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Science 3 January 2003: Vol. 299. no. 5603, pp. 99 - 102 DOI: 10.1126/science.1077998
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Reports
Holocene Deglaciation of Marie Byrd Land, West Antarctica
John O. Stone,
Gregory A. Balco,
David E. Sugden,
Marc W. Caffee,
Louis C. Sass III,
Seth G. Cowdery,
Christine Siddoway
Surface exposure ages of glacial deposits in the Ford
Ranges of western Marie Byrd Land indicate continuous thinning of the West Antarctic Ice Sheet by more than 700 meters near the coast throughout the past 10,000 years. Deglaciation lagged the disappearance of ice sheets in the Northern Hemisphere by thousands of years and may
still be under way. These results provide further evidence that parts
of the West Antarctic Ice Sheet are on a long-term trajectory of
decline. West Antarctic melting contributed water to the oceans in the
late Holocene and may continue to do so in the future.
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