Über den Charakter der Wärmezeit zwischen Drenthe- und Warthe-Stadial in Norddeutschland
Between the Saale and Warthe stages no real interglacial age existed. It was a time, where a reforestation took place, but only with coniferous, not with warmth-loving deciduous trees. In the northern areas which were still depressed by the ice load, early-interstadial marine ingressions of short du...
| Main Authors: | , |
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| Format: | Article |
| Language: | deu |
| Published: |
Copernicus Publications
1965-12-01
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| Series: | Eiszeitalter und Gegenwart |
| Online Access: | https://www.eg-quaternary-sci-j.net/16/37/1965/egqsj-16-37-1965.pdf |
| Summary: | Between the Saale and Warthe stages no real interglacial age existed. It was a time, where a reforestation took place, but only with coniferous, not with warmth-loving deciduous trees. In the northern areas which were still depressed by the ice load, early-interstadial marine ingressions of short duration occurred. There existed, however, no high-interglacial transgressions of a warm sea. The interval between Drenthe and Warthe could be named a "Super-Interstadial". |
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| ISSN: | 0424-7116 2199-9090 |