Southwest Scandinavia, 40–15 kyr BP: palaeogeography and environmental change

• Published in: Journal of Quaternary Science
• Main Authors: Houmark‐Nielsen, Michael, Henrik Kjær, Kurt
• Other Authors: Danish Natural Science Research Council (CLIENT and CATLINA projects), Carlsbergfondet, SGU, Geological Survey of Sweden
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2003
• Subjects: Ice Sheet; Ice Stream A; Subarctic
• Online Access: http://dx.doi.org/10.1002/jqs.802; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.802; https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.802

Abstract Twelve palaeogeographical reconstructions illustrate environmental changes at the southwest rim of the Scandinavian Ice Sheet 40–15 kyr BP. Synchronised land, sea and glacier configurations are based on the lithostratigraphy of tills and intertill sediments. Dating is provided by optically stimulated luminescence and calibrated accelerator mass spectrometry radiocarbon. An interstadial sequence ca. 40–30 kyr BP with boreo‐arctic proglacial fjords and subarctic flora and occasional glaciation in the Baltic was succeeded by a Last Glacial Maximum sequence ca. 30–20 kyr BP, with the closure of fjords and subsequent ice streams in glacial lake basins in Kattegat and the Baltic. Steadily flowing ice from Sweden bordered the Norwegian Channel Ice Stream. A deglaciation sequence ca. 20–15 kyr BP indicates the transgression of arctic waters, retreat of the Swedish ice and advance of Baltic ice streams succeeded by a return to interstadial conditions. When ameliorated ice‐free conditions prevailed in maritime regions, glaciers advanced through the Baltic and when interstadial regimes dominated the Baltic, glaciers expanded off the Norwegian coast. The largest glacier extent was reached in the North Sea around 29 kyr BP, about 22 kyr BP in Denmark and ca. 18 kyr BP in the Baltic. Our model provides new data for future numerical and qualitative landform‐based models. Copyright © 2003 John Wiley & Sons, Ltd.