Very large release of mostly volcanic carbon during the Palaeocene–Eocene Thermal Maximum

2017/08/01 by Marcus Gutjahr, Andy Ridgwell, Philip F. Sexton +6 · 9 citations
Earth and Planetary Sciences · Environmental Science · #Geology and Paleoclimatology Research #Methane Hydrates and Related Phenomena #Paleontology and Stratigraphy of Fossils

paper · doi:10.1038/nature23646

openalex created_date 2017/07/21 · crossref issued 2017/08/01 · crossref published 2017/08/01 · crossref published-print 2017/08/01 · openalex publication_date 2017/08/01 · crossref created 2017/08/29 · crossref published-online 2017/08/31 · crossref deposited 2023/05/18 · crossref indexed 2026/08/01 · openalex updated_date 2026/08/04

Citations

• Rapid carbon sequestration at the termination of the Palaeocene–Eocene Thermal Maximum
• Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate

Cited by

• Permian–Triassic mass extinction pulses driven by major marine carbon cycle perturbations
• Paleocene/Eocene carbon feedbacks triggered by volcanic activity
• Ocean acidification during the early Toarcian extinction event: Evidence from boron isotopes in brachiopods
• Paleoceanographic changes across the Latest Danian Event in the South Atlantic Ocean and planktic foraminiferal response
• Massive and rapid predominantly volcanic CO 2 emission during the end-Permian mass extinction
• Flood Basalts and Mass Extinctions
• Diversification dynamics of vegetation during the Cenozoic in the Neotropics: a palynological perspective from Colombia
• Extinction event [wikipedia]
• Ocean acidification [wikipedia]