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- W2392587580 abstract "The eolian-sand section along the Great Wall in Yulin,Shaanxi province,is sensitive to climate and environmental changes.The magnetic susceptibility and particle-size analysis in Dabaodang profile showed that the early Holocene(11 500~10 000 a BP),was a transition during the change in eolian regime and dust source because of the weakened northwesterly monsoon along with the global climatic amelioration;the middle Holocene(10 000~4 500 a BP) was relatively humid,while vegetation coverage increased,aeolian activities weakened,silt and clay compositions were significantly increased,weathering pedogenesis was enhanced,and sandy weak paleosols were developed;the late stage of the middle Holocene(4 500~3 000 a BP) was mild and humid in general,but at 4 200~4 000 a BP an arid climate event occurred,with intensive eolian sand activities;the climate was droughty and fluctuating frequently in recent 3 000 a,while eolian sand was significantly coarser,which showing 5 times desert expansions.Natural factors played an important role in the environmental changes in this area,and human activities greatly strengthened and amplified the changes at the modern times." @default.
- W2392587580 created "2016-06-24" @default.
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- W2392587580 date "2010-01-01" @default.
- W2392587580 modified "2023-09-24" @default.
- W2392587580 title "Holocene Climate and Environmental Changes in the Eolian Sand Section of Yulin,Shaanxi Province" @default.
- W2392587580 hasPublicationYear "2010" @default.
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