Sedimentary cycles of trace elements in Salawusu River Valley since 150 ka BP

[1]Dong Guangrong, Gao Shangyu, Li Baosheng, 1982. New discovery of the Fossil Ordos Man. Chinese Science Bulletin, 27 (7): 754-758. (in Chinese) [2]Dong Guangrong, Li Baosheng, Gao Shangyu, 1983. The case study of the vicissitude of Mu Us Sandy Land since the Late Pleistocene according to the Salaw...

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Published inJournal of geographical sciences Vol. 12; no. 1; pp. 65 - 71
Main Authors Yao, C-X, Li, B-S, Jin, H-L, Zhang, D D, Yan, M-C, Zhu, Y-Z, Li, H-X, Zhang, Y-H, Kai-Li, L
Format Journal Article
LanguageEnglish
Published Heidelberg Springer Nature B.V 2002
Dept. of Geography, South China Normal University, Guangzhou 510631, China
State Key Laboratory of Loess and Quarternary Geology, Institute of Earth Environment, CAS, Xi'an 710061, China%Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou 730000, China%Dept. of Geography and Geology, Hong Kong University%Dept. of Hydraulic Engineering, Tsinghua University, Beijing 100084, China%State Key Laboratory of Loess and Quarternary Geology, Institute of Earth Environment, CAS, Xi'an 710061, China%Dept. of Geography, South China Normal University, Guangzhou 510631, China
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Summary:[1]Dong Guangrong, Gao Shangyu, Li Baosheng, 1982. New discovery of the Fossil Ordos Man. Chinese Science Bulletin, 27 (7): 754-758. (in Chinese) [2]Dong Guangrong, Li Baosheng, Gao Shangyu, 1983. The case study of the vicissitude of Mu Us Sandy Land since the Late Pleistocene according to the Salawusu River area strata. Journal of Desert Research, 3(2): 9-14. (in Chinese) [3]Dong Guangrong, Su Zhizhu, Jin Heling, 1998. New understanding of Late Pleistocene Sjara-Osso-Gol formation epoch. Chinese Science Bulletin, 43(17): 1869-1872. (in Chinese) [4]Gao Shangyu, Dong Guangrong, Li Baosheng, 1985. Migration and accumulation of chemical elements in the Quaternary strata of the Salawusu River area in relation to climatic evolution. Geochemica, (3): 269-275. [5]Guan Youzhi, Chen Zhenying, Jia Huilan, 1986. Ancient climate and element distribution in the Quaternary strata in Sjara Osso Gol District. Journal of Desert Research, 6(1): 32-35. (in Chinese) [6]Jia Lanpo, 1950. The Ordos Fossil Man. Shanghai: Longmen United Publishing House, 1-89. (in Chinese) [7]Li Baosheng, David Dian Zhang, Jin Heling et al., 2000. Paleo-monsoon activities of Mu Us Desert, China since 150ka BP: a study of the stratigraphic sequences of the Milanggouwan Section, Salawusu River area. Paleogeography, Paleoclimatology, Paleoecology, 162: 1-16. [8]Li Baosheng, Dong Guangrong, Gao Shangyu, 1988a. Sedimentary palaeogeographic environment of Upper Pleistocene strata and its evolution in the Salawusu River area. Geographical Research, 8(2): 64-71. (in Chinese) [9]Li Baosheng, Dong Guangrong, Gao Shangyu, 1988b. Analysis and discussion on the grain size of the Quaternary stratum profile in Yulin area of the northern Shaanxi. Acta Geographica Sinica, 43(2): 125-133. (in Chinese) [10]Li Baosheng, Dong Guangrong, Wu Zheng, 1993. The establishment of the Upper Pleistocene Chengchuan Formation in northern China. Geological Review, 39(2): 91-100. (in Chinese) [11]Li Baosheng, Jin Heling, Lu Haiyan, 1998. Processes of the deposition and vicissitude of Mu Us Desert, China since 150 ka B.P. Science in China (Series D), 41(3): 248-254. [12]Li Baosheng, Wu Zheng, David Dian Zhang et al., 2001. Environment and its changes in the monsoon sandy region of China during the late Pleistocene and Holocene in China. Acta Geologica Sinica, 75(1): 129-133. (in Chinese) [13]Li Yanxian, Ji Hongxiang, 1981. Discussion of environment and its vicissitude. Vertebrata Palasiatica, 19(4): 337-347. [14]Linsley B, 1996. Oxygen-isotope record of sea level and climate variations in the Sulu Sea over the past 150,000 years. Nature, 380: 234-237. [15]Liu Tungsheng et al., 1985. Loess and the Environment. Beijing: Science Press, 124-128. (in Chinese) [16]Pei Wenzhong, Li Youheng, 1964. Some tentative opinions on the problem of "Sjara-Osso-Gol Series, Inner Monglia. Vertebrata Palasiatica, 8 (2): 99-118. [17]Qi Guoqing, 1975. Quaternary mammalian fossils from Salawusu River District, Nei Mongol (Inner Monglia). Vertebrata Palasiatica, 1975, 13 (4): 239-249. [18]Shao Yajun, 1987. Pollen component and paleoclimate and paleovegetation in Sjara-Osso-Gol River since Late Pleistocene Epoch. Journal of Desert Research, 7(2): 22-27. (in Chinese) [19]Sun Jianzhong, 1991. Quaternary Geology in the Loess Plateau. Beijing: Science Press, 161-168. (in Chinese) [20]Teilhard de Chardin P, Licent E, 1924. On the geology of the northern, western and southern borders of the Ordos, China. Bulletin of the Geological Society of China, 3 (1): 37-44. [21]Wen Qizhong, 1989. Loess Geochemistry in China. Beijing: Science Press, 84-92. (in Chinese) [22]Wu Rukang, 1958. Fossil human parietal bone and femur from Ordos. Vertebrata Palasiatica, 2(1): 208-210. [23]Xie Junyi, Gao Shangyu, Dong Guangrong, 1995. Zoocoenosium in Salawusu. Journal of Desert Research, 15 (4): 313-322. (in Chinese) [24]Yuan Baoying, 1978. Sedimentary environment and stratigraphical subdivision of Sjara-Osso-Gol Formation. Scientia Geologica, (3): 320-334. (in Chinese) [25]Zhang Yuhong, Li Baosheng, Jin Heling et al., 2001. Grain-size cycles in Salawusu River valley since 150 ka BP. Acta Geographica Sinica, 56(3): 333-343. (in Chinese) [26]Zhao Zhenhua, 1997. Geochemical principle of trace elements. Beijing: Science Press, 179. (in Chinese)
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ISSN:1009-637X
1861-9568
DOI:10.1007/BF02837429