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Volumn 284, Issue 5420, 1999, Pages 1654-1657

A mid-European decadal isotope-climate record from 15,500 to 5000 years B.P.

Author keywords

[No Author keywords available]

Indexed keywords

ICE; OXYGEN;

EID: 0033522810     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.284.5420.1654     Document Type: Article
Times cited : (538)

References (36)
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    • p in addition to regional temperatures changes. However, for the period of interest, during deglaciation, such elevation changes give a rise of only ±0.25‰ [S. J. Johnsen, D. Dahl-Jensen, W. Dansgaard, N. Gundestrup, Tellus 47, 624 (1995)], considerably less than needed to explain the observed transatlantic differences.
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    • Johnsen, S.J.1    Dahl-Jensen, D.2    Dansgaard, W.3    Gundestrup, N.4
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    • 18O record is the same as for the well-marked LST ash layer in the littoral cores from Ammersee (14) [R. Klee, R. Schmidt, J. Müller, Limnologia 23, 131 (1993)] and from Swiss Lakes (8).
    • (1977) U.S. Geol. Surv. Prof. Pap. , vol.440
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    • 18O record is the same as for the well-marked LST ash layer in the littoral cores from Ammersee (14) [R. Klee, R. Schmidt, J. Müller, Limnologia 23, 131 (1993)] and from Swiss Lakes (8).
    • (1993) Limnologia , vol.23 , pp. 131
    • Klee, R.1    Schmidt, R.2    Müller, J.3
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    • note
    • 14C measurements for core AS96-1 were performed by M. Paterne (LSCE) and by G. Bonani and I. Hajdas (Eidgenössische Technische Hochschule-Zürich) for core AS92-5. The manuscript profited from discussion with G. Hoffmann, L. Labeyrie, and M. Elliot and from the reviewers' comments. The GRIP project was financed by the national funding bodies of Belgium, Denmark, France, Germany, Iceland, Italy, Switzerland, and the UK as well as the XII Directorate of the European Union and organized with the support of the European Science foundation.


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