Robert, Christian M. et al. (2001): L'Ouverture oceanique au sud de la Tasmanie durant le Paleogene et ses consequences paleoceanographiques; resultats preliminaires de la mineralogie des argiles (Leg ODP 189) Paleogene ocean opening south of Tasmania, and its paleo-oceanographic implications; preliminary results from clay mineral analyses; ODP Leg 189

Leg/Site/Hole:
ODP 189
Identifier:
2001-057031
georefid

Creator:
Robert, Christian M.
Centre d'Oceanologie de Marseille, Sedimentologie et Geodynamique, Marseilles, France
author

Exon, Neville F.
Australian Geological Survey Organisation, Australia
author

Kennett, James P.
University of California at Santa Barbara, United States
author

Malone, Mitchell J.
Ocean Drilling Program, United States
author

Brinkhuis, Henk
Utrecht University, Netherlands
author

Chaproniere, George C. H.
Australian National University, Australia
author

Ennyu, Atsuhito
Pennsylvania State University, United States
author

Fothergill, Patrick
University of Leicester, United Kingdom
author

Fuller, Michael D.
University of Hawaii at Manoa, United States
author

Grauert, Marianne
University of Copenhagen, Denmark
author

Hill, Peter J.
Florida State University, United States
author

Janecek, Thomas R.
Woods Hole Oceanographic Institution, United States
author

Kelly, Daniel Clay
Indiana University, United States
author

Latimer, Jennifer C.
GEOMAR, Federal Republic of Germany
author

Roessig, Kristeen McGonigal
author

Nees, Stefan
author

Ninnemann, Ulysses S.
author

Nuernberg, Dirk
author

Pekar, Stephen F.
author

Pellaton, Caroline C.
author

Pfuhl, Helen A.
author

Roehl, Ursula
author

Schellenberg, Stephen A.
author

Shevenell, Amelia E.
author

Stickley, Catherine E.
author

Suzuki, Noritoshi
author

Touchard, Yannick
author

Wei, Wuchang
author

White, Timothy S.
author

Identification:
L'Ouverture oceanique au sud de la Tasmanie durant le Paleogene et ses consequences paleoceanographiques; resultats preliminaires de la mineralogie des argiles (Leg ODP 189) Paleogene ocean opening south of Tasmania, and its paleo-oceanographic implications; preliminary results from clay mineral analyses; ODP Leg 189
2001
Comptes Rendus de l'Academie des Sciences, Serie II. Sciences de la Terre et des Planetes
Elsevier, Paris, France
332
5
323-329
ODP Leg 189 was designed to test the hypothesis that opening of the Tasmanian Seaway and initiation of circumpolar circulation contributed to the thermal isolation of Antarctica, leading to the development of initial ice-sheet and oceanic thermohaline circulation. The clay assemblages of the Tasmanian region contain the traces of two tectonic stages associated with ocean opening south of the south Tasman Rise near the Palaeocene-Eocene boundary and strike-slip activity between the western Tasmanian land-bridge and Antarctica during the Late Eocene. Earliest Oligocene clays indicate that cooling of Antarctic margins and activity of western boundary circulation progressed with the regional subsidence.
French
Serial
Coverage:Geographic coordinates:
North:25.0000
West:-180.0000East: 180.0000
South:-90.0000

Oceanography; Antarctic Ocean; Antarctica; Australasia; Australia; Cenozoic; Circum-Antarctic region; clay minerals; cooling; drilling; Eocene; glacial geology; ice sheets; Indian Ocean; land bridges; Leg 189; marine sediments; ocean circulation; Ocean Drilling Program; ocean opening; Oligocene; Pacific Ocean; paleo-oceanography; paleoclimatology; Paleogene; sediments; sheet silicates; silicates; South Pacific; Southwest Pacific; subsidence; Tasman Sea; Tasmania Australia; Tasmanian Seaway; tectonics; Tertiary; thermohaline circulation; West Pacific;

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