701],"category_scores_gemma":[0.00032769018,0.00012129377,0.00015218213,0.0007291437,0.00059187337,0.00025345705,0.00056416204,0.00016846535,0.0002680107],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006590203,0.000008918921,0.9726806,0.00005014987,0.000033623015,0.00023523372,0.001710395,0.00007651296,0.010169319,0.00009873743,0.00025260274,0.014617839],"study_design_scores_gemma":[9.0257146e-7,0.000010673283,0.99906725,0.0000057572165,0.000001837483,0.000048850543,0.00031996315,0.000018005318,0.00006887172,0.0000038408357,0.0004526461,0.0000014192361],"about_ca_topic_score_codex":0.23135754,"about_ca_topic_score_gemma":0.5870595,"teacher_disagreement_score":0.23135754,"about_ca_system_score_codex":0.00090949354,"about_ca_system_score_gemma":0.00056551525,"threshold_uncertainty_score":0.4600218},"labels":[],"label_agreement":null},{"id":"W2909881882","doi":"10.1017/s1755691018000567","title":"An enigmatic braincase from Five Points, Ohio (Westphalian D) further supports a stem tetrapod position for aïstopods","year":2018,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Paleontology and Evolutionary Biology","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 Alberta","funders":"","keywords":"Tetrapod (structure); Anatomy; Skull; Occiput; Biology; Process (computing); Paleontology; Computer science","score_opus":0.007086448118471202,"score_gpt":0.2045945697490086,"score_spread":0.1975081216305374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909881882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9794175,0.0004563912,0.0012265247,0.0002506077,0.00005295061,0.000015680736,0.00017560949,0.000025011643,0.018379716],"genre_scores_gemma":[0.99626166,0.0003240978,0.0012887141,0.00006600831,0.000024075018,0.000005253217,0.00016984063,0.0000075204875,0.0018528005],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998796,0.000008280312,0.000009543895,0.000041344272,0.00003711049,0.000024116587],"domain_scores_gemma":[0.99974793,0.000029468647,0.00008537134,0.00003851042,0.000049828395,0.00004891932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015392846,0.00026150278,0.00018200719,0.001155674,0.0018183602,0.0009490086,0.00046109816,0.00052998035,0.0054891026],"category_scores_gemma":[0.00038367364,0.0001373515,0.000135292,0.0008050017,0.0023126383,0.0007319856,0.0012542306,0.00057201966,0.0006538336],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007313014,0.000066304056,0.5642452,0.00066437264,0.00015664136,0.030138316,0.019995213,0.00052814785,0.16607098,0.0067501557,0.0028968307,0.20775647],"study_design_scores_gemma":[0.000010918915,0.000182191,0.9060336,0.00020964436,0.00006564814,0.014953331,0.014213455,0.0003586642,0.0051072054,0.0019371276,0.056895863,0.000032350134],"about_ca_topic_score_codex":0.008343815,"about_ca_topic_score_gemma":0.029776629,"teacher_disagreement_score":0.008343815,"about_ca_system_score_codex":0.0004371156,"about_ca_system_score_gemma":0.0004267911,"threshold_uncertainty_score":0.01836288},"labels":[],"label_agreement":null},{"id":"W3081718081","doi":"10.1017/s1755691020000080","title":"First dinosaur from the Isle of Eigg (Valtos Sandstone Formation, Middle Jurassic), Scotland","year":2020,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Paleontology and Evolutionary Biology","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":"Royal Tyrrell Museum","funders":"Leverhulme Trust; Scottish Natural Heritage; National Geographic Society","keywords":"Geology; Paleontology; Taxon; Group (periodic table); Archaeology; Geography","score_opus":0.011987614030460966,"score_gpt":0.1731129137619784,"score_spread":0.16112529973151743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3081718081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948908,0.00046708295,0.00009326402,0.000022989774,0.000014460305,0.000013696122,0.0013998845,0.000012732632,0.0030849697],"genre_scores_gemma":[0.9942141,0.00032907975,0.00045897666,0.00004702501,0.000011603453,0.000013519392,0.0026141505,0.000007713328,0.0023037314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997136,0.000016087923,0.000027491411,0.000075578995,0.00009159453,0.00007550711],"domain_scores_gemma":[0.9996427,0.000026385882,0.00010443385,0.000031983418,0.00010705602,0.000087540975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024503493,0.00041016858,0.00036372096,0.0036994854,0.0011886831,0.0007404961,0.00039843237,0.0003207065,0.0030047728],"category_scores_gemma":[0.0004064605,0.00019848754,0.00025052403,0.001829166,0.0006840683,0.00026071013,0.0014314892,0.00020295811,0.0008719417],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036398717,0.000041375693,0.92883027,0.00023275106,0.00009034937,0.003595424,0.0049957903,0.00008233367,0.015451203,0.00019073066,0.0013019018,0.04482385],"study_design_scores_gemma":[0.000004321271,0.000083916384,0.9929128,0.000022587683,0.000013762954,0.00067805784,0.0012774037,0.000020547284,0.00020367689,0.000017990704,0.0047604595,0.000004354847],"about_ca_topic_score_codex":0.06656117,"about_ca_topic_score_gemma":0.2369689,"teacher_disagreement_score":0.06656117,"about_ca_system_score_codex":0.0006884348,"about_ca_system_score_gemma":0.00050697674,"threshold_uncertainty_score":0.13234746},"labels":[],"label_agreement":null},{"id":"W4200484353","doi":"10.1017/s1755691021000402","title":"Dynamic ecophenotypy in the Silurian Monograptidae (Graptolithina)","year":2021,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":"Carleton University","funders":"Lietuvos Mokslo