Late Cenozoic history of the Scandinavian and Barents Sea ice sheets

• Published in: Global and planetary change 1996-03, Vol.12 (1), p.11-26
• Main Authors: Mangerud, Jan, Jansen, Eystein, Landvik, Jon Y.
• Format: Article
• Language: English
• Subjects: Marine
• ISSN: 0921-8181; 1872-6364
• DOI: 10.1016/0921-8181(95)00009-7

The oldest ice rafted material (IRD) on the Vøring Plateau is dated to about 11 Ma, and is regarded as evidence that glaciers extended to sea level somewhere around the Nordic Sea at this time. We estimate that the major glaciations of Scandinavia and the Barents Sea-Svalbard area started at 2.5–2.8 Ma, when the amount of IRD on the Vøring Plateau increased strongly, the deep sea δ 18O curves indicate that onset of Northern Hemisphere glaciations, and the climate in The Netherlands was so cold that a major glaciation of Scandinavia is inferred. Most of the time until 0.9 Ma, the ice sheets were of intermediate size; they probably reached the coastal zone of western Norway for long periods. The center of glaciation is inferred to have been further north than during the later glaciations, and we speculate that this was the period of maximum glacial erosion of the Barents Sea. The largest glaciations, and also the warmest interglacials occurred during the last 900 kyrs, when the 100 kyr astronomic cycle became important. For the last glaciation, the Weichselian, the glacial fluctuations are known in greater detail both for Scandinavia and the Svalbard-Barents Sea region. In Scandinavia the glacial fluctuations apparently followed the 23 kyr precession cycle, whereas in the Barents Sea they followed the 41 kyr tilt cycle. In both areas more than one advance reached beyond the coast. We use the Weichselian record to “calibrate” the interpretation of more indirect evidences of glacial fluctuations, and apply the latter to the Scandinavian and Barents Sea glacial history since 2.5 Ma.