Chapter 8 From Greenhouse to Icehouse – The Eocene/Oligocene in Antarctica

2008/01/01 by Jane E. Francis, Sergio A. Marenssi, Richard Levy +8 · 2 citations
Earth and Planetary Sciences · Environmental Science · #Geology and Paleoclimatology Research #Paleontology and Stratigraphy of Fossils #Polar Research and Ecology

paper · doi:10.1016/s1571-9197(08)00008-6

crossref issued 2008/01/01 · crossref published 2008/01/01 · crossref published-print 2008/01/01 · openalex publication_date 2008/01/01 · crossref created 2008/09/12 · openalex created_date 2025/10/10 · crossref deposited 2025/10/28 · crossref indexed 2026/07/30 · openalex updated_date 2026/07/30

Citations

• Eocene circulation of the Southern Ocean: Was Antarctica kept warm by subtropical waters?
• Timing and nature of the deepening of the Tasmanian Gateway
• Provenance, environmental and paleogeographic controls on sandstone composition in an incised-valley system: the Eocene La Meseta Formation, Seymour Island, Antarctica
• Marked Decline in Atmospheric Carbon Dioxide Concentrations During the Paleogene
• Significant Southern Ocean warming event in the late middle Eocene
• Paleogene opening of Drake Passage
• 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
• Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present

Cited by

• Eocene [wikipedia]
• Oligocene [wikipedia]