Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate

2016/04/22 by Eleni Anagnostou, Eleanor H. John, Kirsty M. Edgar +6 · 9 citations
Earth and Planetary Sciences · #Geology and Paleoclimatology Research #Marine and coastal ecosystems #Paleontology and Stratigraphy of Fossils

paper · doi:10.1038/nature17423

openalex publication_date 2016/04/22 · crossref created 2016/04/22 · crossref issued 2016/04/25 · crossref published 2016/04/25 · crossref published-online 2016/04/25 · crossref published-print 2016/05/01 · openalex created_date 2016/06/24 · crossref deposited 2023/05/18 · crossref indexed 2026/07/29 · openalex updated_date 2026/07/30

Citations

• Review and revision of Cenozoic tropical planktonic foraminiferal biostratigraphy and calibration to the geomagnetic polarity and astronomical time scale
• Descent toward the Icehouse: Eocene sea surface cooling inferred from GDGT distributions

Cited by

• Synchronous tropical and polar temperature evolution in the Eocene
• Eocene greenhouse climate revealed by coupled clumped isotope-Mg/Ca thermometry
• Middle Eocene greenhouse warming facilitated by diminished weathering feedback
• Very large release of mostly volcanic carbon during the Palaeocene–Eocene Thermal Maximum
• Late Miocene cooling coupled to carbon dioxide with Pleistocene-like climate sensitivity
• The enigma of Oligocene climate and global surface temperature evolution
• Eocene to Oligocene terrestrial Southern Hemisphere cooling caused by declining pCO2
• High temperatures in the terrestrial mid-latitudes during the early Palaeogene
• Cenozoic [wikipedia]