The evolution of deserts with climatic changes in China since 150 ka B.P

According to the bioclimatic zones, dune mobility and the fabric characteristics of stratigraphic sedimentary facies, the deserts in China are divided into Eastern, Western, Central and Northwestern deserts. Based on the records of stratigraphical facies, climatic proxies, historical data, etc. in e...

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Published inScience China. Earth sciences Vol. 40; no. 4; pp. 370 - 382
Main Author 董光荣 陈惠忠 王贵勇 李孝泽 邵亚军 金炯
Format Journal Article
LanguageEnglish
Published Dordrecht Springer Nature B.V 01.08.1997
Subjects
Auroral kilometric radiation
B.P
Bioclimatology
change
Climate change
climatic
Climatic change influences on glaciers
Deserts
Evolution
Gases
Global warming
Greenhouse effect
Greenhouse gases
History
Records
Sedimentary facies
Solar radiation
Stratigraphy
China, People's Rep
Online AccessGet full text
ISSN1674-7313
1006-9313
1869-1897
1862-2801
DOI10.1007/BF02877568

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Abstract According to the bioclimatic zones, dune mobility and the fabric characteristics of stratigraphic sedimentary facies, the deserts in China are divided into Eastern, Western, Central and Northwestern deserts. Based on the records of stratigraphical facies, climatic proxies, historical data, etc. in each desert region, the evolution of deserts with climatic changes in time and space since 150 ka B. P. in China are dealt with; then the evolution of deserts in relation to the glacial climatic fluctuations caused by solar radiation changes, underlying surface variation and their feedback mechanism is discussed through comparison with global records; finally, in consideration of global wanning due to increasing of greenhouse gases such as CO2, the possible tendency of the evolution of deserts and the climatic changes is discussed.
AbstractList According to the bioclimatic zones, dune mobility and the fabric characteristics of stratigraphic sedimentary facies, the deserts in China are divided into Eastern, Western, Central and Northwestern deserts. Based on the records of stratigraphical facies, climatic proxies, historical data, etc. in each desert region, the evolution of deserts with climatic changes in time and space since 150 ka B. P. in China are dealt with; then the evolution of deserts in relation to the glacial climatic fluctuations caused by solar radiation changes, underlying surface variation and their feedback mechanism is discussed through comparison with global records; finally, in consideration of global warming due to increasing of greenhouse gases such as C02, the possible tendency of the evolution of deserts and the climatic changes is discussed.
According to the bioclimatic zones, dune mobility and the fabric characteristics of stratigraphic sedimentary facies, the deserts in China are divided into Eastern, Western, Central and Northwestern deserts. Based on the records of stratigraphical facies, climatic proxies, historical data, etc. in each desert region, the evolution of deserts with climatic changes in time and space since 150 ka B. P. in China are dealt with; then the evolution of deserts in relation to the glacial climatic fluctuations caused by solar radiation changes, underlying surface variation and their feedback mechanism is discussed through comparison with global records; finally, in consideration of global wanning due to increasing of greenhouse gases such as CO2, the possible tendency of the evolution of deserts and the climatic changes is discussed.
According to the bioclimatic zones, dune mobility and the fabric characteristics of stratigraphic sedimentary facies, the deserts in China are divided into Eastern, Western, Central and Northwestern deserts. Based on the records of stratigraphical facies, climatic proxies, historical data, etc. in each desert region, the evolution of deserts with climatic changes in time and space since 150 ka B. P. in China are dealt with; then the evolution of deserts in relation to the glacial climatic fluctuations caused by solar radiation changes, underlying surface variation and their feedback mechanism is discussed through comparison with global records; finally, in consideration of global warming due to increasing of greenhouse gases such as C0 sub(2), the possible tendency of the evolution of deserts and the climatic changes is discussed.
Author 董光荣 陈惠忠 王贵勇 李孝泽 邵亚军 金炯
AuthorAffiliation Institute of Desert Research Chinese Academy of Sciences Lanzhou 730000 China China
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Cites_doi 10.1007/BF00209163
10.1038/329403a0
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Notes 11-5843/P
DONG Guangrong , CHEN Huizhong, WANG GuiyongLI Xiaoze, SHAO Yajun ,and JIN Jiong(Institute of Desert Research, Chinese Academy of Sciences, Lanzhou 730000, China)
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SubjectTerms Auroral kilometric radiation
B.P
Bioclimatology
change
Climate change
climatic
Climatic change influences on glaciers
Deserts
Evolution
Gases
Global warming
Greenhouse effect
Greenhouse gases
History
Records
Sedimentary facies
Solar radiation
Stratigraphy
Title The evolution of deserts with climatic changes in China since 150 ka B.P
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