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Science 4 June 1999: Vol. 284. no. 5420, pp. 1654 - 1657 DOI: 10.1126/science.284.5420.1654
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Reports
A Mid-European Decadal Isotope-Climate Record from 15,500 to 5000 Years B.P.
Ulrich von Grafenstein,
1*
Helmut Erlenkeuser,
2
Achim Brauer,
3
Jean Jouzel,
1
Sigfus J. Johnsen
4
Oxygen-isotope ratios of precipitation
( 18OP) inferred from deep-lake ostracods
from the Ammersee (southern Germany) provide a climate record with
decadal resolution. The record in detail shows many of the rapid
climate shifts seen in central Greenland ice cores between 15,000 and
5000 years before the present (B.P.). Negative excursions in the
estimated 18OP from both of these records
likely reflect short weakenings of the thermohaline circulation caused
by episodic discharges of continental freshwater into the North
Atlantic. Deviating millennial-scale trends, however, indicate that
climate gradients between Europe and Greenland changed systematically,
reflecting a gradual rearrangement of North Atlantic circulation
during deglaciation.
1 Laboratoire des Sciences du Climat et
de l'Environnement (LSCE), F-91198 Gif-sur-Yvette, France.
2 Leibniz-Labor für Altersbestimmung und
Isotopenforschung der Universität Kiel, Germany.
3 Laboratoire de Botanique Historique et
Palynologie, Faculte des Sciences et Techniques de Saint-Jerome,
Marseille, France, and GeoForschungsZentrum Potsdam, Germany.
4 Department of Geophysics, University of
Copenhagen, Copenhagen, Denmark, and Science Institute, University of
Iceland, Reykjavik, Iceland.
*
To whom correspondence should be addressed. E-mail:
uligraf{at}lsce.cnrs-gif.fr
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