Change in climate, ocean and ice-sheet conditions in the Ross Embayment, Antarctica at 6 ka

Evidence from the Ross embayment, Antarctica, suggests an abrupt cooling and a concomitant increase in sea-ice cover at about 6000 sp (6 ka). Stable-isotope (delta D) concentrations in the Taylor Dome ice core, at the western edge of the Ross embayment, decline rapidly after 6 ka, and continue to de...

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Bibliographic Details
Main Authors: Stieg, Eric J., Hart, Charles P., White, James W.C., Cunningham, Wendy L., Davis, Mathew D., Saltzman, Eric S.
Format: Article in Journal/Newspaper
Language:English
Published: eScholarship, University of California 2014
Subjects:
Online Access:http://www.escholarship.org/uc/item/8zj9599j