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Time Scale and Ice Accumulation During the Last 125,000 Years as Indicated by the Greenland 018 curve

Published online by Cambridge University Press:  01 May 2009

N. A. Mörner
N. A. Mörner
Affiliation:
Department of GeologyUniversity of StockholmStockholm, Sweden
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Summary

The 18 curve from the 1390 m long ice core from Camp Century, Greenland, shows climatic changes that are easily correlated with known glacial and non-glacial events of North America and north Europe and are thus indirectly dated. With a known chronology, the glacial dynamic changes of the Greenland Ice Sheet can be calculated for the last 125,000 years. It is concluded that the dynamics of the Greenland Ice Sheet have changed drastically during this period and that these changes are directly related to major changes of climate and extension of the Wisconsin and Weichselian glaciations. Logarithmic time scales earlier applied to this curve must therefore be incorrect.

Type
Articles
Information
Geological Magazine , Volume 109 , Issue 1 , January 1972 , pp. 17 - 24
Copyright
Copyright © Cambridge University Press 1972

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References

Dansgaard, W., Johnsen, S. J., Møller, J. & Langway, C. C. 1969. One thousand centuries of climatic record from Camp Century on the Greenland Ice Sheet. Science 166, 378–81.CrossRefGoogle ScholarPubMed
Dansgaard, W. 1970. Oxygen isotope variation in ice cap cores. In volume dedicated to R. F. Flint of Yale Univ., Late Cenozoic Glacial Ages, 37–56.Google Scholar
Dreimanis, A. 1970. The Last Ice Age in the eastern Great Lakes region, North America. Proc. INQUA VIII Congress, Paris, 1969 (in press).Google Scholar
Hammen, T., van der, , Maarleveld, G. C., Vogel, J. C. & Zagwijn, W. H. 1967. Stratigraphy, climate succession and radiocarbon dating of the Last Glacial in the Netherlands. Geol. en Mijnbouw 46, 79–95.Google Scholar
Kukla, J. 1969. The cause of the Holocene climatic changes. Geol. en Mijnbouw 48 (3), 307–34.Google Scholar
Mörner, F.-A. 1969. The Late Quaternary history of the Kattegatt Sea and the Swedish West Coast; deglaciation shorelevel displacement, chronology, isostasy and eustasy. Sveriges Geol. Undersökning C-640, 487 pp.Google Scholar
Mörner, F.-A. 1970 a. Late Wisconsin ice marginal changes in the Erie–Ontario lobe area and comparison with Late Weichselian sequence of Southern Scandinavia. Abstracts with programs, Geol. Soc. America, 1970 Ann. Meet., Milwaukee, pp. 751–2.Google Scholar
Mörner, F.-A. 1970 b. Comparison between Late Weichselian and Late Wisconsin ice marginal changes. Eiszeitalter Gegenw. 21, 173–6.Google Scholar
Mörner, F.-A. 1971 a. The position of the ocean level during the interstadial at about 30,000 B.P.—A discussion from a climatic–glaciologic point of view. Canadian J. Earth Sci. 8, 132–43.CrossRefGoogle Scholar
Mörner, F.-A. 1971 b. The cold/warm changes during the Last Ice Age with special reference to the stratigraphy at Dösebacka and Ellesbo, in Southwest Sweden. Stockholm contrib. Geoloey, 24, (in press).Google Scholar
Zagwijn, W. & Paepe, R. 1968. Die Stratigraphie der Weichselzeitlichen Ablagerungen der Niederlande und Belgiens. Eiszeitalter Gegenw. 19, 129–46.Google Scholar