A regional 8200 cal. yr BP cooling event
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Dorthe Klitgaard-Kristensen; Hans Petter Sejrup; Haflidi Haflidason; Sigfus John
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Article
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1998
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John Wiley and Sons
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English
β 139 KB
The most notable change in β¦ 18 O in Greenland ice cores during the Holocene occurs at 8200 cal. yr BP. Here we present a new high-resolution marine record from the northern North Sea, along with tree-ring data from Germany, which contain evidence of a pronounced temperature drop (ΟΎ2Β°C) contemporane