Pliocene Paleoenvironment and Antarctic Ice Sheet Behavior: Evidence from Wright Valley

Investigations in Wright Valley, adjacent to the Transantarctic Mountains in East Antarctica, shed light on the question of whether high-latitude Pliocene climate was warm enough to cause widespread deglaciation of the East Antarctic craton with a concurrent Magellanic moorland-like environment. If...

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Bibliographic Details
Main Authors: Hall, Brenda L., Denton, George H., Lux, Daniel R., Schlüchter, Christian
Format: Text
Language:unknown
Published: DigitalCommons@UMaine 1997
Subjects:
Online Access:https://digitalcommons.library.umaine.edu/ers_facpub/67
https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1066&context=ers_facpub