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Climate and soil moisture environment during development of the fifth palaeosol in Guanzhong Plain

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Abstract

Based on weathering characteristics of the fifth palaeosol layer (S5) of four sections in Guanzhong Plain, the thickness of the weathered profile of the paleosol is determined to be greater than the ordinary soil, a weathered and leached loess layer thicker than 2 m. The distribution depth of the red argillans, the weathered and leached loess layer, Fe2O3, CaCO3 and Sr content under the S5 all indicate that the precipitation in Guanzhong Plain was over 900 mm at that time. The distribution depth of gravity water zone reached 4.2 m at least, and the soil moisture content was generally more than 20% within the range of 4.2 m. At that time there was sufficient soil moisture and no dried earth layer developed in Guanzhong Plain, suitable for the forest to develop. When this soil developed, the mean annual precipitation was more than the annual soil moisture evaporation. The value of soil moisture balance was positive and the atmospheric precipitation could supply the underground water normally. Soil water was weak acidic in the middle and late stages when S5 developed in Guanzhong Plain. It was a kind of subtropical climate and even more humid and warmer than the northern edge of the subtropical climate zone in Guanzhong Plain when the S5 developed. At that time the subtropical climate was prevailing over the northern side and southern side of Qingling Mountains, showing the Mountains no longer to be the boundary between the subtropical zone and the temperate zone in China. The summer monsoon acted intensely and could go over Qingling Mountains frequently bring abundant precipitation.

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References

  1. Liu T S. Loess and Environment (in Chinese). Beijing: Science Press, 1985. 350–351

    Google Scholar 

  2. Guo Z T, Liu D S, Fedoroff N, et al. Climate extremes in loess of China coupled with the strength of deep-water formation in the North Atlantic. Glob Planet Change, 1998, 18: 113–128

    Article  Google Scholar 

  3. Ding Z L, Yu Z W, Rutter N, et al. Towards an orbital time scale for Chinese loess deposits. Quat Sci Rev, 1994, 13: 39–70

    Article  Google Scholar 

  4. Kohfeld K E, Harrison S P. Glacial-interglacial changes in dust deposition on the Chinese Loess Plateau. Quat Sci Rev, 2003, 22: 1859–1878

    Article  Google Scholar 

  5. Porter C, An Z S. Episodic gullying and paleomonsoon cycles on the Chinese Loess Plateau. Quat Res, 2005, 64: 234–241

    Article  Google Scholar 

  6. Thomas S, David S G, Thomas S J, et al. Reinterpreting climate proxy records from late Quaternary Chinese loess: A detailed OSL investigation. Earth-Sci Rev, 2007, 80: 111–136

    Article  Google Scholar 

  7. Lu H Y, Zhang F Q, Li X D. Periodicities of paleoclimatic variations recorded by loess-paleosol sequence in China. Quat Sci Rev, 2004, 23: 1891–1900

    Article  Google Scholar 

  8. Kukla G J, Heller F, Liu X M, et al. Pleistocene climates in China dated by magnetic susceptibility. Geology, 1998, 16: 811–814

    Article  Google Scholar 

  9. Zhao J B. Formation of loess and division of climate cycles. J Desert Res (in Chinese), 2002, 22(3): 257–261

    Google Scholar 

  10. Ding Z L, Liu D S, Liu X M, et al. Thirty seven climatic cycles in the last 2.5 Ma. Chin Sci Bull, 1990, 35(8): 666–671

    Google Scholar 

  11. Lu H Y, An Z S. The paleoclimatic significance of grain size loess-paleosol deposit in Chinese Loess Plateau. Sci China Ser D-Earth Sci, 1998, 41(6): 626–631

    Article  Google Scholar 

  12. Sun D H, An Z S, Wu X H. Evolution of the summer monsoon regime over the Loess Plateau of the last 150 ka. Sci China Ser D-Earth Sci, 1996, 39(5): 503–511

    Google Scholar 

  13. Zhou X, Guo Z T, Peng S Z, et al. Variations of paleo-weathering intensity of the Wucheng loess formation at Xifeng and the implications on environmental changes. Quat Sci (in Chinese), 2007, 27(4): 645–650

    Google Scholar 

  14. Lu H Y, An Z S, Liu H B, et al. Periodicity of East Asian winter and summer monsoon variation during the past 2500 ka recorded by loess deposits at Luochuan on the central Chinese Loess Plateau. Geol Rev (in Chinese) 1998, 44(5): 553–557

    Google Scholar 

  15. An Z S, Wei L Y, Lu Y C. A study on soil stratigraphy in Luochuan loess section. Quat Sci (in Chinese), 1985, 6(1): 166–174

    Google Scholar 

  16. Zhao J B. The study on the red soil of Neogene in Xi’an and Baode in Shanxi. Acta Sediment Sin (in Chinese), 1989, 7(3): 113–120

    Google Scholar 

  17. Sun D H, Liu D S, Chen M Y, et al. Magnetostratigraphy and paleoclimate of red clay sequence from Chinese Loess Plateau. Sci China Ser D-Earth Sci, 1997, 40(4): 337–343

    Article  Google Scholar 

  18. Ding Z L, Rutter N W, Liu X M, et al. Re-arrangement of atmospheric circulation at about 2.6 Ma over northern China: Evidence from grain size records of loess-paleosol ang red clay sequences. Quat Sci Rev (in Chinese), 1994, 19: 547–558

    Article  Google Scholar 

  19. Guo Z T, Ruddiman W F, Hao Q Z, et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in china. Nature, 2002, 416: 159–163

    Article  Google Scholar 

  20. Tang K L. Micromorphology and genesis of buried paleosol in loess deposits of Wugong County, Shaanxi Province. Chin Sci Bull, 1983, (Spec issue): 172–175

