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Environmental Earth Sciences

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01.05.2012 | Original Article

Late Pleistocene lake and glaciation evolution on the northeastern Qinghai–Tibetan Plateau: a review

verfasst von: QiShun Fan, HaiZhou Ma, GuangLiang Hou

Erschienen in: Environmental Earth Sciences | Ausgabe 2/2012

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Abstract

Late Pleistocene paleoclimatic history on northeastern Qinghai–Tibetan Plateau (QTP) has been reconstructed mainly from lake sediments; however, data regarding dry–wet climate changes reported in this region are still not clear and controversial. Based on shoreline features and highstand lacustrine sediments around lakes on the QTP, high lake level histories in this paper were summarized and compared with paleoclimatic records from lake sediments, ice core and glaciation evolution surrounding mountains on the NE QTP during late Pleistocene. The results indicate that periods of high lake level occurred at MIS 5, MIS 3 and early-middle Holocene and most likely corresponding to warm and wet climate periods, while periods of low lake level existed in intervening intervals, corresponding to cold and dry climate periods, which most likely coincide with glacial advances surrounding high mountains. With an exception, no wide glacial advance in study area was found during MIS 3, possibly suggesting that effective moisture is lower than that in the other region of NE QTP in this period.

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Titel: Late Pleistocene lake and glaciation evolution on the northeastern Qinghai–Tibetan Plateau: a review
verfasst von: QiShun Fan
HaiZhou Ma
GuangLiang Hou
Publikationsdatum: 01.05.2012
Verlag: Springer-Verlag
Erschienen in: Environmental Earth Sciences / Ausgabe 2/2012
Print ISSN: 1866-6280
Elektronische ISSN: 1866-6299
DOI: https://doi.org/10.1007/s12665-011-1271-x

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