Glacial and palaeoenvironmental history of the Cape Chelyuskin area, Arctic Russia Per Möller1, Grigorij Fedorov2, Maxim Pavlov2, Marit-Solveig Seidenkrantz3 & Charlotte Sparrenbom4 1 Quaternary Sciences, Dept. of Geology, GeoBiosphere Science Centre, Lund University, Sölvegatan 12, SE-22362 Lund, Sweden 2 Arctic and Antarctic Research Institute, 38 Bering Street, RU-199397 St. Petersburg, Russia 3 Dept. of Earth Science, University of Aarhus, Høegh-Guldbergs Gade 2, DK-8000 Århus, Denmark 4 Swedish Geotechnical Institute, Hospitalsgatan 16A, SE-21133 Malmö, Sweden Keywords Abstract Eemian; glacial geology; glacial stratigraphy; Kara Sea ice sheet; Siberia. Quaternary glacial stratigraphy and relative sea-level changes reveal at least two glacial expansions over the Chelyuskin Peninsula, bordering the Kara Sea Correspondence at about 77°N in the Russian Arctic, as indicated from tills interbedded with Per Möller, Quaternary Sciences, Dept. of marine sediments, exposed in stratigraphic superposition, and from raised- Geology, GeoBiosphere Science Centre, Lund beach sequences mapped to altitudes of at least up to ca. 80 m a.s.l. University, Sölvegatan 12, SE-22362 Lund, Chronological control is provided by accelerator mass spectrometry 14C dating, Sweden. E-mail:
[email protected] electron-spin resonance and optically stimulated luminescence geochronology. doi:10.1111/j.1751-8369.2008.00066.x Major glaciations, followed by deglaciation and marine inundation, occurred during marine oxygen isotope stages 6–5e (MIS 6–5e) and stages MIS 5d–5c. These glacial sediments overlie marine sediments of Pliocene age, which are draped by fluvial sediment of a pre-Saalian age, thereby forming palaeovalley/ basin fills in the post-Cretaceous topography. Till fabrics and glacial tectonics record expansions of local ice caps exclusively, suggesting wet-based ice cap advance, followed by cold-based regional ice-sheet expansion.