Antarctic topography at the Eocene-Oligocene boundary

We present a reconstruction of the Antarctic topography at the Eocene–Oligocene (ca. 34 Ma) climate transition. This provides a realistic key boundary condition for modeling the first big Antarctic ice sheets at this time instead of using the present day bedrock topography, which has changed signifi...

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Bibliographic Details
Published in:Palaeogeography, Palaeoclimatology, Palaeoecology
Main Authors: Wilson, Douglas S., Jamieson, Stewart S.R., Barrett, Peter J., Leitchenkov, German, Gohl, Karsten, Larter, Robert D.
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2012
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/18858/
http://www.sciencedirect.com/science/article/pii/S0031018211002732