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  4. 中国科学院新生代地质与环境重点实验室
Linkage between C-4 vegetation expansion and dune stabilization in the deserts of NE China during the late Quaternary

文献类型：期刊论文

作者Guo, Licheng1,2,3; Xiong, Shangfa1,2,3; Dong, Xinxin4; Ding, Zhongli1,2,3; Yang, Ping5; Zhao, Hua6; Wu, Jiabin1,2,3; Ye, Wei5; Jin, Guiyun7; Wu, Wenwan7
刊名QUATERNARY INTERNATIONAL
出版日期2019-02-01
卷号503页码:10-23
关键词C-4 vegetation Dune stabilization Late Quaternary Desert China
ISSN号1040-6182
DOI10.1016/j.quaint.2018.10.026
英文摘要Knowledge of the role of C-4 vegetation expansion in regulating dune stabilization during the late Quaternary is important for understanding the evolution of the environment and climate in the climatically-sensitive margin of the East Asian summer monsoon. However, due to the lack of both reliable vegetation records and chronological control during episodes of dune activity, the relationship between C-4 vegetation expansion and dune stabilization in the deserts of NE China during the late Quaternary remains unclear. Here, we present a new regional compilation of late Quaternary stable carbon isotopic data from organic matter, together with dated records from sub-aerial sedimentary deposits in the region. Our compilation of vegetation development and dune activity in these deserts suggests that C-4 vegetation expansion, with a main contribution from Chenopodiaceae, and a secondary contribution from Poaceae and Cyperaceae, may have played a critical role in dune semi-stabilization with a northwestward trend, from similar to 13 to 9 ka; and dune stabilization throughout the entire study region, from similar to 9 to 5 ka. In addition, during the late Holocene, intensified millet cultivation (or overgrazing) and/or climatic deterioration at similar to 1.5 ka likely caused an increase in C-4 vegetation abundance in the deserts of NE China, which is associated with a dune mobilization episode. In contrast, after similar to 2.5 ka, decreased vegetation cover and dune mobilization in the Mu Us and Hobq deserts were likely caused by poor land-use practices and historically documented droughts. Overall, C-4 vegetation expansion was the main cause of dune stabilization in these deserts during the late Quaternary.
WOS关键词MU US DESERT ; HOLOCENE ENVIRONMENTAL-CHANGES ; CARBON-ISOTOPIC COMPOSITION ; HUNSHANDAKE SANDY LAND ; CENTRAL INNER-MONGOLIA ; ASIAN SUMMER MONSOON ; LAST GLACIAL MAXIMUM ; NORTHERN CHINA ; LATE PLEISTOCENE ; OSL CHRONOLOGY
资助项目National Key R&D Program of China[2017YFA0603404] ; "Strategic Priority Research Program" of the Chinese Academy of Sciences[XDA19050104] ; "Strategic Priority Research Program" of the Chinese Academy of Sciences[XDB26020401] ; National Natural Science Foundation of China[41272206]
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000460632300003
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; "Strategic Priority Research Program" of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/90900]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Guo, Licheng; Xiong, Shangfa
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
4.Chinese Acad Sci, Bur Gen Affairs, Beijing 100864, Peoples R China
5.Zhejiang Normal Univ, Coll Geog & Environm Sci, Jinhua 321004, Peoples R China
6.Chinese Acad Geol Sci, Inst Hydrogeol & Environm Geol, Shijiazhuang 050061, Hebei, Peoples R China
7.Shandong Univ, Inst Cultural Heritage, Dept Archaeol, Jinan 250100, Shandong, Peoples R China
8.Jiangxi Normal Univ, Sch Geog & Environm, Nanchang 330022, Jiangxi, Peoples R China
推荐引用方式
GB/T 7714		 Guo, Licheng,Xiong, Shangfa,Dong, Xinxin,et al. Linkage between C-4 vegetation expansion and dune stabilization in the deserts of NE China during the late Quaternary[J]. QUATERNARY INTERNATIONAL,2019,503:10-23.
APA Guo, Licheng.,Xiong, Shangfa.,Dong, Xinxin.,Ding, Zhongli.,Yang, Ping.,...&Zheng, Lin.(2019).Linkage between C-4 vegetation expansion and dune stabilization in the deserts of NE China during the late Quaternary.QUATERNARY INTERNATIONAL,503,10-23.
MLA Guo, Licheng,et al."Linkage between C-4 vegetation expansion and dune stabilization in the deserts of NE China during the late Quaternary".QUATERNARY INTERNATIONAL 503(2019):10-23.

入库方式： OAI收割

来源：地质与地球物理研究所

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