Journal of Geographical Sciences >
Formation and evolution of sand deserts in Xinjiang, Northwest China：Ⅱ. The palaeo-environmental reconstruction
Received date: 2013-05-27
Revised date: 2013-07-05
Online published: 2014-03-28
Supported by
National Basic Research Program of China (973 Program), No.2009CB421305; National Natural Science Foundation of China, No.41371060, No.41271049
Based on the palaeoclimatic and palaeoenvironmental evidences of geological history and human history periods, this paper reviews the researches and progresses on the development of the sandy deserts in Xinjiang. It pointed out that the features of tectonic structure in Xinjiang had made both the Tarim Basin and the Junggar Basin being influenced greatly by the foehn effects originated from the planetary wind system of westerly, the East Asian ocean-continental monsoon and the topographical mountain-valley winds. The regional patterns of climate and environment since the Quaternary were characterized by the overall persistent drought accompanied by fluctuations in the secondary scale. Formations of aeolian sediments in the basins and at the margins are a potential response to global climate change, particularly the aridification of the Asian hinterland deduced by the uprising of the Tibetan Plateau and its surrounding highlands. For the question about the formation time of the Taklamakan Desert, because the research methods, objects and information carriers used in previous studies are different, there are many disputes in the academic circles at present. Evidences from aeolian deposits/rocks at the edge and in the hinterland of these sandy deserts and their chronological data indicate that an arid climate and land surface aeolian processes have occurred at the edge of the Tarim Basin and its hinterland areas since the Tertiary period. However, the duration time of these processes at mass scale should have begun after the middle Pleistocene and lasted to the Holocene. Occurrence of dune fields in recent 2000 years in the oasis areas should be greatly influenced by human factors.
Key words： sandy desert; Tertiary; Quaternary; ancient aeolian sediment; palaeoclimate change; Xinjiang
ZHU Bingqi, YU Jingjie, QIN Xiaoguang, Patrick RIOUAL, ZHANG Yichi, XIONG Heigang . Formation and evolution of sand deserts in Xinjiang, Northwest China：Ⅱ. The palaeo-environmental reconstruction[J]. Journal of Geographical Sciences, 2014 , 24(3) : 539 -559 . DOI: 10.1007/s11442-014-1105-3
Amold E, Merrill J, Leinen M, 1998. The effect of source area and atmospheric transport on mineral aerosol collected over the North Pacific Ocean. Global and Planetary Change, 18: 137-159.
Aobluqiv B A, 1958. On Questions of Sand and Loess. Le Z, Liu D S trans. Beijing: Science Press. (in Chinese)
Chang H, An Z, Liu W et al., 2012. Magnetostratigraphic and paleoenvironmental records for a Late Cenozoic sedimentary sequence drilled from Lop Nor in the eastern Tarim Basin. Global and Planetary Change, 80/81: 113-122.
Chen F, Huang X, Zhang J et al., 2006. Humid Little Ice Age in arid Central Asia documented by Bosten Lake, Xinjiang, China. Science in China Series D Earth Sciences, 49(12): 1280-1290.
Chen F, Yu Z, Yang M et al., 2008. Holocene moisture evolution in arid Central Asia and its out-of-phase relationship with Asian monsoon history. Quaternary Science Reviews, 27: 351-364.
Cui Z, Wu Y, Liu G, 1998. On Kunlun-Yellow River tectonic movement. Science in China Series D Earth Sciences, 41(6): 592-600.
ECCPGCAS (Editing Committee of Chinese Physical Geography in Chinese Academy of Sciences), 1984. Chinese Physical Geography: Palaeo-Geography. Beijing: Science Press. (in Chinese)
Ding Z, Ren J, Yang S et al., 1999. Climate instability during the penultimate glaciation: Evidence from two high-resolution loess records, China, Journal of Geophysical Research, 104, 20123-20132.
