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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DigitalCommons@UMaine
1997
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Online Access: | https://digitalcommons.library.umaine.edu/ers_facpub/67 https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1066&context=ers_facpub |