Vegetation and climate during the Weichselian Early Glacial and Pleniglacial in the Nierderlausitz, eastern Germany-macrofossil and pollen evidence.

• Published in: Journal of Quaternary Science
• Main Authors: Bos, J.A.A., Bohncke, S.J.P., Kasse, C., Vandenberghe, J.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2001
• Subjects: Tundra; Cottongrass
• Online Access: https://research.vu.nl/en/publications/34d2bfcf-bfa1-404d-b086-cc1be34f7afb; https://doi.org/10.1002/jqs.606; https://hdl.handle.net/1871.1/34d2bfcf-bfa1-404d-b086-cc1be34f7afb

Cryoturbated organic beds and channel fills, intercalated with sandy and gravelly fluvial units, have been studied in an opencast brown-coal mine near Nochten (Niederlausitz), eastern Germany. The fluvial-aeolian sequence covers parts of the Early, Pleni- and Late-glacial. The detailed chronology is based on 11 radiocarbon and 12 OSL dates, covering the period between ca. 100 kyr and 11 kyr BP. Basal peat deposits are correlated with an Early Weichselian interstadial. During this period boreal forests were present and minimum mean summer temperatures were > 13°C. Early Pleniglacial deposits are absent. The Middle and Late Pleniglacial environments were treeless and different types of tundra vegetation can be recognised. Minimum mean summer temperatures varied between 10 and 15°C. Vegetation and climate is reconstructed in detail for the periods around 34-38 kyr BP and 24-25 kyr BP. Around 34-38 ka, a mixture between a low shrub tundra and a cottongrass tussock-subshrub tundra was present. The botanical and sedimentological data suggest that from the Middle to the Late Pleniglacial, the climate became more continental, aridity and wind strength increased, and the role of a protecting winter snow cover decreased. A sedge-grass-moss tundra dominated around 24 and 25 kyr BP. Copyright © 2001 John Wiley & Sons, Ltd.