<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>16(1)</volume><submitter>Zhao H</submitter><pubmed_abstract>Causal connections among major Ordovician environmental and biological events (i.e., long-term climatic cooling, Hirnantian Glaciation, Great Ordovician Biodiversification Event, and Late Ordovician Mass Extinction) remain in debate, and the hypothesis of volcanism-driven long-term cooling is untested. Here, we present both newly generated and compiled literature data for global volcanic activity (Hg geochemistry), sea-surface temperatures (conodont oxygen isotopes), and chemical weathering intensity (conodont strontium isotopes). This dataset documents a ~25-Myr-long interval of climatic cooling (~470-445 Ma), commencing around the onset of the Middle Ordovician, intensifying during the Late Ordovician, and ultimately culminating in the Hirnantian Glaciation. Cooling was associated with l</pubmed_abstract><journal>Nature communications</journal><pagination>11475</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC12749037</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Volcanism and basalt weathering drove Ordovician climatic cooling.</pubmed_title><pmcid>PMC12749037</pmcid><pubmed_authors>Algeo TJ</pubmed_authors><pubmed_authors>Lyu Z</pubmed_authors><pubmed_authors>Hao F</pubmed_authors><pubmed_authors>Zhang L</pubmed_authors><pubmed_authors>Wang X</pubmed_authors><pubmed_authors>Zhao H</pubmed_authors></additional><is_claimable>false</is_claimable><name>Volcanism and basalt weathering drove Ordovician climatic cooling.</name><description>Causal connections among major Ordovician environmental and biological events (i.e., long-term climatic cooling, Hirnantian Glaciation, Great Ordovician Biodiversification Event, and Late Ordovician Mass Extinction) remain in debate, and the hypothesis of volcanism-driven long-term cooling is untested. Here, we present both newly generated and compiled literature data for global volcanic activity (Hg geochemistry), sea-surface temperatures (conodont oxygen isotopes), and chemical weathering intensity (conodont strontium isotopes). This dataset documents a ~25-Myr-long interval of climatic cooling (~470-445 Ma), commencing around the onset of the Middle Ordovician, intensifying during the Late Ordovician, and ultimately culminating in the Hirnantian Glaciation. Cooling was associated with l</description><dates><release>2025-01-01T00:00:00Z</release><publication>2025 Dec</publication><modification>2026-07-15T07:00:19.827Z</modification><creation>2026-06-30T03:36:16.083Z</creation></dates><accession>S-EPMC12749037</accession><cross_references><pubmed>41387411</pubmed><doi>10.1038/s41467-025-66316-4</doi></cross_references></HashMap>