{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":765,"total_is_capped":false,"direct_labels_cover":4,"predictions_cover":765,"direct_label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline (scores rank; they never assert a category)","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12","author_layer_release":"2026-06-26"},"query_hash":"dcf26a9d8496","filters":{"venue":"Géographie physique et Quaternaire"}},"results":[{"id":"W1875334564","doi":"10.7202/032681ar","title":"Late Wisconsinan and Holocene History of the Laurentide Ice Sheet*","year":2008,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":1053,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Ice sheet; Geology; Ice stream; Ice divide; Antarctic sea ice; Ice shelf; Ice-sheet model; Ice core; Wisconsin glaciation; Holocene; Paleontology; Oceanography; Arctic ice pack; Geomorphology; Physical geography; Sea ice; Cryosphere; Geography","authors":[{"name":"Arthur S. Dyke","is_ca":true},{"name":"V K Prest","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02216480306243791,"gpt":0.2028191387964644,"spread":0.1806543357340265,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007874917,0.0001128498,0.0001522473,0.00002624811,0.0001437985,0.000006361777,0.0001511261,0.00003121178,0.00002380834],"category_scores_gemma":[0.0000136714,0.0000778226,0.0000942266,0.0002405879,0.0006601522,0.0001195953,0.00002524524,0.0001008228,0.000005827697],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000483454,"about_ca_system_score_gemma":0.00004544836,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.03047996,"about_ca_topic_score_gemma":0.1775415,"domain_scores_codex":[0.999313,0.00005570658,0.0001568181,0.0001722134,0.0001486545,0.0001535987],"domain_scores_gemma":[0.9995505,0.00005453761,0.0001083044,0.0002066071,0.00003557585,0.00004445987],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00001034842,0.00001692795,0.961692,0.0000171336,0.00003186238,0.000005476337,0.0009570105,0.0001726717,0.00004207365,0.0001304911,0.01062184,0.02630216],"study_design_scores_gemma":[0.0001472741,0.00002864151,0.9934236,0.00002518581,0.00001448024,0.000007589863,0.00007606616,0.00003387055,0.00002990295,0.0003673372,0.005748023,0.00009800922],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9931349,0.003219083,0.0000129254,0.002125931,0.0003850188,0.0001021283,0.000004093704,0.00002713065,0.0009887997],"genre_scores_gemma":[0.9944946,0.003479339,0.0001465543,0.0005537461,0.00003905159,0.00000150774,0.000006615013,0.000004097765,0.001274508],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1470616,"threshold_uncertainty_score":0.9759762,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1623728788","doi":"10.7202/033011ar","title":"A Review and Reassessment of Travertine Classification","year":2007,"lang":"en","type":"review","venue":"Géographie physique et Quaternaire","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":237,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Geology; Fluvial; Alluvium; Clastic rock; Geochemistry; Alluvial fan; Vegetation (pathology); Deposition (geology); Geomorphology; Sediment; Structural basin; Sedimentary rock","authors":[{"name":"Allan Pentecost","is_ca":false},{"name":"Heather Viles","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.07584827267037313,"gpt":0.3543895908162579,"spread":0.2785413181458848,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0006216628,0.0003729018,0.001414375,0.0002974815,0.00006702483,0.00001853009,0.0002815593,0.0002428222,0.00001163729],"category_scores_gemma":[0.00001716557,0.0002809062,0.0004547158,0.0006146306,0.000448808,0.0001333046,0.000002983437,0.0003692003,0.000006320486],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002185699,"about_ca_system_score_gemma":0.00009447232,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002259612,"about_ca_topic_score_gemma":0.0759087,"domain_scores_codex":[0.9980728,0.0003257275,0.0007240688,0.0004299342,0.0001869051,0.0002605671],"domain_scores_gemma":[0.9986606,0.0001785338,0.0006363022,0.0003516775,0.00004687272,0.0001259669],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.00000442148,0.00002231412,0.002614054,0.02919329,0.0001454296,0.000006216947,0.00001690042,1.826703e-8,1.066621e-7,0.0003046166,0.0003650569,0.9673276],"study_design_scores_gemma":[0.00008199941,0.00008915819,0.8341252,0.02003945,0.0007995737,0.00004527796,0.000007571187,2.518527e-7,2.375826e-7,0.0002880095,0.1442314,0.0002919018],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"review","genre_gemma":"review","genre_scores_codex":[0.0001144326,0.9942222,0.00003002668,0.0002832616,0.00008859805,0.0006398432,0.0000234345,0.00003527106,0.004562931],"genre_scores_gemma":[0.001604546,0.997921,0.000165039,0.0001248262,0.00003648948,0.00001260127,0.000113791,0.000003754805,0.00001799021],"genre_candidate":"review","genre_consensus":"review","teacher_disagreement_score":0.9670357,"threshold_uncertainty_score":0.9999643,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1589699577","doi":"10.7202/1000283ar","title":"L’évolution et l’extension des lacs glaciaires Barlow et Ojibway en territoire québécois","year":2011,"lang":"fr","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":211,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Humanities; Geology; Western europe; Art","authors":[{"name":"Jean‐Serge Vincent","is_ca":true},{"name":"Léon Hardy","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.04013472572614269,"gpt":0.2643944730257057,"spread":0.224259747299563,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001789604,0.0006150058,0.0006290347,0.0004923835,0.000608552,0.0001015513,0.0006897064,0.0007337815,0.0003357125],"category_scores_gemma":[0.0001880031,0.0005698889,0.0004115635,0.000825293,0.003660675,0.001421822,0.0001202372,0.001313716,0.001029704],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001282999,"about_ca_system_score_gemma":0.0003636586,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.4063716,"about_ca_topic_score_gemma":0.9838346,"domain_scores_codex":[0.9936967,0.003088719,0.0005591084,0.0009357651,0.0004645239,0.00125521],"domain_scores_gemma":[0.9978684,0.0006071067,0.0002399766,0.0006660936,0.0001978167,0.0004205921],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003013747,0.0002855015,0.9090187,0.000272779,0.0001868125,0.0003888921,0.008948688,0.0001000675,0.00006410204,0.009055703,0.00219528,0.06918213],"study_design_scores_gemma":[0.0005602725,0.0005945579,0.972047,0.0004647145,0.00008618677,0.0003436875,0.0007033224,0.00009598771,0.0002412557,0.01989542,0.004368394,0.0005991387],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9579685,0.01075312,0.0001457414,0.01919804,0.001572227,0.0004576722,0.00003098904,0.0001954678,0.009678262],"genre_scores_gemma":[0.9670039,0.02703872,0.0009276698,0.001953709,0.000199739,0.0000242126,0.0002509602,0.00003231725,0.002568766],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.577463,"threshold_uncertainty_score":0.9997481,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1949467692","doi":"10.7202/033030ar","title":"British Columbia Vegetation and Climate History with Focus on 6 ka BP","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":197,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":true,"about_ca":true},"ca_institutions":"University of Victoria; Royal British Columbia Museum","funders":"Simon Fraser University","keywords":"Tsuga; Holocene; Vegetation (pathology); Holocene climatic optimum; Plateau (mathematics); Pinus contorta; Physical geography; Geology; Ecology; Geography; Forestry; Oceanography; Biology","authors":[{"name":"Richard J. Hebda","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01096271807787154,"gpt":0.2205378616258857,"spread":0.2095751435480142,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005156614,0.0001161363,0.0001815893,0.00011101,0.0001596519,0.00006643028,0.0001265829,0.0001146508,0.00009936946],"category_scores_gemma":[0.00001080215,0.0001365383,0.00004508169,0.0001880745,0.0006722072,0.0001745933,0.000009937646,0.0002942284,0.00007054862],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002677395,"about_ca_system_score_gemma":0.00002956759,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.06146507,"about_ca_topic_score_gemma":0.9936813,"domain_scores_codex":[0.9987291,0.0001365959,0.0001587238,0.000336894,0.000195292,0.0004434414],"domain_scores_gemma":[0.9994091,0.0001757074,0.00007829934,0.0001564069,0.00004380345,0.0001366812],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001230313,0.00002513385,0.9251894,0.00004374226,0.00002318088,0.0002288298,0.0001503885,0.00001712289,0.000003965691,0.0001165869,0.0007882117,0.07329045],"study_design_scores_gemma":[0.0004245677,0.0003351072,0.9969804,0.00007272061,0.00001141993,0.0001469689,0.00004609639,0.000007776077,0.00001646971,0.001297233,0.0004899903,0.0001712045],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9901817,0.0009371497,0.00002230963,0.0005773993,0.000147269,0.0001807655,0.000001420802,0.00007065867,0.007881311],"genre_scores_gemma":[0.998082,0.0009306058,0.0001261676,0.0005526987,0.00003909701,0.000003641494,0.00004021828,0.000006461861,0.0002190895],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9322162,"threshold_uncertainty_score":0.9447847,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1760486640","doi":"10.7202/004847ar","title":"Pingo Growth and collapse, Tuktoyaktuk Peninsula Area, Western Arctic Coast, Canada: a long-term field study","year":2002,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":196,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"Université de Montréal; Continental (Canada); University of British Columbia","funders":"","keywords":"Permafrost; Thermokarst; Geology; Peninsula; Hydrology (agriculture); Geomorphology; Physical geography; Oceanography; Geography; Archaeology; Geotechnical engineering","authors":[{"name":"Jenny Mackay","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01267506448972321,"gpt":0.218103519501955,"spread":0.2054284550122318,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0001519759,0.0003589846,0.0003563669,0.00008508612,0.000216775,0.00009224976,0.0003399137,0.00008858315,0.0001542054],"category_scores_gemma":[0.00002264453,0.0003102139,0.00008464007,0.0005488338,0.0002277917,0.0002223554,0.000271284,0.0003493257,0.00003778981],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00007367953,"about_ca_system_score_gemma":0.00001733402,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.706624,"about_ca_topic_score_gemma":0.9766347,"domain_scores_codex":[0.9979268,0.0001754277,0.0003491676,0.0006130272,0.0004615987,0.0004740207],"domain_scores_gemma":[0.9990292,0.0001089657,0.0001675307,0.0004063114,0.00001681491,0.000271173],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002454501,0.0002999386,0.9893116,0.00004314436,0.00009696605,0.000202704,0.001336704,0.00005826282,0.000405349,0.00001603637,0.001922852,0.006281843],"study_design_scores_gemma":[0.000856936,0.0003344079,0.9974406,0.00007936411,0.00006104435,0.00003922855,0.0001666048,0.0000324867,0.0002961573,0.000190499,0.00008117803,0.0004214959],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.995433,0.0002259602,0.0000279279,0.002559732,0.0001868853,0.0005934154,0.00000235453,0.00006026071,0.0009104967],"genre_scores_gemma":[0.9968272,0.000674747,0.0000242671,0.001070419,0.00004713926,0.00006744474,0.000005630547,0.00003912745,0.001243966],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2700107,"threshold_uncertainty_score":0.999935,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1518448152","doi":"10.7202/004846ar","title":"Thermally induced movements in ice-wedge polygons, western arctic coast: a long-term study","year":2002,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":195,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"Université de Montréal; University of British Columbia","funders":"","keywords":"Ice wedge; Permafrost; Geology; Polygon (computer graphics); Wedge (geometry); Arctic; Geomorphology; Thermokarst; Aggradation; Confluence; Geometry; Oceanography","authors":[{"name":"Jenny Mackay","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.05430070738813705,"gpt":0.2746749990940802,"spread":0.2203742917059431,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0002543944,0.0003562713,0.0003516271,0.0003498812,0.0001303662,0.000158505,0.0004560686,0.00009685545,0.0005369568],"category_scores_gemma":[0.000007705288,0.0003158126,0.0001360424,0.0006635702,0.0001052002,0.0004615291,0.00004960655,0.0003498604,0.0004810608],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001051273,"about_ca_system_score_gemma":0.00001306083,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.09350716,"about_ca_topic_score_gemma":0.9532469,"domain_scores_codex":[0.9978494,0.0002595408,0.0004018593,0.0005145604,0.000394358,0.0005802722],"domain_scores_gemma":[0.9991222,0.00007683537,0.0001526472,0.0004305952,0.00003727316,0.0001804756],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004831719,0.0004691182,0.9480209,0.00005212945,0.00005580602,0.0002303289,0.00537035,0.0000173814,0.0002952074,0.000001407282,0.00009989565,0.04533919],"study_design_scores_gemma":[0.001210069,0.0003273032,0.9970729,0.0001326448,0.0000155964,0.00001203737,0.0007193647,0.00002401247,0.00004522806,0.00005117193,0.00001761084,0.0003720183],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9972287,0.0003636879,0.000001403713,0.0008679057,0.0003248956,0.000702842,0.00006040667,0.00007651241,0.0003736436],"genre_scores_gemma":[0.9972569,0.0008331879,0.000002028208,0.001137903,0.0001408941,0.00002399077,0.0002429596,0.00002005483,0.0003421279],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8597397,"threshold_uncertainty_score":0.9999294,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1608573363","doi":"10.7202/032605ar","title":"Objective Reconstructions of the Late Wisconsinan Laurentide Ice