Taryba","keywords":"Annulus (botany); Baltica; Phytoplankton; Storm; Upwelling; Period (music); Extinction event; Productivity; Oceanography; Geology; Paleontology; Physical geography; Ecology; Geography; Biology; Biological dispersal; Physics; Nutrient; Ordovician","score_opus":0.005893371581480537,"score_gpt":0.1881469951696773,"score_spread":0.18225362358819677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200484353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993938,0.00007130386,0.00005295307,0.0000033179635,9.082528e-7,0.0000016562177,0.00006478312,0.0000036007636,0.00040769036],"genre_scores_gemma":[0.99951124,0.00003420672,0.00016405295,0.0000062471822,0.0000024028639,0.0000036722067,0.00012691642,0.0000017155586,0.00014951515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998822,0.000018204046,0.0000075861303,0.00005073964,0.000019716239,0.000021511618],"domain_scores_gemma":[0.99968183,0.00005184139,0.00014092057,0.000022805023,0.000046996178,0.000055553017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015726898,0.00015577441,0.00014003702,0.0018976134,0.0004713779,0.0004192459,0.00022814551,0.0002005866,0.0014296528],"category_scores_gemma":[0.00034532137,0.00014120642,0.00012587398,0.0006377699,0.0005902757,0.00020503192,0.00046234127,0.0001385662,0.00021094277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019858712,0.000027702834,0.92110515,0.00006080751,0.000059436305,0.00018171195,0.0016609016,0.00025232343,0.060943846,0.0001385517,0.00010437029,0.015266539],"study_design_scores_gemma":[7.051448e-7,0.000020134514,0.9994357,0.0000022747015,0.0000031856307,0.00007863152,0.00011295469,0.00006990465,0.00013476581,0.000010506643,0.00012973089,0.0000014559517],"about_ca_topic_score_codex":0.003256075,"about_ca_topic_score_gemma":0.014496336,"teacher_disagreement_score":0.003256075,"about_ca_system_score_codex":0.0003557595,"about_ca_system_score_gemma":0.00013377696,"threshold_uncertainty_score":0.0064742565},"labels":[],"label_agreement":null},{"id":"W4233368820","doi":"10.1017/s026359330000095x","title":"Origin of chemically zoned and unzoned cordierites from the South Mountain and Musquodoboit Batholiths, Nova Scotia","year":2004,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Killam Trusts; Dalhousie University","keywords":"Zoning; Batholith; Geology; Geochemistry; Igneous rock; Magma; Mineralogy; Paleontology; Volcano; Law","score_opus":0.007152242317598937,"score_gpt":0.17376789246361374,"score_spread":0.1666156501460148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233368820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99772924,0.00019946999,0.000053913398,0.000010147828,0.0000025050322,0.000017313774,0.0002890565,0.0000055386718,0.0016927087],"genre_scores_gemma":[0.998324,0.000120814,0.0001447414,0.000008775247,0.0000015261764,0.0000072450457,0.00027033722,0.0000049231294,0.0011176016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982315,0.000007733578,0.000010942682,0.000057450823,0.000042039657,0.000058601036],"domain_scores_gemma":[0.9996331,0.000038827104,0.000094954245,0.000020421827,0.00014280813,0.00006995287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018159047,0.00034383094,0.00028664357,0.0025347339,0.0011787905,0.0009380209,0.00036768682,0.00021655129,0.0018032066],"category_scores_gemma":[0.00058540044,0.00023076577,0.0001883668,0.001965692,0.0011083141,0.00014318763,0.0006906853,0.00019012614,0.000330582],"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":[0.00047233768,0.00001886216,0.91346097,0.00020147633,0.000058106583,0.0012979856,0.004244311,0.00036737524,0.06283372,0.00026581666,0.00018403945,0.016594913],"study_design_scores_gemma":[0.000002441736,0.000010215823,0.9980286,0.000012179398,0.000005502726,0.000153884,0.0006226721,0.00007485702,0.0005606484,0.000008693894,0.00051760324,0.0000026235205],"about_ca_topic_score_codex":0.70592034,"about_ca_topic_score_gemma":0.85602826,"teacher_disagreement_score":0.29407966,"about_ca_system_score_codex":0.0033840567,"about_ca_system_score_gemma":0.0018128107,"threshold_uncertainty_score":0.59162307},"labels":[],"label_agreement":null},{"id":"W4233630045","doi":"10.1017/s0263593300007306","title":"Grain-scale and outcrop-scale distribution and movement of melt in a crystallising granite","year":2000,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Chicoutimi","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lineation; Outcrop; Pluton; Foliation (geology); Shearing (physics); Hornblende; Tectonics; Mineralogy; Migmatite; Shear zone; Thin section; Mica; Shear (geology); Geochemistry; Petrology; Biotite; Metamorphic rock; Seismology; Gneiss; Geotechnical engineering","score_opus":0.0040469266284830115,"score_gpt":0.16196527979679207,"score_spread":0.15791835316830904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233630045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995072,0.000018468541,0.00006705446,0.0000034625102,2.813837e-7,0.0000012464608,0.0000919101,0.000013737292,0.00029665465],"genre_scores_gemma":[0.99949515,0.000019921328,0.0001531404,0.0000017627594,4.364929e-7,0.0000014460375,0.00012182688,0.0000075824487,0.00019865013],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999552,0.0000021802855,0.0000021331475,0.000022993721,0.0000074255686,0.000010068433],"domain_scores_gemma":[0.9999069,0.00001680806,0.000027968332,0.00001230687,0.000015584515,0.000020384588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000047353846,0.00010982524,0.00014259478,0.00086