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Science 1 May 1998: Vol. 280. no. 5364, pp. 725 - 728 DOI: 10.1126/science.280.5364.725
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Reports
Deep-Sea Coral Evidence for Rapid Change in Ventilation of the Deep North Atlantic 15,400 Years Ago
Jess F. Adkins,
*
Hai Cheng,
Edward A. Boyle,
Ellen R. M. Druffel,
R.
Lawrence Edwards
Coupled radiocarbon and thorium-230 dates from benthic coral
species reveal that the ventilation rate of the North Atlantic upper
deep water varied greatly during the last deglaciation. Radiocarbon
ages in several corals of the same age, 15.41 ± 0.17 thousand
years, and nearly the same depth, 1800 meters, in the western North
Atlantic Ocean increased by as much as 670 years during the 30- to
160-year life spans of the samples. Cadmium/calcium ratios in one coral
imply that the nutrient content of these deep waters also increased.
Our data show that the deep ocean changed on decadal-centennial time
scales during rapid changes in the surface ocean and the atmosphere.
J. F. Adkins and E. A. Boyle, Department of Earth,
Atmosphere and Planetary Sciences, Massachusetts Institute of
Technology, Cambridge, MA 02139, USA.
H. Cheng and R. L. Edwards, Department of Geology and Geophysics,
University of Minnesota, Minneapolis, MN 55455, USA.
E. R. M. Druffel, Department of Earth System Science,
University of California at Irvine, Irvine, CA 92697-3100, USA.
*
Present address: Geochemistry 62, LDEO, Route 9W, Palisades, NY
10964, USA.
To whom correspondence should be addressed.
Read the Full Text
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