Sheet and the Significance of Deformable Beds","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":176,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Geology; Ice sheet; Ice stream; Bay; Yield (engineering); Geomorphology; Flow (mathematics); Sea ice; Geometry; Oceanography; Cryosphere; Materials science","authors":[{"name":"David Fisher","is_ca":false},{"name":"Niels Reeh","is_ca":false},{"name":"K. Langley","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.009516184632655791,"gpt":0.2119984368675197,"spread":0.2024822522348639,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004048391,0.0001047216,0.0001871291,0.00003236259,0.0002513138,0.00001553728,0.0001710253,0.00003043662,0.00001037765],"category_scores_gemma":[0.00003023114,0.00005820741,0.0001210895,0.0006233578,0.001324235,0.0001394256,0.00002471435,0.0001242547,0.000001111497],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002187096,"about_ca_system_score_gemma":0.00002932653,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.04694808,"about_ca_topic_score_gemma":0.556213,"domain_scores_codex":[0.9992236,0.00007903866,0.0002594798,0.0001228693,0.0001457355,0.0001692569],"domain_scores_gemma":[0.9991854,0.0002654004,0.0002290646,0.0002128211,0.00007689842,0.00003044988],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00009305536,0.00001677672,0.9175548,0.00003251756,0.0001066732,5.104284e-7,0.001899066,0.0009883622,0.0000962229,0.003041007,0.0002686637,0.07590235],"study_design_scores_gemma":[0.0003298881,0.00002838493,0.991901,0.00003973219,0.00003501531,0.000003957868,0.001879463,0.00006796615,0.0004914731,0.004878361,0.0002717916,0.00007299152],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9956868,0.0005497309,0.0001839051,0.001606285,0.0002516597,0.0002753666,0.0000137881,0.00001283454,0.001419645],"genre_scores_gemma":[0.9986172,0.0007861674,0.0002638994,0.0001422639,0.00002712495,0.000003076647,0.000003956357,0.000003045509,0.0001532616],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5092649,"threshold_uncertainty_score":0.9593984,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1606931280","doi":"10.7202/1000322ar","title":"Pingos of the Tuktoyaktuk Peninsula Area, Northwest Territories","year":2011,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":164,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"University of British Columbia","funders":"University of Washington; U.S. Department of Energy","keywords":"Permafrost; Geology; Aggradation; Levelling; Geomorphology; Hydrology (agriculture); Geotechnical engineering; Structural basin; Oceanography","authors":[{"name":"Jenny Mackay","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.04023289147755513,"gpt":0.2262796575190943,"spread":0.1860467660415392,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001316916,0.0001910716,0.0002058083,0.00008786692,0.0001410583,0.00003184261,0.0004598729,0.00006561472,0.0003075551],"category_scores_gemma":[0.00001139563,0.0001268286,0.0002058946,0.0004068352,0.0004261466,0.0002290355,0.00003469376,0.0001586698,0.00003142039],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002000302,"about_ca_system_score_gemma":0.0000261439,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.4696618,"about_ca_topic_score_gemma":0.9645784,"domain_scores_codex":[0.9989253,0.0000865011,0.0002454082,0.0002336583,0.0002400296,0.0002690844],"domain_scores_gemma":[0.9992449,0.00004974549,0.0001669811,0.0003986824,0.00005672844,0.00008300068],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002994162,0.0000314666,0.9865056,0.00003253284,0.00002508868,0.000007603342,0.002733276,0.000006739178,0.0002434913,0.000137651,0.0003790901,0.009867564],"study_design_scores_gemma":[0.0001526104,0.00006900743,0.9952672,0.00007354217,0.00001918264,0.00001003341,0.0002951689,0.000008522961,0.00188455,0.00128535,0.0007643015,0.0001705258],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9956188,0.0001727488,0.000004543236,0.000598928,0.0006005724,0.000173616,0.0002552992,0.00004234811,0.00253312],"genre_scores_gemma":[0.9986867,0.0003997428,0.00003219867,0.0003374473,0.0001344152,0.00000442212,0.0003051778,0.00000796621,0.0000919453],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4949166,"threshold_uncertainty_score":0.5338698,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2096033040","doi":"10.7202/014755ar","title":"Late Quaternary Vegetation History of Northern North America Based on Pollen, Macrofossil, and Faunal Remains*","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":145,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Macrofossil; Biome; Holocene; Deglaciation; Geology; Last Glacial Maximum; Disequilibrium; Quaternary; Climatology; Physical geography; Ecosystem; Oceanography; Paleontology; Geography; Ecology","authors":[{"name":"Arthur S. Dyke","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01330229276534983,"gpt":0.2352352048686807,"spread":0.2219329121033309,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004208686,0.0002060048,0.0002814998,0.0003819814,0.0001044815,0.000009857846,0.0002087106,0.0001155087,0.00002333069],"category_scores_gemma":[0.00001882848,0.0001801929,0.0001085574,0.0003024827,0.0009143665,0.0001274346,0.00001247534,0.0003225511,0.00007221316],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005744842,"about_ca_system_score_gemma":0.00007911004,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005906806,"about_ca_topic_score_gemma":0.5835872,"domain_scores_codex":[0.9983941,0.0002519198,0.0003030742,0.000353167,0.0002857757,0.0004119144],"domain_scores_gemma":[0.9990501,0.0002764553,0.0001964536,0.0002563739,0.0000707186,0.000149913],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003798886,0.0000515864,0.9417983,0.00008169573,0.0000361847,0.0001000221,0.000556602,0.001218671,0.00003889702,0.00002631094,0.00006736995,0.05564449],"study_design_scores_gemma":[0.0004154893,0.0003329915,0.9975491,0.00004802527,0.00001414068,0.00001017226,0.00004790543,0.0005446115,0.00004910202,0.0003840081,0.0004226153,0.0001818539],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9937565,0.000768354,0.0001872659,0.001025392,0.0002331695,0.0001708299,0.000004104109,0.00004796627,0.003806469],"genre_scores_gemma":[0.9983836,0.0004792066,0.0001460921,0.0006191003,0.00004223103,0.000002378284,0.0000863419,0.000007775246,0.0002332436],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5776805,"threshold_uncertainty_score":0.8929363,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1484997366","doi":"10.7202/033087ar","title":"Marine Molluscs as Indicators of Environmental Change in Glaciated North America and Greenland During the Last 18 000 Years","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":141,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":true,"about_ca":true},"ca_institutions":"Université de Montréal; Université Laval; Université du Québec à Montréal; Geological Survey of Canada","funders":"Université de Montréal; University of Toronto; Memorial University of Newfoundland; Natural Sciences and Engineering Research Council of Canada; Queen's University; Dartmouth College","keywords":"Subarctic climate; Arctic; Geology; Oceanography; Boreal; Bay; Deglaciation; Younger Dryas; Preboreal; Glacial period; Ice sheet; Arctic ecology; Moraine; Arctic dipole anomaly; Physical geography; Arctic ice pack; Holocene; Paleontology; Geography; Antarctic sea ice","authors":[{"name":"Arthur S. Dyke","is_ca":true},{"name":"Janis E. Dale","is_ca":true},{"name":"R McNeely","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.008715830459008625,"gpt":0.2284882672315129,"spread":0.2197724367725042,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002206076,0.0001221196,0.0001794597,0.0003191819,0.00008239736,0.0000088589,0.0001861482,0.00007515757,0.000104612],"category_scores_gemma":[0.000007696082,0.00009426467,0.00004382386,0.0005246009,0.0008148275,0.0001007535,0.0000488338,0.0002712627,0.00003554322],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001264075,"about_ca_system_score_gemma":0.000008039052,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01884755,"about_ca_topic_score_gemma":0.6853922,"domain_scores_codex":[0.9989787,0.0001392372,0.0001842861,0.0002101835,0.0001632278,0.0003243139],"domain_scores_gemma":[0.9995587,0.0001089187,0.00009553339,0.0001507661,0.000004151367,0.00008189662],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001095187,0.00002890598,0.9389268,0.00001865888,0.00002634933,0.0001020387,0.0007931309,0.000008609047,0.00001536788,0.000004617927,0.000003158568,0.05996284],"study_design_scores_gemma":[0.000351956,0.00009125483,0.9990705,0.00001141395,0.000005660463,0.00002702512,0.0001469066,0.00000455902,0.00003926962,0.00009532055,0.00005807161,0.00009812538],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9988336,0.0002205525,5.861569e-7,0.0002824321,0.00003973951,0.0001942801,0.000006366196,0.00001331941,0.0004091148],"genre_scores_gemma":[0.9981161,0.001599832,0.00001477132,0.0001548182,0.00002347867,0.0000035609,0.00005156958,0.000004136446,0.00003170914],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6665447,"threshold_uncertainty_score":0.987686,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1525255738","doi":"10.7202/032734ar","title":"Late Wisconsinan Deglaciation and Champlain Sea Invasion in the St. Lawrence Valley, Québec","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":140,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Université de Sherbrooke; Université du Québec à Montréal","keywords":"Geology; Moraine; Deglaciation; Glacial lake; Varve; Glacial period; Oceanography; Ice sheet; Shelf ice; Physical geography; Holocene; Sea ice; Geomorphology; Arctic ice pack; Antarctic sea ice; Geography; Sediment","authors":[{"name":"Michel Parent","is_ca":false},{"name":"Serge Occhietti","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02003189802297546,"gpt":0.255547042058438,"spread":0.2355151440354626,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001663119,0.0001367613,0.0001522501,0.0002014721,0.0002113573,0.00003942742,0.0002327964,0.0001142104,0.00001612229],"category_scores_gemma":[0.00004876792,0.00009642627,0.000043305,0.0004306128,0.000509547,0.0002012448,0.0000184108,0.0003576079,0.00004977876],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001417166,"about_ca_system_score_gemma":0.00005484708,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1008031,"about_ca_topic_score_gemma":0.9931848,"domain_scores_codex":[0.9985584,0.0004093186,0.0001930669,0.0002711122,0.000189728,0.0003783731],"domain_scores_gemma":[0.9991007,0.0005400259,0.00007191714,0.0001908346,0.00002717783,0.00006938128],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006081674,0.00002019108,0.9698695,0.00001856689,0.000009229937,0.00007440222,0.001199591,0.00003375586,0.00001373399,0.0003154898,0.0001125611,0.02827215],"study_design_scores_gemma":[0.0002490982,0.00008422888,0.9952497,0.00003350161,0.000004144707,0.00004979885,0.0002528192,0.00005603493,0.00003293276,0.003677519,0.0001945617,0.0001155928],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9887179,0.0004170716,0.00006006949,0.009335152,0.00006198301,0.0002145768,0.000001735188,0.00002765226,0.001163929],"genre_scores_gemma":[0.9983513,0.0006724093,0.00007106738,0.0007651265,0.00002955228,0.00000312323,0.00004931888,0.000002969867,0.00005507946],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8923817,"threshold_uncertainty_score":0.9051847,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1544670666","doi":"10.7202/033005ar","title":"Interaction Between Bacteria, Nannobacteria, and Mineral Precipitation in Hot Springs of Central Italy","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":140,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Aragonite; Calcite; Dolomite; Carbonate; Precipitation; Geology; Mineralogy; Mineral; Carbonate minerals; Geochemistry; Materials science; Metallurgy; Geography","authors":[{"name":"Robert L. Folk","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01411118957663362,"gpt":0.248316647863399,"spread":0.2342054582867654,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003419782,0.0001534147,0.0002329747,0.0002946236,0.00004477459,0.00003098206,0.000110306,0.0001026826,0.000006692718],"category_scores_gemma":[0.00001440481,0.0001458474,0.00007924106,0.0002869641,0.0002344559,0.0005357927,0.000002660199,0.0001697632,0.000001711325],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002766668,"about_ca_system_score_gemma":0.00001447395,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.0170324,"about_ca_topic_score_gemma":0.497141,"domain_scores_codex":[0.9988903,0.00009487801,0.0003459238,0.0002421554,0.000122367,0.0003043604],"domain_scores_gemma":[0.9994761,0.0001218257,0.0001739366,0.0001072043,0.00002619794,0.00009477253],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001532358,0.00001677182,0.7147248,0.00002484911,0.00002252982,0.00000659046,0.0008609694,0.000004158943,0.002858083,0.00004536174,0.000007645142,0.281275],"study_design_scores_gemma":[0.0003320067,0.0001414432,0.99675,0.00007171128,0.000009817252,0.000005586837,0.0002082988,0.000004764388,0.001817835,0.0004826706,0.00002663447,0.0001492214],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9979632,0.0001981419,0.0000943872,0.0002128989,0.0002414838,0.0001460835,0.000008822665,0.00002369573,0.001111247],"genre_scores_gemma":[0.9993566,0.0001315713,0.0003663834,0.00002230835,0.00007323096,0.000001142336,0.0000394599,0.000001820221,0.00000753414],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4801086,"threshold_uncertainty_score":0.9895133,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2111940944","doi":"10.7202/1000276ar","title":"Glacial style and ice limits, the Quaternary stratigraphic record, and changes of land and ocean level in the Atlantic Provinces, Canada","year":2011,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Quaternary; Seabed