313975,0.0003397663,0.0004689763,0.00021006029,0.00022083196,0.0008707731],"category_scores_gemma":[0.00017030121,0.00014635717,0.00017304033,0.00046742847,0.00047455923,0.00014650251,0.00032275481,0.00016070312,0.00016014128],"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":[0.0014152799,0.00008657652,0.4177288,0.00009310893,0.00010901152,0.0008743152,0.0025454592,0.005656862,0.5526702,0.000357933,0.00018824295,0.018274197],"study_design_scores_gemma":[0.000010250261,0.000071823866,0.9905185,0.0000038811695,0.00001856886,0.00020997648,0.00033323173,0.0018790695,0.006320519,0.00007284439,0.000551808,0.000009519905],"about_ca_topic_score_codex":0.016241774,"about_ca_topic_score_gemma":0.02753974,"teacher_disagreement_score":0.016241774,"about_ca_system_score_codex":0.00060897664,"about_ca_system_score_gemma":0.0001292752,"threshold_uncertainty_score":0.03229451},"labels":[],"label_agreement":null},{"id":"W4234773196","doi":"10.1017/s1755691015000080","title":"TRE volume 105 issue 3 Cover and Front matter","year":2014,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":0,"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":"British Geological Survey; University of Stirling; University of Bristol; University of Glasgow; University of St Andrews; University College, Oxford; Imperial College London; Lunds Universitet; University of Dundee; McGill University","keywords":"Front cover; Cover (algebra); Volume (thermodynamics); Front (military); Environmental science; Action (physics); Engineering; Geography; Meteorology; Physics; Mechanical engineering; Thermodynamics","score_opus":0.007520784185317876,"score_gpt":0.16137985713801817,"score_spread":0.1538590729527003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234773196","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":[0.0008229986,0.001042087,0.0003773034,0.0030163107,0.0071852696,0.000096880765,0.0027354807,0.0017136616,0.9830101],"genre_scores_gemma":[0.0018399323,0.00048900704,0.00014316005,0.0008404269,0.0011971018,0.000023972614,0.0012438472,0.00033481253,0.9938877],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993248,0.000034231696,0.000024617964,0.00013568124,0.00039792887,0.000082724066],"domain_scores_gemma":[0.99846065,0.00017653202,0.000048088194,0.00024440864,0.00067414815,0.00039616163],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00075198506,0.0009975268,0.0009192239,0.0023870096,0.0018061076,0.0070062964,0.0009822737,0.00282894,0.8961415],"category_scores_gemma":[0.0020122898,0.00045735386,0.0008764535,0.0013330036,0.0008130597,0.0019348818,0.0017061335,0.0021940742,0.85159403],"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":[0.000048433183,0.00007488006,0.00022489234,0.00010937782,0.0000071939403,0.00006729901,0.00001583542,0.000042861284,0.00094866473,0.0015558663,0.9464049,0.050499856],"study_design_scores_gemma":[0.000008354144,0.000020453243,0.00092069886,0.000077817254,0.0000037239133,0.00006081488,0.000026292153,0.00008275328,0.00039153686,0.0003764606,0.9980259,0.0000052566],"about_ca_topic_score_codex":0.003304812,"about_ca_topic_score_gemma":0.006051955,"teacher_disagreement_score":0.10385847,"about_ca_system_score_codex":0.0015945763,"about_ca_system_score_gemma":0.0015125507,"threshold_uncertainty_score":0.14814144},"labels":[],"label_agreement":null},{"id":"W4238267563","doi":"10.1017/s0263593300007458","title":"Granite-hosted mineral deposits of the New Ross area, South Mountain Batholith, Nova Scotia, Canada: P, T and X constraints of fluids using fluid inclusion thermometry and decrepitate analysis","year":2000,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Technical University of Nova Scotia; Nova Scotia Department of Energy; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Fluid inclusions; Geochemistry; Halite; Pegmatite; Batholith; Mineralogy; Sphalerite; Meteoric water; Inclusion (mineral); Quartz; Gypsum; Hydrothermal circulation; Pyrite","score_opus":0.0066470366539842915,"score_gpt":0.17273976339998642,"score_spread":0.16609272674600215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4238267563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949411,0.00038378843,0.00012141437,0.00004703705,0.0000032263704,0.000020902164,0.0013287708,0.000019149395,0.0031345864],"genre_scores_gemma":[0.9971289,0.00017076415,0.00031382468,0.000018332124,0.0000011394867,0.000007293295,0.0006625373,0.0000094436455,0.0016877003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998895,0.0000041878716,0.000007717277,0.000033201806,0.000029416968,0.000035957448],"domain_scores_gemma":[0.9997912,0.00001675615,0.000034139543,0.000008957056,0.000099966805,0.00004902863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000106177475,0.00027874997,0.00018174671,0.0017259751,0.0010869664,0.00080088753,0.00041478124,0.0001996604,0.0017398653],"category_scores_gemma":[0.00037752057,0.00022401917,0.00017642186,0.001337638,0.00059041264,0.00014988698,0.00047759316,0.00016763851,0.0004276392],"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":[0.00052246626,0.000047975824,0.8562729,0.0002537091,0.00012866809,0.0016201294,0.0023394933,0.0017258798,0.10852287,0.000581496,0.00097139744,0.027013073],"study_design_scores_gemma":[0.000010691116,0.0000135463215,0.99622774,0.000018789082,0.000015248706,0.000115180526,0.0006072674,0.0005522463,0.0010589744,0.000022308797,0.0013507294,0.000007304125],"about_ca_topic_score_codex":0.9593962,"about_ca_topic_score_gemma":0.98540443,"teacher_disagreement_score":0.040603817,"about_ca_system_score_codex":0.00525157,"about_ca_system_score_gemma":0.0040700776,"threshold_uncertainty_score":0.08168584},"labels":[],"label_agreement":null},{"id":"W4238322466","doi":"10.1017/s1755691014000188","title":"TRE