End-Permian marine extinction due to temperature-driven nutrient recycling and euxinia

2021/10/28 by Dominik Hülse, Kimberly V. Lau, Kimberly Lau +6 · 2 citations
Earth and Planetary Sciences · #Geochemistry and Elemental Analysis #Geology and Paleoclimatology Research #Paleontology and Stratigraphy of Fossils

paper · doi:10.1038/s41561-021-00829-7

crossref issued 2021/10/28 · crossref published 2021/10/28 · crossref published-online 2021/10/28 · openalex publication_date 2021/10/28 · crossref created 2021/10/28 · crossref published-print 2021/11/01 · crossref deposited 2024/09/10 · openalex created_date 2025/10/10 · crossref indexed 2026/04/28 · openalex updated_date 2026/07/29

Citations

• Lethally Hot Temperatures During the Early Triassic Greenhouse
• A negative feedback mechanism for the long‐term stabilization of Earth's surface temperature
• Massive release of hydrogen sulfide to the surface ocean and atmosphere during intervals of oceanic anoxia
• Pyrite framboid diameter as a measure of oxygen deficiency in ancient mudrocks
• Estimates of the magnitudes of major marine mass extinctions in earth history
• Initial pulse of Siberian Traps sills as the trigger of the end-Permian mass extinction
• A nutrient control on marine anoxia during the end-Permian mass extinction

Cited by

• Extinction event [wikipedia]
• Permian–Triassic extinction event [wikipedia]