Disentangling the record of diagenesis, local redox conditions, and global seawater chemistry during the latest Ordovician glaciation

2016/10/24 by Anne‐Sofie C. Ahm, Anne-Sofie C. Ahm, Christian J. Bjerrum +1 · 7 citations
Earth and Planetary Sciences · #Geochemistry and Elemental Analysis #Marine Biology and Ecology Research #Paleontology and Stratigraphy of Fossils

paper · doi:10.1016/j.epsl.2016.09.049

openalex publication_date 2016/10/24 · crossref created 2016/10/24 · crossref issued 2017/02/01 · crossref published 2017/02/01 · crossref published-print 2017/02/01 · crossref deposited 2022/06/22 · openalex created_date 2025/10/10 · crossref indexed 2026/05/20 · openalex updated_date 2026/08/01

Citations

• Mass Extinctions in the Marine Fossil Record
• Trace metals as paleoredox and paleoproductivity proxies: An update
• Deglacial whole-ocean δ13C change estimated from 480 benthic foraminiferal records

Cited by

• Sea level, climate, and ocean poisoning by sulfide all implicated in the first animal mass extinction
• Elevated marine productivity triggered nitrogen limitation on the Yangtze Platform (South China) during the Ordovician-Silurian transition
• Limitation of fixed nitrogen and deepening of the carbonate-compensation depth through the Hirnantian at Dob's Linn, Scotland
• Vertical decoupling in Late Ordovician anoxia due to reorganization of ocean circulation
• Abrupt global-ocean anoxia during the Late Ordovician–early Silurian detected using uranium isotopes of marine carbonates
• Marine redox variability from Baltica during extinction events in the latest Ordovician–early Silurian
• Late Ordovician mass extinction [wikipedia]