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

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 movin...

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Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Alexanderson, Helena, Adrielsson, Lena, Hjort, Christian, Möller, Per, Antonov, O, Eriksson, S, Pavlov, M
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley & Sons Inc. 2002
Subjects:
Geology
glaciation
ice-marginal zone
landsystem
Weichselian
Siberia
Arctic
Kara Sea
Sandar
Taymyr
Ice Sheet
Taymyr Peninsula
Online Access:https://lup.lub.lu.se/record/332267
https://doi.org/10.1002/jqs.677
Description
Summary: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.

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