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Formation of Ulan Buh desert and its environmental changes during the Holocene

✍ Scribed by Chun, Xi ;Chen, Fahu ;Fan, Yuxin ;Xia, Dunsheng ;Zhao, Hui

Book ID
107476521
Publisher
Higher Education Press and Springer
Year
2008
Weight
793 KB
Volume
2
Category
Article
ISSN
1673-7385

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## Abstract Radiocarbon‐dated palaeontological remains and bedding features suggests that climatic changes in the northern Taklimakan Desert since the beginning of the Holocene can be divided into four stages: (i) 12 000–10 000 BP, a cool–to temperate–dry climate resulting in apparent alluvial–fluv