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Evolution__3rd_Edition

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506 PART 4 / <strong>Evolution</strong> and Diversity<br />

Figure 17.7<br />

Plate tectonics (or, informally,<br />

continental drift). (a) The<br />

movements of the continents<br />

during the past 200 million<br />

years. (b) The positions of the<br />

main tectonic plates today.<br />

Vicariance biogeography predicts<br />

...<br />

(a)<br />

Triassic 200 Myr BP<br />

P a n t h a l a s s a<br />

G o n d w a n a<br />

Equator<br />

Paleocene 65 Myr BP<br />

(b)<br />

L a u r a s i a<br />

Tethys<br />

Cretaceous 125 Myr BP<br />

Oligocene 30 Myr BP<br />

Mid-ocean ridge<br />

Trench-island arc<br />

Fracture zone<br />

midges. These midges are distributed around the southern hemisphere (Figure 17.9).<br />

Brundin reconstructed their phylogeny by standard morphological techniques<br />

(Chapter 15) and then used the species’ modern biogeographic distributions to draw a<br />

combined picture of their phylogeny and biogeography, called an area cladogram<br />

(Figure 17.10). If the successive splits in the phylogeny were driven by successive breakups<br />

of the land, the phylogeny would imply a definable sequence of tectonic events.<br />

To begin with, the common ancestor of the modern forms would have occupied<br />

a large area made up of all their modern distributional zones a which implies the<br />

..

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