Hostname: page-component-7479d7b7d-68ccn Total loading time: 0 Render date: 2024-07-12T11:34:43.299Z Has data issue: false hasContentIssue false

Isotopic Fractionation of Norwegian Materials for Radiocarbon Dating

Published online by Cambridge University Press:  18 July 2016

Steinar Gulliksen*
Affiliation:
Radiological Dating Laboratory, The Norwegian Institute of Technology, Trondheim, Norway
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

To improve reporting of radiocarbon dates, Stuiver and Polach (1977) recommend that reported standard errors should include the error in the applied δ13C value, and suggest estimated mean values for δ13C to be applied when not measured. Based on δ13C data for ca 250 samples measured during 1975-1979, mean values for different materials dated by the Trondheim radiocarbon laboratory have been compiled. All material is from Norway and Svalbard (marine bone collagen). For peat, gyttja, and terrestrial bone material, δ13C should be measured to obtain optimal precision in the dates. For shell, wood, charcoal, and marine bones, the standard error in an estimated δ13C value will only increase uncertainty of a date from ±50 years to ca ±55 years.

Type
Dating Various Materials
Copyright
Copyright © The American Journal of Science

References

Craig, Harmon, 1953, The geochemistry of the stable carbon isotopes: Geochim et Cosmochim Acta, v 8, p 5392.10.1016/0016-7037(53)90001-5Google Scholar
Craig, Harmon 1954, Carbon-13 in plants and the relationships between carbon-13 and 14 variations in nature: Jour Geology, v 62, p 115149.10.1086/626141Google Scholar
Craig, Harmon 1957, Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxide: Geochim et Cosmochim Acta, v 12, p 133140.Google Scholar
Donner, Joakim and Jungner, Högne, 1975, Radiocarbon dating of shells from marine Holocene deposits in the Disko Bugt area, West Greenland: Boreas, v 4, p 2545.Google Scholar
Lerman, J C, 1973, Carbon-14 dating: Origin and correction of isotope fractionation errors in terrestrial living matter, in Rafter, T A and Grant-Taylor, T, eds, Internatl radiocarbon conf, 8th, Proc: Wellington, New Zealand, Royal Soc New Zealand, H16-H28.Google Scholar
Lerman, J C, Mook, W G, and Vogel, J C, 1970, C14 in tree rings from different localities, in Olsson, I U, ed, Radiocarbon variations and absolute chronology, Nobel symposium, 12th, Proc: New York, John Wiley & Sons, p 275301.Google Scholar
Mangerud, J and Gulliksen, Steinar, 1974, Apparent radiocarbon ages of recent marine shells from Norway, Spitsbergen, and Arctic Canada: Quaternary Research, v 5, p 263273.Google Scholar
Olsson, I U and Osadebe, F A N, 1974, Carbon isotope variations and fractionation corrections in 14C dating: Boreas, v 3, p 139146.10.1111/j.1502-3885.1974.tb00672.xGoogle Scholar
Olsson, I U, El-Daoushy, M F, Abd-El-Mageed, Abdella, and Klasson, Martin, 1974, A comparison of different methods for pretreatment of bones. I: Geol Fören Stockh Förh, v 96, p 171181.Google Scholar
Stuiver, Minze and Polach, H A, 1977, Discussion: Reporting of 14C data: Radiocarbon, v 19, p 355363.10.1017/S0033822200003672Google Scholar
Troughton, J H, 1973, Carbon isotope fractionation by plants, in Rafter, T A and Grant-Taylor, T, eds, Internatl radiocarbon conf, 8th, Proc: Wellington, New Zealand, Royal Soc New Zealand, E39-E57.Google Scholar