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Geology; November 1998; v. 26; no. 11; p. 1047-1050; DOI: 10.1130/0091-7613(1998)026<1047:CROKIA>2.3.CO;2
© 1998 Geological Society of America
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Cold reversal on Kodiak Island, Alaska, correlated with the European Younger Dryas by using variations of atmospheric 14C content

Irka Hajdas1, Georges Bonani1, Per Bodén2, Dorothy M. Peteet3 and Daniel H. Mann4

1 Institut für Teilchenphysik, Eidgenössische Technische Hochschule Zurich, CH-8093 Zurich, Switzerland
2 Department of Geology and Geochemistry, Stockholm University, S-106 91 Stockholm, Sweden
3 Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964
4 University of Alaska Museum, Fairbanks, Alaska 99775

High-resolution accelerator-mass-spectrometer radiocarbon dating was performed on late-glacial macrofossils in lake sediments from Kodiak Island, Alaska, and on shells in marine sediments from southwest Sweden. In both records, a dramatic drop in radiocarbon ages equivalent to a rise in the atmospheric 14C by ~70{per thousand} coincides with the beginning of the cold period at 11 000 yr B.P. (14C age). Thus, our results show that a close correlation between climatic records around the globe is possible by using a global signature of changes in atmospheric 14C content.




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