Dong G R, 1997. A new progress of the Quaternary geological study on the Taklamakan Desert. Journal of Desert Research, 17(1): 77-79. (in Chinese)
Dong G R, Li S, Li B S, 1991. A preliminary study on the formation and evolution of deserts in China. Journal of Desert Research, 11(4): 23-32. (in Chinese)
Dong Z, Qu J, Wang X et al., 2008. Pseudo-feathery dunes in the Kumtagh Desert. Geomorphology, 100: 328-334.
Fang X, Lu L, Yang S et al., 2002a. Loess in Kunlun Mountains and its implications on desert development and Tibetan Plateau uplift in west China. Science in China Series D Earth Sciences, 45(4): 289-299.
Fang X, Shi Z, Yang S et al., 2002b. Loess in the Tian Shan and its implications for the development of the Gurbantunggut Desert and drying of northern Xinjiang. Chinese Science Bulletin, 47: 1381-1387.
Feng Q, Su Z, Jin H, 1999. Desert evolution and climatic changes in the Tarim River Basin since 12 ka BP. Science in China Series D Earth Sciences, 42 (S1): 101-112.
Guo Z, Ruddiman W, Hao Q et al., 2002. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature, 416: 159-163.
Han S T, 1987. Environmental evolution of Holocene epoch and its exploitation in several areas of Xinjiang. Journal of Desert Research, 7(4): 37-44. (in Chinese)
Han S T, Zai Z, 1992. Characterization of the inter-continental Holocene climate for the region of Balikun Lake in northern Xinjiang. Science in China Series B, 11: 1021-1029. (in Chinese)
Huang Q, Zhou X J, 2000. The climate-environment changes in the south of Gurbantunggut Desert since 80 ka BP. Arid Land Geography, 23(1): 55-60. (in Chinese)
IGCAGS (Institute of Geology, Chinese Academy of Geological Sciences), 1985. Palaeogeography of China. Beijing: Geological Publishing House. (in Chinese)
Jiang Q, Shen J, Liu X, 2007. A high-resolution climatic change since Holocene inferred from multi-proxy of lake sediment in westerly area of China. Chinese Science Bulletin, 52(14): 1970-1979.
Krijgsman W, Hilgen F J, Raffi I et al., 1999. Chronology, causes and progression of the Messinian salinity crisis. Nature, 400: 652-655.
Kutzbach J E, Guetter P J, Ruddiman W F, 1989. Sensitivity of climate to late Cenozoic uplift in Southern Asia and the American West: Numerical experiments. Journal of Geophysical Research, 94: 18393-18407.
Li B S, Jin J, 1988. A preliminary study on the sedimentary strata of the Pulu sandy hills at the south edge of the Taklamakan Desert. Chinese Science Bulletin, 33(2): 140-143. (in Chinese)
Li B S, Lin Y Q, Lu J H et al., 1986. Eolian sand of the Pulu area and the vicissitudes on southern border of Taklamakar Desert in Sinkiang. Journal of Desert Research, 6(4): 43-50. (in Chinese)
Li J F, 1989. Study on The Tree-ring Climatic Hydrology in Xinjiang. Beijing: China Meteorological Press. (in Chinese)
Li J J, 1990. The patterns of environmental changes since late Pleistocene in northwestern China. Quaternary Sciences, 4: 197-204. (in Chinese)
Li Q K, 1992. Fluctuation of closed lake-level and its climatic significance on the middle Kunlun Mountains. Journal of Lake Sciences, 4(1): 19-29. (in Chinese)
Liu D S, 1965. Loess Deposits in China. Beijing: Science Press. (in Chinese)
Liu D S, 1985. Loess and Environment in China. Beijing: Science Press. (in Chinese)
Lu H, Xia X, Liu J et al., 2010. A preliminary study of chronology for a newly-discovered ancient city and five archaeological sites in Lop Nor, China. Chinese Science Bulletin, 55(1): 63-71.
Qin X, Liu J, Jia H et al., 2012. New evidence of agricultural activity and environmental change associated with the ancient Loulan kingdom, China, around 1500 years ago. Holocene, 22(1): 53-61.
