Extension of Radiocarbon Calibration Curve.
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- Kitagawa Hiroyuki
- International Research Center for Japanese Studies
Bibliographic Information
- Other Title
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- `14´Cキャリブレーション年代域の拡大
- 14C キャリブレーション ネンダイイキ ノ カクダイ
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Abstract
Coupled U-Th and 14C measurements on coral samples provided very promising results to extend the radiocarbon calibration curve back to 18, 000 BP (Bard et al., 1993). Based on these results, a radiocarbon calibration curve (and program) has recently been presented (Stuiver and Reimer, 1993) and is now widely used by Quaternary geologist. However, before ca., 12, 500y cal BP, the AMS-14C dates obtained from terrestrial macrofossils from the Swedish glacial varved clays (Björck et al., 1992; Wohlfarth et al., 1993) and from sediments in Lake Soppensee, Switzerland and Lake Holzmmar, Germany (Hajdas, 1993; Hajdas et al., 1993) and in Lake Suigetsu, Japan (Kitagawa et al., 1995) do not support on the radiocarbon calibration curve based on 230Th/234U and 14C measurements on corals. This discrepancy of the radiocarbon calibration curve from two different approaches suggests that the use of the radiocarbon calibration program during the last glacial period is too premature at present stage and the radiocarbon and U-Th dating methods must be examined in detail.
Journal
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- The Quaternary Research (Daiyonki-Kenkyu)
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The Quaternary Research (Daiyonki-Kenkyu) 34 (3), 185-190, 1995
Japan Association for Quaternary Research
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Details 詳細情報について
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- CRID
- 1390282681472493312
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- NII Article ID
- 10002632925
- 10003775194
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- NII Book ID
- AN0034136X
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- ISSN
- 18818129
- 04182642
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- NDL BIB ID
- 3624179
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- Text Lang
- ja
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed