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Extensive glaciation in Transbaikalia, Siberia, at the Last Glacial Maximum
Stockholm University, Faculty of Science, Department of Physical Geography.
Stockholm University, Faculty of Science, Department of Physical Geography.
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Number of Authors: 8
2016 (English)In: Quaternary Science Reviews, ISSN 0277-3791, E-ISSN 1873-457X, Vol. 132, 161-174 p.Article in journal (Refereed) Published
Abstract [en]

Successively smaller glacial extents have been proposed for continental Eurasia during the stadials of the last glacial period leading up to the Last Glacial Maximum (LGM). At the same time the large mountainous region east of Lake Baikal, Transbaikalia, has remained unexplored in terms of glacial chronology despite clear geomorphological evidence of substantial past glaciations. We have applied cosmogenic Be-10 exposure dating and optically stimulated luminescence to establish the first quantitative glacial chronology for this region. Based on eighteen exposure ages from five moraine complexes, we propose that large mountain ice fields existed in the Kodar and Udokan mountains during Oxygen Isotope Stage 2, commensurate with the global LGM. These ice fields fed valley glaciers (>100 km in length) reaching down to the Chara Depression between the Kodar and Udokan mountains and to the valley of the Vitim River northwest of the Kodar Mountains. Two of the investigated moraines date to the Late Glacial, but indications of incomplete exposure among some of the sampled boulders obscure the specific details of the post-LGM glacial history. In addition to the LGM ice fields in the highest mountains of Transbaikalia, we report geomorphological evidence of a much more extensive, ice-cap type glaciation at a time that is yet to be firmly resolved.

Place, publisher, year, edition, pages
2016. Vol. 132, 161-174 p.
Keyword [en]
Glaciation, Transbaikalia, Last Glacial Maximum, Cosmogenic Be-10 exposure dating, Optically stimulated luminescence
National Category
Earth and Related Environmental Sciences
URN: urn:nbn:se:su:diva-127278DOI: 10.1016/j.quascirev.2015.11.018ISI: 000368956900011OAI: diva2:943792
Available from: 2016-06-28 Created: 2016-03-01 Last updated: 2016-06-28Bibliographically approved

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Margold, Martin
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