Climate as the dominant control on C3 and C4 plant abundance in the Loess Plateau: Organic carbon isotope evidence from the last glacial-interglacial loess-soil sequences-Reference-Cited by-同舟云学术

Climate as the dominant control on C3 and C4 plant abundance in the Loess Plateau: Organic carbon isotope evidence from the last glacial-interglacial loess-soil sequences

Published:2003-06 Issue:12 Volume:48 Page:1271-1276
ISSN:1001-6538
Container-title:Chinese Science Bulletin
language:en
Short-container-title:Chin. Sci. Bull.

Author:

Gu Zhaoyan,Liu Qiang,Xu Bing,Han Jiamao,Yang Shiling,Ding Zhongli,Liu Tungsheng

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://link.springer.com/content/pdf/10.1007/BF03183950.pdf

Reference47 articles.

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3. Ceding, T. E., Hams, J. M., MacFadden, B. J. et al., Global vegetation change through the Miocene/Pliocene boundary, Nature, 1997, 389: 153–158.

4. Kuypers, M. M. M., Pancost, R. D., Damste, J. S. S., A large and abrupt fall in atmospheric CO2 concentration during Cretaceous times, Nature, 1999, 399: 342–345.

5. Street-Perrott, F. A., Huang, Y., Perrott, R. A. et al., Impact of lower atmospheric carbon dioxide on tropical mountain ecosystem, Science, 1997, 278: 1422–1426.

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