gouging by ice; Ice sheet; Glacial period; Oceanography; Glacier; Interglacial; Paleontology; Physical geography; Ice stream; Geomorphology; Sea ice; Cryosphere; Geography","authors":[{"name":"Douglas Grant","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.03339141008422255,"gpt":0.2262215748553156,"spread":0.1928301647710931,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004909393,0.000142535,0.0001955766,0.00009838831,0.0001580451,0.00002616615,0.0002284755,0.00007020403,0.000005317494],"category_scores_gemma":[0.00001641426,0.00008198434,0.00001896621,0.0002178383,0.0008070958,0.0001002716,0.00001996628,0.0002650048,5.315027e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":4.395066e-7,"about_ca_system_score_gemma":0.00006825074,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.8636016,"about_ca_topic_score_gemma":0.9997291,"domain_scores_codex":[0.9988073,0.0003960863,0.0001538578,0.0002338099,0.0001518383,0.0002570899],"domain_scores_gemma":[0.999397,0.0002790282,0.00008707291,0.0001582791,0.00002109701,0.0000575272],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001017546,0.00001372627,0.9849917,0.00007414312,0.00002629781,0.00004412205,0.001638802,5.817589e-7,0.000002820125,0.0001672213,0.00006590492,0.01287288],"study_design_scores_gemma":[0.0002440114,0.0002047523,0.9973557,0.00003514261,0.00001451443,0.00007574369,0.0007074477,0.00002518642,0.00001750115,0.001173642,0.00004440798,0.0001019227],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9939367,0.001213502,7.528953e-7,0.004311266,0.00005505604,0.0002547806,0.000009182494,0.000006795239,0.0002120072],"genre_scores_gemma":[0.996056,0.003588111,0.00002387408,0.0002749467,0.00002286523,0.000003565273,0.00001360548,0.000002807755,0.00001421353],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1361275,"threshold_uncertainty_score":0.3343225,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1561544993","doi":"10.7202/032784ar","title":"Quaternary Sedimentation in the St. Lawrence Estuary and Adjoining Areas, Eastern Canada: An Overview Based on High-Resolution Seismo-Stratigraphy","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":123,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Geology; Quaternary; Meltwater; Ice sheet; Ice shelf; Geomorphology; Ice stream; Sediment; Paleontology; Oceanography; Sea ice; Glacier; Cryosphere","authors":[{"name":"James P. M. Syvitski","is_ca":true},{"name":"Daniel Praeg","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01932989611300363,"gpt":0.2529886511943076,"spread":0.233658755081304,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000852659,0.0002740873,0.0001957394,0.000126429,0.0001569423,0.00005857829,0.0002847264,0.00008312032,0.00001836604],"category_scores_gemma":[0.000005524686,0.0002056762,0.00005749648,0.0006466698,0.0002219925,0.0003401091,0.00004407195,0.0003324253,0.000006849195],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00008836878,"about_ca_system_score_gemma":0.00003757382,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.7580369,"about_ca_topic_score_gemma":0.9508878,"domain_scores_codex":[0.9978654,0.0003572555,0.0003432215,0.000474284,0.0005672672,0.000392576],"domain_scores_gemma":[0.9992145,0.0001179441,0.000174375,0.0003452824,0.000009035602,0.0001388871],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002710765,0.0005215823,0.8608857,0.000087373,0.00004654856,0.0002427416,0.00234849,0.02199553,0.001495222,0.002632467,0.0009230725,0.1085502],"study_design_scores_gemma":[0.0005726965,0.0002457393,0.9935993,0.0001490597,0.00001868883,0.000006731865,0.0004550208,0.002643374,0.0002380017,0.001565776,0.0002234699,0.0002821711],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9962167,0.000247964,0.0003473968,0.002028052,0.0001457539,0.0003638389,0.000004739775,0.0000355602,0.0006100673],"genre_scores_gemma":[0.9963018,0.0003363636,0.000231014,0.002944719,0.00004273858,0.00003047256,0.00006929256,0.00002056516,0.00002302415],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.192851,"threshold_uncertainty_score":0.8387233,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1537857246","doi":"10.7202/032467ar","title":"Configuration and Dynamics of the Laurentide Ice Sheet During the Late Wisconsin Maximum","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":122,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"Université de Montréal","funders":"","keywords":"Geology; Ice sheet; Dome (geology); Ice stream; Paleontology; Greenland ice sheet; Glacial period; Wisconsin glaciation; Geomorphology; Oceanography; Cryosphere; Sea ice","authors":[{"name":"Arthur S. Dyke","is_ca":true},{"name":"L A Dredge","is_ca":true},{"name":"Jean‐Serge Vincent","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.008742134924046713,"gpt":0.230589951660095,"spread":0.2218478167360483,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005584845,0.00010707,0.0001275765,0.00007678063,0.0002617353,0.00002446732,0.000237935,0.00008119865,0.00002084789],"category_scores_gemma":[0.0000233986,0.00006215642,0.00006649879,0.0002941531,0.0009687527,0.0001125786,0.00002517167,0.0002762974,0.00001303331],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":8.024876e-7,"about_ca_system_score_gemma":0.0000196701,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003266942,"about_ca_topic_score_gemma":0.7757387,"domain_scores_codex":[0.9990501,0.0002083923,0.0001830474,0.0001483098,0.0001536711,0.0002564557],"domain_scores_gemma":[0.9993743,0.0002097545,0.0001070956,0.0002250145,0.00003980834,0.00004408623],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000540743,0.000008305103,0.9923944,0.00003403311,0.00003036928,0.000007451488,0.0003083412,0.0001201277,0.000112157,0.0009420642,0.00002790697,0.005960699],"study_design_scores_gemma":[0.000178713,0.00002271998,0.9941279,0.00002452724,0.00001132848,0.00003424097,0.0002237772,0.00007129799,0.0006650293,0.004543857,0.00002402857,0.00007260695],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9914141,0.0002244201,0.00004743652,0.006444873,0.0001577782,0.0001805106,0.000003885678,0.00001791822,0.001509048],"genre_scores_gemma":[0.9991884,0.0002697804,0.00001854024,0.0001733919,0.00002043979,0.000001076455,0.00002053545,0.000002855665,0.0003049299],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7724717,"threshold_uncertainty_score":0.4938661,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1497766410","doi":"10.7202/1000282ar","title":"Calving Bay dynamics and ice sheet retreat up the St. Lawrence Valley system","year":2011,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":121,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"National Science Foundation","keywords":"Ice shelf; Geology; Ice stream; Ice sheet; Iceberg; Bay; Ice calving; Oceanography; Continental shelf; Shelf ice; Antarctic sea ice; Seabed gouging by ice; Geomorphology; Sea ice; Arctic ice pack; Cryosphere","authors":[{"name":"Robert Thomas","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02274290138626824,"gpt":0.2132693065499134,"spread":0.1905264051636452,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002296684,0.0001861335,0.0001850221,0.00003101066,0.0004233958,0.00007700932,0.0002724554,0.00005093872,0.00003284305],"category_scores_gemma":[0.0000160374,0.0001228615,0.00008613793,0.0004088008,0.0003016428,0.0002082093,0.00004073813,0.0001617009,0.00002080324],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007105528,"about_ca_system_score_gemma":0.0000163089,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.08154885,"about_ca_topic_score_gemma":0.7416911,"domain_scores_codex":[0.9989385,0.0001011509,0.0001983403,0.0002952997,0.0001892167,0.0002775015],"domain_scores_gemma":[0.9993294,0.0001326231,0.0001033938,0.0002955756,0.00005249519,0.00008646819],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002060207,0.0000113221,0.9080504,0.00005479674,0.0000638327,0.00001287455,0.001858777,0.00006433484,0.000001907871,0.005852394,0.0009693187,0.08303945],"study_design_scores_gemma":[0.0001225656,0.00005255797,0.9940462,0.0000690683,0.00003080089,0.00001094388,0.002797591,0.001855302,0.000003675223,0.0004985685,0.0003423757,0.000170397],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9927949,0.0008536683,0.0004740375,0.001353699,0.0004816366,0.0002103983,0.00002136287,0.000116227,0.003694016],"genre_scores_gemma":[0.9975094,0.00147956,0.0002690587,0.0002987435,0.00006825414,0.000007108577,0.00003101108,0.000007522299,0.0003293747],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6601422,"threshold_uncertainty_score":0.9245672,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2102585023","doi":"10.7202/1000055ar","title":"La mer de Goldthwait au Québec","year":2010,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":112,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"GDG Environnement","funders":"","keywords":"Shore; Glacial period; Estuary; Oceanography; Geology; Sea level; Physical geography; Geography; Paleontology","authors":[{"name":"Jean‐Claude Dionne","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01035161223275778,"gpt":0.2540391039741253,"spread":0.2436874917413676,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006252988,0.0001611276,0.0001785484,0.0001529222,0.0002627553,0.00003457508,0.0003726723,0.0002258246,0.0001968957],"category_scores_gemma":[0.00005367944,0.0001348526,0.000121473,0.0002648476,0.001150228,0.0001113485,0.00001935128,0.0008017295,0.0006689244],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001376345,"about_ca_system_score_gemma":0.0003360062,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.3088602,"about_ca_topic_score_gemma":0.9967893,"domain_scores_codex":[0.998593,0.0003294878,0.0001460088,0.0002767814,0.0001504226,0.0005043297],"domain_scores_gemma":[0.9991124,0.0003261943,0.00005394535,0.0002837906,0.00003350876,0.0001901172],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003339379,0.00002483428,0.9634298,0.00001799968,0.00003475903,0.00007528561,0.0006796071,0.00002514926,0.0001325293,0.0007447061,0.0004613152,0.03434059],"study_design_scores_gemma":[0.0001962838,0.00004401552,0.9945166,0.00000854358,0.000009737477,0.0001405082,0.00008344032,0.00001881771,0.0002104084,0.002351953,0.00225949,0.0001602412],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.979019,0.00007901483,0.0000131021,0.008290185,0.0002410072,0.00009703164,0.00000207015,0.00008888949,0.01216965],"genre_scores_gemma":[0.9985816,0.0000885854,0.0001852845,0.0005301323,0.0001025405,0.000006091716,0.00002351509,0.000006116599,0.0004761504],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.687929,"threshold_uncertainty_score":0.8597893,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1589446141","doi":"10.7202/033007ar","title":"Stable Isotopic Variability within Modern Travertines","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Isotope Analysis in Ecology","field":"Environmental Science","cited_by":106,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"American Chemical Society Petroleum Research Fund","keywords":"Stable isotope ratio; Geology; Saturation (graph theory); Composition (language); Mineralogy; Chemical composition; Chemistry; Environmental chemistry","authors":[{"name":"Henry S. Chafetz","is_ca":false},{"name":"J.R. Lawrence","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.008657301830046945,"gpt":0.2434309848736682,"spread":0.2347736830436212,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001513065,0.0002487673,0.0002929749,0.0001030527,0.0001485889,0.00003060913,0.0004152938,0.0001260576,0.0001857241],"category_scores_gemma":[0.00006544971,0.0002280514,0.0001855437,0.00067862,0.0005416221,0.0003436886,0.0002039014,0.0002622032,0.000262535],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001122627,"about_ca_system_score_gemma":0.00001354464,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.007625379,"about_ca_topic_score_gemma":0.2903012,"domain_scores_codex":[0.9979001,0.0001971955,0.0004554333,0.0005783311,0.0003394612,0.0005294245],"domain_scores_gemma":[0.9989285,0.0001158165,0.0001772267,0.000623723,0.00002006836,0.000134652],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000474136,0.0003070047,0.9019192,0.00001823225,0.0000663924,0.00003038141,0.001324299,0.002535173,0.01463206,0.002743577,0.0009751923,0.07540103],"study_design_scores_gemma":[0.0002648336,0.00005279531,0.9703102,0.000008411634,0.00003017082,0.000006371547,0.00006510233,0.000248467,0.006234765,0.02153995,0.0009472599,0.0002916933],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9689166,0.0000104442,0.02035377,0.0009618882,0.0002026588,0.0002685885,6.215686e-7,0.0001289675,0.00915644],"genre_scores_gemma":[0.9953796,0.0000347954,0.002214299,0.0009792014,0.00006355219,0.00003144309,0.000006415249,0.00002910334,0.001261629],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2826758,"threshold_uncertainty_score":0.9989829,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1590614074","doi":"10.7202/032671ar","title":"Le pergélisol au Québec nordique : bilan et perspectives","year":2007,"lang":"fr","type":"article","venue":"Géographie physique et Quaternaire","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Humanities; Physics; Philosophy","authors":[{"name":"Michel Allard","is_ca":false},{"name":"Maurice