Luminescence chronology of non‐glacial sediments in Changeable Lake, Russian High Arctic, and implications for limited Eurasian ice‐sheet extent during the LGM
Abstract A 10.5 m core from Changeable Lake in the Severnaya Zemlya Archipelago just north of the Taymyr Peninsula intersects ca. 30 cm of diamicton at its base, interpreted as a basal till. Because the upper 10.13 m of this core consists of non‐glacial sediments, a maximum numeric age for these non...
Published in: | Journal of Quaternary Science |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2004
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Subjects: | |
Online Access: | http://dx.doi.org/10.1002/jqs.847 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.847 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.847 |