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《Scientia Geographica Sinica》 2005-04
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Holocene Environmental Change of Pedogenensis in the Middle Reaches of the Jinghe River Basin

Mao Long-Jiang ~(1,2),Huang Chun-Chang~2,Pang Jiang-Li~2(1.Ministry of Education Laboratory for Coast and Island Development,Nanjing University,Nanjing,Jiangsu 210093;2.Department of Tourism and Environment,Research Center for Historical Environment,Socio-Economic Development,Shannxi Normal University,Xi'an,Shannxi 710062)  
Magnetic susceptibility,Total Fe,total organic carbon(TOC), CaCO_3 and Rb,Sr,Rb/Sr measurement in the Holocene in this region,have revealed the characteristics of the environmental change of pedogenensis during late 11 500 years,and human activities of the Predynastic Zhou had some influence on the pedogenensis.The results show that dust deposition was reduced because of the climate warming,and the biological weathering is beginning in the early stage of the Holocene.Between 8500-3100 a B.P.,pedogenic process was very strong.A layer of Heilu soil was formed on this region.From 3100 a B.P.,soil degradation is remarkable.A layer of Loess has been accumulated since 3100 a B.P.,which has the Heilu soil buried.This means that the last 3100 years is the dry period with intensified dust accumulation and soil degradation.The cultivating layer of the Predynastic Zhou(180-150cm) was corresponding with the late Holocene Climate Optimum(3350-3100 a B.P.).Monsoon transformation has led to climate aridity and soil degradation from 3100 a B.P.,which was the dynamic force of the southward migration of nomads from the steppe of the northern Loess Plateau and the Mongolia Plateau,and the people of the Predynastic Zhou of arable farming community was forced to move south to the Guanzhong Basin,and established their capital city "Qiyi" on the Zhouyuan loess tableland.
【Fund】: 教育部人文社会科学重点研究基地重大项目(01JDAZ770014);; 国家社会科学基金项目(04BZS022)
【CateGory Index】: X144;
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