K. Séguin","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02804287777328149,"gpt":0.2682413110062911,"spread":0.2401984332330096,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.001110954,0.0005711761,0.000506375,0.0004175159,0.0005198505,0.000231408,0.0005117409,0.000305547,0.0004961764],"category_scores_gemma":[0.0000427725,0.0005658577,0.0004871948,0.0009052984,0.001157827,0.0008763263,0.00006913467,0.0007208816,0.000538189],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00007183712,"about_ca_system_score_gemma":0.001084169,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9732828,"about_ca_topic_score_gemma":0.9998096,"domain_scores_codex":[0.9967018,0.000403153,0.0005051791,0.0008037022,0.000421707,0.001164488],"domain_scores_gemma":[0.998207,0.00039558,0.0002364216,0.0005313543,0.0001442079,0.000485483],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001851174,0.0003610199,0.8109803,0.0002104738,0.0001576658,0.0002667872,0.05155959,0.0001121862,0.0006863367,0.008491118,0.006481222,0.1205082],"study_design_scores_gemma":[0.0005618226,0.0003005633,0.9243667,0.0002491404,0.00004896664,0.00008368283,0.01576207,0.00001993297,0.0002855617,0.0007601779,0.0568379,0.0007234603],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8808753,0.01183532,0.0002223846,0.08934039,0.001335689,0.0003927136,0.0002798936,0.0001353712,0.01558296],"genre_scores_gemma":[0.9785044,0.01191878,0.00008290421,0.002420306,0.001122395,0.000008807037,0.000654894,0.00004528407,0.00524223],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1197848,"threshold_uncertainty_score":0.9996793,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1539307025","doi":"10.7202/033029ar","title":"Permafrost Distribution in Peatlands of West-Central Canada During the Holocene Warm Period 6000 Years BP","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Permafrost; Peat; Macrofossil; Holocene; Geology; Physical geography; Radiocarbon dating; Period (music); Thermokarst; Geomorphology; Hydrology (agriculture); Paleontology; Oceanography; Geography; Archaeology","authors":[{"name":"S. C. Zoltai","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.009464073228843586,"gpt":0.2158126073498039,"spread":0.2063485341209603,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002611816,0.000169169,0.0001942925,0.00007849621,0.0001098452,0.00003710856,0.0002500883,0.00006032191,0.0001023016],"category_scores_gemma":[0.000008456323,0.0001307903,0.00009214695,0.0004902062,0.0001871571,0.0001375422,0.00001929795,0.0002186535,0.000005863196],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002449433,"about_ca_system_score_gemma":0.00008499072,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.8776273,"about_ca_topic_score_gemma":0.9985353,"domain_scores_codex":[0.99863,0.00006442708,0.0002828471,0.0002264458,0.0002959015,0.0005003339],"domain_scores_gemma":[0.9994794,0.0000590145,0.0001055464,0.0002141845,0.00002951749,0.0001123113],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008778047,0.00002301172,0.9878371,0.00003862681,0.00001266554,0.0001151361,0.001102247,0.0001588178,0.0003452451,0.00001315001,0.000356628,0.009909585],"study_design_scores_gemma":[0.0003660201,0.00003427568,0.9975554,0.00005173905,0.000007987895,0.00002386476,0.0006910705,0.00002490523,0.0005600204,0.000021853,0.0004956891,0.0001671718],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.997021,0.0002852746,0.00000519782,0.001194339,0.0002673024,0.000156671,0.0008944447,0.00001787554,0.0001579131],"genre_scores_gemma":[0.9959313,0.0006769089,0.000002330523,0.0001797433,0.000133945,0.000001790096,0.003026096,0.000006814408,0.00004110413],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1209081,"threshold_uncertainty_score":0.5333475,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2050050497","doi":"10.7202/013142ar","title":"Ice Streams of the Laurentide Ice Sheet","year":2006,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Ice sheet; Ice stream; STREAMS; Geology; Antarctic sea ice; Sea ice; Oceanography; Arctic ice pack; Physical geography; Cryosphere; Geography; Computer science","authors":[{"name":"Monica Winsborrow","is_ca":false},{"name":"Chris D. Clark","is_ca":false},{"name":"Chris R. Stokes","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01009579004725897,"gpt":0.2090216263883109,"spread":0.1989258363410519,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001003089,0.0001334748,0.0001531304,0.000025459,0.0001740271,0.00003004521,0.0002872817,0.00003552001,0.00005152437],"category_scores_gemma":[0.00001051725,0.00008857781,0.0001715115,0.0006182592,0.0002380911,0.0001281273,0.00002426818,0.0001051607,0.00001884547],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002009602,"about_ca_system_score_gemma":0.00001922253,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1621159,"about_ca_topic_score_gemma":0.8116562,"domain_scores_codex":[0.9990984,0.00006265606,0.0002157469,0.0001871045,0.0002327567,0.0002033433],"domain_scores_gemma":[0.999418,0.00008084654,0.0001398528,0.00027948,0.00005034683,0.00003150963],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000009179849,0.00003545297,0.9332607,0.00001927559,0.00002938296,0.000001507713,0.0001133178,0.002221534,0.00006519052,0.001178998,0.009352366,0.05371306],"study_design_scores_gemma":[0.0001487075,0.00002342711,0.99202,0.00002994597,0.00001980906,0.000001174189,0.0001641834,0.00004887309,0.0001627543,0.002510777,0.004759538,0.0001108342],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9929337,0.0005601798,0.00005407748,0.002932054,0.000316576,0.0001417903,0.00001668372,0.00004085561,0.003004075],"genre_scores_gemma":[0.9985294,0.0002950041,0.0001593224,0.0003155567,0.0001179538,0.000002780605,0.00003700334,0.000004758583,0.0005382312],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6495402,"threshold_uncertainty_score":0.8434637,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2139199749","doi":"10.7202/032619ar","title":"Reconstruction of Little Ice Age Events in the Canadian Rocky Mountains","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"FPInnovations; Parks Canada","keywords":"Moraine; Glacier; Dendrochronology; Geology; Radiocarbon dating; Glacial period; Physical geography; Larch; Period (music); Ice field; Tree line; Holocene; Ice core; Snow; Archaeology; Paleontology; Geomorphology; Geography; Climatology; Climate change; Oceanography","authors":[{"name":"B. H. Luckman","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01884888143576687,"gpt":0.2636666960527425,"spread":0.2448178146169756,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001088125,0.00009721689,0.0001376171,0.0003501535,0.0001510553,0.000009699955,0.0002961662,0.0001220246,0.00002793369],"category_scores_gemma":[0.00002774154,0.00007317599,0.00006388601,0.0005858308,0.0003467565,0.0001232248,0.000005748104,0.00032537,0.00005733866],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002687525,"about_ca_system_score_gemma":0.00008075415,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.6230882,"about_ca_topic_score_gemma":0.9997428,"domain_scores_codex":[0.9988232,0.0002619491,0.0001990463,0.0001708806,0.0001642492,0.0003807337],"domain_scores_gemma":[0.9994442,0.000181996,0.00006461833,0.0001869876,0.00003303009,0.00008913043],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002959483,0.00001314325,0.9788386,0.00001485911,0.00001292583,0.00005967633,0.0006237499,0.00005186671,0.000006326668,0.0004272506,0.00004136022,0.01988071],"study_design_scores_gemma":[0.0001557369,0.00004694292,0.9941425,0.00002113603,0.000004038618,0.00006717326,0.0003896335,0.000005829011,0.00005413792,0.004919564,0.0001172003,0.00007604938],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9912099,0.0001176587,0.00001012732,0.002006835,0.0001609631,0.0001666962,0.000002535022,0.00001000378,0.006315345],"genre_scores_gemma":[0.999354,0.0001351091,0.00004877862,0.0003225282,0.00003108578,0.000001994216,0.00004249872,0.000002201992,0.0000617897],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3766546,"threshold_uncertainty_score":0.3794217,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2169964073","doi":"10.7202/004875ar","title":"Études pédoanthracologiques des variations de la limite supérieure des arbres au cours de l’Holocene dans les alpes françaises","year":2002,"lang":"fr","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"Université Laval; Center for Northern Studies; Université de Montréal; Cegep de Sainte Foy","funders":"","keywords":"Forestry; Geology; Humanities; Geography; Art","authors":[{"name":"Brigitte Talon","is_ca":true},{"name":"Christopher Carcaillet","is_ca":true},{"name":"Michel Thinon","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.03842958757763056,"gpt":0.2842527245736891,"spread":0.2458231369960585,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","sts"],"consensus_categories":["sts"],"category_scores_codex":[0.002778844,0.0005612162,0.0007245004,0.0004122655,0.001727673,0.0002392837,0.0007688798,0.00087114,0.0003980877],"category_scores_gemma":[0.0007712021,0.0005187083,0.0004337858,0.0008780963,0.01141779,0.0006441103,0.00007705507,0.00123281,0.0001641902],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002529858,"about_ca_system_score_gemma":0.0002982166,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.04940201,"about_ca_topic_score_gemma":0.7561853,"domain_scores_codex":[0.9917018,0.005190921,0.0005746961,0.0006584941,0.0003155371,0.001558493],"domain_scores_gemma":[0.9946477,0.0040324,0.0002619689,0.0004107376,0.0001814246,0.0004657223],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008268418,0.0004813689,0.9222419,0.0003495588,0.000427234,0.0004700189,0.01534423,0.002033957,0.0001152533,0.006441388,0.001561,0.05045145],"study_design_scores_gemma":[0.0003912621,0.0004419762,0.9735041,0.0003443818,0.0002190946,0.0005103487,0.001962991,0.0006437475,0.0006707631,0.01969769,0.001101613,0.0005120671],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9553404,0.02320052,0.001601515,0.01106445,0.0002803276,0.0003181204,0.00005607843,0.0002210614,0.007917562],"genre_scores_gemma":[0.9275957,0.06755226,0.002853584,0.0004530191,0.0002336318,0.00004631155,0.00006532019,0.00002823439,0.001171899],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7067833,"threshold_uncertainty_score":0.9997265,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1582304572","doi":"10.7202/032844ar","title":"Holocene Sediment Production in Lillooet River Basin, British Colombia: A Sediment Budget Approach","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":true,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Aggradation; Holocene; Sedimentary budget; Sediment; Glacial period; Quaternary; Denudation; Geomorphology; Glacier; Structural basin; Hydrology (agriculture); Physical geography; Sediment transport; Fluvial; Oceanography; Paleontology; Tectonics","authors":[{"name":"P. Jordan","is_ca":true},{"name":"Olav Slaymaker","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01331395009970263,"gpt":0.2232000644497662,"spread":0.2098861143500636,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008155048,0.0002739534,0.000331214,0.00007131313,0.0001546529,0.0000717644,0.0002698693,0.0001695758,0.00001982406],"category_scores_gemma":[0.00001151439,0.0001556369,0.0002096079,0.001034847,0.0002626707,0.0002476028,0.00005093938,0.0002946814,0.00001975017],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000622004,"about_ca_system_score_gemma":0.00001135363,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01896719,"about_ca_topic_score_gemma":0.102881,"domain_scores_codex":[0.997692,0.0001115983,0.0004423797,0.0006999649,0.0004985569,0.0005555068],"domain_scores_gemma":[0.9994422,0.00004380932,0.0001297354,0.0001211464,0.00008073213,0.0001824006],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0003318645,0.002594416,0.4633261,0.00006239245,0.00006952346,0.0001386202,0.0008992488,0.00005299649,0.02770142,0.0002666955,0.009405829,0.4951509],"study_design_scores_gemma":[0.000499283,0.0002493212,0.9889076,0.00009709425,0.0000157702,0.00002139542,0.0003268126,0.000002733694,0.007442943,0.000298888,0.001794551,0.0003435683],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9935727,0.0001449301,0.00001973908,0.00450374,0.0004061116,0.000653038,0.000005478719,0.0001964588,0.0004978577],"genre_scores_gemma":[0.9968165,0.0006795679,0.0001863132,0.001421531,0.0002561756,0.00007764492,0.0001798247,0.000005087085,0.0003773368],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5255815,"threshold_uncertainty_score":0.9875656,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W73467978","doi":"10.7202/032929ar","title":"The Quaternary History of Cumberland Sound, Southeastern Baffin Island: The Marine Evidence","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Geology; Sound (geography); Glacial period; Fjord; Oceanography; Ice sheet; Paleontology; Foraminifera; Iceberg; Ice shelf; Sea ice; Cryosphere; Benthic zone","authors":[{"name":"Anne Jennings","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02672590162462967,"gpt":0.2625350348480366,"spread":0.2358091332234069,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002187233,0.0002052362,0.0002363389,0.0001176444,0.0002665475,0.00003165639,0.0008118212,0.0001177769,0.00008129453],"category_scores_gemma":[0.00008281552,0.000112719,0.0001723971,0.0002600856,0.001676282,0.0001798636,0.00007188928,0.0004808696,0.000202141],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003129335,"about_ca_system_score_gemma":0.00009002385,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01963929,"about_ca_topic_score_gemma":0.928408,"domain_scores_codex":[0.9979318,0.0004532961,0.000390055,0.0003011953,0.0003718878,0.0005517977],"domain_scores_gemma":[0.9975002,0.001566105,0.0002113992,0.0005386496,0.00008261828,0.0001009756],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003401787,0.00001880405,0.9604182,0.00003170801,0.00006220956,0.0000392957,0.0009591515,0.00004088936,0.00001270206,0.000273502,0.0008732529,0.0369301],"study_design_scores_gemma":[0.0002155111,0.0001034464,0.9931364,0.00004140894,0.00001866949,0.00006755648,0.0003087915,0.00004549078,0.00002502729,0.004272943,0.001627259,0.0001374995],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9876827,0.003457695,0.0001183078,0.003883233,0.0006792134,0.0002405708,0.000002011939,0.00003595294,0.003900314],"genre_scores_gemma":[0.995441,0.001729063,0.00002568123,0.0003112156,0.0001129483,0.000004796086,0.00001622385,0.000006945269,0.002352147],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9087687,"threshold_uncertainty_score":0.986889,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2145928624","doi":"10.7202/013146ar","title":"Relict