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Evolution__3rd_Edition

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..<br />

Dispersal is enabled by various<br />

physical factors ...<br />

. . . which may be accidental<br />

CHAPTER 17 / <strong>Evolution</strong>ary Biogeography 497<br />

average to the south. In practice, though, individuals would move southwards as well<br />

and extend the species range as they did so. If a species originated in one area and<br />

subsequently dispersed to fill out its existing distribution, the place where it originated<br />

is called its center of origin.<br />

Various dispersal routes might have been followed in the biogeographic history of a<br />

species. Simpson distinguished dispersal by means of corridors, filter bridges, and sweepstakes.<br />

Two places are joined by a corridor if they are part of the same land mass a<br />

Georgia and Texas, for example. Animals can move easily along a corridor and any two<br />

places joined by a corridor will have a high degree of faunal similarity. A filter bridge is<br />

a more selective connection between two places, and only some kinds of animals will<br />

manage to pass over it. For instance, when the Bering Strait was above water, mammals<br />

moved from North America to Asia and vice versa, but no South American mammals<br />

moved to Asia and no Asian species moved to South America. The reason is presumably<br />

that the land bridges at Alaska and Panama were so far apart, so narrow, and so different<br />

in ecology that no species managed to disperse across them. Finally, sweepstakes<br />

routes are hazardous or accidental dispersal mechanisms by which animals move from<br />

place to place. The standard examples are island hopping and natural rafts. Many<br />

land vertebrates live in the Caribbean Islands, and (if their biogeography is correctly<br />

explained by dispersal) they might have moved from one island to other, perhaps being<br />

carried on a log or some other sort of raft.<br />

There is good evidence for the power of dispersal. In 1883, for example, a volcanic<br />

eruption covered the small Indonesian island of Krakatau with ash and killed all the<br />

plants and animals. Biologists then recorded the recolonization of the island, particularly<br />

for birds and plants. The recolonization was astonishingly rapid. Fifty years later,<br />

the island was already recovered with tropical forest, which supported 271 plant species<br />

and 31 bird species. Invertebrate animals, such as insects, had come too, though their<br />

numbers were less closely monitored. The immigrants mainly came from the neighboring<br />

islands of Java (25 miles (40 km) away) and Sumatra (50 miles (80 km) away);<br />

the birds would have dispersed by active flight and the plants would have been carried<br />

as seeds. Dispersal, therefore, in the right circumstances can have a clear effect on the<br />

ranges of species.<br />

17.4 Geographic distributions are influenced by climate,<br />

such as in the ice ages<br />

The current geological age is called the Quaternary, which began 2.5 million years<br />

ago (see Section 18.2, p. 525, for geological time). During the Quaternary, the climate<br />

has mainly been cooler than in the preceding Tertiary, and the temperature has cycled<br />

up and down. Many of the cooler times have been glacial periods, and the warmer<br />

times interglacials. These climatic changes have happened recently enough for the fossil<br />

record in some cases to be revealingly complete. When the weather turns cool, the<br />

ranges of animal and plant species tend to contract and move south (in the northern<br />

hemisphere). At any one site, the local ecology changes to one characteristic of the<br />

cooler climate. A change from a temperate to a tundra-type ecosystem, for example,

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