Large temperature drop across the Eocene–Oligocene transition in central North America

2007/02/01 by Alessandro Zanazzi, Matthew J. Kohn, Bruce J. MacFadden +1 · 4 citations
Earth and Planetary Sciences · Environmental Science · #Evolution and Paleontology Studies #Geology and Paleoclimatology Research #Isotope Analysis in Ecology

paper · doi:10.1038/nature05551

crossref issued 2007/02/01 · crossref published 2007/02/01 · crossref published-print 2007/02/01 · openalex publication_date 2007/02/01 · crossref created 2007/02/07 · crossref deposited 2023/05/18 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/28 · crossref indexed 2026/08/04

Citations

• Cooler winters as a possible cause of mass extinctions at the Eocene/Oligocene boundary
• Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2
• THE EVOLUTIONARY STRATEGY OF THE EQUIDAE AND THE ORIGINS OF RUMEN AND CECAL DIGESTION
• Cenozoic Deep-Sea Temperatures and Global Ice Volumes from Mg/Ca in Benthic Foraminiferal Calcite

Cited by

• Global Cooling During the Eocene-Oligocene Climate Transition
• Increased seasonality through the Eocene to Oligocene transition in northern high latitudes
• Eocene to Oligocene terrestrial Southern Hemisphere cooling caused by declining pCO2
• Oligocene [wikipedia]