Sediment record of environmental change at Lake Lop Nur (Xinjiang, NW China) from 13.0 to 5.6 cal ka BP

Jingzhong Wang; Hongjuan Jia

doi:10.1007/s00343-017-6079-4

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Sediment record of environmental change at Lake Lop Nur (Xinjiang, NW China) from 13.0 to 5.6 cal ka BP

OriginalPaper | Updated：2023-05-16

- Sediment record of environmental change at Lake Lop Nur (Xinjiang, NW China) from 13.0 to 5.6 cal ka BP
- Sediment record of environmental change at Lake Lop Nur (Xinjiang, NW China) from 13.0 to 5.6 cal ka BP
- 海洋湖沼学报（英文） 2017年35卷第5期页码：1070-1078
- Affiliations：
  
  Experiment & Practice Teaching Center Heibei GEO University
- Author bio：
- Funds：
  
  Supported by the National Natural Science Foundation of China (No. 41271205) and the PhD Research Startup Foundation of Heibei GEO Univerity (No. BQ201604)
- DOI：10.1007/s00343-017-6079-4
  中图分类号：
- 网络首发：2016-09-29，
  
  纸质出版：2017
- Accepted：
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Sediment record of environmental change at Lake Lop Nur (Xinjiang, NW China) from 13.0 to 5.6 cal ka BP[J]. 海洋湖沼学报（英文）, 2017,35(5):1070-1078.

Wang, J., Jia, H. Sediment record of environmental change at Lake Lop Nur (Xinjiang, NW China) from 13.0 to 5.6 cal ka BP., Chin. J. Ocean. Limnol. 35, 1070–1078 (2017). https://doi.org/10.1007/s00343-017-6079-4
Sediment record of environmental change at Lake Lop Nur (Xinjiang, NW China) from 13.0 to 5.6 cal ka BP[J]. 海洋湖沼学报（英文）, 2017,35(5):1070-1078. DOI： 10.1007/s00343-017-6079-4.

Wang, J., Jia, H. Sediment record of environmental change at Lake Lop Nur (Xinjiang, NW China) from 13.0 to 5.6 cal ka BP., Chin. J. Ocean. Limnol. 35, 1070–1078 (2017). https://doi.org/10.1007/s00343-017-6079-4 DOI：

摘要

Abstract

Lake Lop Nur is located in the eastern part of the Tarim Basin in Xinjiang

northwestern China. A 220-cm-long sediment core was collected from the center of the ear-shaped depression forming the basin and dated with AMS14C. Grain size

total organic matter (TOC)

total nitrogen (TN)

and TOC/TN (C/N) analyses were used to reconstruct climatic conditions from 13.0 to 5.6 cal ka BP. The results showed five main climatic stages. Zone I (13.0–11.3 cal ka BP) was a wet–dry environment

whereas Zone II (11.3–8.9 cal ka BP) consisted of a primarily wet environment. Zone III (8.9–7.7 cal ka BP) was subdivided into Zone IIIa (8.9–8.2 cal ka BP) that indicated lake constriction and dry climate

and Zone IIIb (8.2–7.7 cal ka BP) in which the proxies indicated wet conditions. In Zone IV (7.7–6.6 cal ka BP)

the climate presented a bit wet conditions. In Zone V (6.6–5.6 cal ka BP)

abundant glauberite is present in the sediment and silt dominates the lithology; these results indicate the lake shrank and the overall climate was dry. Abrupt environmental events were also identified

including six dry events at 11.0

10.5

9.3

8.6

8.2

and 7.6 cal ka BP and one flood event from 7.8 to 7.7 cal ka BP in the Early–Middle Holocene.

关键词

Keywords

references

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