Abstract
A paleosol dated for about 500–700 kaBP and developed on a glacial deposit at ∼3 000 m a.s.l. in the Yulong Mountains is studied using soil chemical, morphological and mineralogical methods. The analytical results indicate that this soil was formed under tropical and humid conditions and can be classified as red soil, which cannot be formed in the present alpine environment at the studied site. This implies that the southeast margin of the Tibetan Plateau has experienced intense uplift since the formation of the paleosol. According to the necessary conditions for the formation of the modern red soil in China, we estimate that the uplift height of the Plateau since 500–700 kaBP would have exceeded 800 m.
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Miller, K. G., Fairbanks, R. G., Tertiary oxygen isotope synthesis, sea-level history, and continental margin erosion, Paleoceanography, 1987, 2(1): 1.
Flower, B. P., Kennett, J. P., Middle Miocene ocean-climate transition: high-resolution oxygen and carbon isotopic records from Deep Sea Drilling Project site 588A, southwest Pacific, Paleoceanography, 1993, 8(6): 811.
Ruddiman, W. F., Kutzbach, J. E., Forcing of the late Cenozoic Northern Hemisphere climate by plateau left in Southern Asia and the American West, Journal of Geophysical Research, 1989, 94(D15): 18409.
Liu, T. S., Zheng, M. P., Guo, Z. T., Initiation and evolution of the Asian monsoon system timely coupled with the ice-sheet growth and the tectonic movements in Asia, Quaternary Sciences (in Chinese), 1998(3): 194.
Raymo, M. E., Ruddiman, W. F., Froelich, P. N., The influence of late Cenozoic mountain building on oceanic geochemical cycle, Geology, 1988, 16(7): 649.
Manabe, S., Terpstra, T. B., The effects of mountains on the general circulation of the atmosphere as identified by numerical experiments, Journal of the Atmospheric Sciences, 1974, 31(1): 3.
Prell, W. L., Kutzbach, J. E., Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution, Nature, 1992, 360: 647.
Ramstein, G., Fluteau, F., Besse, J. et al., Effect of orogeny, plate motion and land-sea distribution on Eurasian climate change over the past 30 million years, Nature, 1997, 386: 788.
Ruddiman, W. F., Tectonic Uplift and Climate Change, New York: Plenum Press, 1997, 1–233.
Gao, Y. X., Chen, H. Z., Wu, Z. D., The relationship between the paleosols and the uplift of the Tibetan Plateau, in Studies on the Period, Amplitude and Type of the Uplift of the Qinghai-Tibetan Plateau (ed. The Comprehensive Scientific Expedition to the Qinghai-Tibetan Plateau, Academia Sinica) (in Chinese), Beijing: Science Press, 1981, 90–101.
Zhao, X. T., Qu, Y. X., Li, T. S., Pleistocene glaciations along the eastern foot of the Yulong Mountains, Journal of Glaciology and Geocryology (in Chinese), 1999, 21(3): 242.
Wu, Z. Y., Zhu, Y. C., The Vegetation in Yunnan (in Chinese), Beijing: Science Press, 1987, 770–789.
The Nanjing Institute of Soils Sciences, Academia Sinica, The Physical and Chemical Analysis of Soils (in Chinese), Shanghai: Shanghai Scientific and Technological Press, 1978, 169–176.
Stoops, G. J., Buol, S. W., Micromorphology of Oxisols, in Soil Micromorphology and Soil Classification (eds. Douglas, L. A., Thompson, M. L.), Madison: SSSA Special Publication, 1985, 105–120.
Duchaufour, Ph. Pédologie, Tome 1 Pédogenése et Classification, Paris, New York, Barcelone, Milan: Masson, 1983, 1–477.
The Nanjing Institute of Soils Sciences, Academia Sinica, Soils in China (in Chinese), Beijing: Science Press, 1978, 441–520.
Zhou, S. Z., Zhang, R. Y., Zhang, C., Meteorology and Climatology (in Chinese), Beijing: Higher Education Press, 1984, 63–69.
Kaiser, K., The climates of Europe during the Quaternary ice age, in Quaternary Geology and Climate (ed. Wright, H. E. Jr.), Washington D. C: National Academy of Sciences, 1969, 10–37.
Shi, Y. F., Zheng, B. X., Li, S. J. et al., Studies on altitude and climatic environment in the middle and east parts of the Tibetan Plateau during Quaternary Maximum Glaciation, Journal of Glaciology and Geocryology (in Chinese), 1995, 17(2): 97.
Guo, Z. T., Liu, T. S., Fedoroff, N. et al., Climate extremes in loess of China coupled with the strength of deep-water formation in the North Atlantic, Global and Planetary Change, 1998, 18: 113.
CLIMAP Project Members, The surface of the ice-age Earth, Science, 1976, 191: 1131.
Wang, S. M., Shi, Y. F., Shen, J. et al., Preliminary study on the paleoclimate and paleoevironment evolution of the east of Qinghai-Tibetan Plateau since 800 kaBP, in Annual of the Development and Evolution, Environment Variations and Biosystem on the Qinghai-Tibetan Plateau (ed. Qinghai-Tibetan Plateau Project Members) (in Chinese) (1994), Beijing: Science Press, 1995, 236–248.
Wu, X. H., Wang, F. B., An, Z. S. et al., Episodic uplifts of the Qinghai-Tibetan Plateau and its corresponding altitude during the Late Cenozoic, in Loess, Quaternary Geology and Global Change Part III (eds. Liu, T. S., An, Z. S.) (in Chinese), Beijing: Science Press, 1992, 1–13.
Li, J. J., Uplift of Qinghai-Xizang (Tibet) Plateau and Global Change, Lanzhou: Lanzhou University Press, 1995, 1 110.
Yang, D. Y., The Quaternary dust-fall accumulation and the monsoon variability in eastern China, Quaternary Sciences (in Chinese), 1991(4): 354.
Guo, Z. T., Liu, T. S., Fedoroff, N. et al., Shift of the monsoon intensity on the Plateau at ca. 0.85 MaBP, Chinese Science Bulletin, 1993, 38: 586.
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Guo, Z., Yao, X., Zhao, X. et al. A tropical paleosol at high elevation in the Yulong Mountains and its implication on the uplift of the Tibetan Plateau. Chin.Sci.Bull. 46, 69–72 (2001). https://doi.org/10.1007/BF03183213
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DOI: https://doi.org/10.1007/BF03183213