Response of dune mobility and pedogenesis to fluctuations in monsoon precipitation and human activity in the Hulunbuir dune field, northeastern China, since the last deglaciation
Zeng, Lin; Yi, Shuangwen; Lu, Huayu; Chen, Yingyong; Lei, Fang; Xu, Zhiwei; Wang, Xianyan; Zhang, Wenfang
刊名GLOBAL AND PLANETARY CHANGE
2018-09
卷号168页码:1-14
关键词Dune activity OSL dating Hulunbuir dune field East Asian monsoon human activity
ISSN号0921-8181
DOI10.1016/j.gloplacha.2018.06.001
产权排序[Zeng, Lin] Chinese Acad Sci, Inst Soil Sci, Nanjing 210008, Jiangsu, Peoples R China ; [Zeng, Lin] Chinese Acad Sci, Key Lab Coastal Environm Proc & Ecol Remediat, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China ; [Zeng, Lin ; Yi, Shuangwen ; Lu, Huayu ; Lei, Fang ; Xu, Zhiwei ; Wang, Xianyan] Nanjing Univ, Sch Geog & Ocean Sci, Nanjing 210023, Jiangsu, Peoples R China ; [Chen, Yingyong] Henan Univ, Coll Environm & Planning, Kaifeng 475004, Peoples R China ; [Zhang, Wenfang] Chinese Acad Sci, State Key Lab Lake Sci & Environm, Nanjing Inst Geog & Limnol, Nanjing 210008, Jiangsu, Peoples R China
文献子类Article
英文摘要The Hulunbuir dune field is located at the northern margin of the temperate monsoon zone in East Asia, and changes in dune activity and pedogenesis in the dune field are highly sensitive to the advance and retreat of the East Asian summer monsoon (EASM) and to human activity. Thus, the stratigraphic sequences of paleosol and aeolian sand of the dune field have great potential for reconstructing the history of dune activity and pedogenesis and their response to past fluctuations in monsoon precipitation and the intensity of human activity. However, our knowledge of the evolution of the landscape and paleoclimate of the dune field is limited. Here, we present the results of analyses of quartz optically stimulated luminescence (OSL), grain size and magnetic susceptibility (MS) from 13 representative sections in the Hulunbuir dune field. The grain-size analysis indicates that the sand layers are composed of typical aeolian sand, and the MS variations of the aeolian sand and sandy paleosol sequences mainly reflect changes in the intensity of pedogenesis. We combine our new OSL dating results with previously published OSL ages to refine the chronology of sand dune development. An OSL age hiatus in both aeolian sand and paleosol during the 5-7 ka indicates that aeolian deposition in Hulunbuir ceased almost completely during this period, which corresponds to the peak in EASM strength. Thus, our study provides new evidence for a delayed response of the EASM maximum to peak insolation forcing (11-10 ka) in the mid-latitude monsoon margin. In addition, we speculate that peaks in probability density (PD) from 1.2-0.7 ka and from 0.25-0 ka of aeolian sand accumulation correspond to population increases and the development of cultivation and animal husbandry in the Hulunbuir dune field.
WOS关键词EAST-ASIAN MONSOON ; HOLOCENE ENVIRONMENTAL-CHANGES ; REGENERATIVE-DOSE PROTOCOL ; GRAIN-SIZE CHARACTERISTICS ; CENTRAL INNER-MONGOLIA ; NORTH-CENTRAL CHINA ; LATE QUATERNARY ; GLACIAL MAXIMUM ; LOESS PLATEAU ; MU-US
WOS研究方向Geography, Physical ; Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000440882300001
资助机构Global Change Program of Ministry of Science and Technology of China [2016YFA0600503] ; National Natural Science Foundation of China [41690111, 41472138, 41701263] ; China Postdoctoral Science Foundation [2017M611942, 2017M611943]
内容类型期刊论文
源URL[http://ir.yic.ac.cn/handle/133337/24517]  
专题烟台海岸带研究所_中科院海岸带环境过程与生态修复重点实验室
作者单位1.Henan Univ, Coll Environm & Planning, Kaifeng 475004, Peoples R China;
2.Chinese Acad Sci, State Key Lab Lake Sci & Environm, Nanjing Inst Geog & Limnol, Nanjing 210008, Jiangsu, Peoples R China
3.Nanjing Univ, Sch Geog & Ocean Sci, Nanjing 210023, Jiangsu, Peoples R China;
4.Chinese Acad Sci, Key Lab Coastal Environm Proc & Ecol Remediat, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China;
5.Chinese Acad Sci, Inst Soil Sci, Nanjing 210008, Jiangsu, Peoples R China;
推荐引用方式
GB/T 7714
Zeng, Lin,Yi, Shuangwen,Lu, Huayu,et al. Response of dune mobility and pedogenesis to fluctuations in monsoon precipitation and human activity in the Hulunbuir dune field, northeastern China, since the last deglaciation[J]. GLOBAL AND PLANETARY CHANGE,2018,168:1-14.
APA Zeng, Lin.,Yi, Shuangwen.,Lu, Huayu.,Chen, Yingyong.,Lei, Fang.,...&Zhang, Wenfang.(2018).Response of dune mobility and pedogenesis to fluctuations in monsoon precipitation and human activity in the Hulunbuir dune field, northeastern China, since the last deglaciation.GLOBAL AND PLANETARY CHANGE,168,1-14.
MLA Zeng, Lin,et al."Response of dune mobility and pedogenesis to fluctuations in monsoon precipitation and human activity in the Hulunbuir dune field, northeastern China, since the last deglaciation".GLOBAL AND PLANETARY CHANGE 168(2018):1-14.
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