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Expansion and contraction of Chinese deserts during the Quaternary

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Abstract

Episodic dune formations during the Quaternary are found in many deserts of China. The causes of desert expansions on different time scales are not the same. Desert extension at about 1.1 and 0.9 Ma ago were the response to the active tectonic movements, whereas the desert evolutions on the ten-thousand years time scale were the response to the orbital scale climatic changes. Spatial scale studies on desert evolution indicate that desert margins shifted greatly during the last glacial maximum (LGM) and the Holocene optimum, its changing from 125°E of the LGM to 105°E of the climatic optimum. Historical desertification in the semiarid China is not a response to climate drought but largely associated with the human impacts (mainly over-cultivation) since about 2300 years ago, which leads to the reworking of the underlying LGM sands.

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References

  1. Rognon, P., Late Quaternary climatic construction for the Magherb (North Africa), Palaeogeography, Palaeoecology, Palaeoclimatology, 1987, 58: 11–34.

    Article  Google Scholar 

  2. Petit-Maire, N., Page, N., Remote sensing and past climatic changes in tropical deserts: example of the Sahara, Episode, 1992, 15: 113–117.

    Google Scholar 

  3. Lancaster, N., Palaeoclimatic evidence from sand seas, Palaeogeography, Palaeoclimatology, Palaeoecology, 1990, 76: 279–290.

    Article  Google Scholar 

  4. Lancaster, N., Relations between dune generations in the Gran Desierto of Mexico, Sedimentology, 1992, 39: 631–644.

    Article  Google Scholar 

  5. Lancaster, N., Tchakerian, V. P., Geomorphology and sediments of sand ramps in the Mojave Desert, Geomorphology, 1996, 17: 151–165.

    Article  Google Scholar 

  6. Chawla, S., Dhir, R. P., Singhvi, A. K., Thermoluminescence chronology of sand profiles in the Thar Desert and their implications, Quaternary Science Reviews, 1992, 11: 25–32.

    Article  Google Scholar 

  7. Forman, S., Goetz, A. F. H., Yuhas, R. H., Large-scale stabilized dunes on the High Plains of Colorado: Understanding the landscape response to Holocene climates with the aid of images from space, Geology, 1992, 20: 145–148.

    Article  Google Scholar 

  8. Nanson, G. C., Price, D. M., Short, S. A. Wetting and drying of Australia over the past 300 ka, Geology, 1992, 20: 791–794.

    Article  Google Scholar 

  9. Madole, R. F., Spatial and temporal patterns of Late Quaternary eolian deposition, Eastern Colorado, U.S.A., Quaternary Science Reviews, 1995, 14: 155–177.

    Article  Google Scholar 

  10. Rendell, H. M., Sheffer, N. L., Luminescence dating of sand ramps in the Eastern Mojave Desert, Geomorphology, 1996, 17: 187–197.

    Article  Google Scholar 

  11. Liu, T. S., Gu, X. F., An, Z. S. et al., The dust fall in Beijing, China on April 18, 1980, Spec. Pap. Geol. Soc. Am., 1981, 186: 149–157.

    Google Scholar 

  12. Sun, J. M., Liu, T. S., Lei, Z. F., Sources of heavy dust fall in Beijing, China on April 16, 1998, Geophys. Res. Lett., 2000, 27: 2105–2108.

    Article  Google Scholar 

  13. Sun, J. M., Zhang, M. Y., Liu, T. S., Spatial and temporal characteristics of dust storms in China and its surrounding regions, 1960–1999: Relations to source area and climate, Journal of Geophysical Research (series D), 2001, 106: 10325–10334.

    Google Scholar 

  14. Liu, T. S., Loess on the Middle Reaches of the Yellow River (in Chinese), Beijing: Science Press, 1964, 132.

    Google Scholar 

  15. Liu, T. S., Loess Deposits in China (in Chinese), Beijing: Science Press, 1965.

    Google Scholar 

  16. Liu, T. S. et al. (Eds), Composition and Texture of Loess (in Chinese). Beijing: Science Press, 1966, 132.

    Google Scholar 

  17. Smalley, I. J., Possible formation mechanisms for the modal coarse-silt quartz particles in loess deposits, Quaternary International, 1990, 7/8: 23–28.

    Article  Google Scholar 

  18. Liu, T. S. et al. Loess and Environment, Beijing: China Ocean Press, 1985, 31–92.

    Google Scholar 

  19. Malier, B. A., Thompson, R., Paleorainfall reconstructions from pedogenic magnetic susceptibility variations in the Chinese loess and paleosols, Quaternary Research, 1955, 44: 383–391.

    Google Scholar 

  20. Guo, B., Zhu, R. X., Yue, L. P. et al., The records of Cobb Mountain magnetic subchron in Chinese loess, Science in China, Ser. D (in Chinese), 1998, 28: 327–333.

    Google Scholar 

  21. Sun, J. M., Liu, T. S. Stratigraphie evidence for the uplift of the Tibetan Plateau between ~1.1 and ~0.9 myr ago, Quaternary Research, 2000, 54: 309–320.

