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Duration of Last Interglacial Conditions in Northwestern Greece

Published online by Cambridge University Press:  20 January 2017

Polychronis C. Tzedakis ,
Michael R. Frogley  and
Timothy H.E. Heaton
Polychronis C. Tzedakis*
Affiliation:
School of Geography, University of Leeds, Leeds, LS2 9JT, United Kingdom
Michael R. Frogley
Affiliation:
Centre for Environmental Research, School of Chemistry, Physics and Environmental Science, University of Sussex, Falmer, Brighton, BN1 9QJ, United Kingdom
Timothy H.E. Heaton
Affiliation:
NERC Isotope Geosciences Laboratory, Kingsley Dunham Centre, Keyworth, Nottingham, NG12 5GG, United Kingdom
*
1To whom correspondence should be addressed. E-mail: [email protected].
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Abstract

A new astronomical calibration method for long pollen records from southern Europe is applied to the last interglacial interval of the Ioannina sequence, northwestern Greece. This shows that the last interglacial in this region, as defined by the presence of forest communities, lasted ca. 15,500 yr, from 127,300 to 111,800 yr B.P. Interglacial conditions developed within marine isotope substage (MIS) 5e and persisted into MIS 5d, lagging changes in global ice volume.

Type
Research Article
Information
Quaternary Research , Volume 58 , Issue 1 , July 2002 , pp. 53 - 55
Copyright
University of Washington

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References

Berger, A. Long-term variations of caloric insolation resulting from the earth's orbital elements. Quaternary Research 9, (1978). 139 167.Google Scholar
Berger, A., Guiot, J., Kukla, G., and Pestiaux, P. Long-term variations of monthly insolation as related to climatic changes. Geologische Rundschau 70, (1981). 748 758.Google Scholar
Frogley, M.R. Biostratigraphy, Palaeoecology and Geochemistry of a Long Lacustrine Sequence from NW Greece. (1997). University of Cambridge, Cambridge.Google Scholar
Frogley, M.R., Tzedakis, P.C., and Heaton, T.H.E. Climate variability in NW Greece during the last interglacial. Science 285, (1999). 1886 1889.Google Scholar
Magri, D., and Tzedakis, P.C. Orbital signatures and long-term vegetation patterns in the Mediterranean. Quaternary International 73/74, (2000). 69 78.CrossRefGoogle Scholar
Shackleton, N.J., Chapman, M., Sánchez-Goñi, M.F., Pailler, D., and Lancelot, Y. The classic marine isotope substage 5e. Quaternary Research 58, (2002). 14 16.CrossRefGoogle Scholar
Tzedakis, P.C. Long-term tree populations in northwest Greece through multiple Quaternary climatic cycles. Nature 364, (1993). 437 440.CrossRefGoogle Scholar
Tzeakis, P. C, Frogley, M. R, and Heaton, T. H. E. (in press), Last interglacial conditions in southern Europe: Evidence from Ioannina, northwest Greece, Global and Planetary Change.Google Scholar
Tzedakis, P.C., Andrieu, V., de Beaulieu, J.-L., Crowhurst, S., Follieri, M., Hooghiemstra, H., Magri, D., Reille, M., Sadori, L., Shackleton, N.J., and Wijmstra, T.A. Comparison of terrestrial and marine records of changing climate of the last 500,000 yr. Earth and Planetary Science Letters 150, (1997). 171 176.Google Scholar