Evidence for an earliest Oligocene ice sheet on the Antarctic Peninsula

There is growing consensus that development of a semipermanent ice sheet on Antarctica began at or near the Eocene-Oligocene (E-O) boundary. Beyond ice-rafted debris in oceanic settings, however, direct evidence for a substantial ice sheet at this time has been limited and thus far restricted to Eas...

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Bibliographic Details
Published in:Geology
Main Authors: Ivany, L.C., Van Simaeys, S., Domack, E.W., Samson, S.D.
Format: Article in Journal/Newspaper
Language:English
Published: 2006
Subjects:
Online Access:http://www.vliz.be/nl/open-marien-archief?module=ref&refid=231700