volume 104 issue 3-4 Cover and Front matter","year":2013,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Bristol; Lunds Universitet; Imperial College London; University College, Oxford; McGill University","keywords":"Front cover; Cover (algebra); Volume (thermodynamics); Front (military); Environmental science; Computer science; Engineering; Geography; Meteorology; Physics; Mechanical engineering; Thermodynamics","score_opus":0.007758589984664556,"score_gpt":0.1589921543866109,"score_spread":0.15123356440194635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4238322466","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":[0.00076450105,0.00095233653,0.00035968493,0.0024267242,0.0050847987,0.00008169826,0.002745472,0.0013163981,0.9862684],"genre_scores_gemma":[0.0019249681,0.0005854618,0.00018167424,0.00068146957,0.000873239,0.000025544727,0.0014703833,0.0003826079,0.9938747],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99929583,0.000039581428,0.000022825629,0.000118346055,0.00043029102,0.000093017115],"domain_scores_gemma":[0.9984869,0.0001727008,0.00004873694,0.00025379274,0.00068732764,0.0003505882],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007403162,0.00094989524,0.0008556655,0.0025927052,0.0017458784,0.0068393806,0.0010523138,0.0027678867,0.89305276],"category_scores_gemma":[0.0019001331,0.00043508876,0.0008198028,0.0015938492,0.00082470215,0.001983035,0.0017783263,0.002160296,0.8336432],"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":[0.000047295554,0.00007409606,0.00024083117,0.00011503056,0.0000062134427,0.000057143694,0.000015229421,0.000049505277,0.0010632857,0.0019817704,0.9421674,0.05418228],"study_design_scores_gemma":[0.000007822661,0.000019978323,0.0010230541,0.000078497855,0.0000035891483,0.000063272164,0.000029696472,0.00009400798,0.0004877307,0.00048976764,0.9976968,0.0000057155885],"about_ca_topic_score_codex":0.0042044376,"about_ca_topic_score_gemma":0.007434542,"teacher_disagreement_score":0.10694724,"about_ca_system_score_codex":0.0018981122,"about_ca_system_score_gemma":0.0016428385,"threshold_uncertainty_score":0.15254724},"labels":[],"label_agreement":null},{"id":"W4239331735","doi":"10.1017/s1755691013000133","title":"TRE volume 104 issue 1 Cover and Front matter","year":2013,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":0,"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":"Lunds Universitet; British Geological Survey; University of Stirling; University of Bristol; University of Glasgow; Imperial College London; University College, Oxford; McGill University","keywords":"Front cover; Cover (algebra); Front (military); Volume (thermodynamics); Action (physics); Environmental science; Geography; Engineering; Meteorology; Physics; Mechanical engineering","score_opus":0.007870003597018792,"score_gpt":0.1590263815093442,"score_spread":0.15115637791232542,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239331735","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":[0.000813008,0.0014429394,0.00037148103,0.0033565923,0.009106851,0.00010546677,0.0028215707,0.0015544337,0.9804277],"genre_scores_gemma":[0.0015061742,0.00066684035,0.00014554294,0.00073822145,0.0014932349,0.000025702968,0.0013040781,0.00032939133,0.9937908],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992767,0.000040124076,0.000024788613,0.00013349729,0.00043515352,0.00008980757],"domain_scores_gemma":[0.9981875,0.00022734057,0.0000582992,0.00027488908,0.00083129696,0.00042069925],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007699669,0.0010971298,0.0010190348,0.0026996057,0.001845497,0.0068412116,0.001125505,0.0028539398,0.89333874],"category_scores_gemma":[0.002245644,0.00049174106,0.00081906683,0.0017114482,0.0008060202,0.0020796352,0.0017051429,0.0022297916,0.8395655],"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":[0.00004366306,0.00007222023,0.00019785861,0.00012171455,0.000006031651,0.00005389134,0.00001302295,0.00004226766,0.0007398934,0.0012646253,0.9441158,0.053328857],"study_design_scores_gemma":[0.000007668582,0.000019200354,0.00095100387,0.00008559259,0.0000034974082,0.000057660727,0.000023783556,0.00008323449,0.00034527484,0.00035083308,0.9980666,0.000005582892],"about_ca_topic_score_codex":0.0031627407,"about_ca_topic_score_gemma":0.006005716,"teacher_disagreement_score":0.10666126,"about_ca_system_score_codex":0.001721046,"about_ca_system_score_gemma":0.001601289,"threshold_uncertainty_score":0.15213937},"labels":[],"label_agreement":null},{"id":"W4242130972","doi":"10.1017/s0263593300000985","title":"Deciphering the petrogenesis of deeply buried granites: whole-rock geochemical constraints on the origin of largely undepleted felsic granulites from the Moldanubian Zone of the Bohemian Massif","year":2004,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Austrian Science Fund","keywords":"Felsic; Granulite; Geology; Geochemistry; Massif; Zircon; Metamorphism; Petrogenesis; Petrology; Anatexis; Protolith; Continental crust; Fractional crystallization (geology); Crust; Mafic; Partial