Qu J J, Zuo G C, Zhang K C, 2005. Relationship between the formation and evolution of the Kumtag Desert and the regional Neotectonic Movement. Arid Land Geography, 28(4): 424-428. (in Chinese)
Shi Y F, Kong Z H, Wang S M, 1992. The basic characteristics of the Holocene warm climate and environment in China. In: The Holocene Warm Climate and Environment in China. Beijing: Science Press, 1-17. (in Chinese)
Shi Z T, Song Y G, An Z S, 2006. Evolution of Gurbantunggut Desert recorded by Tianshan Loess. Journal of Desert Research, 26(5): 675-679. (in Chinese)
Sun D, An Z, Su R et al., 2003. Eolian sedimentary records for the evolution of monsoon and westerly circulations of northern China in the last 2.6 Ma. Science in China Series D Earth Sciences, 46 (10): 1049-1059.
Sun J, Liu T, 2006. The age of the Taklimakan Desert. Science, 312: 1621-1621.
Sun J, Ye J, Wu W et al., 2010. Late Oligocene-Miocene mid-latitude aridification and wind patterns in the Asian interior. Geology, 38(6): 515-518.
Sun J, Zhang L, Deng C et al., 2008. Evidence for enhanced aridity in the Tarim Basin of China since 5.3 Ma. Quaternary Science Reviews, 27: 1012-1023.
Sun J, Zhang Z, Zhang L, 2009. New evidence on the age of the Taklimakan Desert. Geology, 37(2): 159-162.
Tang J, Su Z, Ding F et al., 2010. Formative age and evolution of Kumtagh Desert. Arid Land Geography, 33(3): 325-333. (in Chinese)
Wang S M, Feng M, 1991. A relationship between the Daihai Lake environmental change in the Inner Mongolia and the strength of the Southeastern Monsoon. Science in China Series B, 7: 759-768. (in Chinese)
Wang T, 2002. Deserts and Desertification in China. Shijiazhuang: Hebei Science and Technology Publishing House. (in Chinese)
Wu G J, Pan B T, Guan Q Y et al., 2002. The maximum glaciation and desert expansion in China during MIS16. Journal of Glaciology and Geocryology, 24(5): 544-549. (in Chinese)
Wu Z, 1981. Approach to the genesis of the Taklamakan Desert. Acta Geographica Sinica, 36(3): 280-291. (in Chinese)
Wu Z, 1982. Sandy Deserts in China. Beijing: The Commercial Press.. (in Chinese)
Wu Z, 1997. The basic characteristic of landform development in the Jungar Basin. In: Wu Z (ed.). Studies on the Sandy Deserts and the Coastal Dunes in China. Beijing: Science Press, 29-43. (in Chinese)
Wunnemann B, Mischke S, Chen F, 2006. A Holocene sedimentary record from Bosten Lake, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 234: 223-238.
XDCAS (Xinjiang Division of Chinese Academy of Sciences), 1987. The Scientific Survey and Study on the Luobupo. Beijing: Science Press. (in Chinese)
Xia X C, 1987. The Basic characteristics of the Kumtag Desert. In: XDCAS (Xinjiang Division of Chinese Academy of Sciences) (eds.). The Scientific Survey and Study on the Luobupo. Beijing: Science Press, 78-94. (in Chinese)
Xia X C, Li C S, Zhou X J et al., 1991. Desertification and Aeolian Sand Disaster Control in Xinjiang. Beijing: Science Press, 1-39. (in Chinese)
Xiao J, Chang Z, Wen R et al., 2009. Holocene weak monsoon intervals indicated by low lake levels at Hulun Lake in the monsoonal margin region of northeastern Inner Mongolia, China. Holocene, 19(6): 899-908.
Xiao J, Si B, Zhai D et al., 2008. Hydrology of Dali Lake in central-eastern Inner Mongolia and Holocene East Asian monsoon variability. Journal of Paleolimnology, 40: 519-528.
