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Volume 23 Issue 2
Apr 2012
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Article Contents
Hongjuan Jia, Xiaoguang Qin, Jiaqi Liu. Environmental Changes Recorded by Major Elements in Loulan Stupa Section during Early–Middle Holocene. Journal of Earth Science, 2012, 23(2): 155-160. doi: 10.1007/s12583-012-0240-y
Citation: Hongjuan Jia, Xiaoguang Qin, Jiaqi Liu. Environmental Changes Recorded by Major Elements in Loulan Stupa Section during Early–Middle Holocene. Journal of Earth Science, 2012, 23(2): 155-160. doi: 10.1007/s12583-012-0240-y

Environmental Changes Recorded by Major Elements in Loulan Stupa Section during Early–Middle Holocene

doi: 10.1007/s12583-012-0240-y
Funds:

the Key Consultation Project of Chinese Academy of Engineering 2008-ZD-05

the National Natural Science Foundation of China 40472094

the National Natural Science Foundation of China 40772212

National Project NP2010-033

More Information
  • Corresponding author: Hongjuan Jia, jhjzjw@sina.com
  • Received Date: 10 May 2011
  • Accepted Date: 26 Sep 2011
  • Publish Date: 01 Apr 2012
  • Holocene palaeoweathering conditions and environmental changes of Loulan (楼兰) Stupa Section were reconstructed by major elements analysis results and optical stimulated luminescence dating results. Major element results show source rock change little, with the composition equivalent to granodiorite. The low R value and high CIA (chemical index of alteration) value indicating the section at primary weathering phases. The muddy silt and silty clay have low R value and high CIA value and total iron content. In contrast, the sandy clay silt and sandy silt have high R value and low CIA and total iron value. Deglaciation time climate was relatively humid. In comparison to previous and posterior hiatus, the Middle-Holocene climate was relatively wet but still displayed high-frequency and high-amplitude fluctuations.

     

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