Simulating the biogeochemical effects of volcanic CO2 degassing on the oxygen-state of the deep ocean during the Cenomanian/Turonian Anoxic Event (OAE2)

2011/04/30 by Sascha Flögel, S. Flögel, Klaus Wallmann +10 · 2 citations
Earth and Planetary Sciences · Environmental Science · #Marine and coastal ecosystems #Methane Hydrates and Related Phenomena #Paleontology and Stratigraphy of Fossils

paper · doi:10.1016/j.epsl.2011.03.018

openalex publication_date 2011/04/30 · crossref created 2011/04/30 · crossref issued 2011/05/01 · crossref published 2011/05/01 · crossref published-print 2011/05/01 · crossref deposited 2019/06/10 · openalex created_date 2025/10/10 · crossref indexed 2026/06/19 · openalex updated_date 2026/06/20

Citations

• A key role for iron-bound phosphorus in authigenic apatite formation in North Atlantic continental platform sediments
• Preservation of Organic Matter in Marine Sediments: Controls, Mechanisms, and an Imbalance in Sediment Organic Carbon Budgets?
• Sedimentary Corg:P ratios, paleocean ventilation, and Phanerozoic atmospheric pO2
• CO2 as a primary driver of Phanerozoic climate

Cited by

• Enhanced phosphorus recycling during past oceanic anoxia amplified by low rates of apatite authigenesis
• Extinction event [wikipedia]