Huber, Matthew et al. (2004): Eocene circulation of the Southern Ocean; was Antarctica kept warm by subtropical waters?

Leg/Site/Hole:
ODP 189
ODP 189 1168
ODP 189 1170
ODP 189 1171
ODP 189 1172
Identifier:
2005-029086
georefid

10.1029/2004PA001014
doi

Creator:
Huber, Matthew
Purdue University, Earth and Atmospheric Sciences, West Lafayette, IN, United States
author

Brinkhuis, Henk
Utrecht University, Netherlands
author

Stickley, Catherine E.
Cardiff University, United Kingdom
author

Doos, Kristofer
Stockholm University, Sweden
author

Sluijs, Appy
San Diego State University, United States
author

Warnaar, Jeroen
Geological Survey of Canada (Atlantic), Canada
author

Schellenberg, Stephen A.
author

Williams, Graham L.
author

Identification:
Eocene circulation of the Southern Ocean; was Antarctica kept warm by subtropical waters?
2004
Paleoceanography
American Geophysical Union, Washington, DC, United States
19
4
Near the Eocene's close, the climate system underwent one of the largest shifts in Earth's history: Antarctic terrestrial ice sheets suddenly grew and ocean productivity patterns changed. Here we reconstruct Eocene paleoceanographic circulation in the Tasmanian region, using (1) biogeographical distributions of phytoplankton, including data from recently drilled Ocean Drilling Program Leg 189 sites and (2) fully coupled climate model simulations. We find that the EAC did not penetrate to high latitudes and ocean heat transport in the region was not greater than modern. (mod. journ. abstr.)
English
Coverage:Geographic coordinates:
North:-42.3600
West:144.2400East: 149.5600
South:-48.3000

Stratigraphy; algae; Antarctic ice sheet; Antarctica; Australasia; Australia; biogeography; Cenozoic; climate change; cores; currents; data processing; diatoms; digital simulation; Dinoflagellata; East Australian Current; Eocene; gateways; glacial geology; ice sheets; Indian Ocean; Leg 189; marine sediments; microfossils; ocean currents; Ocean Drilling Program; ODP Site 1168; ODP Site 1170; ODP Site 1171; ODP Site 1172; Pacific Ocean; paleo-oceanography; paleocirculation; paleoclimatology; paleocurrents; Paleogene; paleogeography; paleotemperature; palynomorphs; phytoplankton; plankton; Plantae; reconstruction; sediments; South Pacific; South Tasman Rise; Southern Ocean; Southwest Pacific; subtropical environment; Tasman Sea; Tasmania Australia; Tasmanian Gateway; Tertiary; West Pacific;

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