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Ehrmann, W. U. et al. (1992): History of Antarctic glaciation; an Indian Ocean perspective
Leg/Site/Hole:
Related Expeditions:
ODP 119
ODP 120
Identifier:
ID:
2007-093173
Type:
georefid
Creator:
Name:
Ehrmann, W. U.
Affiliation:
Alfred-Wegener-Institut fuer Polar- und Meeresforschung, Federal Republic of Germany
Role:
author
Name:
Hambrey, J. J.
Affiliation:
University of Michigan, United States
Role:
author
Name:
Baldauf, J. G.
Affiliation:
University of Wales College of Cardiff, United Kingdom
Role:
author
Name:
Barron, J.
Affiliation:
Bundesanstalt fuer Geowissenschaften und Rohstoffe, Federal Republic of Germany
Role:
author
Name:
Larsen, B.
Affiliation:
Lamont-Doherty Geological Observatory of Columbia University, United States
Role:
author
Name:
Mackensen, A.
Affiliation:
Cambridge University, United Kingdom
Role:
author
Name:
Wise, S. W., Jr.
Affiliation:
Ocean Drilling Program, United States
Role:
author
Name:
Zachos, J. C.
Affiliation:
U. S. Geological Survey, United States
Role:
author
Identification:
Title:
History of Antarctic glaciation; an Indian Ocean perspective
Year:
1992
Source:
In: Duncan, Robert A. (editor), Rea, David K. (editor), Kidd, Robert B. (editor), von Rad, Ulrich (editor), Weissel, Jeffrey K. (editor), Synthesis of results from scientific drilling in the Indian Ocean
Publisher:
American Geophysical Union, Washington, DC, United States
Volume:
70
Issue:
Pages:
423-446
Abstract:
This paper summarizes the principal scientific results from Legs 119 and 120 of the Ocean Drilling Program as they relate to the Cenozoic glacial and climatic history of Antarctica. These two legs cored 16 sites on a south-north transect from the Antarctic continental shelf of Prydz Bay to the north Kerguelen Plateau. Glacigenic sediments were recovered in Prydz Bay. The Kerguelen Plateau yielded pelagic and glaciomarine sediments. Clay sediments and ice-rafted debris and oxygen isotope composition of foraminifera are integrated. Long-term cooling is indicated from 52 Ma with several major advance and retreat phases. Major increases of ice occurred in both the middle Miocene and late Miocene with the latter associated with the growth of the West Antarctic ice sheet. (SNT)
Language:
English
Genre:
Serial
Rights:
URL:
Coverage:
Geographic coordinates:
North:25.0000
West:-180.0000
East: 180.0000
South:-90.0000
Keywords:
Isotope geochemistry; Sedimentary petrology; Stratigraphy; algae; Antarctica; benthic taxa; calcium carbonate; chemical ratios; clastic sediments; clay; clay minerals; Foraminifera; framework silicates; glacial environment; glaciation; ice rafting; Indian Ocean; Invertebrata; isotopes; Kerguelen Plateau; Leg 119; Leg 120; nannofossils; O-18/O-16; Ocean Drilling Program; opal; oxygen; planktonic taxa; Plantae; Protista; Prydz Bay; Ross Sea; sedimentation; sediments; sheet silicates; silica minerals; silicates; smectite; Southern Ocean; stable isotopes;
.
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