Sedimentary facies and evolution of aeolianites on Shidao Island, Xisha Islands

Qiang Zhao; Shiguo Wu; Hong Xu; Qiliang Sun; Bin Wang; Yunbao Sun; Fei Cao; Xiaosu He

doi:10.1007/s00343-011-0018-6

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Sedimentary facies and evolution of aeolianites on Shidao Island, Xisha Islands

OriginalPaper | Updated：2023-05-16

- Sedimentary facies and evolution of aeolianites on Shidao Island, Xisha Islands
- Sedimentary facies and evolution of aeolianites on Shidao Island, Xisha Islands
- 海洋湖沼学报（英文） 2011年29卷第2期页码：398-413
- Affiliations：
  
  1. Key Laboratory of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences
  2. Graduate University of Chinese Academy of Sciences
  3. Key Laboratory of Marine Resources and Environmental Geology Qingdao Institute of Marine Geology Ministry of Land and Resources
  4. Hangzhou Research Institute of Petroleum Geology CNPC
  5. China University of Geosciences
- Author bio：
- Funds：
  
  Supported by the National Basic Research Program of China (973 Program) (No. 2009CB219406), the Knowledge Innovation Program of CAS (KZCX2-YW-229), and National Science & Technology Major Project (No. 2008zx05025-003-03)
- DOI：10.1007/s00343-011-0018-6
  中图分类号：
- 网络首发：2011-03-02，
  
  纸质出版：2011
- Accepted：
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Sedimentary facies and evolution of aeolianites on Shidao Island, Xisha Islands[J]. 海洋湖沼学报（英文）, 2011,29(2):398-413.

Zhao, Q., Wu, S., Xu, H. et al. Sedimentary facies and evolution of aeolianites on Shidao Island, Xisha Islands., Chin. J. Ocean. Limnol. 29, 398–413 (2011). https://doi.org/10.1007/s00343-011-0018-6
Sedimentary facies and evolution of aeolianites on Shidao Island, Xisha Islands[J]. 海洋湖沼学报（英文）, 2011,29(2):398-413. DOI： 10.1007/s00343-011-0018-6.

Zhao, Q., Wu, S., Xu, H. et al. Sedimentary facies and evolution of aeolianites on Shidao Island, Xisha Islands., Chin. J. Ocean. Limnol. 29, 398–413 (2011). https://doi.org/10.1007/s00343-011-0018-6 DOI：

摘要

Abstract

The aeolianite deposits on Shidao Island of the Xisha Islands

the South China Sea

contain five stages of aeolian biocalcarenites and four paleosols. The aeolian biocalcarenites consist of two sedimentary facies: dune and interdune deposits. In the dunes

large-scale festoon cross-bedding

humped cross-bedding and high-angle foreset bedding are well developed

and in the interdunes

large-scale flat-bedding and low-angle wedge shaped cross-bedding are well developed. The sedimentary structures and lamella features indicate that the aeolian deposits are driven mainly by the northeast monsoon. The aeolian biocalcarenite and paleosols may reflect the arid and humid climates of the East Asian monsoon

respectively. By comparison with the stalagmite oxygen isotope climosequence of Hulu Cave

Nanjing

we inferred that the aeolianite formed in the last glacial stage

and the paleosols were formed during relatively long-term warm events.

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Keywords

references

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