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Deposits and Soils of the Past 130,000 Years at the Desert–Loess Transition in Northern China

Published online by Cambridge University Press:  20 January 2017

Jimin Sun  and
Zhongli Ding
Jimin Sun*
Affiliation:
Institute of Geology, Chinese Academy of Sciences, P.O. Box 9825, Beijing, 100029, China
Zhongli Ding
Affiliation:
Institute of Geology, Chinese Academy of Sciences, P.O. Box 9825, Beijing, 100029, China
*
1E-mail: jmsun@igcas.igcas.ac.cn.
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Abstract

The desert–loess transitional zone in north-central China has long been thought sensitive to Quaternary climatic change. However, reconstruction of Quaternary climates in this area has been hindered by incompleteness of geological sections. Here we report the analytical results of two recently found sand–loess–soil sections. Both sections have thick eolian deposits from the last interglacial–glacial cycle and can be correlated with one another. Field observations, thermoluminescence dating, and other laboratory analyses show that the last interglacial period produced three paleosols and two intercalated loess layers. Loess from the last glacial period is interbedded with three sand horizons that represent desert extension. The expansion and contraction of desert in northern China may have been forced by the east Asia monsoon.

Information

Type
Original Articles
Information
Quaternary Research , Volume 50 , Issue 2 , September 1998 , pp. 148 - 156
Copyright
University of Washington

