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Volume 17 Issue 4
Dec 2006
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Article Contents
Zhizhong ZHAO, Fuchu JIANG, Xihao WU, Shubing WANG, Yansong QIAO, Ke LIU, Sumin WANG. Sanmenxia Loess and Paleoenvironmental Change. Journal of Earth Science, 2006, 17(4): 283-290.
Citation: Zhizhong ZHAO, Fuchu JIANG, Xihao WU, Shubing WANG, Yansong QIAO, Ke LIU, Sumin WANG. Sanmenxia Loess and Paleoenvironmental Change. Journal of Earth Science, 2006, 17(4): 283-290.

Sanmenxia Loess and Paleoenvironmental Change

Funds:

the China Geological Survey 200312300034

the Ministry of Land and Resources of China 20010209

More Information
  • Corresponding author: Zhao Zhizhong: zhaozz@cags.net.cn
  • Received Date: 10 Jun 2006
  • Accepted Date: 25 Sep 2006
  • The Caocun (曹村) loess profile of Zhangbianyuan (张汴塬) is located at the southeast margin of the Loess Plateau, which is a typical representative of loess stratum in the Sanmenxia (三门峡) area. In the 145 m thick profile, a loess-paleosol sequence occurs from L1 to L33, underlain by a red clay bed. The B/M boundary was recorded at the bottom of L7, the Jaramillo event at S11 to S12, the Olduval event at L23 to L26, and the M/G boundary at the bottom of L33 near the red clay. The magnetic susceptibility of the loess deposits, as well as the carbonate and granularity components, indicates that there have been many periodic paleoclimate changes, including a total of 13 cold events that each lasted more than 40 000 a. A high-resolution chronostratigraphic profile has been established using an age model according to grain characteristics. A clear correlation exists between records of the paleomonsoon in the Caocun loess succession and SPECMAP from 3×105 a B.P. to the present. The Caocun profile can act as a control site in the southeastern Loess Plateau. Its paleoenvironmental records relate to eastern Asian paleomonsoon theory.

     