Late Wisconsinan Dune Fields of the Northern Great Plains, Canada*","year":2006,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"Mount Allison University; Simon Fraser University; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Ice sheet; Anticyclone; Aeolian processes; Physical geography; Taiga; Tundra; Boreal; Vegetation (pathology); Climatology; Oceanography; Geomorphology; Paleontology; Geography; Arctic; Forestry","authors":[{"name":"S A Wolfe","is_ca":true},{"name":"D. J. Huntley","is_ca":true},{"name":"Jeff Ollerhead","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.007491939037670499,"gpt":0.2010816801744502,"spread":0.1935897411367797,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001755972,0.0001497773,0.000209568,0.00006996237,0.0001976159,0.00001247629,0.0003609877,0.0001117825,0.00003153439],"category_scores_gemma":[0.00001639103,0.0001007458,0.0001120414,0.0003590638,0.0005380079,0.0000697207,0.00002369798,0.0003036174,0.00001975538],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001472975,"about_ca_system_score_gemma":0.0001921839,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9427984,"about_ca_topic_score_gemma":0.9999385,"domain_scores_codex":[0.9987473,0.0002350876,0.0002224807,0.0002203424,0.0002335933,0.0003411444],"domain_scores_gemma":[0.9993019,0.0001413522,0.0001141669,0.000334966,0.00005420285,0.00005342314],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000296951,0.00001241049,0.9935046,0.00002312865,0.00002735837,0.00003716248,0.00006251341,0.001101725,0.00001060118,0.0002095875,0.001706997,0.003274198],"study_design_scores_gemma":[0.0001841875,0.00003727426,0.9962867,0.00002870299,0.00001141159,0.00002299348,0.00002401811,0.00002985013,0.0002482425,0.002474672,0.000536508,0.0001153773],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9852715,0.0003471036,0.000004955844,0.01006544,0.0002445089,0.0001468477,0.000005441072,0.00002141757,0.003892784],"genre_scores_gemma":[0.9984785,0.0001247093,0.00001881172,0.0004072014,0.00004184526,0.000002086251,0.00003897465,0.000004221642,0.0008836708],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0571402,"threshold_uncertainty_score":0.4108293,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1912764219","doi":"10.7202/013147ar","title":"Stable Isotope Records from Mount Logan, Eclipse Ice Cores and Nearby Jellybean Lake. Water Cycle of the North Pacific Over 2000 Years and Over Five Vertical Kilometres: Sudden Shifts and Tropical Connections","year":2006,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Volcano; Climatology; Troposphere; Ice core; Oceanography; Paleontology","authors":[{"name":"David Fisher","is_ca":true},{"name":"Cameron P. Wake","is_ca":false},{"name":"K. J. Kreutz","is_ca":false},{"name":"K. Yalcin","is_ca":false},{"name":"Eric J. Steig","is_ca":false},{"name":"Paul A. Mayewski","is_ca":false},{"name":"Lesleigh Anderson","is_ca":false},{"name":"James Zheng","is_ca":true},{"name":"Summer Rupper","is_ca":false},{"name":"Christian Zdanowicz","is_ca":true},{"name":"Michael N. Demuth","is_ca":true},{"name":"M. Waszkiewicz","is_ca":false},{"name":"Dorthe Dahl‐Jensen","is_ca":false},{"name":"Kumiko Goto‐Azuma","is_ca":false},{"name":"J. B. Bourgeois","is_ca":true},{"name":"Roy M. Koerner","is_ca":true},{"name":"J. Sekerka","is_ca":true},{"name":"E. C. Osterberg","is_ca":false},{"name":"Mark B. Abbott","is_ca":false},{"name":"Bruce P. Finney","is_ca":false},{"name":"Stephen Burns","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.008084859966191495,"gpt":0.2166681126934085,"spread":0.208583252727217,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001187321,0.0001675821,0.0002645963,0.0001237672,0.0002063872,0.00006218335,0.000140543,0.0001325099,0.0001701969],"category_scores_gemma":[0.0000177347,0.0001118905,0.0000602851,0.0002369288,0.00124207,0.000187837,0.00005976286,0.0003032151,0.00001579171],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001660649,"about_ca_system_score_gemma":0.00002561369,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.03704287,"about_ca_topic_score_gemma":0.7967456,"domain_scores_codex":[0.9986241,0.0002670102,0.0002154194,0.0003609477,0.0001780472,0.0003544836],"domain_scores_gemma":[0.9992704,0.0003303199,0.00004279754,0.0002210364,0.00002839842,0.0001069926],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001518496,0.0000397851,0.9975468,0.00002102054,0.00005297578,0.00002037244,0.0005764789,0.00004530993,0.00004224084,0.0002557528,0.0005012724,0.0007461412],"study_design_scores_gemma":[0.0005086525,0.0001090872,0.9944151,0.0000223536,0.00003197889,0.00001161905,0.0001532366,0.00009344726,0.00008703031,0.003682527,0.0007406033,0.0001443821],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9977851,0.0004250563,0.000003483762,0.001057024,0.0001343356,0.0001992081,0.00006712604,0.00001866474,0.0003099941],"genre_scores_gemma":[0.9989777,0.0005308853,0.00003251677,0.0001134258,0.00008283541,0.00000405484,0.00007703614,0.000006158445,0.0001753598],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7597027,"threshold_uncertainty_score":0.9693695,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1588025288","doi":"10.7202/1000277ar","title":"La déglaciation et les épisodes lacustre et marin sur le versant québécois des basses terres de la baie de James","year":2011,"lang":"fr","type":"article","venue":"Géographie physique et Quaternaire","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Moraine; Geology; Glacier; Humanities; Physical geography; Forestry; Geomorphology; Geography; Art","authors":[{"name":"Léon Hardy","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.04157133370411949,"gpt":0.2494418691330551,"spread":0.2078705354289356,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.001055679,0.0003814775,0.0003386563,0.0001032194,0.0004132998,0.0002341782,0.000328512,0.0002659054,0.0001290568],"category_scores_gemma":[0.0001625881,0.000363285,0.0002659347,0.0005218862,0.001133242,0.0007374188,0.00007109499,0.0004717967,0.00002642908],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003225758,"about_ca_system_score_gemma":0.0004073855,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.8857588,"about_ca_topic_score_gemma":0.9560522,"domain_scores_codex":[0.9970662,0.001357947,0.0003346265,0.0004150063,0.0002380144,0.0005882148],"domain_scores_gemma":[0.9983379,0.0009161862,0.0002117225,0.0002668917,0.00008953102,0.0001777457],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00005709208,0.0002178976,0.7640002,0.000144298,0.0001952001,0.00005285925,0.01347676,0.0005863475,0.00004136419,0.004740237,0.005857877,0.2106299],"study_design_scores_gemma":[0.0004073568,0.0001296173,0.954389,0.0002965782,0.00009684714,0.00001945858,0.005912371,0.0001775544,0.0001812987,0.006029775,0.03196071,0.0003994079],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9784095,0.008112879,0.0007607095,0.007731971,0.0002582928,0.000192526,0.00005038474,0.000125206,0.004358549],"genre_scores_gemma":[0.9576299,0.0366556,0.003364266,0.0009071822,0.0001113707,0.00002298268,0.0000756285,0.00002753121,0.001205576],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2102304,"threshold_uncertainty_score":0.9998819,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2095803380","doi":"10.7202/032875ar","title":"A Conceptual Model for Growth and Decay of the Cordilleran Ice Sheet","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Ice sheet; Glacial period; Glacier morphology; Glacier; Ice stream; Ice-sheet model; Ice shelf; Physical geography; Wisconsin glaciation; Ice core; Geomorphology; Greenland ice sheet; Cryosphere; Paleontology; Climatology; Sea ice; Geography","authors":[{"name":"R J Fulton","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0238387870888652,"gpt":0.2406830879321175,"spread":0.2168443008432523,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001789029,0.0001082405,0.0001455213,0.00002275071,0.0001808871,0.00001460846,0.0001532953,0.00003559272,0.000004160373],"category_scores_gemma":[0.00001943484,0.000072762,0.0001064609,0.0002718753,0.0004733785,0.00009425646,0.00001789645,0.00006749957,6.543674e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001182423,"about_ca_system_score_gemma":0.0000195345,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.008767355,"about_ca_topic_score_gemma":0.3118474,"domain_scores_codex":[0.9993093,0.00002092512,0.0001793761,0.0001645635,0.0001320123,0.0001938106],"domain_scores_gemma":[0.9994739,0.0001930495,0.000094264,0.0001312991,0.00005630171,0.00005121731],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00009702171,0.00002929355,0.9138217,0.00004222483,0.00006931512,8.261167e-7,0.002849249,0.002284811,0.0002079031,0.01186064,0.001303232,0.06743378],"study_design_scores_gemma":[0.0003067956,0.00005281247,0.9948043,0.00001899574,0.0000181461,0.000001032617,0.000662259,0.001460272,0.0001970175,0.002122949,0.0002514174,0.0001039512],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9924764,0.0003799062,0.004607856,0.001620913,0.0001435548,0.0002618649,0.00001907607,0.00002001402,0.00047044],"genre_scores_gemma":[0.9980834,0.000412293,0.00078648,0.0005841195,0.00004582779,0.000003668865,0.00001045519,0.000004315691,0.00006945574],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.30308,"threshold_uncertainty_score":0.9978334,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W34731351","doi":"10.7202/032882ar","title":"The Cordilleran Ice Sheet and the Glacial Geomorphology of Southern and Central British Colombia","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geological and Tectonic Studies in Latin America","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Wisconsin glaciation; Glacial landform; Glacial period; Ice sheet; Pleistocene; Post-glacial rebound; Deglaciation; Paleontology; Landform; Ice age; Geomorphology; Physical geography; Oceanography; Ice stream; Moraine; Sea ice; Cryosphere; Geography","authors":[{"name":"June M. Ryder","is_ca":false},{"name":"R J Fulton","is_ca":false},{"name":"John J. Clague","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.005577857835466766,"gpt":0.2026124966834311,"spread":0.1970346388479643,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0004623613,0.0001179247,0.0002238626,0.00001955001,0.0003793102,0.00004464684,0.000188285,0.00005150019,0.0001043827],"category_scores_gemma":[0.00006384945,0.00006710088,0.0000726033,0.0001883044,0.004317373,0.00003192094,0.00004868211,0.0001742481,0.000004970396],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001107103,"about_ca_system_score_gemma":0.000009363093,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.08210679,"about_ca_topic_score_gemma":0.4748417,"domain_scores_codex":[0.9989349,0.0001566728,0.0002186933,0.0002023893,0.0001425271,0.0003448343],"domain_scores_gemma":[0.9989306,0.000719049,0.0001261954,0.0001255963,0.00003148541,0.00006704424],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0002313169,0.000008643263,0.3424739,0.000007306185,0.00004990812,0.00001420094,0.0005391115,0.000009701805,0.000007759157,0.0003852877,0.000362832,0.65591],"study_design_scores_gemma":[0.0006898691,0.0001134705,0.9927737,0.00001120784,0.00001694506,0.0000468176,0.0006877942,0.00001965163,0.00000556332,0.004277497,0.00126377,0.00009373523],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9915835,0.001788913,0.00004788042,0.003097553,0.0001991584,0.0001953632,0.0000157446,0.00002155769,0.003050334],"genre_scores_gemma":[0.9961017,0.003207152,0.00006459359,0.0004918471,0.00006264389,0.000002157307,0.000009072712,0.000002924465,0.00005793592],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6558163,"threshold_uncertainty_score":0.9983923,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2130550509","doi":"10.7202/033027ar","title":"Paleovegetation and Paleoclimatic Changes in the Yukon at 6 ka BP","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Alder; Tundra; Black spruce; Vegetation (pathology); Shrub; Physical geography; Ecology; Geography; Forestry; Taiga; Geology; Arctic; Biology","authors":[{"name":"Les C. Cwynar","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01764418320405483,"gpt":0.2624545696878778,"spread":0.2448103864838229,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001353561,0.0001497472,0.000172191,0.0002427229,0.000191943,0.00003245487,0.0002187837,0.0001140238,0.00002635736],"category_scores_gemma":[0.00002955575,0.000102999,0.00004512947,0.0004418656,0.0004741092,0.0001219711,0.00001761056,0.0002810694,0.00009957184],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":9.157831e-7,"about_ca_system_score_gemma":0.000009133932,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00139085,"about_ca_topic_score_gemma":0.9396992,"domain_scores_codex":[0.9985744,0.0003386883,0.0001806182,0.0002619292,0.0002121259,0.0004322348],"domain_scores_gemma":[0.9990586,0.0005770447,0.00007461292,0.0001996613,0.00002144108,0.00006864697],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00005729818,0.00001776152,0.9706326,0.0000566897,0.00001167199,0.00007644595,0.00160013,0.00001584459,0.00002822927,0.0002955731,0.00006239452,0.02714537],"study_design_scores_gemma":[0.0002757877,0.00009488918,0.9955572,0.00002979226,0.000008145185,0.00007645537,0.0004330003,0.00002745151,0.00006935737,0.003197684,0.0001074438,0.0001227514],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9874915,0.0009237573,0.00001749366,0.008326875,0.0001001803,0.0002619487,0.000001053857,0.00002774937,0.002849372],"genre_scores_gemma":[0.9970827,0.001427931,0.00006544149,0.001254348,0.00004215607,0.000006393193,0.0000516656,0.000003337037,0.00006606756],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9383084,"threshold_uncertainty_score":0.4200176,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2124680961","doi":"10.7202/014754ar","title":"Glacial