A Late Pleistocene sequence at Margreteberg, southwestern Sweden
At Margreteberg, southwestern Sweden, a comple Pleistocene sequence has been stratigraphically investigated. Strata of clay, silt, sand, peat and solifluction layers are overlain by till‐like sediments which are covered by sandy‐clayey strata. By means of biostratigraphical analyses (foraminifera, o...
| Published in: | Boreas |
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| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
1988
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1111/j.1502-3885.1988.tb00130.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1988.tb00130.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1988.tb00130.x |
| Summary: | At Margreteberg, southwestern Sweden, a comple Pleistocene sequence has been stratigraphically investigated. Strata of clay, silt, sand, peat and solifluction layers are overlain by till‐like sediments which are covered by sandy‐clayey strata. By means of biostratigraphical analyses (foraminifera, olluscs, wood remains, pollen and diatoms), a reconstruction of the palaeoenvirnmental development has been obtained. Radiocarbon measurements and amiono acis ratios have been carried out in order to date the sediments. The foraminifera in the lowermost clay strata indicate Arctic or boreal‐Arctic marine environment during the Late Saalian or Late Elsterian perods The δ 18 Ovalues and molluscs also suggest that the clay was deposited in glaciomarine conditions. Amino acid ratios (D/L=0.25) of Hiatella in the clay imply an age between the Holsteinian and Eemian Interglacials. Teh peat layers contain a pollen flora. Prtedominated by Picea and Pinus, and are pollen analytically dated to the end of the Eemian interglacial. The solofluction sediments most probably were fromed during the first stage (s) of the Early weichselian and may include the initaial phase of the Brorup Interstadial (the Rodebaek interstadial). During this stage(s) aretic‐Subarctic conditions previaled reflected by a pollen flora with a predominance of herbs and shrubs. Acidophilous and aerohpilous diatoms indicate oligotrophic shallow wate conditions in an Arctic environment, when almost no leaching of mineral solis occurred. The solofluction sediments also contain reworked interglacial (Eemian) pollen and brackish‐Marine diatoms. Radiocarbon dating of the peat, wood and solofluction sediments yieded infinnite ages>40,000B.P. |
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