{"id":"W2019150136","doi":"10.1016/j.palaeo.2008.06.012","title":"Oxygen isotope values from high-latitudes: Clues for Permian sea-surface temperature gradients and Late Palaeozoic deglaciation","year":2008,"lang":"en","type":"article","venue":"Palaeogeography Palaeoclimatology Palaeoecology","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":108,"is_retracted":false,"has_abstract":false,"ca_institutions":"Carleton University; University of Ottawa; Brock University","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration","keywords":"Permian; Geology; Deglaciation; Latitude; δ18O; Isotopes of oxygen; Seawater; Oceanography; Global cooling; Sea ice; Paleontology; Climatology; Stable isotope ratio; Climate change; Glacial period; Geochemistry","routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false,"invisible_to_affiliation_only":false},"retraction":null,"screen":null,"direct_labels":[],"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001662257,0.0002205111,0.0001766422,0.0006015377,0.0002986701,0.0005419258,0.000147716,0.0001830523,0.001319235],"category_scores_gemma":[0.0003574685,0.0001537637,0.00009026222,0.00084813,0.0002579188,0.000363017,0.0001954457,0.0002682597,0.0001955607],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001809798,"about_ca_system_score_gemma":0.0001550715,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00529037,"about_ca_topic_score_gemma":0.01898631,"domain_scores_codex":[0.9999596,0.000006789317,0.000004959048,0.0000113781,0.000008238116,0.00000895754],"domain_scores_gemma":[0.9998667,0.0000209745,0.0000379517,0.000012293,0.00003469109,0.00002744056],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002342266,0.00001311751,0.9496129,0.00003301714,0.00003606655,0.0001046213,0.000416202,0.00009218298,0.03303388,0.0002424223,0.0001780666,0.01600333],"study_design_scores_gemma":[0.000004598327,0.00002103302,0.9952751,0.000005723747,0.00001959308,0.0001903255,0.0002378747,0.0001393153,0.00294198,0.0001731059,0.0009882156,0.000003040671],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9948611,0.001036874,0.0004533881,0.0001313567,0.00001715823,0.000002010404,0.0004000844,0.00001057275,0.003087401],"genre_scores_gemma":[0.9984646,0.0004401425,0.000408831,0.000033945,0.00001532255,0.00000106186,0.0002235888,0.000007629192,0.0004049697],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.00529037,"threshold_uncertainty_score":0.01051915,"prediction_status":"machine_predicted_unvalidated"},"machine_scores":{"provisional":true,"baseline":true,"maturity_gate_passed":false,"score_opus":0.01181329165631714,"score_gpt":0.2181861103684989,"score_spread":0.2063728187121817,"validation_status":"score_only:v0-immature-baseline","note":"Baseline scores from an immature model (maturity gate not passed). Scores rank; they never assert a category."}}