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File:Fires-in-the-Cenozoic-a-late-flowering-of-flammable-ecosystems-fpls-05-00749-g005.jpg

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English: Examples of the shifts in d13C associated with the rise of savannas from the Late Miocene derived from palaeosols (A)Quade and Cerling (1995), (B)Fox and Koch (2003), and (C) tooth enamel (Cerling et al., 1997). Figure from Osborne (2008; with author’s permission).
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Source Image file from Bond W (2015). "Fires in the Cenozoic: a late flowering of flammable ecosystems". Frontiers in Plant Science. DOI:10.3389/fpls.2014.00749. PMC: 4283521.
Author Bond W
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current22:42, 20 January 2015Thumbnail for version as of 22:42, 20 January 2015709 × 1,355 (100 KB)Recitation-bot (talk | contribs)Automatic upload of media from: doi:10.3389/fpls.2014.00749

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