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. 2013 May 30;112(1):151–160. doi: 10.1093/aob/mct106

Fig. 5.

Fig. 5.

Occurrence of dispersal events through time for the sapindaceous clade inferred by the Lagrange analyses (grey bars). Climatic oscillations (blue lines), estimated from the variation of oxygen-18 isotope concentration through time, is also displayed (Zachos et al., 2001). Ma, million years ago.