4.2 Article

Lake level reconstruction for 12.8-2.3 ka of the Ngangla Ring Tso closed-basin lake system, southwest Tibetan Plateau

期刊

QUATERNARY RESEARCH
卷 83, 期 1, 页码 66-79

出版社

CAMBRIDGE UNIV PRESS
DOI: 10.1016/j.yqres.2014.07.012

关键词

Tibetan Plateau; Holocene; Indian Summer Monsoon; Radiocarbon; U-Th series dating; Shoreline dating; Paleolake

资金

  1. Comer Science and Education Foundation
  2. Henry Luce Foundation
  3. NSF [1211299, 1103403, 0908792]
  4. Geological Society of America
  5. NSF-China [41101189]
  6. Div Atmospheric & Geospace Sciences
  7. Directorate For Geosciences [1103403] Funding Source: National Science Foundation
  8. Division Of Earth Sciences
  9. Directorate For Geosciences [1211299, 0908792] Funding Source: National Science Foundation

向作者/读者索取更多资源

We present a shoreline-based, millennial-scale record of lake-level changes spanning 12.8-23 ka for a large closed-basin lake system on the southwestern Tibetan Plateau. Fifty-three radiocarbon and eight U-Th series ages of tufa and beach cement provide age control on paleoshorelines ringing the basin, supplemented by nineteen ages from shell and aquatic plant material from natural exposures generally recording lake regressions. Our results show that paleo-Ngangla Ring Tso exceeded modern lake level (4727 m asp continuously between similar to 12.8 and 2.3 ka. The lake was at its highstand 135 m (4862 m asl) above the modem lake from 103 ka to 8.6 ka. This is similar to other closed-basin lakes in western Tibet, and coincides with peak Northern Hemisphere summer insolation and peak Indian Summer Monsoon intensity. The lake experienced a series of millennial-scale oscillations centered on 11.5, 10.8, 83, 5.9 and 3.6 ka, consistent with weak monsoon events in proxy records of the Indian Summer Monsoon. It is unclear whether these events were forced by North Atlantic or Indian Ocean conditions, but based on the abrupt lake-level regressions recorded for Ngangla Ring Tso, they resulted in significant periodic reductions in rainfall over the western Tibetan Plateau throughout the Holocene. (C) 2014 University of Washington. Published by Elsevier Inc All rights reserved.

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