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...

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Bibliographic Details
Main Authors: Shipboard Scientific Party, Shevenell, Amelia E.
Format: Conference Object
Language:unknown
Published: Digital Commons @ University of South Florida 2001
Subjects:
Online Access:https://digitalcommons.usf.edu/msc_facpub/660
https://digitalcommons.usf.edu/cgi/viewcontent.cgi?article=1673&context=msc_facpub