Wilson, Gary S. et al. (2001): Eocene-Oligocene Antarctic and Southern Ocean climatic deterioration; phase relationships between climatic and oceanic cooling

Leg/Site/Hole:
ODP 113
ODP 113 689
Identifier:
2004-019715
georefid

Creator:
Wilson, Gary S.
University of Oxford, Department of Earth Sciences, Oxford, United Kingdom
author

Roberts, Andrew P.
University of Southampton, United Kingdom
author

Morgans, Hugh E. G.
Institute of Geological and Nuclear Sciences, New Zealand
author

Florindo, Fabio
Istituto Nazionale di Geofisica e Vulcanologia, Italy
author

Verosub, Kenneth L.
University of California at Davis, United States
author

Sagnotti, Leonardo
author

Identification:
Eocene-Oligocene Antarctic and Southern Ocean climatic deterioration; phase relationships between climatic and oceanic cooling
2001
In: Florindo, Fabio (editor), Cooper, Alan K. (editor), Extended abstracts for the International ANTOSTRAT symposium on The geologic record of the Antarctic ice sheet from drilling, coring and seismic studies
Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
16
199-200
ODP Site 689, Maud Rise, Weddell Sea, provides evidence of Eocene-Oligocene Antarctica and Southern Ocean paleoclimate deterioration. This study focuses on the phase relationships between climatic and oceanic cooling. (MTE)
English
Coverage:Geographic coordinates:
North:-64.3100
West:3.0559East: 3.0600
South:-64.3101

Stratigraphy; Antarctica; Cenozoic; climate change; Eocene; ice; isotope ratios; isotopes; Leg 113; Maud Rise; O-18/O-16; Ocean Drilling Program; ODP Site 689; Oligocene; oxygen; paleo-oceanography; paleocirculation; paleoclimatology; Paleogene; paleotemperature; sea ice; Southern Ocean; stable isotopes; Tertiary; Weddell Sea;

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