Carbon cycle feedbacks and the initiation of Antarctic glaciation in the earliest Oligocene

2005/04/04 by James C. Zachos, J ZACHOS, Lee R. Kump +1 · 3 citations
Earth and Planetary Sciences · Environmental Science · #Geology and Paleoclimatology Research #Methane Hydrates and Related Phenomena #Paleontology and Stratigraphy of Fossils

paper · doi:10.1016/j.gloplacha.2005.01.001

openalex publication_date 2005/04/04 · crossref created 2005/04/04 · crossref issued 2005/05/01 · crossref published 2005/05/01 · crossref published-print 2005/05/01 · crossref deposited 2019/01/27 · openalex created_date 2025/10/10 · crossref indexed 2026/07/01 · openalex updated_date 2026/07/28

Citations

• Atmospheric carbon dioxide concentrations over the past 60 million years
• Paleobotanical Evidence for Near Present-Day Levels of Atmospheric CO 2 During Part of the Tertiary
• Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2
• High‐resolution (104 years) deep‐sea foraminiferal stable isotope records of the Eocene‐Oligocene climate transition
• The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years
• GEOCARB II; a revised model of atmospheric CO 2 over Phanerozoic time
• Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present
• Cenozoic Deep-Sea Temperatures and Global Ice Volumes from Mg/Ca in Benthic Foraminiferal Calcite

Cited by

• Potential links between continental rifting, CO2 degassing and climate change through time
• Oligocene [wikipedia]
• Paleogene [wikipedia]