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TIAN Xu, HU Bangqi, WANG Feifei, HUANG Wei, DING Xue, SONG Weiyu, XU Fangjian. 2020. Clay mineral provenance and its response to paleochimate in the central Okinawa Trough since the last Deglaciation (19 ka)[J]. Geology in China, 47(5): 1501-1511. doi: 10.12029/gc20200515
Citation: TIAN Xu, HU Bangqi, WANG Feifei, HUANG Wei, DING Xue, SONG Weiyu, XU Fangjian. 2020. Clay mineral provenance and its response to paleochimate in the central Okinawa Trough since the last Deglaciation (19 ka)[J]. Geology in China, 47(5): 1501-1511. doi: 10.12029/gc20200515
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Clay mineral provenance and its response to paleochimate in the central Okinawa Trough since the last Deglaciation (19 ka)

  • 1.

    National Deep Sea Center, Qingdao 266237, Shandong, China

  • 2.

    Qingdao Institute of Marine Geology, China Geological Survey, Ministry of Natural Resources, Qingdao 266071, Shandong, China

  • 3.

    Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266071, Shandong, China

  • 4.

    School of Geosciences, China University of Petroleum, Qingdao 266580, Shandong, China

    • Fund Project: Supported by the National Natural Science Foundation of China (No.41976192, 41576058), the Open Foundation of the State Key Laboratory of Loess and Quatemary Geology (No. SKLLQG1707, SKLLQG1805), the Project of China Geological Survey (No. DD20191010, No. DD20160137).
More Information
  • Author Bio: TIAN Xu, male, bom in 1989, engineer, mainly engages in the study of marine sedimentology and mineralogy,E-mail:tianxuaq@163.com
  • Corresponding author: HU Bangqi, male, bom in 1983, associate researcher, mainly engages in the study of marine sedimentology, E-mail:bangqilu@gmail.com  
Received Date:  03 April 2020
Revised Date:  12 August 2020
Publish Date:  25 October 2020
    Abstract

  • In this paper, the authors discussed the clay mineral provenances and their environmental significance since the last Deglaciation on the basis of clay minerals and AMS14C dating analysis carried out for Core CS2, which was located in the central Okinawa Trough. The results show that Core CS2 mainly consists of illite and lesser amounts of chlorite, with associated kaolinite and smectite. Downcore variability of clay mineral content allows Core CS2 to be divided into three units. The sediments were primarily derived from Changjiang with lesser amounts from Huanghe and Taiwan in unit 1 (19-12 ka BP) and unit 2 (12-8 ka BP), which was mainly controlled by sea level change. In unit 3 (8- 0 ka BP), the sediments were primarily derived from Changjiang and Taiwan, with lesser amounts from Huanghe, which was mainly controlled by Kuroshio evolution. The ratios of (smectite+ kaolinite)/(illite+chlorite) at CS2 were adopted as proxies for East Asian monsoon evolution. The consistent variation of this clay proxy with those from Sanbao Cave δ18O and GISP2 δ18O shows that two profound shifts of the East Asian winter monsoon intensity and the intensity of winter monsoon relative to summer monsoon occurred at 16.4-14.8 ka BP and12.8-11.6 ka BP.

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