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Bomb-Produced Carbon-14 in the Surface Water of the Pacific Ocean

Published online by Cambridge University Press:  18 July 2016

Timothy W Linick
Timothy W Linick*
Affiliation:
Mt Soledad Radiocarbon Laboratory, Department of Chemistry, University of California, San Diego, La Jolla, California 92093
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Abstract

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The distribution of 14C concentrations in the dissolved inorganic carbon in the surface waters of the Pacific Ocean is shown to have a primarily latitudinal pattern with Δ14C maxima at mid-latitudes in both hemispheres and a minimum at the equator. Oceanographic causes of this phenomenon are discussed.

Type
Oceanography
Information
Radiocarbon , Volume 22 , Issue 3: Heidelberg , 1980 , pp. 599 - 606
Copyright
Copyright © The American Journal of Science

References

Bien, G S and Suess, H E, 1967, Transfer and exchange of 14C between the atmosphere and the surface water of the Pacific Ocean, in Radioactive dating and methods of low level counting: Vienna, IAEA, p 105–115.Google Scholar
Cromwell, T, 1953, Circulation in a meridional plane in the Central Equatorial Pacific: Jour Marine Research, v 12, p 196–213.Google Scholar
Deacon, G E R, 1963, The southern ocean, in Hill, M N, ed, The Sea, vol II: New York, Wiley (Interscience), p 281–296.Google Scholar
Druffel, E M and Linick, T W, 1978, Radiocarbon in annual coral rings of Florida: Geophys Research Letters, v 5, p 913–916.Google Scholar
Keeling, C D, 1968, Carbon dioxide in surface ocean waters, 4. Global distribution: Jour Geophys Research, v 73, p 4543–4553.Google Scholar
Knauss, J A, 1963, Equatorial current systems, in Hill, M N, ed, The Sea, vol II: New York, Wiley (Interscience), p 235–252.Google Scholar
Linick, T W, 1975, Uptake of bomb-produced carbon-14 by the Pacific Ocean: PhD dissert, Univ California, San Diego, 255 p.Google Scholar
Linick, T W 1977, La Jolla natural radiocarbon measurements VII: Radiocarbon, v 19, p 19–48.Google Scholar
Linick, T W 1978, La Jolla measurements of radiocarbon in the oceans: Radiocarbon, v 20, p 333–359.Google Scholar
Linick, T W and Suess, H E, 1972, Bomb produced radiocarbon in the surface water of the Pacific Ocean, in Rafter, T A and Grant-Taylor, T E, eds, Internatl conf on radiocarbon dating, 8th, Proc: Wellington, New Zealand, Royal Soc New Zealand, p C87-C93.Google Scholar
Rafter, T A, 1968, Carbon-14 variations in nature, part 3—14C measurements in the South Pacific and Antarctic Oceans: New Zealand Jour Sci, v 11, p 551–589.Google Scholar
Rafter, T A and O'Brien, B J, 1970, Exchange rates between the atmosphere and the ocean as shown by recent C-14 measurements in the South Pacific, in Olsson, I U, ed, Radiocarbon variations and absolute chronology, Nobel symposium, 12th, Proc: New York, John Wiley & Sons, p 355–377.Google Scholar
Rafter, T A and O'Brien, B J 1972, 14C measurements in the South Pacific Ocean — a recalculation of the exchange rates between the atmosphere and the ocean, in Rafter, T A and Grant-Taylor, T E, eds, International conf on radiocarbon dating, 8th, Proc: Wellington, New Zealand, Royal Soc New Zealand, p C17-C42.Google Scholar
Reid, J L, 1962, On the circulation, phosphate-phosphorus content and zooplankton volumes in the upper part of the Pacific Ocean: Limnol Oceanog, v 7, p 287–306.Google Scholar
Rotschi, H, 1970, Variations of equatorial currents, in Wooster, W S, ed, Scientific exploration of the South Pacific: Washington, DC, Natl Acad Sci, p 75–83.Google Scholar
Sverdrup, H U, Johnson, M W, and Fleming, R H, 1942, The oceans, their physics, chemistry, and general biology: Englewood Cliffs, New Jersey, Prentice-Hall, 1087 p.Google Scholar
Wooster, W S and Reid, J L, 1963, Eastern boundary currents, in Hill, M N, ed, The Sea, vol II: New York, Wiley (Interscience), p 253–280.Google Scholar