Depositional history of the North Taymyr ice-marginal zone, Siberia - a landsystem approach

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Bibtex

@article{188dfd8f780340dda736454c2b141a0b,
title = "Depositional history of the North Taymyr ice-marginal zone, Siberia - a landsystem approach",
abstract = "The sediment-landform associations of the northern Taymyr Peninsula in Arctic Siberia tell a tale of ice sheets advancing from the Kara Sea shelf and inundating the peninsula, probably three times during the Weichselian. In each case the ice sheet had a margin frozen to its bed and an interior moving over a deforming bed. The North Taymyr ice-marginal zone (NTZ) comprises ice-marginal and supraglacial landsystems dominated by thrust-block moraines 2-3 km wide and large-scale deformation of sediments and ice. Large areas are still underlain by remnant glacier ice and a supraglacial landscape with numerous ice-walled lakes and kames is forming even today. The proglacial landsystem is characterised by subaqueous (e.g. deltas) or terrestrial (e.g. sandar) environments, depending on location/altitude and time of formation. Dating results (OSL, C-14) indicate that the NTZ was initiated ca. 80 kyr BP during the retreat of the Early Weichselian ice sheet and that it records the maximum limit of a Middle Weichselian glaciation (ca. 65 kyr BP). During both these events, proglacial lakes were dammed by the ice sheets. Part of the NTZ was occupied by a thin Late Weichselian ice sheet (20-12 kyr BP), resulting in subaerial proglacial drainage. Copyright (C) 2002 John Wiley Sons, Ltd.",
keywords = "glaciation, ice-marginal zone, landsystem, Weichselian, Siberia",
author = "Helena Alexanderson and Lena Adrielsson and Christian Hjort and Per M{\"o}ller and O Antonov and S Eriksson and M Pavlov",
year = "2002",
doi = "10.1002/jqs.677",
language = "English",
volume = "17",
pages = "361--382",
journal = "Journal of Quaternary Science",
issn = "1099-1417",
publisher = "John Wiley and Sons Inc.",
number = "4",

}