Euxinia caused the Late Ordovician extinction: Evidence from pyrite morphology and pyritic sulfur isotopic composition in the Yangtze area, South China

2017/11/16 by Caineng Zou, Zhen Qiu, Hengye Wei +3 · 1 citation
Earth and Planetary Sciences · #Geochemistry and Elemental Analysis #Marine Biology and Ecology Research #Paleontology and Stratigraphy of Fossils

paper · doi:10.1016/j.palaeo.2017.11.033

openalex publication_date 2017/11/16 · crossref created 2017/11/16 · crossref issued 2018/12/01 · crossref published 2018/12/01 · crossref published-print 2018/12/01 · crossref deposited 2025/06/27 · openalex created_date 2025/10/10 · openalex updated_date 2026/06/02 · crossref indexed 2026/06/04

Citations

• The Late Ordovician Mass Extinction
• Do all mass extinctions represent an ecological crisis? Evidence from the Late Ordovician
• Changes in marine productivity and redox conditions during the Late Ordovician Hirnantian glaciation
• Pyrite formation in euxinic and semi-euxinic sediments
• A sulfidic driver for the end-Ordovician mass extinction
• Climate change and the selective signature of the Late Ordovician mass extinction
• End Ordovician extinctions: A coincidence of causes
• Environmental changes in the Late Ordovician-early Silurian: Review and new insights from black shales and nitrogen isotopes
• Massive release of hydrogen sulfide to the surface ocean and atmosphere during intervals of oceanic anoxia
• A kinetic model of Phanerozoic taxonomic diversity. III. Post-Paleozoic families and mass extinctions
• Pyrite framboid diameter as a measure of oxygen deficiency in ancient mudrocks

Cited by

• Late Ordovician mass extinction [wikipedia]