The Cenozoic Southern Ocean. Tectonics, Sedimentation, and Climate Change Between Australia and Antarctica. Volume 151. Geophysical Monograph Series

  • ID: 2489219
  • Book
  • Region: Antarctica, Australia
  • 368 Pages
  • John Wiley and Sons Ltd
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Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 151.

Ocean circulation and hence global climate are nowhere more strongly changed than through the opening or closing of gateways or seaways that link major oceans. The break–up of Gondwana, and the northward flight of its continental fragments from Antarctica, is a case in point. Profound climatic consequences resulted from shifts in ocean and atmospheric circulation due to drastic changes in global geography.
During the Cenozoic, the northward flight of southern continents led to the opening of gateways at southern high latitudes while progressively restricting and closing gateways in the low latitudes. Considerable previous research has dealt with the opening and expansion of the two Cenozoic gateways the Tasmanian Gateway south of Australia and the Drake Passage south of America which allowed the Antarctic Circumpolar Current (ACC) to develop and progressively isolate Antarctica thermally. It is generally accepted that full opening of the Tasmanian Gateway occurred earlier than that of Drake Passage, although the time of opening of Drake Passage remains controversial. It has long been proposed that a climatic threshold leading to major initial Antarctic ice sheet accumulation occurred during the Eocene–Oligocene transition as the Tasmanian Gateway opened, triggering ACC formation and resultant thermal isolation of the Antarctic continent (Gateway Hypothesis). South of Australia, Paleogene rifting slowly opened the Australo–Antarctic Gulf, but the Indian and Pacific Oceans remained separated by the Tasmanian land bridge until the latest Eocene, preventing earlier development of the ACC; waters derived from low latitudes efficiently transported heat towards the Antarctic continent, contributing to the maintenance of global greenhouse conditions. Early ocean drilling in the Tasmanian Gateway between Australia and Antarctica provided a basic framework of paleoenvironmental changes associated with the opening, but stratigraphic resolution was too limited to fully test potential interrelationships of plate tectonics, circum–polar circulation and global climate. So, until recently, the timing of events has been inadequately constrained.

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Preface vii

IntroductionNeville F. Exon, James R Kennett, and Mitchell J. Malone 1

Cretaceous Through Cenozoic

Cenozoic Reconstructions of the Australia–New Zealand–South Pacific Sector of AntarcticaSteven C. Cande and Joann M. Stock 5

Tectonics and Basin Development of the Offshore Tasmanian Area Incorporating Results
From Deep Ocean DrillingPeter J. Hill and Neville E Exon 19

Cenozoic Environments in the Tasmanian Area of the Southern Ocean (ODP Leg 189):
Inferences From Bulk and Clay MineralogyChristian Robert 43

On the Magnetostratigraphy of the East Tasman Plateau, Timing of the Opening of
the Tasmanian Gateway and Paleoenvironmental ChangesMike Fuller and Yannick Touchard 63

Magnetostratigraphy of the Pliocene–Pleistocene Sequence and of the Eocene–Oligocene
Transition at ODP Leg 189 Hole 1168Y. Touchard and M. Fuller 79

Eocene And Older

The Cretaceous/Paleogene Transition on the East Tasman Plateau, Southwestern PacificStephen A. Schellenberg, Henk Brinkhuis, Catherine E. Stickley, Michael Fuller, Frank T. Kyte, and Graham L Williams 93

On the Search for the Paleocene/Eocene Boundary in the Southern Ocean: Exploring ODP
Leg 189 Holes 1171D and 1172D, Tasman SeaUrsula Rohl, Henk Brinkhuis, Appy Sluijs, and Mike Fuller 113

Sea Level and Astronomically Induced Environmental Changes in Middle and Late Eocene
Sediments From the East Tasman PlateauUrsula Rohl, Henk Brinkhuis, Catherine E. Stickley, Mike Fuller, Stephen A. Schellenberg,Gerold Wefer, and Graham L. Williams 127

A Chemostratigraphic and Geochemical Facies Analysis of Strata Deposited in an Eocene
Australo–Antarctic Seaway: Is Cyclicity Evidence for Glacioeustasy?Timothy S. White 153

Oligocene And Younger

Changes in South Ocean Circulation in Late Oligocene to Early Miocene TimeHelen A. Pfuhl, I. Nicholas McCave, Stephen A. Schellenberg, and Patrizia Ferretti 173

Quantitative Miocene Calcareous Nannofossil Biostratigraphy From the Tasmanian GatewayKristeen L McGonigal 191

Early to Middle Miocene Paleoceanography in the Southern High Latitudes Off TasmaniaAtsuhito Ennyu and Michael A. Arthur 215

Paleocenographic Change During the Middle Miocene Climate Revolution: An Antarctic
Stable Isotope PerspectiveA.E. Shevenell and J.P Kennett 235

Late Neogene History of Paleoproductivity and Ice Rafting South of TasmaniaLiselotte Diester–Haass and Stefan Nees 253

A Deep–Sea Record of the Late Miocene Carbon Shift From the Southern Tasman SeaR.A. Tedford and D. C. Kelly 273

Paleo–Export Production, Terrigenous Flux and Sea Surface Temperatures Around Tasmania
Implications for Glacial/lnterglacial Changes in the Subtropical Convergence ZoneDirk Nurnberg, Natasja Brughmans, Joachim Schdnfeld, Ulysses Ninnemann, and Christian Dullo 291

Syntheses

Tectono–Sedimentary History of Uppermost Cretaceous Through Oligocene Sequences From
the Tasmanian Region, A Temperate Antarctic MarginNeville F. Exon, Henk Brinkhuis, Christian M. Robert, James P. Kennett, Peter). Hill andMichael K. Macphail 319

Paleoceanographic Evolution of the Tasmanian Seaway and its Climatic ImplicationsJames P. Kennett and Neville F. Exon 345

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Neville F. Exon
James P. Kennett
Mitchell J. Malone
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