Phased uplift of the northeastern Tibetan Plateau inferred from a pollen record from Yinchuan Basin, northwestern China
Li, Xinling1; Hao, Qingzhen2,3; Wei, Mingjian1; Andreev, Andrei A.4,5; Wang, Junping1; Tian, Yanyan; Li, Xiaolei1; Cai, Maotang6; Hu, Jianmin6; Shi, Wei6
刊名SCIENTIFIC REPORTS
2017-12-21
卷号7
ISSN号2045-2322
DOI10.1038/s41598-017-16915-z
文献子类Article
英文摘要The uplift of the Tibetan Plateau (TP) significantly affected both regional and global climates. Although there is evidence that the Tibetan Plateau experienced uplift during the Quaternary, the timing and amplitude are poorly constrained. However, the increased availability of long sedimentary records of vegetation change provides an opportunity to reconstruct the timing of the uplift. Here, we present a well-dated, high-resolution pollen record for the last 2.6 Ma from the Yinchuan Basin, which was incised by the Yellow River with its source in the northeastern Tibetan Plateau. Variations in the Artemisia/Chenopodiaceae (A/C) ratio of the reveal changes in moisture conditions in the Yinchuan Basin during glacial-interglacial cycles, as well as a gradual long-term aridification trend which is consistent with progressive global cooling. However, fluctuations in the percentages of Picea and Abies differ from those of the A/C ratio and we propose that they reflect changes in the vegetation and environment of high elevation areas. The Picea and Abies records reveal two phases of increased representation, at 2.1 and 1.2 Ma, which may indicate phases in the uplift of the northeastern Tibetan Plateau. Thus, they provide independent evidence for the timing of the uplift of the Tibetan Plateau during the Quaternary.
WOS关键词LOESS PLATEAU ; ASIAN ARIDIFICATION ; SURFACE POLLEN ; NORTHERN CHINA ; CLIMATE ; MONSOON ; EVOLUTION ; DESERT ; MA ; VEGETATION
WOS研究方向Science & Technology - Other Topics
语种英语
出版者NATURE PUBLISHING GROUP
WOS记录号WOS:000418562100063
资助机构National Natural Science Foundation of China(41771224 ; National Natural Science Foundation of China(41771224 ; National Science Fund for Distinguished Young Scholars of China(41625010) ; National Science Fund for Distinguished Young Scholars of China(41625010) ; China Geological Survey (CGS)(1212011120099 ; China Geological Survey (CGS)(1212011120099 ; Connotation Development - International Exchange and Joint Cultivation of Graduate Students(028165519300) ; Connotation Development - International Exchange and Joint Cultivation of Graduate Students(028165519300) ; 41471007) ; 41471007) ; 1212011220259) ; 1212011220259) ; National Natural Science Foundation of China(41771224 ; National Natural Science Foundation of China(41771224 ; National Science Fund for Distinguished Young Scholars of China(41625010) ; National Science Fund for Distinguished Young Scholars of China(41625010) ; China Geological Survey (CGS)(1212011120099 ; China Geological Survey (CGS)(1212011120099 ; Connotation Development - International Exchange and Joint Cultivation of Graduate Students(028165519300) ; Connotation Development - International Exchange and Joint Cultivation of Graduate Students(028165519300) ; 41471007) ; 41471007) ; 1212011220259) ; 1212011220259) ; National Natural Science Foundation of China(41771224 ; National Natural Science Foundation of China(41771224 ; National Science Fund for Distinguished Young Scholars of China(41625010) ; National Science Fund for Distinguished Young Scholars of China(41625010) ; China Geological Survey (CGS)(1212011120099 ; China Geological Survey (CGS)(1212011120099 ; Connotation Development - International Exchange and Joint Cultivation of Graduate Students(028165519300) ; Connotation Development - International Exchange and Joint Cultivation of Graduate Students(028165519300) ; 41471007) ; 41471007) ; 1212011220259) ; 1212011220259) ; National Natural Science Foundation of China(41771224 ; National Natural Science Foundation of China(41771224 ; National Science Fund for Distinguished Young Scholars of China(41625010) ; National Science Fund for Distinguished Young Scholars of China(41625010) ; China Geological Survey (CGS)(1212011120099 ; China Geological Survey (CGS)(1212011120099 ; Connotation Development - International Exchange and Joint Cultivation of Graduate Students(028165519300) ; Connotation Development - International Exchange and Joint Cultivation of Graduate Students(028165519300) ; 41471007) ; 41471007) ; 1212011220259) ; 1212011220259)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/82182]  
专题中国科学院地质与地球物理研究所
通讯作者Hao, Qingzhen; Wei, Mingjian; Andreev, Andrei A.
作者单位1.Capital Normal Univ, Coll Resource Environm & Tourism, Beijing 100048, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, POB 9825, Beijing, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China
4.Univ Cologne, Inst Geol & Mineral, Zulpicher Str 49a, D-50674 Cologne, Germany
5.Kazan Fed Univ, Inst Geol & Petr Technol, Kazan 420008, Russia
6.Chinese Acad Geol Sci, Inst Geomech, Beijing 100081, Peoples R China
推荐引用方式
GB/T 7714
Li, Xinling,Hao, Qingzhen,Wei, Mingjian,et al. Phased uplift of the northeastern Tibetan Plateau inferred from a pollen record from Yinchuan Basin, northwestern China[J]. SCIENTIFIC REPORTS,2017,7.
APA Li, Xinling.,Hao, Qingzhen.,Wei, Mingjian.,Andreev, Andrei A..,Wang, Junping.,...&Shi, Wei.(2017).Phased uplift of the northeastern Tibetan Plateau inferred from a pollen record from Yinchuan Basin, northwestern China.SCIENTIFIC REPORTS,7.
MLA Li, Xinling,et al."Phased uplift of the northeastern Tibetan Plateau inferred from a pollen record from Yinchuan Basin, northwestern China".SCIENTIFIC REPORTS 7(2017).
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