Volume 44 Issue 8
Aug.  2019
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Chen Hongjin, Xu Zhaokai, Cai Mingjiang, Li Tiegang, 2019. Provenance of Clay-Sized Detrital Sediments and Its Paleoenvironmental Implications at Site U1456 in the Eastern Arabian Sea since 30 ka. Earth Science, 44(8): 2803-2817. doi: 10.3799/dqkx.2018.185
Citation: Chen Hongjin, Xu Zhaokai, Cai Mingjiang, Li Tiegang, 2019. Provenance of Clay-Sized Detrital Sediments and Its Paleoenvironmental Implications at Site U1456 in the Eastern Arabian Sea since 30 ka. Earth Science, 44(8): 2803-2817. doi: 10.3799/dqkx.2018.185
shu

Provenance of Clay-Sized Detrital Sediments and Its Paleoenvironmental Implications at Site U1456 in the Eastern Arabian Sea since 30 ka

doi: 10.3799/dqkx.2018.185
  • 1.

    Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

  • 2.

    University of Chinese Academy of Sciences, Beijing 100049, China

  • 3.

    Laboratory of Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China

  • 4.

    Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanology, SOA, Qingdao 266061, China

  • Received Date: 2019-01-18
  • Publish Date: 2019-08-15
    Abstract
  • AMS 14C dating, clay minerals, major elements and grain size at site U1456 from International Ocean Discovery Program were analyzed, in order to constrain the source-to-sink processes of clay-sized detrital sediments and their paleoenvironmental significance in the eastern Arabian Sea. The clay mineral assemblages at site U1456 since 30 ka are dominated by smectite and illite, with minor chlorite and kaolinite. Provenance analysis results suggest that clay-sized detrital sediments are primarily derived from the Indus River and Deccan Trap. Southwest Asian monsoon probably is the main factor affecting the weathering and erosion in the western Himalaya and the Indian subcontinent since 30 ka. Relatively reduced contribution from the Indus River to the study area during weak southwest Asian monsoon intervals should correlate with the southward migration of the Intertropical Convergence Zone and the extension of glacial cover over the Himalayas during the Last Glacial Maximum, and thus reduction in the Indus River runoff as well as available exposure area for erosion and weathering over the Himalayas. The weathering and erosion on the continent revealed by K/Al ratio show coherent variations to the previous southwest Asian monsoon records, indicating the efficiency of K/Al ratio for tracking the regional climate signal in the eastern Arabian Sea since the late Quaternary.

     

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