Antarctic Ice Sheet: Stable Isotope Analyses of Byrd Station Cores and Interhemispheric Climatic Implications

Oxygen- and hydrogen-isotope analyses from the core hole through the Antarctic Ice Sheet at Byrd Station define temperature variations over more than 75,000 years. Synchronism between major climatic changes in Antarctica and the Northern Hemisphere is strongly indicated. The Wisconsin cold interval...

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Bibliographic Details
Published in:Science
Main Authors: Epstein, Samuel, Sharp, R. P., Gow, A. J.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Association for the Advancement of Science 1970
Subjects:
Antarctic
Byrd
Byrd Station
The Antarctic
Antarc*
Antarctica
Ice Sheet
Online Access:https://authors.library.caltech.edu/59061/
https://resolver.caltech.edu/CaltechAUTHORS:20150729-111103383
Description
Summary:Oxygen- and hydrogen-isotope analyses from the core hole through the Antarctic Ice Sheet at Byrd Station define temperature variations over more than 75,000 years. Synchronism between major climatic changes in Antarctica and the Northern Hemisphere is strongly indicated. The Wisconsin cold interval extended from 75,000 to 11,000 years ago. Three intra-Wisconsin warmer phases were all colder than pre- or post-Wisconsin times, which suggests that North American and Eurasian continental ice sheets did not disappear at any time during the Wisconsin.

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