Eocene to Oligocene terrestrial Southern Hemisphere cooling caused by declining pCO2

2021/08/02 by Vittoria Lauretano, Alan T. Kennedy-Asser, Alan Kennedy-Asser +6 · 1 citation
Earth and Planetary Sciences · #Geology and Paleoclimatology Research #Marine and coastal ecosystems #Paleontology and Stratigraphy of Fossils

paper · doi:10.1038/s41561-021-00788-z

crossref issued 2021/08/02 · crossref published 2021/08/02 · crossref published-online 2021/08/02 · openalex publication_date 2021/08/02 · crossref created 2021/08/02 · crossref published-print 2021/09/01 · crossref deposited 2023/11/06 · openalex created_date 2025/10/10 · crossref indexed 2026/06/15 · openalex updated_date 2026/08/01

Citations

• Timing and nature of the deepening of the Tasmanian Gateway
• Increased seasonality through the Eocene to Oligocene transition in northern high latitudes
• A novel proxy for terrestrial organic matter in sediments based on branched and isoprenoid tetraether lipids
• Large temperature drop across the Eocene–Oligocene transition in central North America
• Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2
• Global Cooling During the Eocene-Oligocene Climate Transition
• Geochemical Climofunctions from North American Soils and Application to Paleosols across the Eocene‐Oligocene Boundary in Oregon
• Global continental and ocean basin reconstructions since 200Ma
• Eocene cooling linked to early flow across the Tasmanian Gateway
• Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate
• Synchronous tropical and polar temperature evolution in the Eocene
• An astronomically dated record of Earth’s climate and its predictability over the last 66 million years

Cited by

• Oligocene [wikipedia]