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Geology; September 1997; v. 25; no. 9; p. 783-786; DOI: 10.1130/0091-7613(1997)025<0783:AOEFLQ>2.3.CO;2
© 1997 Geological Society of America
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Arctic Ocean evidence for late Quaternary initiation of northern Eurasian ice sheets

Robert F. Spielhagen1, Georges Bonani2, Anton Eisenhauer3, Martin Frank4, Thomas Frederichs5, Heidemarie Kassens1, Peter W. Kubik6, Augusto Mangini4, Niels Nøgaard Pedersen1, Norbert R. Nowaczyk7, Stefan Schäper4, Ruediger Stein8, Jörn Thiede1, Ralf Tiedemann1 and Monika Wahsner8

1 GEOMAR Research Center for Marine Geosciences, 24148 Kiel, Germany
2 Institute for Particle Physics, ETH Hönggerberg, 8093 Zürich, Switzerland
3 Geochemical Institute, Göttingen University, 37077 Göttingen, Germany
4 Heidelberg Academy of Sciences, 69120 Heidelberg, Germany
5 Department of Geosciences, University of Bremen, 28334 Bremen, Germany
6 Paul Scherrer Institute c/o Institute for Particle Physics, ETH Hönggerberg, 8093 Zürich, Switzerland
7 GeoForschungsZentrum Potsdam, 14473 Potsdam, Germany
8 Alfred-Wegener Institute for Polar and Marine Research, 27586 Bremerhaven, Germany

A high-resolution multiparameter stratigraphy allows the identification of late Quaternary glacial and interglacial cycles in a central Arctic Ocean sediment core. Distinct sandy layers in the upper part of the otherwise fine-grained sediment core from the Lomonosov Ridge (lat 87.5°N) correlate to four major glacials since ca. 0.7 Ma. The composition of these ice-rafted terrigenous sediments points to a glaciated northern Siberia as the main source. In contrast, lithic carbonates derived from North America are also present in older sediments and indicate a northern North American glaciation since at least 2.8 Ma. We conclude that large-scale northern Siberian glaciation began much later than other Northern Hemisphere ice sheets.




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