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404 GEOGRAPHICAL ZOOLOGY. [part iv.<br />

liar ; and it has about 40 peculiar genera in ten families, about<br />

half of these genera belonging to the Scincidse. Only 3<br />

families of almost universal distribution are common to the<br />

Australian and Neotropical regions, with one species of the<br />

American Iguanidse in the Fiji Islands, so that, as far as this<br />

order is concerned, these two regions have little resemblance.<br />

The Neotropical region has 15 families, 6 of which are peculiar<br />

to it, and it possesses more than 50 peculiar genera. These ai-e<br />

distributed among 12 families, but more than half belong to the<br />

Iguanidse, and half the remainder to the Teidee,—the two families<br />

especially characteristic of the Neotropical region. All the Ne-<br />

arctic families which are not of almost universal distribution are<br />

peculiarly Neotropical, showing that the Lacertilia of the former<br />

region have probably been derived almost exclusively from the<br />

latter.<br />

On the whole the distribution of the Lacertilia shows a<br />

remarkable amount of specialization in each of the great tropical<br />

regions, whence we may infer that Southern Asia, Tropical<br />

Africa, Australia, and South America, each obtained their original<br />

stock of this order at very remote periods, and that there has<br />

since been little intercommunication between them. The peculiar<br />

affinities indicated by such cases as the Lepidosternidse, found<br />

only in the tropics of Africa and South America, and Tachydromiis<br />

in Eastern Asia and West Africa, may be the results either of<br />

once widely distributed families surviving only in isolated locali-<br />

ties where the conditions are favourable,—or of some partial and<br />

temporary geographical connection, allowing of a limited degree<br />

of intermixture of faunas. The former appears to be the more<br />

probable and generally efficient cause, but the latter may have<br />

operated in exceptional cases.<br />

Fossil Lacertilia.<br />

These date back to the Triassic period, and they are found in<br />

most succeeding formations, but it is not till the Tertiary period<br />

that forms allied to existing genera occur. These are at present<br />

too rare and too ill-defined to throw much light on the geo-<br />

graphical distribution of the order.

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