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Science 2 October 1998: Vol. 282. no. 5386, pp. 92 - 95 DOI: 10.1126/science.282.5386.92
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Reports
Synchronous Climate Changes in Antarctica and the North Atlantic
E. J. Steig,
*
E. J. Brook,
J. W. C. White,
C. M. Sucher,
M. L. Bender,
S. J. Lehman,
D.
L. Morse,
E. D. Waddington,
G. D. Clow
Central Greenland ice cores provide evidence of abrupt changes in
climate over the past 100,000 years. Many of these changes have also
been identified in sedimentary and geochemical signatures in deep-sea
sediment cores from the North Atlantic, confirming the link between
millennial-scale climate variability and ocean thermohaline
circulation. It is shown here that two of the most prominent North
Atlantic events--the rapid warming that marks the end of the last
glacial period and the Bølling/Allerød-Younger Dryas
oscillation--are also recorded in an ice core from Taylor Dome, in the
western Ross Sea sector of Antarctica. This result contrasts with
evidence from ice cores in other regions of Antarctica, which show an
asynchronous response between the Northern and Southern Hemispheres.
E. J. Steig, J. W. C. White, S. J. Lehman,
Institute of Arctic and Alpine Research, University of Colorado,
Boulder, CO 80309, USA. E. J. Brook, Department of Geology,
Washington State University, Vancouver, WA 98686, USA. C. M. Sucher, Graduate School of Oceanography, University of Rhode Island,
Narragansett, RI 02882, USA. M. L. Bender, Department of
Geosciences, Princeton University, Princeton, NJ 08544, USA. D. L. Morse, Institute for Geophysics, University of Texas, Austin, TX 78759, USA. E. D. Waddington, Geophysics Program, University of
Washington, Seattle, WA 98195, USA. G. D. Clow, United States
Geological Survey, Denver Federal Center, Englewood, CO 80225, USA.
*
To whom correspondence should be addressed. E-mail:
steig{at}colorado.edu
Present address: Department of Earth and Environmental
Science, University of Pennsylvania, Philadelphia, PA 19104, USA.
Read the Full Text
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