Leg 189 Summary
The Cenozoic Era is unusual in its development of major ice sheets. Progressive high-latitude cooling during the Cenozoic eventually formed major ice sheets, initially on Antarctica and later in the Northern Hemisphere. In the early 1970s, a hypothesis was proposed that climatic cooling and an Antar...
Main Authors: | , |
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Format: | Conference Object |
Language: | unknown |
Published: |
Digital Commons @ University of South Florida
2001
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Subjects: | |
Online Access: | https://digitalcommons.usf.edu/msc_facpub/660 https://digitalcommons.usf.edu/cgi/viewcontent.cgi?article=1673&context=msc_facpub |