Assemblage characteristics of clay minerals and its implications to evolution of eolian dust input to the Parece Vela Basin since 1.95 Ma

Jie Ming; Anchun Li; Jie Huang; Shiming Wan; Qingyong Meng; Fuqing Jiang; Wenwen Yan

doi:10.1007/s00343-014-3066-x

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Assemblage characteristics of clay minerals and its implications to evolution of eolian dust input to the Parece Vela Basin since 1.95 Ma

OriginalPaper | Updated：2023-05-16

- Assemblage characteristics of clay minerals and its implications to evolution of eolian dust input to the Parece Vela Basin since 1.95 Ma
- Assemblage characteristics of clay minerals and its implications to evolution of eolian dust input to the Parece Vela Basin since 1.95 Ma
- 海洋湖沼学报（英文） 2014年32卷第1期页码：174-186
- Affiliations：
  
  1. Key Laboratory of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences
  2. University of Chinese Academy of Sciences
  3. First Institute of Oceanography State Oceanic Administration
- Author bio：
- Funds：
  
  Supported by the National Basic Research Program of China (973 Program) (No. 2007CB411703) and the National Natural Science Foundation of China (No. 40976026)
- DOI：10.1007/s00343-014-3066-x
  中图分类号：
- 网络首发：2014-02-21，
  
  纸质出版：2014
- Accepted：
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Assemblage characteristics of clay minerals and its implications to evolution of eolian dust input to the Parece Vela Basin since 1.95 Ma[J]. 海洋湖沼学报（英文）, 2014,32(1):174-186.

Ming, J., Li, A., Huang, J. et al. Assemblage characteristics of clay minerals and its implications to evolution of eolian dust input to the Parece Vela Basin since 1.95 Ma., Chin. J. Ocean. Limnol. 32, 174–186 (2014). https://doi.org/10.1007/s00343-014-3066-x
Assemblage characteristics of clay minerals and its implications to evolution of eolian dust input to the Parece Vela Basin since 1.95 Ma[J]. 海洋湖沼学报（英文）, 2014,32(1):174-186. DOI： 10.1007/s00343-014-3066-x.

Ming, J., Li, A., Huang, J. et al. Assemblage characteristics of clay minerals and its implications to evolution of eolian dust input to the Parece Vela Basin since 1.95 Ma., Chin. J. Ocean. Limnol. 32, 174–186 (2014). https://doi.org/10.1007/s00343-014-3066-x DOI：

摘要

Abstract

To understand the provenance and evolution of eolian input in the last 1.95 Ma in the Parece Vela Basin in the eastern Philippine Sea

the clay mineral assemblage of a gravity core PV090510 from the basin was investigated using paleogeomagnetic dating and X-ray diffraction. The assemblage of the core mainly consisted of smectite (∼46%) and illite (∼40%)

with some chlorite (∼10%) and kaolinite (∼4%). Analysis of the provenance of these minerals suggested that smectite was mainly derived from volcanic rocks of the Mariana Arc

while illite

chlorite

and kaolinite were mainly transported as eolian dust by the East Asian monsoon from central Asia. We used the ratio of (illite+chlorite+kaolinite)/smectite as a proxy for Asian eolian input to the Parece Vela Basin since 1.95 Ma. This ratio followed glacial and interglacial cycles and was consistent with the intensity of the East Asian monsoon and aridity of central Asia since 1.95 Ma. The changes of the ratio reflected three different stages of the East Asian monsoon and provenance climate.

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