melting; Facies; Basalt; Geomorphology","score_opus":0.010000940912245664,"score_gpt":0.17391700488297146,"score_spread":0.1639160639707258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4242130972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99880755,0.00024054653,0.0001400848,0.000014526789,0.0000014735914,0.000004313673,0.000096356765,0.000009498433,0.000685671],"genre_scores_gemma":[0.999642,0.00004975009,0.00011432338,0.0000033776832,8.964859e-7,0.0000013710237,0.00006819222,0.000003719997,0.000116154944],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999486,0.0000043139576,0.0000028717427,0.000016557382,0.0000101453115,0.000017554252],"domain_scores_gemma":[0.9999473,0.000009925472,0.000016935659,0.000006109089,0.000009749941,0.000009971297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016512132,0.00024181469,0.00020685497,0.001634254,0.00040842683,0.0005856904,0.00026553974,0.00018420546,0.001542993],"category_scores_gemma":[0.00018855117,0.00014914478,0.00014770305,0.000598162,0.0005445347,0.0003016726,0.00060335937,0.0001268086,0.0001712726],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034469378,0.000021505364,0.77479124,0.0001228255,0.00011825967,0.0007253481,0.0016404792,0.0012513752,0.19478035,0.0004334216,0.00010672872,0.025663784],"study_design_scores_gemma":[0.000002123579,0.000011039738,0.99790204,0.0000056376102,0.000009394642,0.00007054151,0.00024270336,0.0003001122,0.0010402789,0.000035535944,0.0003784189,0.0000022032946],"about_ca_topic_score_codex":0.022460742,"about_ca_topic_score_gemma":0.04305154,"teacher_disagreement_score":0.022460742,"about_ca_system_score_codex":0.00056298106,"about_ca_system_score_gemma":0.0002579464,"threshold_uncertainty_score":0.044659972},"labels":[],"label_agreement":null},{"id":"W4244880472","doi":"10.1017/s1755691009016016","title":"Parental magmas of Grenville Province massif-type anorthosites, and conjectures about why massif anorthosites are restricted to the Proterozoic","year":2009,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":"Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Underplating; Crust; Massif; Partial melting; Mantle (geology); Basalt; Fractional crystallization (geology); Subduction; Proterozoic; Petrology; Tectonics; Paleontology","score_opus":0.0056297697380722125,"score_gpt":0.17261252103326233,"score_spread":0.1669827512951901,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244880472","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916021,0.00045350182,0.00045775186,0.00021872832,0.000008980921,0.000004993013,0.00017628427,0.00004618498,0.007031373],"genre_scores_gemma":[0.999071,0.00007454517,0.0001604683,0.000013147067,0.0000022035879,0.0000011639255,0.00008541178,0.000009350751,0.00058251806],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998248,0.0000172187,0.000008833823,0.00006950713,0.000023783092,0.000055772412],"domain_scores_gemma":[0.99975306,0.000034891324,0.000069971815,0.000034140714,0.000071588525,0.000036322504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004304972,0.0002395612,0.0002628724,0.0007132993,0.0005329174,0.0012510694,0.0004908272,0.00041253553,0.002271799],"category_scores_gemma":[0.0008472552,0.00016268196,0.00023202132,0.00044422326,0.0006810614,0.00045102526,0.0002594554,0.00021680353,0.0003041455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00066441804,0.000041410134,0.8111812,0.0001491791,0.00020170386,0.0010278977,0.0017448916,0.005298559,0.12477504,0.010365416,0.00057856616,0.043971743],"study_design_scores_gemma":[0.000024593583,0.000053809767,0.9829164,0.000051081508,0.000035555575,0.0002649145,0.00076842896,0.0036099309,0.004343748,0.0012705436,0.006642187,0.000018706223],"about_ca_topic_score_codex":0.120677724,"about_ca_topic_score_gemma":0.18995164,"teacher_disagreement_score":0.120677724,"about_ca_system_score_codex":0.0020042162,"about_ca_system_score_gemma":0.0006027101,"threshold_uncertainty_score":0.2399506},"labels":[],"label_agreement":null},{"id":"W4246161178","doi":"10.1017/s1755691010999945","title":"TRE volume 101 issue 2 Cover and Front matter","year":2010,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":0,"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":"Lunds Universitet; British Geological Survey; Macquarie University; University of Bristol; University of Glasgow; James Cook University; Imperial College London; University College, Oxford; McGill University","keywords":"Front cover; Cover (algebra); Volume (thermodynamics); Front (military); Action (physics); Content (measure theory); Environmental science; Computer science; Geography; Engineering; Meteorology; Mathematics; Physics; Mechanical engineering","score_opus":0.007145790945801427,"score_gpt":0.16474868062736023,"score_spread":0.1576028896815588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4246161178","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":[0.00085940136,0.0012713065,0.00032588444,0.0034563395,0.00892416,0.000098137956,0.002305752,0.0011302436,0.9816288],"genre_scores_gemma":[0.0016429602,0.00050199346,0.00012610554,0.00068746344,0.0012486182,0.00002119609,0.0010464601,0.0002475456,0.9944776],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99938893,0.000033676803,0.000020584175,0.000119340446,0.00035987413,0.000077562974],"domain_scores_gemma":[0.9986829,0.00015732535,0.000036953414,0.00019922071,0.000574098,0.00034950435],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007069909,0.0010787016,0.0009882264,0.0021059979,0.0018033439,0.0067237443,0.0010178578,0.0028766093,0.88534504],"category_scores_gemma":[0.0019741734,0.0004609617,0.000793241,0.0011956481,0.0007350456,0.0020827348,0.0016483158,0.0021955236,0.8257329],"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":[0.000060426315,0.00007325851,0.00021249504,0.00011812813,0.0000069318135,0.00008328419,0.000016445803,0.00004782249,0.0009790324,0.0016613188,0.94423795,0.052502915],"study_design_scores_gemma":[0.000008942508,0.000019487321,0.0008060614,0.00006503628,0.0000032540565,0.00007001778,0.000024651721,0.0000783085,0.00036613428,0.0003781522,0.998175,0.0000050301282],"about_ca_topic_score_codex":0.0028882513,"about_ca_topic_score_gemma":0.005716714,"teacher_disagreement_score":0.11465496,"about_ca_system_score_codex":0.0015249657,"about_ca_system_score_gemma":0.0013117408,"threshold_uncertainty_score":0.16354138},"labels":[],"label_agreement":null},{"id":"W4250644199","doi":"10.1017/s1755691011999976","title":"TRE