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References

An, Z.S., Wang, J., and Li, H. (1977). Palaeomagnetic research of the Luochuan loess section. Geochemical 4, 239–249.Google Scholar
An, Z.S., Kukla, G., Porter, S., and Xiao, J.L. (1991). Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of Central China during the last 130 000 years. Quaternary Research 36, 29–36.CrossRefGoogle Scholar
An, Z.S., Kukla, G., Porter, S.C., and Xiao, J.L. (1991). Late Quaternary dust flow on the Chinese Loess Plateau. Catena 18, 125–132.CrossRefGoogle Scholar
Banerjee, S.K., Hunt, C.P., and Liu, X.M. (1993). Separation of local signals from the regional paleomonsoon record of the Chinese loess plateau: A rock-magnetic approach. Geophysical Research Letters 20, 843–846.CrossRefGoogle Scholar
Berger, A., and Loutre, M.F. (1991). Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10, 297–317.CrossRefGoogle Scholar
Bronger, A., and Heinkele, T. (1989). Micromorphology and genesis of paleosols in the Luochuan loess section, China: Pedostratigraphic and environmental implications. Geoderma 45, 123–143.CrossRefGoogle Scholar
Ding, Z.L., Rutter, N., Han, J.T., and Liu, T.S. (1992). A coupled environmental system formed at about 2.5 Ma in East Asia. Palaeogeography, Palaeoclimatology, Palaeoecology 94, 223–242.Google Scholar
Ding, Z., Yu, Z., Rutter, N.W., and Liu, T. (1994). Towards an orbital time scale for Chinese loess deposits. Quaternary Science Reviews 13, 39–70.CrossRefGoogle Scholar
Ding, Z.L., Liu, T.S., Rutter, N.W., Yu, Z.W., Guo, Z.T., and Zhu, R.X. (1995). Ice-volume forcing of East Asia winter monsoon variations in the past 800,000 years. Quaternary Research 44, 149–159.CrossRefGoogle Scholar
Dong, G.R., Li, B.S., Gao, S.Y., Wu, Z., and Shao, Y.J. (1983). The Quaternary ancient eolian sands in the Ordos Plateau. Acta Geographic Sinica 38, 341–347.Google Scholar
Fine, P., and Singer, M.J. (1989). Pedogenic factors affecting magnetic susceptibility of northern California soils. Soil Science Society of America Journal 53, 1119–1127.Google Scholar
Fine, P., Singer, M.J., LaVen, R., Verosub, K.L., and Southard, R.J. (1989). Role of pedogenesis in distribution of magnetic susceptibility in two California chronosequences. Geoderma 44, 287–306.CrossRefGoogle Scholar
Forman, S.L. (1991). Late Pleistocene chronology of loess deposition near Luochuan, China. Quaternary Research 36, 19–28.CrossRefGoogle Scholar
Guo, Z., Liu, T., Guiot, J., Wu, N., Lu, H., Han, J., Liu, J., and Gu, Z. (1996). High frequency pulses of East Asia monsoon climate in the last two glaciations: Link with the North Atlantic. Climate Dynamics 12, 701–709.CrossRefGoogle Scholar
Han, J.M., Hus, J.J., Paepe, R., Vandenberghe, R.E., and Liu, T.S. (1991). The rock magnetic properties of the Malan and Lishi formations in the Loess Plateau of China. Loess, Environment and Global Change Science Press, Beijing.p. 30–47Google Scholar
Heller, F., and Liu, T.S. (1982). Magnetostratigraphic dating of loess deposits in China. Nature 300, 431–433.CrossRefGoogle Scholar
Heller, F., and Liu, T.S. (1984). Magnetism of Chinese loess deposits. Geophysical Journal of the Royal Astronomical Society 77, 125–141.CrossRefGoogle Scholar
Hou, R.Z. (1973). The Mu Us Desert evolution as indicated by the ruins of ancient castles along the Sajara River. Cultural Relic 1, 35–41.Google Scholar
Hunt, C.P., Singer, M.J., Kletetschka, G., TenPas, J., and Verosub, K. (1995). Effect of citrate-bicarbonate-dithionite treatment on fine-grained magnetite and maghemite. Earth and Planetary Science Letters 130, 87–94.CrossRefGoogle Scholar
Imbrie, J., Hays, J.D., Martinson, D.B., McIntyre, A., Mix, A.C., Morley, J.J., Pisias, N.G., Prell, W.L., and Shackleton, N.J. (1984). The orbital theory of Pleistocene climate: Support from a revised chronology of the marine delta 18O record.. In Milankovitch and Climate (Part I) Berger, A., Imbrie, J., Hays, J., Kukla, G., and Saltzman, B. (1984). Reidel, Dordrecht.269–305.Google Scholar
Kukla, G. (1987). Loess stratigraphy in central China. Quaternary Science Reviews 6, 191–219.CrossRefGoogle Scholar
Kukla, G., Heller, F., Liu, X.M., Xu, T.C., Liu, T.S., and An, Z.S. (1988). Pleistocene climates in China dated by magnetic susceptibility. Geology 16, 811–814.2.3.CO;2>CrossRefGoogle Scholar
Kukla, G., and An, Z.S. (1989). Loess stratigraphy in central China. Palaeogeography Palaeoclimatology Palaeoecology 72, 203–255.CrossRefGoogle Scholar
Kukla, G., An, Z.S., Melice, J.L., Gavin, J., and Xiao, J.L. (1990). Magnetic susceptibility record of Chinese loess. Transaction of the Royal Society of Edinburgh: Earth Sciences 81, 263–288.CrossRefGoogle Scholar
Liu, T.S. (1966). Composition and Texture of Loess. Science Press, Beijing.p. 132Google Scholar
Liu, T.S. (1985). Loess and the Environment. China Ocean Press, Beijing.p. 31–238Google Scholar
Lu, Y.C., Mortlock, A.J., Price, D.M., and Readhead, M.L. (1987). Thermoluminescence dating of coarse-grain quartz from the Malan loess at Zhaitang section, China. Quaternary Research 28, 356–363.Google Scholar
Lu, Y.C., Zhang, J.Z., and Xie, J. (1988). Thermoluminescence dating of loess and paleosols from the Lantian section, Shaanxi Province, China. Quaternary Science Reviews 7, 251–255.Google Scholar
Maher, B., and Thompson, R. (1991). Mineral magnetic record of the Chinese loess and palaeosol. Geology 19, 3–6.2.3.CO;2>CrossRefGoogle Scholar
Mehra, O.P., and Jackson, M.L. (1960). Iron oxide removal from soils and clays by a dithionite-citrate system buffered with sodium bicarbonate. Clay and Clay Minerals 5, 317–327.Google Scholar
(1991). Land Desertification in the Northern Loess Plateau. Science Press, Beijing.p. 12–76Google Scholar
Musson, F.M., Clarke, M.L., and Wintle, A.G. (1994). Luminescence dating of loess from the Liujiapo section, Central China. Quaternary Science Reviews 13, 407–410.CrossRefGoogle Scholar
Pye, K., and Zhou, L.P. (1989). Late Pleistocene and Holocene aeolian dust deposition in North China and the Northwest Pacific Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology 73, 11–23.CrossRefGoogle Scholar
Singer, M.J., Fine, P., Verosub, K.L., and Chadwick, O.A. (1992). Time dependence of magnetic susceptibility of soil chronosequences on the California Coast. Quaternary Research 37, 323–332.CrossRefGoogle Scholar
Sun, J.M., Ding, Z.L., and Yuan, B.Y. (1995). Desertification process of Mu Us Desert since 2000 a B. P. Arid Land Geography 18, 36–42.Google Scholar
Sun, J.M., Ding, Z.L., and Liu, T.S. (1997). Geological evidence of Mu Us Desert evolution during the last 500 ka. Scientia Geologica Sinica 6, 97–106.Google Scholar
Sun, J.M., and Ding, Z.L. (1997). Spatial and temporal changes of dry and wet climate during the last 130,000 years in the Loess Plateau. Quaternary Science 2, 168–175.Google Scholar
Verosub, K.L., Fine, P., Singer, M.L., and TenPas, J. (1993). Pedogenesis and paleoclimate: Interpretation of the magnetic susceptibility record of Chinese loess-paleosol sequences. Geology 21, 1011–1014.2.3.CO;2>CrossRefGoogle Scholar
Zhou, L.P., Oldfield, F., Wintle, A.G., Robinson, S.G., and Wang, J.T. (1990). Partly pedogenic origin of magnetic variations in Chinese loess. Nature 346, 737–739.CrossRefGoogle Scholar
Zhu, Z.D. (1980). An Outline on Chinese Deserts. Science Press, Beijing.p. 249–260Google Scholar