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SCIENCE CHINA Earth Sciences  2011, Vol. 54 Issue (4): 603-614    DOI: 10.1007/s11430-010-4111-z
Article
Holocene climate variation denoted by Barkol Lake sediments in northeastern Xinjiang and its possible linkage to the high and low latitude climates
XUE JiBin1, ZHONG Wei1,2,3*
1 School of Geography, South China Normal University, Guangzhou 510631, China;
2 Key Laboratory of Oasis Ecology (Ministry of Education), Xinjiang University, Urumqi 830046, China;
3 Key Laboratory of Western China’s Environmental Systems (Ministry of Education), Lanzhou University, Lanzhou 730000, China
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