  21. An Z S, Wei L Y. The reason and significance of deposition iron’s clay adhesive. Chin Sci Bull (in Chinese), 1979, 24(8): 356–359

    Google Scholar 

  22. Xiong Y, Li Q K. Soil of China (in Chinese). Beijing: Science Press, 1987. 67–82

    Google Scholar 

  23. Liu Y J, Cao L M, Li Z L, et al. Geochemistry of Element (in Chinese). Beijing: Science Press, 1984. 360–365

    Google Scholar 

  24. Li T J, Zheng Y S. Wang Y. Geography of Soil (in Chinese). Beijing: Higher Education Press, 1983. 134–151

    Google Scholar 

  25. Huang X Q, Li H M, Jin B X. Hydrology (in Chinese). Beijing: Higher Education Press, 1998. 228–236

    Google Scholar 

  26. Zhao J B. Karst processes in loess strata between 500 and 10 ka BP in the Guanzhong Plain. Geol Rev (in Chinese), 1999, 45(5): 548–554

    Google Scholar 

  27. Zhao J B. The new theory on Quaternary environmental research. J Geogr Sci (in Chinese), 2004, 14(2): 242–250

    Google Scholar 

  28. Yang W Z, Shao M A. Soil Moisture Research in Loess Plateau (in Chinese). Beijing: Science Press, 2000. 67–93

    Google Scholar 

  29. Du J, Zhao J B. Research on moisture content and moisture restore in different vegetation in Xi’an area. J Soil Water Conserv (in Chinese), 2006, 20(6): 60–63

    Google Scholar 

  30. Chen B Q, Zhao J B, Li Y H. Research of soil water character below artificial forest of the rany year in Luochuan area of Yan’an. Arid Land Geogr (in Chinese), 2006, 29(4): 532–536

    Google Scholar 

  31. Zhao J B, Du J, Zhou Q, et al. The dried soil layers under apple trees plantation of in Xi’an. Acta Ecol Sin (in Chinese), 2005, 25(8): 2115–2120

    Google Scholar 

  32. Zhao J B, Sun G Z, Yue Y L, et al. Research of dried earth layer and its formation in the artificial forest land in Guanzhong Plain. Geogr Res (in Chinese), 2007, 26(4): 764–772

    Google Scholar 

  33. Zhu H J, He Y G. Geography of Soil (in Chinese). Beijing: Higher Education Press, 2001. 42–43

    Google Scholar 

  34. Yang W Z. Soil water resources and afforestation in the Loess Plateau. J Nat Resour (in Chinese), 2001, 16(5): 433–438

    Google Scholar 

  35. Li Y S. Effects of forest on water circle on the Loess Plateau. J Nat Resour (in Chinese), 2001, 16(5): 428–432

    Google Scholar 

  36. Wang L, Shao M A, Hou Q C. A study on quantitative index of dried soil layers. J Soil Water Conserv (in Chinese), 2000, 14(4): 87–90

    Google Scholar 

  37. Lin B H, Liu R M. Stable isotope evidence on summer monsoon change in recent 800 ka in the Loess Plateau. Chin Sci Bull, 1992, 37(18): 1691–1693

    Google Scholar 

  38. Sun X J, Song C Q, Wang F Y, et al. Vegetation history of the southern Loess Plateau of China during the last 100000 years based on pollen date. Acta Bot Sin (in Chinese), 1996, 38(12): 982–988

    Google Scholar 

  39. Zhao J B. Vegetation and climate during development of reddish-brown fossil soil layer. Chin Sci Bull, 1985, 30(2): 215–218

    Google Scholar 

  40. Tang K L, He X B. Rediscussion on loess paleosol evolution and climatic change on the Loess Plateau during the Holocene. Quat Sci (in Chinese), 2004, 24(2): 129–138

    Google Scholar 

  41. Lu H Y, Liu D S, Wu N Q, et al. Phytolith record of vegetation succession in the southern Loess Plateau since Late Pleistocene. Quat Sci (in Chinese), 1999, 19(4): 336–347

    Google Scholar 

  42. Guo Z T, Liu D S, An Z S. Paleosols of the last 0.15 Ma in the Weinan loess section and their paleoclimatic significance. Quat Sci (in Chinese), 1994, 14(3): 256–269

    Google Scholar 

  43. Zhu Z C. The discussion on difficulty problem in paleovegetation in loess strata. Chin Sci Bull, 1982, (24): 1515–1518

  44. Zhao J B. Paleosol developed and paleoenvironment in the Guanzhong Plain during 420–350 ka BP. Acta Geogr Sin (in Chinese), 2005, 60(1): 32–40

    Google Scholar 

  45. Fedoroff N, Goldberg P. Comparative micromorphology of two Late Pleistocene paleosols (in the Paris Basin). Catena, 1982, 9: 227–251

    Google Scholar 

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Authors and Affiliations

  1. College of Tourism and Environment Sciences, Shaanxi Normal University, Xi’an, 710062, China

    JingBo Zhao, Jing Gu & Juan Du

  2. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, 710075, China

    JingBo Zhao & Jing Gu

Authors
  1. JingBo Zhao
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  2. Jing Gu
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  3. Juan Du
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Correspondence to JingBo Zhao.

Additional information

Supported by the National Natural Science Foundation of China (Grant No. 40672108) and State Key Laboratory of Loess and Quaternary Geology, Chinese Academy of Sciences (Grant No. SKLLQ0605)

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Zhao, J., Gu, J. & Du, J. Climate and soil moisture environment during development of the fifth palaeosol in Guanzhong Plain. Sci. China Ser. D-Earth Sci. 51, 665–676 (2008). https://doi.org/10.1007/s11430-008-0047-y

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  • DOI: https://doi.org/10.1007/s11430-008-0047-y

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