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Problems of the Duration of the Eemian Interglacial in Europe North of the Alps

Published online by Cambridge University Press:  20 January 2017

Charles Turner
Charles Turner*
Affiliation:
Department of Earth Sciences, The Open University, Milton Keynes, MK7 6AA, United Kingdom
*
1To whom correspondence should be addressed. E-mail: [email protected].
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Abstract

Suggestions that the duration of the Eemian interglacial was about 11,000 yr, based on annually laminated sediment sequences in Germany, have been challenged in favor of a much longer interval. However, biostratigraphic evidence demonstrates why the Eemian sequences at Grande Pile and Ribains cannot be reliably used for alignment with the marine sequence, as applied by Kukla et al. (2002, this issue) to estimate the duration of this interglacial. The long chronology they propose would imply not just coniferous but, for up to 5000 yr, fully temperate forest in central France coexisting with treeless heath and steppe tundra conditions in northwestern Europe, an unlikely climatic and ecological scenario. The proposal that the Eemian Interglacial in western Europe lasted for 17,000 or even 23,000 yr is rejected. A duration of no more than 13,000 yr is preferred, at least for sites north of the Alps and Pyrenees. The duration of temperate conditions in the Mediterranean region is less certain.

Keywords

Eemianlast interglacialMelisey 1Herning Stadialinterglacial duration
Type
Research Article
Information
Quaternary Research , Volume 58 , Issue 1 , July 2002 , pp. 45 - 48
Copyright
University of Washington

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References

Caspers, G. Die eem- und weichselzeitliche Hohlform von Gross Todtshorn (Kr. Harburg; Niedersachsen)—Geologische und palynologische Untersuchungen zu Vegetation und Klimaverlauf der letzten Kaltzeit. Freund, H., and Caspers, G. Vegetation und Paläoklima der Weichsel-Kaltzeit im nordlichen Mitteleuropa—Ergebnisse paläobotanischer, -faunistischer und geologischer Untersuchungen. (1997). Schriftenreihe der Deutschen Geologischen Gesellschaft, 7 59.Google Scholar
Caspers, G., Merkt, J., Müller, H., and Freund, H. The Eemian interglaciation in northwestern Germany. Quaternary Research 58, (2002). 49 52.CrossRefGoogle Scholar
Chapman, M.R., and Shackleton, N.J. Global ice-volume fluctuations, North Atlantic ice-rafting events, and deep-ocean circulation changes between 130 and 70 ka. Geology 27, (1999). 795 798.Google Scholar
de Beaulieu, J.L., and Reille, M. A long Upper Pleistocene pollen record from Les Echets, near Lyon, France. Boreas 13, (1984). 111 132.CrossRefGoogle Scholar
de Beaulieu, J.L., and Reille, M. Long Pleistocene pollen sequences from the Velay Plateau (Massif Central, France). I Ribains maar. Vegetation History and Archaeobotany 1, (1992). 233 242.Google Scholar
Follieri, M., Magri, D., and Sadori, L. 250,000 year pollen record from Valle di Castiglione (Roma). Pollen et Spores 30, (1988). 329 356.Google Scholar
Frenzel, B., and Bludau, W. On the duration of the interglacial to glacial transition at the end of the Eemian Interglacial (deep sea stage 5 E): Botanical and sedimentological evidence. Berger, W.H., and Labeyrie, L.D. Abrupt Climate Change. (1987). Reidel, Dordrecht. 151 162.Google Scholar
Grüger, E. Die Seeablagerungen vom Samerberg Obb, und ihre Stellung im Jungpleistozän. Eiszeitalter und Gegenwart 29, (1979). 23 34.Google Scholar
Grüger, E. Palynostratigraphy of the last Interglacial cycle in Germany. Quaternary International 3–4, (1989). 69 79.CrossRefGoogle Scholar
Hahne, J., Kemle, S., Merkt, J., and Meyer, K.-D. Eem-, weichsel- und saalezeitliche Ablagerungen der Bohrung “Quakenbrück GE 2”. Geologisches Jahrbuch A 134, (1994). 9 69.Google Scholar
Kukla, G.J. The Last Interglacial. Science 287, (2000). 987 988.CrossRefGoogle Scholar
Kukla, G., de Beaulieu, J.-L., Svobodova, H., Andrieu-Ponel, V., Thouveny, N., and Stockhausen, H. Tentative correlation of pollen records of the Last Interglacial at Grande Pile and Ribains with Marine Isotope Stages. Quaternary Research 58, (2002). 32 35.Google Scholar
Kukla, G., McManus, J.F., Rousseau, D.-D., and Chuine, L. How long and how stable was the last Interglacial?. Quaternary Science Reviews 16, (1997). 605 612.Google Scholar
Müller, H. Pollenanalytische Untersuchungen und Jahresschichten-zählungen an der eemzeitlichen Kieselgur von Bispingen/Luhe. Geologisches Jahrbuch A 21, (1974). 149 169.Google Scholar
Müller, U. (2001). Die Vegetations- und Klimaentwicklung im jüngeren Quartär anhand ausgewählter Profile aus dem südwestdeutschen Alpenvorland. Tübinger Geowissenschaftliche Arbeiten D , 7, 118, pp.Google Scholar
Ponel, P. Rissian, Eemian and Würmian Coleoptera assemblages from La Grande Pile (Vosges, France). Palaeogeography, Palaeoclimatology, Palaeoecology 114, (1995). 1 41.Google Scholar
Pons, A., de Beaulieu, J.-L., Guiot, J., and Reille, M. Vingt cinq ans de recherche en analyse pollinique. Ecologia Mediterranea XVI, (1990). 169 193.CrossRefGoogle Scholar
Reille, M., and de Beaulieu, J.-L. Pollen analysis of a long upper Pleistocene continental sequence in a Velay maar. Palaeogeography, Palaeoclimatology, Palaeoecology 80, (1990). 35 48.Google Scholar
Sánchez, Goñi M.F., Eynaud, F., Turon, J.-L., and Shackleton, N.J. High resolution palynological record off the Iberian margin: Direct land-sea correlation for the Last Interglacial complex. Earth and Planetary Science Letters 171, (1999). 123 137.Google Scholar
Sánchez, Goñi M.F., Turon, J.-L., Eynaud, F., Shackleton, N.J., and Cayre, O. Direct land-sea correlation of the Eemian, and its comparison with the Holocene: A high-resolution palynological record off the Iberian margin. Geologie en Mijnbouw/Netherlands Journal of Geosciences 79, (2000). 345 354.CrossRefGoogle Scholar
Shackleton, N.J., Chapman, M., Sánchez Goñi, M.F., Pailler, D., and Lancelot, Y. The classic Marine Isotope Stage 5e. Quaternary Research 58, (2002). 14 16.Google Scholar
Turon, J.-L. Direct land/sea correlations in last interglacial complex. Nature 309, (1984). 673 676.Google Scholar
Woillard, G.M. Grande Pile peat bog: A continuous pollen record from the last 140,000 years. Quaternary Research 9, (1978). 1 21.Google Scholar
Woillard, G.M. Abrupt end of the last interglacial s.s. in north-east France. Nature 281, (1979). 558 562.Google Scholar
Zagwijn, W.H. An analysis of Eemian climate in Western and Central Europe. Quaternary Science Reviews 15, (1996). 451 469.CrossRefGoogle Scholar