<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Rigo M</submitter><funding>Italian MUR</funding><funding>Italian MUR (Ministero dell'Università e della Ricerca)</funding><funding>Japan Society for the Promotion of Science</funding><pagination>15574</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC11227520</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>14(1)</volume><pubmed_abstract>The latest Triassic was characterised by protracted biotic extinctions concluding in the End-Triassic Extinction (~ 200 Ma) and a global carbon cycle perturbation. The onset of declining diversity is closely related to reducing conditions that spread globally from upper Sevatian (uppermost Norian) to across the Norian-Rhaetian boundary, likely triggered by unusually high volcanic activity. We correlate significant organic carbon cycle perturbations to an increase of CO&lt;sub>2&lt;/sub> in the ocean-atmosphere system, likely outgassed by the Angayucham igneous province, the onset of which is indicated by the initiation of a rapid decline in &lt;sup>87&lt;/sup>Sr/&lt;sup>86&lt;/sup>Sr and &lt;sup>188&lt;/sup>Os/&lt;sup>187&lt;/sup>Os seawater values. A possible causal mechanism involves elevated CO&lt;sub>2&lt;/sub> levels ca</pubmed_abstract><journal>Scientific reports</journal><pubmed_title>Unveiling a new oceanic anoxic event at the Norian/Rhaetian boundary (Late Triassic).</pubmed_title><pmcid>PMC11227520</pmcid><funding_grant_id>JP20K04113</funding_grant_id><funding_grant_id>16KK0104</funding_grant_id><funding_grant_id>PRIN 2017W2MARE</funding_grant_id><pubmed_authors>Cardinali A</pubmed_authors><pubmed_authors>Onoue T</pubmed_authors><pubmed_authors>Jin X</pubmed_authors><pubmed_authors>Tomimatsu Y</pubmed_authors><pubmed_authors>Wu Q</pubmed_authors><pubmed_authors>Katz ME</pubmed_authors><pubmed_authors>Rigo M</pubmed_authors><pubmed_authors>Maron M</pubmed_authors><pubmed_authors>Du Y</pubmed_authors><pubmed_authors>Bertinelli A</pubmed_authors><pubmed_authors>van Wieren CS</pubmed_authors><pubmed_authors>Satolli S</pubmed_authors><pubmed_authors>Tackett LS</pubmed_authors><pubmed_authors>Campbell H</pubmed_authors><pubmed_authors>Lei JZX</pubmed_authors><pubmed_authors>Zaffani M</pubmed_authors><pubmed_authors>Concheri G</pubmed_authors><pubmed_authors>Godfrey L</pubmed_authors><pubmed_authors>Sato H</pubmed_authors></additional><is_claimable>false</is_claimable><name>Unveiling a new oceanic anoxic event at the Norian/Rhaetian boundary (Late Triassic).</name><description>The latest Triassic was characterised by protracted biotic extinctions concluding in the End-Triassic Extinction (~ 200 Ma) and a global carbon cycle perturbation. The onset of declining diversity is closely related to reducing conditions that spread globally from upper Sevatian (uppermost Norian) to across the Norian-Rhaetian boundary, likely triggered by unusually high volcanic activity. We correlate significant organic carbon cycle perturbations to an increase of CO&lt;sub>2&lt;/sub> in the ocean-atmosphere system, likely outgassed by the Angayucham igneous province, the onset of which is indicated by the initiation of a rapid decline in &lt;sup>87&lt;/sup>Sr/&lt;sup>86&lt;/sup>Sr and &lt;sup>188&lt;/sup>Os/&lt;sup>187&lt;/sup>Os seawater values. A possible causal mechanism involves elevated CO&lt;sub>2&lt;/sub> levels ca</description><dates><release>2024-01-01T00:00:00Z</release><publication>2024 Jul</publication><modification>2025-04-22T15:31:30.127Z</modification><creation>2025-04-06T01:26:14.96Z</creation></dates><accession>S-EPMC11227520</accession><cross_references><pubmed>38971867</pubmed><doi>10.1038/s41598-024-66343-z</doi></cross_references></HashMap>