Isostatic Adjustment of the Laurentian Great Lakes Basin: Using the Empirical Record of Strandline Deformation for Reconstruction of Early Holocene Paleo-Lakes and Discovery of a Hydrologically Closed Phase*","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Post-glacial rebound; Holocene; Meltwater; Glacial period; Structural basin; Paleontology; Geomorphology; Physical geography; Geography","authors":[{"name":"C F M Lewis","is_ca":true},{"name":"Steve Blasco","is_ca":true},{"name":"Pierre L. Gareau","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.04524151850598668,"gpt":0.3009867328905373,"spread":0.2557452143845507,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006280721,0.0001155132,0.0003055396,0.0001247922,0.00008929953,0.000006616202,0.000164201,0.0001067223,0.00000815396],"category_scores_gemma":[0.0000422653,0.00006582044,0.0001518807,0.0002976632,0.001209109,0.0001754142,0.00001267676,0.0001339079,1.429479e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":8.747592e-7,"about_ca_system_score_gemma":0.00004077825,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008448528,"about_ca_topic_score_gemma":0.1098889,"domain_scores_codex":[0.9987599,0.0002560331,0.0004695195,0.0001495721,0.0001731864,0.0001918269],"domain_scores_gemma":[0.9989675,0.000341711,0.0004080998,0.0001580199,0.00009428254,0.00003033962],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001144066,0.00007131779,0.9594515,0.0001704737,0.00007452342,6.96682e-7,0.000580033,0.0000857641,0.0008946574,0.00006425351,0.000004893262,0.03745783],"study_design_scores_gemma":[0.0009902656,0.0007072875,0.9912915,0.00009195602,0.00006447203,0.0000200264,0.0002784657,0.0003306826,0.004182582,0.001977452,0.00000171556,0.00006360161],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9978877,0.0001865329,0.0007865947,0.0005139968,0.0001301792,0.000414483,0.00003896298,0.000005137454,0.00003645896],"genre_scores_gemma":[0.9993093,0.0002312953,0.0003594559,0.00003344883,0.00002254521,0.000002090657,0.00003518218,0.000002431345,0.000004271037],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1090441,"threshold_uncertainty_score":0.9063533,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1484330554","doi":"10.7202/008604ar","title":"The Development and Historic Use of Habitat Structures in Channel Restoration in the United States: The Grand Experiment in Fisheries Management","year":2004,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":72,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Overfishing; Blueprint; Fish <Actinopterygii>; Government (linguistics); Habitat; Fishery; Business; Environmental planning; Geography; Ecology; Engineering; Biology","authors":[{"name":"Douglas Thompson","is_ca":false},{"name":"Gregory N. Stull","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02069811863392217,"gpt":0.2298576176672167,"spread":0.2091594990332945,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003804029,0.0001278188,0.0001023098,0.0001055209,0.0001321799,0.0000290418,0.0002163238,0.00003587486,0.000001070763],"category_scores_gemma":[0.000004796965,0.00006998702,0.0000197853,0.0005970874,0.0004688483,0.0002031111,0.00003908103,0.0001368274,6.856038e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00007315029,"about_ca_system_score_gemma":0.000008089568,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.007589052,"about_ca_topic_score_gemma":0.5237812,"domain_scores_codex":[0.9990408,0.0001325032,0.0002637169,0.0001833266,0.0002040996,0.0001754996],"domain_scores_gemma":[0.9996743,0.00006784273,0.00007321079,0.0001642725,0.000004497063,0.00001592599],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0004945758,0.000529497,0.6733903,0.0001257275,0.00006093269,0.00007605622,0.2130922,0.08641383,0.000323816,0.004170602,0.0005029765,0.02081948],"study_design_scores_gemma":[0.0005199508,0.00004556039,0.9867849,0.0000423152,0.000004479724,8.55167e-7,0.002256598,0.000009786869,0.0007057285,0.0073019,0.002229026,0.00009887147],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9950902,0.0001903937,0.00006933363,0.004180144,0.00004169899,0.0003802273,3.017457e-7,0.000007666186,0.0000400393],"genre_scores_gemma":[0.9981335,0.00125754,0.00008806559,0.0003319123,0.000003296372,0.0001516967,0.00001236275,0.000006316715,0.00001530647],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5161922,"threshold_uncertainty_score":0.9990195,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1525426281","doi":"10.7202/032680ar","title":"The Middle Wisconsinan History of the Laurentide Ice Sheet","year":2008,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Ice sheet; Arctic ice pack; Glacial period; Oceanography; Wisconsin glaciation; Sea ice; Antarctic sea ice; Arctic; Bay; Physical geography; Cryosphere; Climatology; Ice stream; Paleontology; Geography","authors":[{"name":"L A Dredge","is_ca":true},{"name":"L H Thorleifson","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.03637098323297466,"gpt":0.2238668771143184,"spread":0.1874958938813438,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0003574047,0.000132241,0.0001700367,0.00006665262,0.0003764829,0.000007929169,0.0005915716,0.000085361,0.00003976613],"category_scores_gemma":[0.00004656826,0.00007374331,0.000175205,0.0002705847,0.002794585,0.000107998,0.00003341142,0.0003420849,0.00008588601],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002242211,"about_ca_system_score_gemma":0.0001597084,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00608467,"about_ca_topic_score_gemma":0.5946116,"domain_scores_codex":[0.9985632,0.0004511091,0.000205526,0.0002065967,0.0002383596,0.0003352323],"domain_scores_gemma":[0.9989884,0.0003205907,0.0001296598,0.0004432412,0.00005691555,0.0000612018],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003882427,0.00001876758,0.9854652,0.00001632166,0.00003681934,0.00001647715,0.0006783408,0.00004715825,0.00001635136,0.0005680789,0.009963277,0.00313444],"study_design_scores_gemma":[0.0001523512,0.0000407725,0.9911577,0.00002236069,0.000009478562,0.00007287782,0.00009415981,0.00001301629,0.00008265501,0.001559015,0.006705197,0.00009038636],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9828372,0.003064654,0.000003481976,0.005121293,0.0007085414,0.0001553396,0.000001876812,0.00002691584,0.008080697],"genre_scores_gemma":[0.9939949,0.001639517,0.00002547036,0.0003627734,0.00003607388,0.000003705703,0.000009802475,0.000003819745,0.003923956],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.588527,"threshold_uncertainty_score":0.9999192,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1578545653","doi":"10.7202/032735ar","title":"Debris Accumulation Patterns on Talus Slopes in Surprise Valley, Alberta","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":69,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Rockfall; Snow; Debris; Deposition (geology); Erosion; Debris flow; Physical geography; Sedimentary depositional environment; Geomorphology; Period (music); Hydrology (agriculture); Landslide; Geography; Oceanography; Sediment; Geotechnical engineering","authors":[{"name":"Brian H. Luckman","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01338930711976441,"gpt":0.2690917671960208,"spread":0.2557024600762565,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003884198,0.0002338039,0.0001928699,0.0001657995,0.00008174726,0.00004728355,0.0002588708,0.0001504347,0.0000985933],"category_scores_gemma":[0.00002674655,0.0001887267,0.0001424329,0.0005083842,0.0001540969,0.000385275,0.0001172274,0.0002863402,0.0003930786],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00009616446,"about_ca_system_score_gemma":0.000006464351,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.09177839,"about_ca_topic_score_gemma":0.5630307,"domain_scores_codex":[0.998453,0.00008396537,0.0003198548,0.000371223,0.0003489824,0.0004229238],"domain_scores_gemma":[0.9993063,0.0001236476,0.0001139167,0.000321447,0.000008490175,0.0001262174],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001268876,0.0001773822,0.7996287,0.000009522628,0.00002386394,0.00005522168,0.001063443,0.002909424,0.0004314983,0.0002135252,0.00115352,0.194207],"study_design_scores_gemma":[0.0004923776,0.00008130776,0.9944322,0.0000907786,0.000009270199,0.000004818583,0.00007862918,0.00003535871,0.000787244,0.0006429687,0.003067003,0.0002780334],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9918309,0.0000151509,0.0006299756,0.001616061,0.0002019486,0.0002572357,0.00000126331,0.00005542256,0.005392047],"genre_scores_gemma":[0.9982641,0.0003529627,0.00008254121,0.0007375766,0.00004611001,0.00001398049,0.00002127521,0.00002700548,0.000454422],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4712524,"threshold_uncertainty_score":0.9142696,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1479930719","doi":"10.7202/004763ar","title":"Modifications des systèmes fluviatiles à la transition Pléniglaciaire-Tardiglaciaire et à l’Holocène : l’exemple du bassin de la Somme (Nord de la France)","year":2002,"lang":"fr","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Geology; Humanities; Art","authors":[{"name":"Pierre Antoine","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02045867978479236,"gpt":0.2653355028210173,"spread":0.2448768230362249,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.002653527,0.0005338305,0.0006025385,0.0004248136,0.0009854265,0.0003100183,0.0006017549,0.0009142098,0.0003100333],"category_scores_gemma":[0.0001901733,0.0005500225,0.0004300801,0.0009535449,0.005454298,0.0007159576,0.00003760551,0.001372016,0.0003553722],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001820436,"about_ca_system_score_gemma":0.0002252455,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01447989,"about_ca_topic_score_gemma":0.1353046,"domain_scores_codex":[0.9899696,0.007258743,0.0005103529,0.0006979686,0.0003718903,0.001191489],"domain_scores_gemma":[0.9963337,0.002448268,0.0002028552,0.0004895294,0.000122519,0.0004031601],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00007752812,0.0005298206,0.9136535,0.0004380623,0.0002311541,0.0003940487,0.01159502,0.00318195,0.0001068295,0.007084143,0.004586536,0.05812141],"study_design_scores_gemma":[0.0009058749,0.0001640319,0.9592457,0.0003929952,0.0001255463,0.0007094423,0.0004808742,0.00274382,0.0001428288,0.02789648,0.006651262,0.0005411443],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9440349,0.01012386,0.002030117,0.02903939,0.0002473733,0.0003845799,0.00007597362,0.00021516,0.01384864],"genre_scores_gemma":[0.9718674,0.02367466,0.001006194,0.0009389312,0.0001947995,0.0000752932,0.0001665179,0.00003562666,0.002040533],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1208247,"threshold_uncertainty_score":0.9996951,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1951089109","doi":"10.7202/032470ar","title":"Âge de la déglaciation finale et histoire postglaciaire de la végétation dans la partie centrale du Nouveau-Québec","year":2007,"lang":"fr","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Humanities; Art; Geology; Physics","authors":[{"name":"Pierre J. H. Richard","is_ca":false},{"name":"Alayn C. Larouche","is_ca":false},{"name":"Michel A. Bouchard","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.008094083796456233,"gpt":0.2565786473273952,"spread":0.248484563530939,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.003895317,0.0003883722,0.0003749243,0.0003095425,0.0006423287,0.0001464534,0.000411087,0.0007459563,0.0001013156],"category_scores_gemma":[0.0002550181,0.0004138798,0.0002710376,0.0006199926,0.003138086,0.0005155703,0.00004015861,0.001079501,0.000203782],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000498328,"about_ca_system_score_gemma":0.0006808708,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1022022,"about_ca_topic_score_gemma":0.8781321,"domain_scores_codex":[0.9938761,0.003689856,0.0004501454,0.0005282337,0.0003403507,0.001115295],"domain_scores_gemma":[0.996701,0.002264871,0.000257617,0.0003154484,0.00009917437,0.0003618728],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002626727,0.0002941157,0.9460469,0.0001809538,0.0001058043,0.0007901174,0.009541252,0.001039101,0.0001905902,0.006631003,0.002796746,0.03212078],"study_design_scores_gemma":[0.0006868899,0.0001865715,0.9785581,0.0001531355,0.00007715554,0.0005816194,0.0009151766,0.0003271605,0.000361889,0.004990736,0.01276358,0.0003979871],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9588406,0.003344445,0.001109441,0.0214304,0.0004721499,0.0002754496,0.00001751845,0.0001176892,0.0143923],"genre_scores_gemma":[0.9907281,0.004976454,0.0003842204,0.0009964275,0.0001793496,0.00001463013,0.0002239517,0.00002467964,0.002472125],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7759299,"threshold_uncertainty_score":0.9998313,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W41839949","doi":"10.7202/032946ar","title":"Late and Postglacial Paleoenvironments of the Gulf of St. Lawrence: Marine and Terrestrial Palynological Evidence","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Centre National de la Recherche Scientifique; Université du Québec à Montréal; U.S. Department of Energy","keywords":"Meltwater; Palynology; Geology; Oceanography; Holocene; Dinoflagellate; Salinity; Pollen; Dinocyst; Ice sheet; Younger Dryas; Glacier; Paleontology; Ecology","authors":[{"name":"Anne de Vernal","is_ca":false},{"name":"Joël