Xiong H G, Zhong W, TashPolat T et al., 2000. The coupling relationship between the nature and the man in south edge of Tarim Basin. Acta Geographica Sinica, 55(2): 191-198. (in Chinese)
Yang X, 2001. The oases along the Keriya River in the Taklamakan Desert, China, and their evolution since the end of the last glaciation. Engvironmental Geology, 41: 314-320.
Yang X, Liu Z, Zhang F et al., 2006a. Hydrological changes and land degradation in the southern and eastern Tarim Basin, Xinjiang, China. Land Degradation & Development, 17: 381-392.
Yang X, Preusser F, Radtke U, 2006b. Late Quaternary environmental changes in the Taklamakan Desert, weatern China, inferred from OSL-dated lacustrine and aeolian deposits. Quaternary Science Reviews, 25: 923-932.
Yang X, Rost K T, Lehmkuhl F et al., 2004. The evolution of dry lands in northern China and in the Republic of Mongolia since the Last Glacial Maximum. Quaternary International, 118/119: 69-85.
Yang X, Scuderi L, Paillou P et al., 2011. Quaternary environmental changes in the drylands of China: A critical review. Quaternary Science Reviews, 30: 3219-3233.
Yang X, Shi C, Li B et al., 2008. Some aspects about Chinese Geomorphology: Recent progresses from an earth system science perspective. Quaternary Sciences, 28(4): 521-534. (in Chinese)
Yang X, Zhu Z, Jaekel D et al., 2002. Late Quaternary palaeoenvironment change and landscape evolution along the Keriya River, Xinjiang, China: The relationship between high mountain glaciation and landscape evolution in foreland desert regions. Quaternary International, 97: 155-166.
Ye W, 2000. The climatic characteristics and environmental patterns during Holocene in North Xinjiang. Journal of Desert Research, 20(2): 185-191. (in Chinese)
Yonenobu H, Itoh T, 2000. 14C dating of the Niya site in the Tarim Basin. Nuclear Instruments and Methods in Physics Research B, 172: 741-744.
Yong T S, Yang C M, 1986. Several questions about the strata at the northeastern edge of the Jungar Basin. Xinjiang Petroleum Geology, 7(2): 44-47. (in Chinese)
Zhang F, Wang T, Yimit H et al., 2011. Hydrological changes and settlement migrations in the Keriya River delta in central Tarim Basin ca. 2.7-1.6 ka BP: Inferred from 14C and OSL chronology. Science China Earth Sciences, 54: 1971-1980.
Zhang Z, Wang H, Guo Z et al., 2007. Impacts of tectonic changes on the reorganization of the Cenozoic paleoclimatic patterns in China. Earth and Planetary Science Letters, 257: 622-634.
Zheng H, Chen H, Cao J, 2002. Palaeoenvironmental implication of the Plio-Pleistocene loess deposits in southern Tarim Basin. Chinese Science Bulletin, 47(8): 700-704.
Zheng H, Powell C M, An Z et al., 2000. Pliocene uplift of the northern Tibetan Plateau. Geology, 28(8): 715-718.
Zhong W, 1996. Some important progresses of recent research in Quaternary environmental changes in Xinjiang. Arid Land Geography, 19(3): 88-95. (in Chinese)
Zhong W, Xue J, Shu Q et al., 2007. Climate change during the last 4000 years in the southern Tarim Basin, Xinjiang, Northwest China. Journal of Quaternary Science, 2007, 22(7): 659-665.
Zhou T R, 1963. Major types of the Quaternary continental sediments in Xinjiang and its relationship with the development of Xinjiang geomorphology and climate. Acta Geographica Sinica, 29: 109-129. (in Chinese)
Zhu Z D, 1987. Desertification processes and developmental tendency in Taklimakan Desert region. Journal of Desert Research, 17(3): 19-31. (in Chinese)
Zhu Z D, Chen Y P, Wu Z et al., 1981. Study on the Aeolian Geomorphology of the Taklamakan Desert. Beijing: Science Press. (in Chinese)
Zhu Z D, Wu Z, Liu S et al., 1980. Outline of Chinese Sandy Deserts. rev. ed. Beijing: Science Press. (in Chinese)
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