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  • An, Z. S., 1987. Loess-Paleosol Sequences and Chronology at Lantian Man Localities: Aspects of Loess Research. China Ocean Press, Beijing. 192-203 (in Chinese).
    An, Z. S., Kukla, G., Liu, T. S., 1989. Loess Stratigraphy in Luochuan. Quaternary Research, (2): 155-168.
    An, Z. S., Liu, D. S., Lu, Y. C., et al., 1990. The LongTerm Paleomosoon Variation Recorded by the LoessPaleosol Sequence in Central China. Quaternary International, 7/8: 91-95. doi: 10.1016/1040-6182(90)90042-3
    An, Z. S., Wu, X. H., Wang, P. X., et al., 1991a. Paleomonsoonin China since Recent 130 ka (Ⅰ): Paleomonsoon Record. Sciencein China (Series D), (10): 1076-1084 (in Chinese).
    An, Z. S., Kukla, G. J., Porter, S. C., et al., 1991b. Magnetic Susceptibility Evidence of Monsoon Variation on the Loess Plateau of Central China during the Last 130000 Years. Quaternary Research, 36: 29-36. doi: 10.1016/0033-5894(91)90015-W
    Cande, S. C., Kent, D. V., 1995. Revised Geomagnetic Polarity Time Scale for the Late Cretaceous and Cenozoic. Journal of Geophysical Research, 100 (B4): 6093-6095. doi: 10.1029/94JB03098
    Ding, Z. L., Liu, T. S., 1989. Progresses of Loess Research in China (Part1): Loess Stratigraphy. Quaternary Sciences, (1): 24-35 (in Chinese with English Abstract).
    Ding, Z. L., Yu, Z. W., Liu, T. S., 1991. The New Development of Loess Studies in China (3): Time-Scale. Quaternary Sciences, (4): 336-341 (in Chinese with English Abstract).
    Heller, F., Liu, T. S., 1984. Magnetism of Chinese Loess Deposits. Geophys. Res. Lett. , 13: 1169-1172.
    Jiang, F. C., Wu, X. H., Sun, D. H., et al., 1998. Loess Stratigraphy of Mangshan, Zhongyuan. Journal of Geomechanics, (4): 12-18 (in Chinese with English Abstract).
    Kukla, G., An, Z. S., Liu, T. S., 1990. Loess Stratigraphy in the Middle of China: Loess, Quaternary Geology and Global Change (PartⅡ). Science Press, Beijing. 115-133.
    Liu, T. S., 1985. Loess and Environment. Science Press, Beijing. 107-109 (in Chinese).
    Liu, X. M., Liu, T. S., Xu, T. C., et al., 1988. The Chinese Loess in Xifeng (Ⅰ): The Primary Study on Magnetostratigraphy of a Loess Profile in Xifeng Area, Gansu Province. Geophys. J. , 92: 345-348. doi: 10.1111/j.1365-246X.1988.tb01146.x
    Lu, Y. C., 1981. CaCO3 Content Change of Loess Stratigraphy and Climate Cycle in Pleistocene. Scientia Geologica Sinica, (2): 122-131 (in Chinese with English Abstract).
    Martinson, D. G., Pisia, N. G., Hays, J. D., et al., 1987. Age Dating and the Orbital Theory of the Ice Ages: Development of a High-Resolution 0 to 300000-Year Chronostratigraphy. Quaternary Research, (27): 1-29.
    Porter, S. C., An, Z. S., 1995. Correlation between Climate Events in the North Atlantic and China during the Last Glaciation. Nature, 375: 305-308. doi: 10.1038/375305a0
    Rutter, N. W., 1992. Loess in China and Global Change. Translated by Ding, Z. L. . Quaternary Sciences, (1): 2-11 (in Chinese).
    Sun, J. Z., Zhao, J. B., 1991. Quaternary of Loess Plateauin China. Beijing Science and Technology Press, Beijing. 23-26 (in Chinese).
    Teng, Z. H., 1988. Two Loess Profiles and Their Stratigraphic Division in the Western Henan. Stratigraphy Magazine, 12 (4): 290-297 (in Chinese with EnglishAbstract).
    Wang, S. B., Jiang, F. C., Wu, X. H., 1999. Paleomonsoon Events fromthe Last Glacial Stagein Sanmenxia Area to the Early of Holocene Epoch. Acta Geoscientica Sinica, (4): 433-437 (in Chinese with English Abstract).
    Wen, Q. Z., 1989. Geochemistry of Loess in China. Science Press, Beijing. 143-146 (in Chinese).
    Wu, X. H., An, Z. S., Wang, S. M., 1997. Loess and Paleomonsoon. Earth Science Frontiers, 4 (1-2): 77-78 (in Chinese with English Abstract).
    Wu, X. H., Jiang, F. C., Xiao, H. G., et al., 1999. Mangshan Loess of Zhongyuan and Tectonic Movement since Recent 200 ka as Well as Climate Change. Science in China (Series D), (1): 75-81 (in Chinese).
    Xiao, H. G., Jiang, F. C., Wu, X. H., et al., 1997. Loess Stratigraphy of Sanmenxia Area: Loess, the Yellow River and the Yellow River Culture. Yellow River Hydraulic Publishing House, Zhengzhou. 1-7 (in Chinese).
    Xiao, J. L., Zheng, H. B., Zhao, H., 1992. Variation of Winter Monsoon Intensity on the Loess Plateau, Central China during 130000 Years: Evidence from Grain Size Distribution. Quaternary Research, 31: 13-19. doi: 10.4116/jaqua.31.13
    Xie, F. C., Jiang, Z. F., 1987. The Basic Character of the Loess in the Western Henan. Henan Geology, 5 (3): 42-48 (in Chinese).
    Yue, L. P., 1985. Study on Paleomagnetics of Shan County and Xifeng Profiles: The New Development of Loess Studies in China. Shaanxi People's Publishing House, Xi'an (in Chinese).
    Yue, L. P., 1984. Study on Paleomagnetics of the Loess Profile of Zhangbianyuan, Shaan County. Journal of Northwest University, (4): 79 (in Chinese with English Abstract).
    Yue, L. P., Xue, X. X., 1996. Paleomagnetism of Loess in China. Beijing Science and Technology Press, Beijing. 38-40 (in Chinese).
    Zheng, H. B., An, Z. S., Shaw, J., et al., 1992. Magnetostratigraphic Research of the Loess Profile at the Duanjiabo: Loess, Quaternary Geology and Global Change (Ⅲ). Science Press, Beijing. 44-61 (in Chinese with English Abstract).
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