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Long-Term Variability of Temperature and 14C in the Gulf Stream: Oceanographic Implications

Published online by Cambridge University Press:  18 July 2016

Ellen M Druffel*
Affiliation:
Department of Chemistry, Woods Hole Oceanographic Institution Woods Hole, Massachusetts 02543
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Abstract

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Variability in temperature and 14C levels are recorded in coralline aragonite that grew in the Gulf Stream during the past four centuries. In particular, 18O/16O ratios reflect a decrease of ca 1°C in surface water temperature during the latter part of the Little Ice age. 14C levels also rose in the surface waters of the Gulf Stream and in atmospheric CO2 during the Maunder minimum. These observations indicate that ocean circulation may have been significantly different in the North Atlantic around the beginning of the 18th century.

Type
IV. Oceanography
Copyright
Copyright © The American Journal of Science 

References

Broecker, W S and Olson, E A, 1961, Lamont radiocarbon measurements VIII: Radiocarbon, v 3, p 176204.Google Scholar
Buddemeier, R W, Maragos, J E, and Knutson, D W, 1974, Radiographic studies of reef coral exoskeletons: rates and patterns of coral growth: Jour Experimental Marine Biol Ecol, v 14, p 179200.Google Scholar
Druffel, E M, 1980, Radiocarbon in annual corals rings from Belize and Florida, in Stuiver, Minze and Kra, Renee, eds, Internatl radiocarbon conf, 10th, Proc: Radiocarbon, v 22, no 2, p 363371.Google Scholar
Druffel, E M, 1982, Banded corals: Changes in oceanic carbon-14 levels during the Little Ice Age: Science, v 218, p 1319.Google Scholar
Druffel, E M and Linick, T W, 1978, Radiocarbon in annual coral rings from Florida: Geophys Research Letters, v 5, p 913916.Google Scholar
Druffel, E M and Suess, H E, in press, On the radiocarbon record in banded corals: Exchange parameters and net transport of 14CO2 between atmosphere and surface ocean: Jour Geophys Research.Google Scholar
Dunbar, R B, and Wellington, G M, 1981, Stable isotopes in a branching coral monitor seasonal temperature variation: Nature, v 293, p 453455.Google Scholar
Eddy, J A, 1976, The Maunder minimum: Science, v 192, p 1189.Google Scholar
Fairbanks, R G and Dodge, R E, 1979, Annual periodicity of the 18O/16O and 13C/12C ratios in the coral Montastrea annularis : Geochim et Cosmochim Acta, v 43, p 10091020.Google Scholar
Hudson, J A, Shinn, E A, Halley, R B, and Lidz, B, 1976, Sclerochronology: a tool for interpreting past environments: Geology, v 4, p 361364.Google Scholar
Jenkins, W J, 1982, On the climate of a subtropical ocean gyre: Decade time-scale variations in water mass renewal in the Sargasso Sea, Jour Marine Research, v 40, p 265290.Google Scholar
Knutson, D W, Buddemeier, R W, and Smith, S V, 1972, Coral chronometers: seasonal growth bands in reef corals: Science, v 177, p 270272.Google Scholar
MacIntyre, I G, and Smith, S V, 1974, X-radiographic studies of skeletal development in modern coral colonies, in Internatl symposium coral reefs, 2nd, Proc: Brisbane, p 277287.Google Scholar
Moore, W S and Krishnaswami, S, 1974, Correlation of x-radiography revealed banding in corals with radiometric growth rates, in Internatl coral reef Symposium, 2nd, Proc: Brisbane, p 269276.Google Scholar
Nozaki, Y, Rye, D M, Turekian, K K, and Dodge, R E, 1978, A 200-year record of carbon-13 and carbon-14 variations in a Bermuda coral: Geophys Research Letters, v 5, p 825828.Google Scholar
Stommel, H, 1979, Determination of water mass properties of water pumped down from the Ekman layer to the geostrophic flow below: Natl Acad Sci, 76th, Proc: Washington, DC, p 3051–55.Google Scholar
Stuiver, M, 1980, Solar variability and climatic change during the current millennium: Nature, v 286, p 868871.CrossRefGoogle Scholar
Stuiver, M and Quay, P M, 1980, Changes in atmospheric 14C attributed to a variable sun: Science, v 207, p 1119.Google Scholar
Stuiver, M, 1981, Atmospheric 14C changes resulting from fossil fuel CO2 release and cosmic ray flux variability: Earth Planetary Sci Letters, v 53, p 349362.Google Scholar
Suess, H E, 1980, The radiocarbon record in tree rings of the last 8000 years, in Stuiver, Minze and Kra, Renee, eds, Internatl radiocarbon conf, 10th, Proc: Radiocarbon, v 22, no 2, p 200209.Google Scholar
Tans, P P, de Jong, A F M, and Mook, W G, 1979, Natural atmospheric 14C variation and the Suess effect: Nature, v 280, p 826.Google Scholar
Toggweiler, J F, 1980, Time histories of Sr-90 in Pacific surface water as recorded by head forming corals: EOS, v 61, no. 46, p 984.Google Scholar
Waldmeier, M, 1961, The sunspot activity in the years 1610–1960: Zurich, Schultess.Google Scholar