|Table of Contents|

Grain Size Characteristics of Sediments in the Southeastern Margin of Mu Us Desert, China and Their Implication for Environmental Change During the Late Holocene(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2023年第06期
Page:
1285-1298
Research Field:
环境与可持续发展
Publishing date:

Info

Title:
Grain Size Characteristics of Sediments in the Southeastern Margin of Mu Us Desert, China and Their Implication for Environmental Change During the Late Holocene
Author(s):
JIA Fei-fei XU Cheng-lin ZHANG Jian-wei SUN Ru
(School of Geographical Sciences, Liaoning Normal University, Dalian 116029, Liaoning, China)
Keywords:
Late Holocene environmental change sandy sediment aeolian activity grain size characteristic end-member analysis OSL dating Mu Us Desert
PACS:
K903; P532
DOI:
10.19814/j.jese.2023.05035
Abstract:
The Mu Us Desert, located in the edge of the East Asian monsoon region in China, is an ideal place to study the changes in paleoclimate and environment because of its sensitivity to climate change. The sedimentary strata with a thickness of 273 cm in the southeastern margin of Mu Us Desert were used to reconstruct the environmental change process since 2.6 ka B.P. in the study area by analyzing the grain size end-member characteristics of sediment and environmental indication significance, and combined with optically stimulated luminescence(OSL)dating results and magnetic susceptibility indicators. The results show that ① the grain size composition of sediment is mainly composed of coarse silt, very fine sand and fine sand, among which the fine sand volume fraction is the most with an average of 57.29%; the fine sand volume fraction of the silty sand layer is significantly lower than that of the sand layer, and the coarse silt and very fine sand increase significantly; the grain size frequency distribution curves of sediments mostly show typical characteristics of aeolian sediments with high and narrow peaks and good sorting. ② The sediment grain size can be divided into three end-member components; EM1 is the finest end-member component, indicating a short-term strong dust storm activity; EM2 and EM3 are saltation subcomponents transported under different wind dynamic conditions; EM3 indicates the intensity of local aeolian activity. ③ The environmental change process of Late Holocene in study area can be divided into three stages. Before 2.6 ka B.P., the winter monsoon is strong and the climate is cold and dry; after 2.6 ka B.P., the winter monsoon weakens and the climate tends to be warm and humid; in the past century, wind-sand activities are enhanced, and human activities have a greater impact.

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Last Update: 2023-12-01