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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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