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...
Published in: | Palaeogeography, Palaeoclimatology, Palaeoecology |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Elsevier
2012
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/18858/ http://www.sciencedirect.com/science/article/pii/S0031018211002732 |