Carbon isotopic composition of modern soil and paleosol as a response to vegetation change on the Chinese Loess Plateau

Author:

Liu Weiguo,Ning Youfeng,An Zhisheng,Wu Zhenghai,Lu Huayu,Cao Yunning

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference31 articles.

1. Liu, T. S., Loess and the Environment (in Chinese), Beijing: Ocean Press, 1985, 44–106.

2. An, Z. S., Kukla, G., Porter, S. C. et al., Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years, Quaternary Research, 1991, 36: 29–36.

3. An Zhisheng, Wang Sumin, Wu Xihao et al., Eolian evidence from the Chinese Loess Plateau the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qing-Xizhang Plateau uplift forcing, Science in China, Ser. D, 1999, 42(3): 258–271.

4. Lu Huayu, An Zhisehng, Paleoclimateic implication of grain size of loess-paleosol deposit in Chinese Loess Plateau, Science in China, Ser. D, 1998, 41(6): 626–631.

5. Lin Benhai, Liu Rongmo, The stable isotope evidence of the variance of the Summer Monsoon in the Loess Plateau from recent 800ka, Chinese Science Bulletin (in Chinese), 1992, (18): 1691–1693.

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