Abstract
AbstractSuggestions 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 Kuklaet 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.
Publisher
Cambridge University Press (CUP)
Subject
General Earth and Planetary Sciences,Earth-Surface Processes,Arts and Humanities (miscellaneous)
Reference25 articles.
1. Global ice-volume fluctuations, North Atlantic ice-rafting events, and deep-ocean circulation changes between 130 and 70 ka
2. Palynostratigraphy of the last interglacial/glacial cycle in Germany
3. Die eem- und weichselzeitliche Hohlform von Gross Todtshorn (Kr. Harburg; Niedersachsen)—Geologische und palynologische Untersuchungen zu Vegetation und Klimaverlauf der letzten Kaltzeit;Caspers,1997
4. High resolution palynological record off the Iberian margin: direct land-sea correlation for the Last Interglacial complex
5. 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;Frenzel,1987
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