ZHANG Yongwei，TIAN Xu，XU Fangjian，et al. Provenance and environmental response of terrigenous debris in the southeastern continental shelf of Hainan Island since 7.8 kaBP[J]. Marine Geology & Quaternary Geology，2023，43(1)：27-36. DOI: 10.16562/j.cnki.0256-1492.2022073101
Citation: ZHANG Yongwei，TIAN Xu，XU Fangjian，et al. Provenance and environmental response of terrigenous debris in the southeastern continental shelf of Hainan Island since 7.8 kaBP[J]. Marine Geology & Quaternary Geology，2023，43(1)：27-36. DOI: 10.16562/j.cnki.0256-1492.2022073101
shu

Provenance and environmental response of terrigenous debris in the southeastern continental shelf of Hainan Island since 7.8 kaBP

  • 1.

    School of Geosciences, China University of Petroleum (Huadong), Qindao 266580, China

  • 2.

    Qingdao Marine Comprehensive Proving Ground Co., Ltd, Qingdao 266200, China

  • 3.

    College of Marine Geosciences, Ocean University of China, Qingdao 266100, China

  • 4.

    College of Marine Science, Hainan University, Haikou 570228, China

  • 5.

    Marine Geological Institute of Hainan Province, Haikou 570206, China

  • 6.

    Xiamen Seismic Survey Research Center, Xiamen 361021, China

More Information
  • Received Date: July 30, 2022
  • Revised Date: August 22, 2022
  • Accepted Date: August 22, 2022
  • Available Online: November 23, 2022
    Graphical Abstract
    • Abstract
  • Grain-size, bulk Rare Earth Element (REE), and heavy mineral analysis of Core X2 at southeastern Hainan Island were carried out. The provenances of terrigenous clasts and their environmental responses of this study area since 7.8 kaBP were discussed. Two endmembers were identified by grain-size endmember simulation. The EM1 endmember corresponded to the fine-grained material transported by the ocean current system, while the EM2 endmember corresponded to the coarse-grained material input from nearby rivers in Hainan Island; therefore, the two endmembers represented two different transport mechanisms. Results show that since 7.8 kaBP, the provenance of terrigenous detrital of Core X2 was relatively stable, mainly from Hainan Island. After 4 kaBP, the grain size, REE, and heavy mineral characteristic parameters of Core X2 had changed significantly, which has a good correspondence to the intensification of El Nino and Southern Oscillation (ENSO). It is speculated that the increase of rainfall caused by frequent ENSO events is the main reason for the enhancement of weathering degree in the study area. Compared with the characteristics of REE, the heavy mineral assemblages of Core X2 were more significantly affected by weathering and denudation in the source area. Therefore, study on heavy mineral index is suggested in the future study of environmental evolution.
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    • References (60)
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