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Volume 29 Issue 3
Aug 2018
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Journal of Earth Science  > 2018  >  29(3): 695-706.
Fuyuan An, Zhongping Lai, Xiangjun Liu, Yixuan Wang, Qiufang Chang, Baoliang Lu, Xiaoyun Yang. Luminescence Chronology and Radiocarbon Reservoir Age Determination of Lacustrine Sediments from the Heihai Lake, NE Qinghai-Tibetan Plateau and Its Paleoclimate Implications. Journal of Earth Science, 2018, 29(3): 695-706. doi: 10.1007/s12583-017-0972-9
Citation: Fuyuan An, Zhongping Lai, Xiangjun Liu, Yixuan Wang, Qiufang Chang, Baoliang Lu, Xiaoyun Yang. Luminescence Chronology and Radiocarbon Reservoir Age Determination of Lacustrine Sediments from the Heihai Lake, NE Qinghai-Tibetan Plateau and Its Paleoclimate Implications. Journal of Earth Science, 2018, 29(3): 695-706. doi: 10.1007/s12583-017-0972-9
shu

Luminescence Chronology and Radiocarbon Reservoir Age Determination of Lacustrine Sediments from the Heihai Lake, NE Qinghai-Tibetan Plateau and Its Paleoclimate Implications

doi: 10.1007/s12583-017-0972-9
  • 1.

    Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China

  • 2.

    Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China

  • 3.

    University of Chinese Academy of Sciences, Beijing 100049, China

  • 4.

    State Key Laboratory of Cryosphere Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China

  • 5.

    School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

  • 6.

    Department of Geology, Baylor University, Waco 76798, USA

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  • Corresponding author: Fuyuan An, dongzhu8@sina.com
  • Received Date: 24 Apr 2017
  • Accepted Date: 01 Sep 2017
  • Publish Date: 01 Jun 2018
    Abstract
  • The accurately determining the lake 14C reservoir age has a crucial significance for climatic reconstruction. In this study, the optically stimulated luminescence (OSL) dating method is employed to date samples from highstand lacustrine sediments, palaeoshoreline, fluvial terrace, and the alluvial fan of the Heihai Lake catchment. Accelerator mass spectrometry (AMS) 14C dating was also used to date fossil plants from highstand lacustrine sediments. Based on the calculations of linear regression with OSL against radiocarbon ages for same layers of two sections, the quantitative 14C reservoir ages were estimated to lie between 3 353 and 3 464 yr during the 1.8 to 2.4 ka, which showed temporal variation. The sources of old carbon are the dissolution of carbonate bedrocks distributed along the Kunlun Mountain. The OSL ages of the different members of the hydatogen sedimentary system at Heihai Lake catchment indicate that a stronger hydrologic condition occurred from 3.0±0.2 to 1.8±0.2 ka, with a maximum lake level of 9 m higher than present. This humid stage was widely recorded in different sediments on the QTP and Chinese Loess Plateau (CLP), indicating its broad synchronicity across the Asian Summer Monsoon region. The enhanced East Asian Summer Monsoon (EASM) and the Indian Summer Monsoon (ISM) resulted in the increase of moisture availability for the Heihai Lake area during this stage.

     

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