volume 102 issue 1 Cover and Front matter","year":2011,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":0,"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":"Lunds Universitet; British Geological Survey; Macquarie University; University of Bristol; University of Glasgow; James Cook University; Imperial College London; University College, Oxford; McGill University","keywords":"Front cover; Cover (algebra); Volume (thermodynamics); Front (military); Action (physics); Environmental science; Computer science; Engineering; Physics; Mechanical engineering; Thermodynamics","score_opus":0.013955406574090662,"score_gpt":0.1630011246451314,"score_spread":0.14904571807104072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250644199","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":[0.0008264938,0.0015107548,0.00034858065,0.0035810485,0.010497724,0.000108559405,0.00286701,0.0014339255,0.978826],"genre_scores_gemma":[0.0014718081,0.00058228115,0.000120356286,0.0006544011,0.001436998,0.000022022055,0.0012282209,0.00024954078,0.9942345],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993618,0.00003305094,0.000021351505,0.00011837273,0.0003857406,0.00007974485],"domain_scores_gemma":[0.99857414,0.00015913429,0.0000460858,0.0002203511,0.00064858433,0.00035180827],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000672028,0.0011268514,0.0010163903,0.0023385286,0.0017149852,0.0063533937,0.0010677685,0.0027106367,0.8893864],"category_scores_gemma":[0.0019554324,0.00048122133,0.0007709045,0.0013917449,0.00067672937,0.0019407553,0.001628562,0.0020771655,0.8264676],"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":[0.00005075281,0.00006783806,0.00018546538,0.00012264313,0.0000060821385,0.00007112582,0.000012296983,0.00004038433,0.0008875936,0.0011592737,0.94493866,0.052457996],"study_design_scores_gemma":[0.000008240708,0.000018971195,0.0008852692,0.00007107326,0.0000031207583,0.00006513707,0.00002183284,0.00007212995,0.00035461152,0.00031970785,0.9981749,0.0000049723876],"about_ca_topic_score_codex":0.0028953105,"about_ca_topic_score_gemma":0.0056016394,"teacher_disagreement_score":0.8893864,"about_ca_system_score_codex":0.0015268167,"about_ca_system_score_gemma":0.0013336391,"threshold_uncertainty_score":0.15777677},"labels":[],"label_agreement":null},{"id":"W4254565896","doi":"10.1017/s1755691009999996","title":"TRE volume 100 issue 1-2 Cover and Front matter","year":2009,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","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":"McGill University","funders":"","keywords":"Front cover; Cover (algebra); Volume (thermodynamics); Front (military); Action (physics); Environmental science; Engineering; Meteorology; Geography; Physics; Mechanical engineering; Thermodynamics","score_opus":0.008886050348517475,"score_gpt":0.17094955484654872,"score_spread":0.16206350449803125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254565896","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":[0.0008345197,0.0014722415,0.00044048016,0.0025809817,0.005610488,0.00008412441,0.0025231142,0.0010884613,0.9853656],"genre_scores_gemma":[0.001857787,0.0008145291,0.00019669345,0.0006203328,0.00073559984,0.000022722368,0.0014234465,0.00035419376,0.99397475],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993519,0.000036246696,0.000021279597,0.00011074925,0.00040679576,0.0000729476],"domain_scores_gemma":[0.9987269,0.00015764768,0.000039554106,0.00019745805,0.0005889227,0.00028943273],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0006919259,0.0010657355,0.00088328525,0.0024093552,0.0014637616,0.006583385,0.0011148009,0.002634172,0.87742174],"category_scores_gemma":[0.0019225522,0.0004535392,0.00071713293,0.0015350268,0.0007340438,0.002355474,0.0017262462,0.0021732727,0.8247148],"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":[0.000054151544,0.0000805607,0.00024798565,0.00012950931,0.0000072824023,0.000078003366,0.00001608759,0.000057173613,0.0012085281,0.0022230344,0.9229578,0.07293994],"study_design_scores_gemma":[0.000007803683,0.000017685064,0.00075456104,0.00007527182,0.0000031709753,0.000073539646,0.000026004067,0.000087220375,0.0004732444,0.00058259565,0.99789375,0.000005238945],"about_ca_topic_score_codex":0.0027547313,"about_ca_topic_score_gemma":0.0055305315,"teacher_disagreement_score":0.12257826,"about_ca_system_score_codex":0.0014093234,"about_ca_system_score_gemma":0.0011588588,"threshold_uncertainty_score":0.17484295},"labels":[],"label_agreement":null},{"id":"W4255226161","doi":"10.1017/s1755691015000171","title":"TRE volume 105 issue 4 Cover and Front matter","year":2014,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"British Geological Survey; University of Stirling; University of Bristol; University of Glasgow; University of St