Description and ESR dating of the Holsteinian interglaciation |
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| Authors: | G. Linke O. Katzenberger R. Grün |
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| Affiliation: | 1. Geologisches Landesamt, Hamburg, Oberstr. 88, D-2000 Hamburg 13, F.R.G.;2. Geologisches Institut der Universität zu Köln, Zülpicherstr. 49, D-5000 Köln 1, F.R.G.;3. Department of Geology, McMaster University, Hamilton — Ontario, L8S 4M1 Canada |
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| Abstract: | The classical region of the Holsteinian interglacial is in the vicinity of Hamburg and the Lower Elbe. It is defined on the basis of pollen and is clearly distinguishable from the Eemian interglacial (Hallik, 1960; Müller, 1974). The Holsteinian interglacial is represented by a sequence of sediments up to 100 m in thickness. These consist of limnic, fluvial, and marine beds and show a transgression up to the height of present sea-level.Twenty-seven molluscs from Holsteinian deposits were used for ESR dating. The ages show that the Holsteinian may be correlated with stage 7 of the deep sea record V28-238 (Shackleton and Opdyke, 1973). |
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