Abstract

Seasonal variations in 18 O content, in acidity, and in dust content have been used to count annual layers in the Dye 3 deep ice core back to the Late Glacial. In this way the Pleistocene/Holocene boundary has been absolutely dated to 8770 BC with an estimated error limit of ± 150 years. If compared to the conventional 14 C age of the same boundary a value of Δ 14 C = 53 ± 13‰ is obtained. This Δ 14 C value suggests that 14 C levels during the Late Glacial were not substantially higher than during the Postglacial.

Keywords

Radiocarbon datingHolocenePleistoceneGlacial periodGeologyIce coreQuaternaryCore (optical fiber)Physical geographyPaleontologyOceanographyGeographyMaterials science

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Publication Info

Year
1986
Type
article
Volume
28
Issue
2A
Pages
284-291
Citations
125
Access
Closed

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C. U. Hammer, Henrik Clausen, Henrik Tauber (1986). Ice-Core Dating of the Pleistocene/Holocene Boundary Applied to a Calibration of the<sup>14</sup>C Time Scale. Radiocarbon , 28 (2A) , 284-291. https://doi.org/10.1017/s0033822200007384

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DOI
10.1017/s0033822200007384