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1Modern pollen assemblages from surface lake sediments in northwestern China and their importance as indicators of vegetation and climate显示文摘The modern pollen assemblages of surface lake sediments and topsoils in northwestern China were studied to understand the relationship of modern pollen data with contemporary vegetation and climate, and the differences between the pollen assemblages of surface lake sediments and topsoils. The results show that Chenopodiaceae and Artemisia are dominant elements in the pollen assemblages of northwestern China. Additionally, Ephedra, Cyperaceae, Asteraceae, Poaceae, Picea, Pinus, and Betula are also important pollen taxa. Both pollen assemblages and principal component analysis indicate that pollen data from surface lake sediments and topsoils can be used to differentiate the main vegetation types of this region(desert, steppe, meadow and forest). However, differences exist between modern pollen assemblages of the two types of sediments due to the different relevant source areas of pollen and degrees of pollen preservation. For example, the larger relevant source area of surface lake sediment results in a higher abundance of Betula in pollen assemblage from surface lake sediment, whereas the tendency to disintegrate thin-walled pollen types in topsoil leads to a higher proportion of resistant pollen, such as Asteraceae. Linear regression analysis indicates that the Artemisia/Chenopodiaceae(A/C) ratio in pollen assemblages of surface lake sediments can be used to indicate humidity changes in the study area. However, the A/C ratio in topsoils should be used carefully. Our results suggest that pollen data from surface lake sediments would be better references for interpreting the fossil pollen assemblages of lake cores or lacustrine profiles.QIN Feng ZHAO Yan LI Quan CAI MaoTang 2015Science China Earth Sciences2015,58,9:11
2Plio-cene-Pleistocene stepwise drying of Central Asia: evi-dence from paleomagnetism and sporopollen record of thedeep borehole SG-3 in the western Qaidam Basin, NETibetan Plateau 显示文摘CAI Maotang FANG Xiaomin WU Fuli 2012Global and Planetary Change2012,94,:1
3Effects of structure multiplicity on mechanism of radiation crosslinking of polymers显示文摘Zhang Lihua Zhou Maotang Chen Dongliu 1994Radiation Physics Chemistry1994,44,3:1
4Pliocene–Pleistocene stepwise drying of Central Asia: Evidence from paleomagnetism and sporopollen record of the deep borehole SG-3 in the western Qaidam Basin, NE Tibetan Plateau显示文摘Maotang Cai Xiaomin Fang Fuli Wu Yunfa Miao Erwin Appel 2012Global and Planetary Change2012,,:1
5Deep Drilling Campaign in the Western Qaidam Basin,NE Tibetan Plateau and their Revealed Global Temperature Forcing of Salt Formation in the Late Miocene-Quaternary显示文摘The Qaidam Basin in the NE Tibetan Plateau has contributed the largest amount of potash in China.However,how the potash was formed has long been a subject of debate.Here we carried out a deepFANG Xiaomin LI Minghui Erwin APPEL WANG Jiuyi HAN Wenxia ZHANG Weilin YANG Yibo CAI Maotang 2014Acta Geologica Sinica(English Edition)2014,88,S1:0
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