［1］Liu, T. S., Loess and the Environment, Beijing: China Ocean Press, 1985, 1-251.［2］Chen, L. X., Zhu, Q. G., Luo, H. B. et al., East Asian Monsoon, Beijing: China Meteorology Press, 1991, 28-61.［3］An, Z. S., Liu, T. S., Lu, Y. C. et al., The long-term palaeomonsoon variation recorded by the loess-palaeosol sequence in central China, Quaternary International, 1990, (7/8): 91-95.［4］Guo, Z. T., Liu, T. S., Fedoroff, N. et al., Shift of the monsoon intensity on the Loess Plateau at ca. 0.85 MaBP, Chinese Science Bulletin, 1993, 38(2): 586-591.［5］Chen, J., An, Z. S., Wang, Y. J. et al., Distributions of Rb and Sr in the Luochuan loess-paleosol sequence of China during the last 800 ka: Implications for paleomonsoon variations, Science in China, Ser. D, 1999, 42(3): 225-232.［6］Chen, J., Wang, Y. J., Ji, J. F. et al., Rb/Sr variations and its climatic stratigraphical significance of a loess-paleosol profile from Luochuan, Shaanxi Province, Quaternary Sciences (in Chinese), 1999, 19(4): 350-356.［7］Guo, Z. T.,Liu, T. S., Fedoroff, N. et al., Climate extremes in loess of China coupled with the strength of deep-water for-mation in the North Atlantic, Global and Planetary Change, 1998, 18: 113-128.［8］Guo, Z. T., Liu, T. S., An, Z. S., Paleosols of the last 0.15 Ma in the Weinan loess section and their paleoclimate signifi-cance, Quaternary Sciences (in Chinese), 1994, 14(3): 256-269.［9］Guo, Z, T,, Fedoroff, N., Liu, T. S., Micromorphology of the loess-paleosol sequence of the last 130 ka in China and pa-leoclimatic event, Science in China (in Chinese), Ser. D, 1996, 26(3): 392-398.［10］Guo, Z., Liu, T., Guiot, J., et al., High frequency pulses of East Asian monsoon climate in the last two glaciations: Link with the North Atlantic, Climate Dynamics, 1996, 12: 701-709.［11］Guo, Z. T., Peng, S. Z., Wei, L. Y. et al., Weathering signals of Millennial-Scale oscillations of the East Asian Summer monsoon over the last 220 ka, Chinese Science Bulletin, 1999, 44 (supplement 1): 20-25.［12］Ding, Z. L., Yu, Z. W., Rutter, N. W. et al., Towards an orbital time scale for Chinese loess deposits, Quaternary Science Review, 1994,13: 39-70.［13］Duchaufour, Ph., Pedologie, Tome 1: Pedogenese et Classification, Paris-New York-Barcelone-Milan: Masson, 1983, 1-477.［14］Singer, M. J., Bowen, L. H., Verosub, K. L. et al., Mossbauer spectroscopic evidence for citrate-bicarbonate-dithionite ex-traction of maghemite from soils, Clays and Clay Minerals,1995, 43: 1-7.［15］Hunt, C. P., Singer, M. J., Kletetschka, G. et al., Effect of citrate-bicarbonate-dithionite treatment on fine-grained mag-netite and maghemite, Earth Planet. Sci. Lett., 1995, 130: 87-94.［16］Mehra, O., Jackson, M. L., Iron oxide removal from soil and clay by a dithionite-citrate system buffered with sodium bi-carbonate, Clay and Clay Minerals, 1960, 7: 317-327.［17］McKeague, J. A., Manual on soil sampling and methods of analysis, Toronto: Canadian Society of Soil Science, 1981, 1-212.［18］Kukla, G., An, Z. S., Melice, J. L. et al., Magnetic susceptibility record of Chinese loess, Transaction of Royal Society of Edinburgh, Earth Sciences, 1990, 81: 263-288.［19］Guo, Z. T., Wei, L. Y., Lu, H. Y. et al., Changes in the composition of Late Pleistocene aeolian dust and the environmental significance, Quaternary Sciences (in Chinese), 1999, 19(1): 41-48.［20］Heller, F., Liu, X. M., Liu, T. S. et al., Magnetic susceptibility of loess in China, Earth and Planetary Science Letters, 1991,103: 301-310.［21］Yang, J. D., Chen, J., An, Z. S. et al., Variations in 87Sr/86Sr Ratios of calcites in Chinese loess: A proxy for chemical weathering associated with the East Asian Summer monsoon, Palaeogeography Palaeoclimatology Palaeoecology, 2000,157: 151-159.［22］Verosub, K. L., Fine, P., Singer, M. J. et al., Pedogenesis and paleoclimate: Interpretation of the magnetic susceptibility record of Chinese loess-paleosol sequences, Geology, 1993, 21: 1011-1014.［23］Banerjee, S. K., Hunt, C. P., Liu, X., Separation of local signals from the regional paleomonsoon record of the Chinese loess plateau: A rock magnetic approach, Geophys. Res. Lett., 1993, 20: 843-846.［24］Vidic, N. J., TenPas, J. D., Verosub, K. L. et al., Separation of pedogenic and lithogenic components of magnetic suscepti-bility in the Chinese loess/paleosol sequence as determined by the CBD procedure and a mixing analysis, Geophys. J. Int., 2000, 142: 551-562.［25］Deng, C. L., Yuan, B. Y., Zhu, R. X. et al., Magnetic susceptibility of Holocene loess-black loam sequence from Jiaodao, Shanxi, before and after citrate-bicarbonate-dithionite extraction, Chinese Journal of Geophysics (in Chinese), 2000, 43(4): 514-520.［26］Hunt, C. P., Banerjee, S. K., Han, J. M. et al., Rock-magnetic proxies of climate change in the loess-palaeosol sequences of the western Loess Plateau of China, 1995, Geophys. J. Int., 1995, 123: 232-244.［27］Liu, X. M., Liu, T. S., Heller, F. et al., The grain size of magnetic minerals in Chinese loess and its implications for paleo-climate, Science in China (in Chinese), Ser. B, 1991, 21(6): 639-644.［28］Chen, F. H., Bloemendal, J., Feng, Z. D. et al., East Asian monsoon variations during oxygen isotope stage 5: Evidence from the northwestern margin of the Chinese Loess Plateau, Quaternary Science Reviews, 1999, 18: 1127-1135.［29］Pan, B. T., Wang, J. M., Loess record of Qinghai-Xizang Plateau monsoon variations in the eastern part of the plateau since the Last Interglacial, Quaternary Sciences (in Chinese), 1999, 19(4): 330-335.［30］Imbrie, J., Imbrie, J. Z., Modeling the climate response to orbital variation, Science, 1980, 207: 943-953.［31］Liu, T. S., Quaternary Environment (in Chinese), Beijing: Science Press, 1997, 189-239.
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