Last Glacial Maximum to Holocene sea surface conditions at Umnak Plateau, Bering Sea, as inferred from diatom, alkenone, and stable isotope records
The Bering Sea gateway between the Pacific and Arctic oceans impacts global climate when glacial-interglacial shifts in shore line position and ice coverage change regional albedo. Previous work has shown that during the last glacial termination and into the Holocene, sea level rises and sea ice cov...
Main Authors: | , , , , |
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Format: | Text |
Language: | unknown |
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2010
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Online Access: | https://works.bepress.com/julie_brigham_grette/13 |