The Role of Carbon Dioxide During the Onset of Antarctic Glaciation

Author:

Pagani Mark1,Huber Matthew2,Liu Zhonghui3,Bohaty Steven M.4,Henderiks Jorijntje5,Sijp Willem6,Krishnan Srinath1,DeConto Robert M.7

Affiliation:

1. Department of Geology and Geophysics, Yale University, New Haven, CT 06520, USA.

2. Earth and Atmospheric Sciences Department and the Purdue Climate Change Research Center (PCCRC), Purdue University, West Lafayette, IN 47906, USA.

3. Department of Earth Sciences, The University of Hong Kong, Hong Kong, People’s Republic of China.

4. School of Ocean and Earth Science, University of Southampton, Southampton SO14 3ZH, UK.

5. Department of Earth Sciences, Uppsala University, SE-75 236 Uppsala, Sweden.

6. Climate Change Research Centre, Faculty of Science, University of New South Wales, Sydney 2052, Australia.

7. Department of Geosciences, University of Massachusetts-Amherst, Amherst, MA 01003, USA.

Abstract

Antarctica glaciation began soon after a large decrease in the concentration of atmospheric carbon dioxide around 35 million years ago.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference112 articles.

1. Rapid stepwise onset of Antarctic glaciation and deeper calcite compensation in the Pacific Ocean

2. The glacial record from the Prydz Bay continental shelf, East Antarctica;Hambrey M. J.;Proc. Ocean Drill. Program, Sci. Results,1991

3. M. J. Hambrey P. J. Barrett in The Antarctic Paleoenvironment: A Perspective on Global Change Part 2 J. P. Kennett D. A. Warnke Eds. (vol. 60 of Antarctic Research Series American Geophysical Union Washington DC 1993) pp. 91–124.

4. Implications of sediment composition on the southern Kerguelen Plateau for paleoclimate and depositional environment;Ehrmann W. U.;Proc. Ocean Drill. Program, Sci. Results,1991

5. Antarctic continental weathering changes during Eocene-Oligocene cryosphere expansion: Clay mineral and oxygen isotope evidence

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