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.
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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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Identifiers
- DOI
- 10.1017/s0033822200007384