Qinghai lake fluctuation and climatic change singce the last glaciation

Wang Sumin; Wang Yunfei; Wu Ruijin; Li Jianren

doi:10.1007/BF02850676

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Qinghai lake fluctuation and climatic change singce the last glaciation

OriginalPaper | Updated：2023-05-16

- Qinghai lake fluctuation and climatic change singce the last glaciation
- Qinghai lake fluctuation and climatic change singce the last glaciation
- 海洋湖沼学报（英文） 1991年9卷第2期页码：170-183
- Affiliations：
  
  Nanjing Institute of Geography and Limnology Academia Sinica
- Author bio：
- Funds：
  
  14;C dating data in the paper were measured by the Laboratory of Loess and Quaternary Geology, Academia Sinica.
- DOI：10.1007/BF02850676
  中图分类号：
- 纸质出版：1991
- Accepted：
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Qinghai lake fluctuation and climatic change singce the last glaciation[J]. 海洋湖沼学报（英文）, 1991,9(2):170-183.

Sumin, W., Yunfei, W., Ruijin, W. et al. Qinghai lake fluctuation and climatic change singce the last glaciation., Chin. J. Ocean. Limnol. 9, 170–183 (1991). https://doi.org/10.1007/BF02850676
Qinghai lake fluctuation and climatic change singce the last glaciation[J]. 海洋湖沼学报（英文）, 1991,9(2):170-183. DOI： 10.1007/BF02850676.

Sumin, W., Yunfei, W., Ruijin, W. et al. Qinghai lake fluctuation and climatic change singce the last glaciation., Chin. J. Ocean. Limnol. 9, 170–183 (1991). https://doi.org/10.1007/BF02850676 DOI：

摘要

Abstract

Qinghai Lake is located in a hydrologically closed basin at the conjunction of SE and SW monsoons and westerlies. Its frequent lake level fluctuations arising from climatic and monsoonal changes have left a series of geological records since the last glaciation. The coarse sediments in Core QD1

the sporopollen assemblage representing steppe

the eolian paleo-sanddunes in the east and southeast banks and the fossil glacial topography all indicated frigid and arid climatic conditions and large scale shrinkage of the lake during the last glacial maximum.

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references

Chen Kezao et al., 1985. The preliminary study on sedimentary characteristics and paleoclimatic evolution of Charhan salt lake. Qaidam Basin,Scientia Sinica (Series B).5: 463–473.

Du Naiqiu and Kong Zhaochen, 1989. A preliminary investigation of the vegetational and climatic changes since 11 000 years in Qinghai Lake—An analysis based on palynology in Core QH 85-14 C.Acta Botanica Sinica,31: 803–814. (in Chinese)

Servant, M. and S. Servant, 1983. The lacustrine environment and its evolution in “Lake Chad”. Edited by Carmouze, J. P. et al. Dr. W. Junk Publisher, pp. 11–26.

The Lop Nur Lake Expedition, Xinjiang Branch of Academia Sinica, 1987. “Scientific Investigation and Research on Lop Nur Lake. Science Press pp. 1–325 (in Chinese).

Wang Fubao, 1987. Climatic change in Qinghai-Xizang (Tibet) region of China during the Holocene.Quaternary Research.28: 50–60

Zhang Pengxi, 1988. The evolution of the water body environment in Qinghai Lake since the postglacial age.Acta Sedimentologica Sinica 6(2): 1–14. (in Chinese)

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