An event stratigraphy for the Last Termi
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Svante BjΓΆrck; Michael J. C. Walker; Les C. Cwynar; Sigfus Johnsen; Karen-Luise
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Article
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1998
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John Wiley and Sons
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English
β 158 KB
It is suggested that the GRIP Greenland ice-core should constitute the stratotype for the Last Termination. Based on the oxygen isotope signal in that core, a new event stratigraphy spanning the time interval from ca. 22.0 to 11.5 k GRIP yr BP (ca. 19.0-10.0 k 14 C yr BP) is proposed for the North A