Guiot","is_ca":false},{"name":"J. L. Turon","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02334050124372146,"gpt":0.2625719819032135,"spread":0.2392314806594921,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006202347,0.0001182815,0.0002185397,0.00008087416,0.00009195997,0.000008641114,0.0002249601,0.000126867,0.00003853291],"category_scores_gemma":[0.00007698486,0.00007653028,0.00006024782,0.0001978991,0.001846045,0.0001039847,0.00008814422,0.0002344799,0.000003253529],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":3.77575e-7,"about_ca_system_score_gemma":0.00001434229,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00243107,"about_ca_topic_score_gemma":0.1675065,"domain_scores_codex":[0.9988534,0.0002272945,0.0002451107,0.0002257889,0.0001995145,0.0002488926],"domain_scores_gemma":[0.9992329,0.0003651333,0.0001372118,0.0001805997,0.00001487933,0.00006923731],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002678094,0.00002080887,0.9721301,0.00002875663,0.00002673574,0.00001370054,0.0001303719,0.000009787816,0.0001715087,0.00007130457,0.00001117668,0.02711798],"study_design_scores_gemma":[0.0003223405,0.0001920095,0.9961839,0.00004750213,0.00001536953,0.00002089971,0.00003563138,0.00001452006,0.0003804231,0.002695082,0.00001619846,0.00007614373],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9978949,0.0003949816,0.00000711298,0.001205743,0.0001125402,0.00016912,0.000003828139,0.000007912357,0.0002038298],"genre_scores_gemma":[0.9978149,0.001971684,0.00006903453,0.00007347234,0.00002711,8.783093e-7,0.00000797073,0.000001837301,0.00003311016],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1650754,"threshold_uncertainty_score":0.8476844,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1588354924","doi":"10.7202/004859ar","title":"Late Wisconsinan deglaciation and glacial lake development in the Appalachians of southeastern Québec","year":2002,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":true,"about_ca":true},"ca_institutions":"Université de Montréal; Université du Québec à Montréal; Geological Survey of Canada","funders":"Université de Montréal; Université du Québec à Montréal","keywords":"Geology; Deglaciation; Moraine; Glacial lake; Shelf ice; Ice sheet; Varve; Younger Dryas; Glacial period; Ice stream; Oceanography; Geomorphology; Physical geography; Sea ice; Cryosphere; Sediment; Geography","authors":[{"name":"Michel Parent","is_ca":true},{"name":"Serge Occhietti","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02009604712386404,"gpt":0.2254540547887607,"spread":0.2053580076648967,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004085218,0.0001128812,0.0001593095,0.000150636,0.000115863,0.00001901015,0.0001748097,0.00007446408,0.00003723624],"category_scores_gemma":[0.00001688338,0.00007995854,0.00003812946,0.0002533279,0.0004082792,0.0001002174,0.00001151429,0.0002023391,0.00006244813],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":3.48639e-7,"about_ca_system_score_gemma":0.00003085077,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01135635,"about_ca_topic_score_gemma":0.9905595,"domain_scores_codex":[0.998917,0.0003103217,0.0002037753,0.0001815627,0.0001526798,0.000234616],"domain_scores_gemma":[0.9995934,0.00014064,0.00007703684,0.0001301793,0.00002010627,0.00003860784],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002423638,0.00002973863,0.9576542,0.00002501415,0.00001563424,0.00001360175,0.005754958,0.00003617048,0.000003027847,0.00007145922,0.00001814817,0.03635378],"study_design_scores_gemma":[0.0002598561,0.00004644861,0.9985408,0.00002286179,0.00000534764,0.00001786929,0.000215081,0.0000767135,0.00002090712,0.0004411599,0.0002641477,0.00008886488],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9938021,0.0003235909,0.00001586382,0.004421524,0.00004471505,0.0001600933,0.000001610239,0.00001346037,0.001217058],"genre_scores_gemma":[0.9993837,0.0001905104,0.00006834618,0.0002114044,0.00001689056,0.000004524448,0.00001735241,0.00000245438,0.0001047788],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9792032,"threshold_uncertainty_score":0.9952271,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1524637515","doi":"10.7202/1000346ar","title":"The Holocene transgression in the Golfe du Lion, southwestern France: Paleogeographic and paleobotanical evolution","year":2011,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Marine transgression; Sedimentology; Holocene; Geology; Facies; Palynology; Paleontology; Sea level; Sedimentary rock; Oceanography; Structural basin; Pollen; Ecology","authors":[{"name":"Jean-Claude Aloïsi","is_ca":false},{"name":"André Monaco","is_ca":false},{"name":"Nadine Planchais","is_ca":false},{"name":"J. Thommeret","is_ca":false},{"name":"Y. Thommeret","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01685832600825289,"gpt":0.2280677052992059,"spread":0.211209379290953,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001140522,0.0001983343,0.0001921272,0.0001451957,0.00050638,0.00005270563,0.0005150375,0.0001758738,0.00001569376],"category_scores_gemma":[0.00002921323,0.0001083772,0.0001093016,0.0006232702,0.001397357,0.0001837835,0.00001926876,0.0005684404,0.00004525375],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":5.104602e-7,"about_ca_system_score_gemma":0.00001992007,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004921995,"about_ca_topic_score_gemma":0.4411229,"domain_scores_codex":[0.9977437,0.0008911307,0.0002718341,0.000352597,0.0002605149,0.0004802419],"domain_scores_gemma":[0.99907,0.0003836498,0.00008727107,0.0003290359,0.00004117631,0.0000888167],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001070008,0.00004063509,0.9837704,0.00001685012,0.00002085927,0.00005387319,0.001615961,0.000009454115,0.000003497714,0.0004588687,0.00002949506,0.01387309],"study_design_scores_gemma":[0.0004120219,0.0001424625,0.9922971,0.00004140293,0.00001303305,0.00007973306,0.0005336802,0.00003888296,0.000007881674,0.006230726,0.00006190516,0.0001411631],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9916742,0.002857486,0.00005009815,0.00455946,0.0001782464,0.00028314,0.000002411208,0.0000378286,0.0003571194],"genre_scores_gemma":[0.9945822,0.004965109,0.00002792273,0.0003149577,0.00005278044,0.0000185704,0.00001682808,0.000004763013,0.0000169181],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4362009,"threshold_uncertainty_score":0.7440616,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1580007720","doi":"10.7202/033031ar","title":"The Paleoecological Record of 6 ka BP Climate in the Canadian Prairie Provinces","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Taiga; Boreal; Grassland; Holocene; Foothills; Precipitation; Physical geography; Climate change; Glacier; Arid; Climatology; Environmental science; Geology; Geography; Ecology; Forestry; Archaeology; Oceanography","authors":[{"name":"Robert E. Vance","is_ca":false},{"name":"Alwynne B. Beaudoin","is_ca":false},{"name":"Brian H. Luckman","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01874015417349864,"gpt":0.2692715092873986,"spread":0.2505313551139,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003163024,0.0001432652,0.0001886742,0.0001898231,0.0005218118,0.00005007346,0.0006883108,0.0001633721,0.00002253953],"category_scores_gemma":[0.00009225656,0.00007570074,0.00009570275,0.000586316,0.00135817,0.0001055842,0.00001693315,0.0005218261,0.00006948967],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002427158,"about_ca_system_score_gemma":0.0001467183,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.2843849,"about_ca_topic_score_gemma":0.9999151,"domain_scores_codex":[0.9978637,0.0005809123,0.0003171398,0.0002396615,0.0002400154,0.0007586144],"domain_scores_gemma":[0.9982803,0.001151913,0.0001175159,0.0002822199,0.00005091071,0.0001171229],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008734772,0.00001949166,0.9592749,0.00001642915,0.00001447889,0.000101149,0.000301707,0.00001408209,9.330347e-7,0.002118329,0.000422839,0.0376283],"study_design_scores_gemma":[0.0001470876,0.000162365,0.9915344,0.0000140525,0.000005048832,0.00002559731,0.0004400356,0.000006772759,0.00001182451,0.004743036,0.002813324,0.00009649559],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9690326,0.0003263419,0.000002704849,0.01881625,0.0002262315,0.0003567175,0.000003281658,0.00001687367,0.01121896],"genre_scores_gemma":[0.9984283,0.0006450902,0.00004657037,0.000754414,0.00004721658,0.000008644195,0.00002262543,0.00000262329,0.00004452445],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7155302,"threshold_uncertainty_score":0.7203804,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2130273002","doi":"10.7202/008301ar","title":"Three amphi-Atlantic century-scale cold events during the Bølling-Allerød warm period","year":2004,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; University of Bern","keywords":"Younger Dryas; Preboreal; Deglaciation; Holocene; Geology; Oceanography; Ice core; Climatology; North Atlantic oscillation; Abrupt climate change; Period (music); Climate change; Global warming; Effects of global warming","authors":[{"name":"Zicheng Yu","is_ca":false},{"name":"Ulrich Eicher","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01101214202971178,"gpt":0.2286623802867978,"spread":0.217650238257086,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003663983,0.0002788497,0.0002888882,0.0001664066,0.0006670998,0.00006375489,0.0006715136,0.000173639,0.00007977233],"category_scores_gemma":[0.00001680224,0.0001954424,0.0002182914,0.0005157605,0.0006707437,0.0002062769,0.00004897536,0.0006067485,0.0005894891],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000351199,"about_ca_system_score_gemma":0.00006736554,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.009876377,"about_ca_topic_score_gemma":0.7680657,"domain_scores_codex":[0.9979806,0.0001759618,0.0002763623,0.0004654016,0.0003667805,0.00073488],"domain_scores_gemma":[0.9991033,0.00009639384,0.0001116613,0.0004644377,0.00005478156,0.0001694243],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008594276,0.00005617103,0.9965547,0.00005566969,0.00007850462,0.00009590416,0.0006735018,0.0009205939,0.00006609102,0.0003651232,0.00004823753,0.000999547],"study_design_scores_gemma":[0.0007266988,0.00008948415,0.9941217,0.00006412799,0.00001917103,0.0001153975,0.0001934756,0.00001151423,0.0001933904,0.003973933,0.0002475112,0.000243592],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.989403,0.0006289513,0.00006598114,0.008626343,0.0004061537,0.0003936625,0.000004231356,0.0001133466,0.0003583477],"genre_scores_gemma":[0.997624,0.00164781,0.0001066671,0.0003221505,0.000132056,0.00001522455,0.00004903953,0.0000110113,0.00009208989],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7581893,"threshold_uncertainty_score":0.9967169,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1532701708","doi":"10.7202/033091ar","title":"Aspects taphonomiques de la stratigraphie et de la datation de charbons de bois dans les sols : exemple de quelques sols des Alpes","year":2007,"lang":"fr","type":"article","venue":"Géographie physique et Quaternaire","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Forestry; Geology; Humanities; Mineralogy; Art; Geography","authors":[{"name":"Christopher Carcaillet","is_ca":false},{"name":"Brigitte Talon","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0224692991167294,"gpt":0.3376402710320692,"spread":0.3151709719153398,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.006508603,0.0005871062,0.0005671189,0.0004641526,0.0009200951,0.0003340204,0.0008353297,0.0006898281,0.00001612456],"category_scores_gemma":[0.0003804989,0.0006679213,0.0004315647,0.0009352672,0.007760754,0.000863533,0.0001532106,0.000870518,0.000005805844],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0005681416,"about_ca_system_score_gemma":0.00154811,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1899199,"about_ca_topic_score_gemma":0.9310181,"domain_scores_codex":[0.9918626,0.004648358,0.0006145596,0.0007062111,0.000311038,0.00185725],"domain_scores_gemma":[0.9963449,0.002046259,0.0004294272,0.0004349925,0.0001044696,0.0006399195],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008343012,0.0004291175,0.5693899,0.000140407,0.0001924682,0.0002520178,0.08186764,0.0001177214,0.02346523,0.2773858,0.0009255319,0.04575068],"study_design_scores_gemma":[0.000412518,0.0001712609,0.7249268,0.0003436459,0.00009128454,0.00007397046,0.005528275,0.00004483221,0.01868882,0.2467036,0.002479759,0.0005352396],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9529656,0.002327549,0.02954055,0.005994231,0.0001592734,0.0004225298,0.00005522379,0.0003080681,0.008226941],"genre_scores_gemma":[0.9549001,0.02659074,0.01612801,0.001301067,0.0005470493,0.0001413287,0.00005139721,0.00009028373,0.0002499803],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7410981,"threshold_uncertainty_score":0.9995772,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2115362315","doi":"10.7202/013137ar","title":"Evidence from Keewatin (Central Nunavut) for Paleo-Ice Divide Migration*","year":2006,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":true,"about_ca":true},"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada; Indigenous and Northern Affairs Canada","keywords":"Geology; Ice stream; Ice divide; Ice sheet; Deglaciation; Seabed gouging by ice; Ice age; Glacial period; Physical geography; Geomorphology; Cryosphere; Geography; Climatology; Sea ice","authors":[{"name":"I McMartin","is_ca":true},{"name":"Penny J. Henderson","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02638725244661806,"gpt":0.2597331674147954,"spread":0.2333459149681774,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003337859,0.0002304418,0.0002681197,0.0001320865,0.0002812227,0.0000780895,0.0004054532,0.0001644134,0.0001080359],"category_scores_gemma":[0.00008459607,0.000201159,0.0001958263,0.0003266069,0.0005451503,0.0004017671,0.0000176624,0.00025915,0.0002024005],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001643556,"about_ca_system_score_gemma":0.00006153705,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.05084133,"about_ca_topic_score_gemma":0.957524,"domain_scores_codex":[0.9980292,0.0002923976,0.0003086924,0.0004869683,0.0002486262,0.0006340986],"domain_scores_gemma":[0.9983841,0.0009779261,0.0001274857,0.0003034359,0.00008192177,0.0001251223],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001232115,0.00003422206,0.9861772,0.00003323939,0.00003864043,0.00001781173,0.000261054,0.000668598,0.00013986,0.0002050579,0.002669293,0.009631812],"study_design_scores_gemma":[0.000331994,0.00009566897,0.9813467,0.00009013798,0.00002553681,0.000007107479,0.0000512324,0.0001952578,0.0006348129,0.01650295,0.0004838302,0.0002347825],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9863505,0.001745237,0.00112359,0.009566494,0.0003100554,0.0004068736,0.00002986392,0.000102406,0.000364935],"genre_scores_gemma":[0.9967414,0.0008651707,0.0008612709,0.0003776612,0.0002940035,0.00002954801,0.0005047305,0.000007698376,0.0003185045],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9066827,"threshold_uncertainty_score":0.9554792,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1515483066","doi":"10.7202/032858ar","title":"Isolation