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Radiocarbon Age Calibration of Marine Samples Back to 9000 Cal Yr BP

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Stuiver, Minze, Pearson, G W, Braziunas, Tom·1986·Radiocarbon

Abstract

Calibration curves spanning several millennia are now available in this special issue of Radiocarbon. These curves, nearly all derived from the 14 C age determinations of wood samples, are to be used for the age conversion of samples that were formed through use of atmospheric CO 2. When samples are formed in reservoirs (eg, lakes and oceans) that differ in specific 14 C content from the atmosphere, an age adjustment is needed because a conventional 14 C age, although taking into account 14 C (and 13 C) fractionation, does not correct for the difference in specific 14 C activity (Stuiver & Polach, 1977). The 14 C ages of samples grown in these environments are too old, and a reservoir age correction has to be applied. This phenomenon has been referred to as the reservoir effect (Stuiver & Polach, 1977).

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Metadata

Authors
Stuiver, M., Pearson, G. W., & Braziunas, T.
Venue
Radiocarbon
Published
1986
Volume
28
Issue
2B
Pages
980-1021
ISSN
  • 0033-8222 (ISSN-L)
  • 1945-5755
OpenAlex
W1600028230
Cited by
739
References
1
FWCI
13.95
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Radiocarbon Age Calibration of Marine Samples Back to 9000 Cal Yr BP. https://app.cochat.ai/papers/10.1017/s0033822200060264
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Stuiver, M., Pearson, G. W., & Braziunas, T. (1986). Radiocarbon Age Calibration of Marine Samples Back to 9000 Cal Yr BP. Radiocarbon. https://doi.org/10.1017/s0033822200060264

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