    Article  Google Scholar 

  22. Shackleton, N. J., Pisias, N. G., Atmospheric carbon dioxide, orbital forcing, and climate. Geophysical Monograph Series 32, 1985, 412–417.

    Google Scholar 

  23. Shackleton, N. J., Berger, A., Peltier, W. R., An alternative astronomical calibration of the Lower Pleistocene timescale based on ODP Site 677, Transactions of the Royal Society of Edinburgh: Earth Science, 1990, 81: 251–261.

    Google Scholar 

  24. Shackleton, N. J., Crowhurst, S., Hagelberg, T. et al., Anew late Neogene timescale: Application to leg 138 sites, Proceedings of the Ocean Drilling Program, Scientific Results, 1995a, 138: 73–101.

    Google Scholar 

  25. Shackleton, N. J., Hall, M. A., Pate, D., Pliocene stable isotope stratigraphy of ODP site 846, Proceedings of the Ocean Drilling Program, Scientific Results, 1995b, 138: 337–353.

    Google Scholar 

  26. Shi, Y. F., Zhen, B. X., Li, X. J. et al., Studies on altitude and climate environment in the Middle and East parts of Tibetan Plateau during Quaternary maximum glaciation, Journal of Glaciology and Geocryology (in Chinese), 1995, 17: 97–112.

    Google Scholar 

  27. Sun, J. M., Ding, Z. L., Liu, T. S. et al., 580,000 year environmental reconstruction from eolian deposits at the Mu Us Desert margin, China, Quaternary Science Reviews, 1999, 18: 1351–1364.

    Article  Google Scholar 

  28. Liu, T. S., Ding, Z. L., Stepwise coupling of monsoon circulation to global ice volume variations during the late Cenozoic, Global Planet Change, 1993, 7: 119–130.

    Article  Google Scholar 

  29. Ding, Z. L., Yu, Z. Y., Rutter, N. W. et al., Towards an orbital time scale for Chinese loess deposits, Quaternary Science Reviews, 1994, 13: 39–70.

    Article  Google Scholar 

  30. Hovan, S. A., Rea, D. K., Pisias, N. G., Late Pleistocene continental climate and oceanic variability recorded in Northwest Pacific sediments, Paleoceanography, 1991, 6: 349–370.

    Article  Google Scholar 

  31. Hovan, S. A., Rea, D. K., Pisias, N. G. et al., A direct link between the China loess and marine18O records: Eolian flux to the north Pacific, Nature, 1989, 340: 296–298.

    Article  Google Scholar 

  32. Berger, A., Pleistocene climatic variability at astronomical frequencies, Quaternary International, 1989, 2: 1–14.

    Article  Google Scholar 

  33. Schlesinger, W. H., Reynolds, J. F., Cunningham, G. L. et al., Biological feedbacks in global desertification, Science, 1990, 247: 1043–1048.

    Article  Google Scholar 

  34. Merrill, J. T., Belck, R., Uematsu, M., Meteorological analysis of long-range transport of mineral aerosols over the North Pacific, J. Geophys. Res., 1989, 94: 8584–8598.

    Article  Google Scholar 

  35. Duce, R. A. et al., The atmospheric input of trace species to the world ocean, Global Biogeochem, Cycles, 1991, 5: 193–259.

    Article  Google Scholar 

  36. Rea, D. K., The paleoclimatic record provided by eolian deposition in the deep sea: the geological history of wind, Rev. Geophys., 1994, 32: 159–195.

    Article  Google Scholar 

  37. Wang, P. X., The ice-age China Sea-status and problems, Quaternary Sciences, 1990, 2: 111–124.

    Google Scholar 

  38. Pawluk, S., Bal, S., Micromorphology of selected mollic epipedons (eds. Douglas L. A., Thonpson, M. L.), Soil Micromorphology and Soil Classification, 1985, 63–84.

  39. Gao, Q. Z., Dong, G. R., Zou, X. Y. et al., The Chagelebulu section: A strata record of the advances and retreats of the monsoons in East Asia since Late Pleistocene, Journal of Desert Research, 1996, 16: 112–119.

    Google Scholar 

  40. Sun, J. M., Ding, Z. L., Liu, T. S., Desert distributions during the glacial maximum and climatic optimum: Example of China. Episodes, 1998, 21: 28–31.

    Google Scholar 

  41. Sun, J. M., Origin of eolian sand mobilization during the past 2300 years in the Mu Us Desert, China, Quaternary Research, 2000, 53: 73–88.

    Article  Google Scholar 

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Authors and Affiliations

  1. Institute of Geology and Geophysics, Chinese Academy of Sciences, 100029, Beijing, China

    Dongsheng Liu & Jimin Sun

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  1. Dongsheng Liu
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  2. Jimin Sun
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Liu, D., Sun, J. Expansion and contraction of Chinese deserts during the Quaternary. Sci. China Ser. D-Earth Sci. 45 (Suppl 1), 91–101 (2002). https://doi.org/10.1007/BF02878394

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  • DOI: https://doi.org/10.1007/BF02878394

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