Late Miocene global cooling and the rise of modern ecosystems-Reference-Cited by-同舟云学术

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Late Miocene global cooling and the rise of modern ecosystems

Published:2016-09-26 Issue:11 Volume:9 Page:843-847
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Herbert Timothy D.,Lawrence Kira T.,Tzanova Alexandrina,Peterson Laura Cleaveland,Caballero-Gill Rocio,Kelly Christopher S.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo2813.pdf

Reference63 articles.

1. Schuster, M. et al. The age of the Sahara desert. Science 311, 821 (2006).

2. Dupont, L. M., Rommerskirchen, F., Mollenhauer, G. & Schefuß, E. Miocene to Pliocene changes in South African hydrology and vegetation in relation to the expansion of C4 plants. Earth Planet. Sci. Lett. 375, 408–417 (2013).

3. Arakaki, M. et al. Contemporaneous and recent radiations of the world’s major succulent plant lineages. Proc. Natl Acad. Sci. USA 108, 8379–8384 (2011).

4. Ehleringer, J. R., Cerling, T. E. & Helliker, B. R. C4 photosynthesis, atmospheric CO2 and climate. Oecologia 112, 285–299 (1997).

5. Cerling, T. E. et al. Global vegetation change through the Miocene/Pliocene boundary. Nature 389, 153–158 (1997).

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