Andrews; University College, Oxford; Imperial College London; Lunds Universitet; University of Dundee; McGill University","keywords":"Front cover; Cover (algebra); Volume (thermodynamics); Front (military); Action (physics); Environmental science; Engineering; Geography; Meteorology; Physics; Mechanical engineering","score_opus":0.007573649771398767,"score_gpt":0.16163066926920353,"score_spread":0.15405701949780476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255226161","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":[0.0008199582,0.0010281045,0.00035643153,0.0031374756,0.0071619963,0.00009745745,0.0027693405,0.0016443384,0.98298496],"genre_scores_gemma":[0.0017398152,0.00045701384,0.00013470296,0.0007818298,0.0011687743,0.000023043553,0.0012251973,0.00031091744,0.99415874],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992873,0.00003708412,0.000025856985,0.00013988835,0.0004217118,0.00008818223],"domain_scores_gemma":[0.99838066,0.00018249982,0.000051211297,0.00025569313,0.0007091845,0.00042070323],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007788441,0.0010349661,0.00094314956,0.002572402,0.0018740393,0.0070646117,0.0010237162,0.002897095,0.90080756],"category_scores_gemma":[0.0021172443,0.0004815074,0.0008833766,0.0013711975,0.0008375555,0.0019974597,0.0017931415,0.002225222,0.85394716],"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":[0.000048295005,0.000075820186,0.00022736545,0.000108798566,0.000007317194,0.00006623007,0.000015756168,0.0000431648,0.0009158535,0.0015532202,0.9476721,0.049266085],"study_design_scores_gemma":[0.000008347748,0.000020464695,0.0009006416,0.00007581588,0.0000037229831,0.000057496225,0.000026478132,0.00007899333,0.00038096032,0.0003635272,0.9980782,0.0000052134405],"about_ca_topic_score_codex":0.0033880086,"about_ca_topic_score_gemma":0.0061588497,"teacher_disagreement_score":0.09919244,"about_ca_system_score_codex":0.0016878695,"about_ca_system_score_gemma":0.0015912373,"threshold_uncertainty_score":0.14148599},"labels":[],"label_agreement":null},{"id":"W4288077408","doi":"10.1017/s1755691022000081","title":"Sequence stratigraphy and microplankton palaeoenvironmental dynamics across the Jurassic–Cretaceous transition in the Canadian Arctic","year":2022,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Paleontology and Stratigraphy of Fossils","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":"Dinoflagellate; Paleontology; Sverdrup; Geology; Arctic; Outcrop; Cretaceous; Marine transgression; Sequence stratigraphy; Sea level; Lithology; Oceanography; Structural basin; Sedimentary depositional environment","score_opus":0.007213578557088116,"score_gpt":0.19063828609289776,"score_spread":0.18342470753580964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4288077408","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968573,0.00057738187,0.000078842924,0.0000626772,0.0000040901386,0.0000054453308,0.0012260949,0.00000935141,0.0011788293],"genre_scores_gemma":[0.99858665,0.00019684208,0.00007733097,0.000007775993,0.0000012109567,0.0000024560059,0.00045901036,0.0000024896342,0.0006663261],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998109,0.000008112647,0.000008807052,0.000047567857,0.00004629137,0.00007845344],"domain_scores_gemma":[0.99938333,0.000032436677,0.0001072292,0.000015056346,0.00032545676,0.00013647864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025444347,0.00023644582,0.00016800656,0.0026548088,0.0018190276,0.0009572488,0.00046592604,0.00019720457,0.001691692],"category_scores_gemma":[0.0005857311,0.0001428317,0.00022229529,0.0027207914,0.0005370247,0.00021315362,0.00039801552,0.00021058807,0.00014824657],"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":[0.000064815446,0.000009146238,0.98019654,0.000040751154,0.000049653423,0.00010045402,0.0029300328,0.00024528467,0.0026865117,0.00024751466,0.0005082062,0.012921255],"study_design_scores_gemma":[5.0488364e-7,0.000003896038,0.998519,0.00000779515,0.0000058139835,0.00002058011,0.00072468276,0.000118569806,0.000053222342,0.000009502348,0.00053405133,0.0000023739426],"about_ca_topic_score_codex":0.98590094,"about_ca_topic_score_gemma":0.9953235,"teacher_disagreement_score":0.0140990615,"about_ca_system_score_codex":0.008276899,"about_ca_system_score_gemma":0.009097683,"threshold_uncertainty_score":0.06005335},"labels":[],"label_agreement":null},{"id":"W4415366126","doi":"10.1017/s1755691024000161","title":"A dipterid-grade lungfish from the Tournaisian Horton Group of Nova Scotia, Canada","year":2024,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Paleontology and Evolutionary Biology","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":true,"ca_institutions":"University of Calgary; Carleton University","funders":"","keywords":"Lungfish; Tournaisian; Carboniferous; Biological dispersal; Laurasia; Extinction (optical mineralogy); Extinction event; Group (periodic