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...

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Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Berger, Glenn W., Melles, Martin, Banerjee, Debabrata, Murray, Andrew S., Raab, Alexandra
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2004
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