Anoxia as a cause of the Permian/Triassic mass extinction: facies evidence from northern Italy and the western United States

1992/05/01 by Paul B. Wignall, P.B. Wignall, A. Hallam · 4 citations
Earth and Planetary Sciences · #Geochemistry and Elemental Analysis #Marine Biology and Ecology Research #Paleontology and Stratigraphy of Fossils

paper · doi:10.1016/0031-0182(92)90182-5

crossref issued 1992/05/01 · crossref published 1992/05/01 · crossref published-print 1992/05/01 · openalex publication_date 1992/05/01 · crossref created 2003/08/07 · crossref deposited 2019/03/15 · openalex created_date 2025/10/10 · crossref indexed 2026/07/22 · openalex updated_date 2026/07/28

Citations

• A unique geochemical record at the Permian/Triassic boundary
• Why was there a delayed radiation after the end‐Palaeozoic extinctions?
• Sampling bias, gradual extinction patterns and catastrophes in the fossil record
• The End-Permian Mass Extinction

Cited by

• Geochemical evidence from bio-apatite for multiple oceanic anoxic events during Permian–Triassic transition and the link with end-Permian extinction and recovery
• Flood Basalts and Mass Extinctions
• Erosional truncation of uppermost Permian shallow-marine carbonates and implications for Permian-Triassic boundary events
• Permian–Triassic extinction event [wikipedia]