Lamont Radiocarbon Measurements VI

Author:

Broecker Wallace S.,Olson Edwin A.

Abstract

In contrast to previous radiocarbon measurement lists, this list contains only known-age samples, most of which formed during the past ten years. The measurements were made largely in order to gain an understanding of the distribution of radiocarbon within the dynamic carbon reservoir both today and at times in the past. Since all materials forming in this reservoir today do not have the same C14/C12 ratio, such an understanding is necessary in order to arrive at the most accurate possible estimate of the age of samples submitted for dating. This is particularly important when high accuracy (i.e., <100 years error) is required on subaerially grown samples and also when attempting to extend the method to samples which formed in reservoirs other than the atmosphere (for example, the ocean and freshwater systems).

Publisher

Cambridge University Press (CUP)

Subject

General Earth and Planetary Sciences,Archaeology

Reference23 articles.

1. Broecker W. S. , Tucek C. S. , and Olson E. A. , in press, Radiocarbon analysis of oceanic CO2: Internat. Jour. Applied Radiation and Isotopes.

2. The Natural Distribution of Radiocarbon and the Exchange Time of Carbon Dioxide Between Atmosphere and Sea

3. The Distribution of Carbon-14 in Nature

4. The atom bomb effect. Recent increase in the 14C content of the atmosphere, biosphere, and surface waters of the ocean;Rafter;New Zealand Jour. Sci. and Technology, sec. B,1957

5. Atomic Bomb Effect: Variation of Radiocarbon in Plants, Shells, and Snails in the Past 4 Years

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