of Lacustrine Basins and Marine Regression in the Kuujjuaq Area, Northern Québec, as Inferred from Diatom Analysis","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Diverse Academic Research Areas","field":"Social Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Diatom; Geology; Bay; Holocene; Oceanography; Sediment; Glacial period; Sea level; Structural basin; Last Glacial Maximum; Physical geography; Paleontology; Geography","authors":[{"name":"Reinhard Pienitz","is_ca":false},{"name":"Guy Lortie","is_ca":false},{"name":"Michel Allard","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02215716390986861,"gpt":0.3315795749497203,"spread":0.3094224110398517,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001547284,0.0001486359,0.0002645649,0.0005154852,0.0001602228,0.00005876542,0.0004171788,0.0001238042,0.00003204879],"category_scores_gemma":[0.0002878901,0.000108777,0.0001471575,0.002131022,0.0005508407,0.0003454841,0.0001313533,0.0003164452,0.000007380521],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00006991521,"about_ca_system_score_gemma":0.0001362963,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.8719575,"about_ca_topic_score_gemma":0.9936332,"domain_scores_codex":[0.997946,0.0004446825,0.0003173674,0.0002869831,0.0006870716,0.0003178681],"domain_scores_gemma":[0.9987473,0.0005132135,0.000218624,0.0002866861,0.0001140636,0.0001200565],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008916186,0.00007829455,0.9207903,0.000004907743,0.0001231565,0.00001828941,0.01064015,0.00002316543,0.0002708377,0.0007909086,0.0001759406,0.06699492],"study_design_scores_gemma":[0.0003254192,0.00002937468,0.9897719,0.0000407069,0.0000685474,2.555312e-7,0.004638391,0.00002077657,0.0001320684,0.003836325,0.001019277,0.0001169487],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9893001,0.0001156876,0.0001907093,0.00714723,0.00003056782,0.0002688801,0.000006812884,0.00003324608,0.002906754],"genre_scores_gemma":[0.9976071,0.001852573,0.00006798407,0.000166009,0.00007429111,0.00001171631,0.00004339385,0.00001006667,0.0001668493],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1216756,"threshold_uncertainty_score":0.4435797,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1509482655","doi":"10.7202/032598ar","title":"Variations in Lake Levels during the Holocene in North America: An Indicator of Changes in Atmospheric Circulation Patterns","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"Université de Montréal","funders":"","keywords":"Holocene; Westerlies; Geology; Trough (economics); Latitude; Arid; Atmospheric circulation; Climatology; Period (music); Physical geography; Oceanography; Geography; Paleontology","authors":[{"name":"Sandy P. Harrison","is_ca":true},{"name":"Sarah E. Metcalfe","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01749794867734379,"gpt":0.2556144503534136,"spread":0.2381165016760698,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005656721,0.0001152784,0.0001969308,0.0002088181,0.00006002474,0.00001001566,0.0002425018,0.00009361071,0.00004220229],"category_scores_gemma":[0.00002035364,0.00009405895,0.00003338814,0.001303244,0.0002408022,0.000164077,0.00001548278,0.0003224677,0.00001123724],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002589058,"about_ca_system_score_gemma":0.00002711191,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.0120066,"about_ca_topic_score_gemma":0.9914464,"domain_scores_codex":[0.9986625,0.0003150844,0.000268816,0.0002437719,0.0001540961,0.0003557282],"domain_scores_gemma":[0.9994433,0.0001688127,0.0001222507,0.0001977608,0.00001796533,0.00004993047],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004236258,0.00007963474,0.9840179,0.00003046213,0.000008707874,0.00004620598,0.001973293,0.002275074,0.00001086266,0.0000285827,3.079639e-7,0.01148658],"study_design_scores_gemma":[0.0003280561,0.0000548177,0.998817,0.00002299304,0.00000229465,0.000006005726,0.0003051589,0.0001302695,0.00003105378,0.0002024326,0.000002517594,0.00009744982],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9986614,0.00006955889,0.00004870169,0.0008510092,0.00005122505,0.0002312977,0.00001116906,0.00001408659,0.0000615449],"genre_scores_gemma":[0.999492,0.0002237446,0.00006005206,0.0001115212,0.00002033861,0.00000834072,0.0000758243,0.000003851979,0.000004320754],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9794397,"threshold_uncertainty_score":0.9945725,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1510751208","doi":"10.7202/032581ar","title":"La déglaciation d’une partie du versant hudsonien québécois : bassins des rivières Nastapoca, Sheldrake et à l’Eau Claire","year":2007,"lang":"fr","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Humanities; Geology; Physics; Art","authors":[{"name":"Michel Allard","is_ca":false},{"name":"Maurice K. Séguin","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02142301400470233,"gpt":0.2674535821153161,"spread":0.2460305681106137,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.003116507,0.0006084458,0.0006320643,0.0005250934,0.000814401,0.0001910738,0.0006134549,0.0007484775,0.0002399277],"category_scores_gemma":[0.0001853552,0.000568466,0.0004179335,0.001417984,0.003834855,0.0009599944,0.0000885145,0.001300973,0.0007415265],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001749722,"about_ca_system_score_gemma":0.0003598916,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.2083067,"about_ca_topic_score_gemma":0.9915134,"domain_scores_codex":[0.9945104,0.001821332,0.0006802679,0.0008369386,0.0005872684,0.001563773],"domain_scores_gemma":[0.9970518,0.001392222,0.0003161944,0.0005336279,0.0001964674,0.0005097202],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003086955,0.0002604907,0.8439558,0.0002370073,0.0002336075,0.0006947632,0.008444153,0.0004426499,0.00002850179,0.005369539,0.002045301,0.1379795],"study_design_scores_gemma":[0.00083488,0.0004285351,0.971554,0.0003104298,0.00009428048,0.0002576495,0.002111642,0.00016927,0.000207734,0.005875956,0.01757396,0.0005815949],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9413085,0.005661436,0.0005631354,0.03734708,0.001169304,0.0004165745,0.00002775457,0.0001578992,0.01334832],"genre_scores_gemma":[0.9850565,0.01140592,0.0003109146,0.001227105,0.0002864189,0.00001510285,0.0002313688,0.00003093796,0.001435728],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7832066,"threshold_uncertainty_score":0.9996767,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W183903665","doi":"10.7202/032835ar","title":"The Last (Koy-Yukon) Interglaciation in the Northern Yukon: Evidence from Unit 4 at Ch’ijee’s Bluff, Bluefish Basin","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":true,"about_ca":true},"ca_institutions":"","funders":"University of Alberta; Universitetet i Tromsø","keywords":"Tephra; Geology; Marine isotope stage; Stage (stratigraphy); Bluff; Interglacial; Macrofossil; Tephrochronology; Archaeology; Paleontology; Glacial period; Geography; Volcano; Holocene","authors":[{"name":"John Matthews","is_ca":false},{"name":"Charles E. Schweger","is_ca":false},{"name":"Jan A. Janssens","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0256384422142397,"gpt":0.2698220379490987,"spread":0.244183595734859,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00238695,0.0002531777,0.0002445841,0.0001899063,0.0005894068,0.0001154331,0.0009955807,0.0001902039,0.00005654375],"category_scores_gemma":[0.000180454,0.0001558823,0.0001508218,0.0008613075,0.0008489691,0.0003377078,0.00006432386,0.0007002742,0.0005719867],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005860376,"about_ca_system_score_gemma":0.0000532281,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.02418186,"about_ca_topic_score_gemma":0.9919393,"domain_scores_codex":[0.9970173,0.00100578,0.0004018132,0.0004390001,0.0004515732,0.0006845378],"domain_scores_gemma":[0.9965407,0.002539024,0.0001809344,0.0005494828,0.00008645897,0.0001034596],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003419417,0.00003084784,0.9704288,0.00001127811,0.0000410118,0.0001046005,0.002417898,0.0001040266,0.00001147455,0.00008919534,0.0002756789,0.02614323],"study_design_scores_gemma":[0.0003492995,0.0001028078,0.9953915,0.00008618823,0.00001450695,0.00003233051,0.0009220561,0.00004052064,0.0001157026,0.002229726,0.0005303844,0.0001849988],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9829238,0.0010079,0.00004459908,0.01376153,0.0003506466,0.0003492854,0.000004856451,0.00004884186,0.001508536],"genre_scores_gemma":[0.9970323,0.001497241,0.00002244629,0.00098826,0.0001431335,0.00001176757,0.0001041497,0.000007766589,0.0001929438],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9677575,"threshold_uncertainty_score":0.9823162,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1901459860","doi":"10.7202/009109ar","title":"Aridity on the Canadian Plains","year":2004,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":true,"about_ca":true},"ca_institutions":"Impact; Environment and Climate Change Canada; University of Regina","funders":"","keywords":"Arid; Aridity index; Context (archaeology); Climate change; Climatology; Environmental science; Ecosystem; Global warming; Precipitation; Physical geography; Geography; Ecology; Geology; Oceanography; Meteorology","authors":[{"name":"David Sauchyn","is_ca":true},{"name":"Elaine Barrow","is_ca":true},{"name":"Ron F. Hopkinson","is_ca":false},{"name":"Peter R. Leavitt","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02411503275658926,"gpt":0.236098599907927,"spread":0.2119835671513377,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000296487,0.0001919267,0.0001342132,0.0002050544,0.0004785022,0.0001524448,0.0003930438,0.00007128948,0.00005825076],"category_scores_gemma":[0.00005278616,0.0001282427,0.0001208285,0.0004335198,0.0003113196,0.0001440114,0.00000884997,0.0002955439,0.0007890806],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002249103,"about_ca_system_score_gemma":0.0002157309,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.8966827,"about_ca_topic_score_gemma":0.9995865,"domain_scores_codex":[0.9987178,0.0001406984,0.000140663,0.0002737901,0.000282006,0.00044506],"domain_scores_gemma":[0.9991206,0.0001857483,0.0000601723,0.0003716575,0.00002508459,0.000236739],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000147073,0.00007650736,0.8161629,0.0000304618,0.0001070365,0.0002765864,0.001106751,0.01114186,0.00008717505,0.02885295,0.003499925,0.1385108],"study_design_scores_gemma":[0.0001628149,0.0000821351,0.9899463,0.00004729239,0.000006157221,0.00001008983,0.00005550311,0.000005005488,0.0003424124,0.006605231,0.002561087,0.0001759875],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9638768,0.00004961778,0.000006844354,0.02915572,0.0002471992,0.0001855694,0.00002448938,0.0001035357,0.00635019],"genre_scores_gemma":[0.9971817,0.0001656635,0.00004423813,0.002385059,0.00009364864,0.00000424189,0.00003518989,0.000008551781,0.0000816656],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1737834,"threshold_uncertainty_score":0.9999889,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1683742879","doi":"10.7202/033006ar","title":"Early Diagenesis of Plitvice Lakes Waterfall and Barrier Treavertine Deposits","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Spar; Calcite; Geology; Diagenesis; Waterfall; Speleothem; Tufa; Mineralogy; Geochemistry; Paleontology; Carbonate; Cave; Archaeology; Materials science","authors":[{"name":"Henry S. Chafetz","is_ca":false},{"name":"Dušan Srdoč","is_ca":false},{"name":"Nada Horvatinčić","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.00992976574424658,"gpt":0.2233515331360282,"spread":0.2134217673917816,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003288825,0.0001978353,0.0002613044,0.0001966923,0.0001215129,0.0000296031,0.0001804021,0.0001159937,0.000007021307],"category_scores_gemma":[0.00001152392,0.0001604772,0.0001226758,0.0002929923,0.0004357303,0.0002629999,0.000003367737,0.000129312,0.000005419048],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":7.083881e-7,"about_ca_system_score_gemma":0.00001360544,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01504075,"about_ca_topic_score_gemma":0.5817917,"domain_scores_codex":[0.9987984,0.00009139284,0.0002980832,0.0002905878,0.000179859,0.0003417097],"domain_scores_gemma":[0.9993243,0.0001520797,0.0001206351,0.0001919443,0.00004055708,0.0001704602],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00009348995,0.00001750009,0.6796524,0.00002831361,0.00005075691,0.00002537086,0.0005472653,0.000003179022,0.001550266,0.0001026724,0.00001347403,0.3179153],"study_design_scores_gemma":[0.0002995332,0.0001672486,0.9895921,0.00003661617,0.00003071226,0.00001393562,0.00007554147,0.000003800392,0.008739168,0.0008245726,0.00002847257,0.0001882931],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9920942,0.002604662,0.0001506921,0.0002478455,0.000105215,0.000126544,0.000008003679,0.00005075114,0.004612056],"genre_scores_gemma":[0.9990531,0.0004984522,0.0002669616,0.00007941614,0.00004458188,0.000001436331,0.00000784217,0.000002549586,0.00004565926],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5667509,"threshold_uncertainty_score":0.9915182,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}