Late Ordovician climate change and extinctions driven by elevated volcanic nutrient supply

2021/12/01 by Jack Longman, Benjamin J. W. Mills, Benjamin Mills +5 · 5 citations
Earth and Planetary Sciences · #Geochemistry and Elemental Analysis #Geology and Paleoclimatology Research #Paleontology and Stratigraphy of Fossils

paper · doi:10.1038/s41561-021-00855-5

crossref issued 2021/12/01 · crossref published 2021/12/01 · crossref published-print 2021/12/01 · openalex publication_date 2021/12/01 · crossref published-online 2021/12/02 · crossref created 2021/12/02 · crossref deposited 2023/02/09 · openalex created_date 2025/10/10 · crossref indexed 2026/07/29 · openalex updated_date 2026/08/01

Citations

• Erosion of Deccan Traps determined by river geochemistry: impact on the global climate and the 87Sr/86Sr ratio of seawater
• End Ordovician extinctions: A coincidence of causes
• Episodic nature of continental arc activity since 750 Ma: A global compilation
• A high-resolution summary of Cambrian to Early Triassic marine invertebrate biodiversity
• Extending full-plate tectonic models into deep time: Linking the Neoproterozoic and the Phanerozoic

Cited by

• The influence of Late Ordovician volcanism on the marine environment based on high-resolution mercury data from South China
• Ordovician–Silurian true polar wander as a mechanism for severe glaciation and mass extinction
• Seawater sources of Hg enrichment in Ordovician-Silurian boundary strata, South China
• Extinction event [wikipedia]
• Late Ordovician mass extinction [wikipedia]