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Plate tectonics drive tropical reef biodiversity dynamics

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Figure

Figure 1 | Distribution of shallow and deep ocean sea floor across the past 140 Myr. The latitudinal tropical limit was obtained from the fossil distributionof coral species
Figure 2 | Hopping biodiversity hotspots. Shown are the hopping hotspot observed from coral fossils (left) and simulated with the parapatric model20 Ma:(right) for three time periods, Eocene (a), Miocene (b) and Quaternary/current (c)
Figure 3 | Nestedness pattern in the Central Indo-Pacific region. Observed (cells from the most species-rich cells (red) to the less species-rich ones (blue)

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