CHEN Haitao, KONG Fanbiao, XU Shujian, LOU Zhaojun, ZHANG Junqiang. Geochemical characteristics of major elements and their paleoenvironmental significance of the Xianjingyuan loess in Shandong Province[J]. Marine Geology & Quaternary Geology, 2020, 40(6): 189-197. DOI: 10.16562/j.cnki.0256-1492.2020060803
Citation: CHEN Haitao, KONG Fanbiao, XU Shujian, LOU Zhaojun, ZHANG Junqiang. Geochemical characteristics of major elements and their paleoenvironmental significance of the Xianjingyuan loess in Shandong Province[J]. Marine Geology & Quaternary Geology, 2020, 40(6): 189-197. DOI: 10.16562/j.cnki.0256-1492.2020060803
shu

Geochemical characteristics of major elements and their paleoenvironmental significance of the Xianjingyuan loess in Shandong Province

  • 1.

    College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China

  • 2.

    Shandong Provincial Key Laboratory of Water and Soil Conservation and Environmental Protection, College of Resources and Environment, Linyi University, Linyi 276000, China

  • 3.

    School of Geography and Environment, Shandong Normal University, Jinan 250014, China

  • 4.

    Changdao County Natural Resources Bureau, Yantai 265800, China

  • 5.

    Institute of Geology and Paleontology, Linyi University, Linyi 276000, China

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  • Received Date: June 07, 2020
  • Revised Date: August 04, 2020
  • Available Online: December 17, 2020
    Graphical Abstract
    • Abstract
  • The loess deposited in the Miaodao Islands has great significance to the revealing of paleoclimatic and paleoenvironmental changes. In this study, we analyzed the compositional characteristics of the major elements of the Xianjingyuan loess on the Nanchangshan island. Combined with the chemical weathering indexes and integrated elemental parameters, we discussed in this paper the characteristics and intensity of chemical weathering and climate changes during the accumulation of Xianjingyuan loess. Also made are comparisons to the Tuoji loess, Pingyin loess and Luochuan loess-palaeosol. It is revealed that: (1) The Xianjingyuan loess is dominated by the major elements of SiO2, Al2O3 and CaO, and the abundance of major elements are in an order of SiO2＞Al2O3＞CaO＞TFe2O3＞K2O＞Na2O＞MgO＞TiO2＞P2O5＞MnO; (2) Chemical weathering indicators indicated that the Xianjingyuan loess was in an initial stage of chemical weathering; and the integrated element parameters suggest that the region had experienced five times of climatic change from warm and humid to cold and dry, and the climate environment of Xianjingyuan has a good response to the global climate environment; (3) The dust sources and the paleoclimate environment are highly similar to the loess found in Shandong Province, but the regional environment was effected by geographic location and topographic conditions, the obvious difference between Xianjingyuan loess and Pingyin loess suggest that there is difference in dust sources; (4) the difference between the major elements and chemical weathering in Xianjingyuan loess and Luochuan loess-palaeosol owes its origin to the difference of dust sources.
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    • References (48)
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