table)","score_opus":0.006099734899939772,"score_gpt":0.17672357593695515,"score_spread":0.17062384103701536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415366126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971174,0.00025025292,0.000086184584,0.000042454696,0.0000104540495,0.000021101472,0.00047915833,0.0000059643876,0.0019870193],"genre_scores_gemma":[0.99811494,0.00013554218,0.00019186083,0.000044343225,0.0000027183733,0.0000069299344,0.00036176274,0.0000020945129,0.0011397497],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998503,0.000005300098,0.000008240051,0.000039639854,0.0000398514,0.000056786615],"domain_scores_gemma":[0.9996816,0.000018223633,0.00005427906,0.000013349451,0.00012942465,0.00010321005],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012208888,0.00032697897,0.00017806336,0.0016282466,0.0019287906,0.0006872015,0.0003902209,0.00023203394,0.0016109846],"category_scores_gemma":[0.0003000783,0.00017218236,0.00014638997,0.0013981875,0.0006583604,0.00015599915,0.0005994524,0.00022901727,0.00022943997],"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":[0.00010275495,0.000021545658,0.9708673,0.00006243771,0.00003428883,0.002248335,0.0022702364,0.000104462044,0.011473945,0.000086658416,0.00057383924,0.012154174],"study_design_scores_gemma":[0.0000024097255,0.000016174314,0.9965569,0.000017866663,0.0000072271605,0.00047210767,0.0015858777,0.000060972103,0.0001685592,0.00000788222,0.0011006388,0.0000034151258],"about_ca_topic_score_codex":0.89883435,"about_ca_topic_score_gemma":0.97647774,"teacher_disagreement_score":0.10116565,"about_ca_system_score_codex":0.0033028712,"about_ca_system_score_gemma":0.003318418,"threshold_uncertainty_score":0.2035228},"labels":[],"label_agreement":null},{"id":"W4415366237","doi":"10.1017/s1755691024000100","title":"Placing the Scottish Romer's Gap tetrapods within a Tournaisian time frame","year":2024,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","topic":"Evolution and Paleontology Studies","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":"Tournaisian; Tetrapod (structure); Assemblage (archaeology); Section (typography); Palynology; Carboniferous; Chronology","score_opus":0.008719133563262564,"score_gpt":0.19974594447453503,"score_spread":0.19102681091127247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415366237","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99013686,0.00025413264,0.00017745308,0.00024073555,0.000024510873,0.000008987805,0.00048116237,0.000011907292,0.008664112],"genre_scores_gemma":[0.9980215,0.000054570926,0.00021587935,0.000051882686,0.000011793723,0.0000040381947,0.00031204367,0.0000045033853,0.0013238579],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996488,0.000041382453,0.00001715313,0.000093353075,0.000093426635,0.00010584727],"domain_scores_gemma":[0.99890804,0.000091043585,0.00038876632,0.000068842164,0.0003127065,0.0002306303],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058751774,0.00015900617,0.00018457096,0.0018373514,0.001220307,0.0008337796,0.00039248882,0.00026548278,0.005082525],"category_scores_gemma":[0.00091625476,0.00008450306,0.00015451564,0.0011699804,0.0007537772,0.000303719,0.0010975274,0.0003462607,0.00049840804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005146196,0.000041768188,0.9218447,0.00007060502,0.000059328228,0.0016022007,0.007771584,0.0001236636,0.013856691,0.0012862668,0.0028522545,0.049976256],"study_design_scores_gemma":[0.0000024039111,0.00004696306,0.99404424,0.000010508488,0.00000371403,0.00013148965,0.001719047,0.000044257496,0.00012684043,0.000033202985,0.0038329624,0.000004326195],"about_ca_topic_score_codex":0.09617904,"about_ca_topic_score_gemma":0.28182107,"teacher_disagreement_score":0.09617904,"about_ca_system_score_codex":0.0013492781,"about_ca_system_score_gemma":0.00048511373,"threshold_uncertainty_score":0.1912384},"labels":[],"label_agreement":null},{"id":"W4415434035","doi":"10.1017/s1755691025100741","title":"Testing the correlation of marine bands of the Carboniferous Lower Limestone Formation (Midland Valley of Scotland) using foraminiferal quantitative biostratigraphy","year":2025,"lang":"en","type":"article","venue":"Earth and Environmental Science Transactions of the Royal Society of Edinburgh","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":"Carboniferous; Biostratigraphy; Foraminifera; Fauna; Nova scotia","score_opus":0.01540304090612928,"score_gpt":0.224710670037767,"score_spread":0.20930762913163772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415434035","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999273,0.000027672826,0.00019609905,0.0000049745927,0.0000011678749,0.000002587456,0.00013214751,0.0000042889596,0.0003580187],"genre_scores_gemma":[0.99957603,0.0000088928655,0.00014663907,0.0000027273184,0.0000013456574,0.000002621316,0.00018854864,0.0000016934628,0.00007145282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927086,0.00012391446,0.00007778722,0.00017456649,0.0002064592,0.00014647942],"domain_scores_gemma":[0.99803716,0.00065588835,0.0005883442,0.00011304258,0.00042112314,0.00018439314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000767458,0.00029004717,0.00026204612,0.0025232574,0.00039522257,0.00097367686,0.0003052261,0.00025359337,0.0011672404],"category_scores_gemma":[0.0035952693,0.00014626188,0.0002117886,0.0014313414,0.0004444867,0.0003337923,0.000717844,0.00013652677,0.00028792705],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048247042,0.000009769457,0.9914117,0.0000144113865,0.000043300162,0.00009600699,0.0003681175,0.00024529782,0.002746049,0.000056171113,0.000053231364,0.004907674],"study_design_scores_gemma":[0.0000020831444,0.00002841604,0.9988188,0.0000028263487,0.0000056181966,0.000032539345,0.00032987917,0.00040880466,0.0001939108,0.000013636323,0.00016142968,0.0000020861885],"about_ca_topic_score_codex":0.027554309,"about_ca_topic_score_gemma":0.056082934,"teacher_disagreement_score":0.027554309,"about_ca_system_score_codex":0.00036884253,"about_ca_system_score_gemma":0.0002923983,"threshold_uncertainty_score":0.054787815},"labels":[],"label_agreement":null}]}