History of late Pleistocene glaciations in the central Sayan-Tuva Upland (southern Siberia)

This work describes the history of late Pleistocene glaciations in the central Sayan-Tuva Upland (southern Siberia). Geological and geomorphological analysis as well as 10Be surface-exposure dating revealed the glacier fluctuations in this continental area. The available published data show that the...

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Bibliographic Details
Published in:Quaternary science reviews 2012-08, Vol.49, p.16-32
Main Authors: Arzhannikov, Sergei G., Braucher, Regis, Jolivet, Marc, Arzhannikova, Anastasia V., Vassallo, Riccardo, Chauvet, Alain, Bourlès, Didier, Chauvet, Frédéric
Format: Article
Language:English
Subjects:
Cosmogenic 10Be
Earth Sciences
East Sayan Ridge
Glaciology
Late Pleistocene glaciations
Moraines
Sciences of the Universe
Southern Siberia
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Summary:This work describes the history of late Pleistocene glaciations in the central Sayan-Tuva Upland (southern Siberia). Geological and geomorphological analysis as well as 10Be surface-exposure dating revealed the glacier fluctuations in this continental area. The available published data show that the glaciers were formed in the MIS 6 and probably survived in the MIS 5. Data are also available concerning glacial advances in different periods of MIS 4, MIS 3 and MIS 2. ELAs were 2030–2230 m. Two distinct 10Be exposure ages groups are highlighted reflecting the time of formation of glacial deposits in the MIS 2 associated to the Big Sayan Ridge outlet glaciers. The Sentsa – Sailag group (terminal moraine) has a mean exposure age of 16.44 ± 0.38 ka. The Jombolok (terminal moraine) – Jombolok (outwash plain) group has a mean exposure age of 22.80 ± 0.56 ka. The last glaciation that occurred at MIS 2 is characterized by the absence of ice cap on the Azas volcanic Plateau and of ice field in the Todza Basin. The thickness of the valley glacier was 300–400 m. At MIS 2, the terminal moraines were ∼1300–1400 m a.s.l. in the Tissa, Sentsa, Jombolok and Sailag river valleys. ► The 10Be-dating has been undertaken in glacial deposits of the East Sayan Ridge. ► Mean exposure ages of 16.44 ± 0.38 and 22.8 ± 0.56 ka were obtained for terminal moraine. ► Glaciers formed prior to MIS 5 and advanced in MIS 4, MIS 3 and MIS 2. ► Late Pleistocene ELAs were 2030–2230 m.
ISSN:0277-3791
1873-457X
DOI:10.1016/j.quascirev.2012.06.005