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CHAP. xiv.J THE NEOTROPICAL REGION. 57<br />

Buprestidee.—In this family there are no peculiar genera.<br />

All the large South American groups are absent, the only im-<br />

portant and characteristic genus being Stenogaster.<br />

Longicorns.—This important group is largely developed, the<br />

country being well adapted to them ; and their distribution<br />

presents some features of interest.<br />

In the Prionidse there are 6 peculiar genera, the largest being<br />

Holonotus with 3 species ; two others, Derotraclius and Mallaspis,<br />

are characteristic ; 3 more are common to South America, and 1<br />

to Cuba. The Cerambycidse are much more numerous, and there<br />

are 24 peculiar genera, the most important being Sphenothecus,<br />

Entomosterna, and Cyphosterna ; while Crioprosopus and Ifetalep-<br />

tus are characteristic of the sub-region, although extending into<br />

South America ; about 12 Neotropical genera extend to Mexico<br />

or Guatemala, while 12 more stop short, as far as yet known, at<br />

Nicaragua. Lamiidse have a very similar distribution ; 13 genera<br />

are peculiar, the most important being Monilema, Hamatoderus,<br />

and Carneades, wliile Phcea and Lagochirus are characteristic.<br />

About sixteen typical Neotropical genera extend to Mexico, and<br />

15 more only reach Nicaragua, among which are such important<br />

genera as Anisopus, Leptwgus, and Callia.<br />

The land-shells are not sufficiently known to furnish any<br />

corresponding results. They are however mostly of South<br />

American genera, and have comparatively little affinity for those<br />

of the Antilles.<br />

Relations of the Mexican sub -region to the North and South<br />

American Continents.—The sudden appearance of numerous<br />

South American forms of Edentata in temperate North America,<br />

in Post-Tertiary times, as narrated in Chapter VII., together<br />

with such, facts as the occurrence of a considerable number<br />

of identical species of sea fish on the two sides of the Central<br />

American isthmus, render it almost certain that the union of<br />

North and South America is comparatively a recent occur-<br />

rance, and that during the Miocene and Pliocene periods, they<br />

were separated by a wide arm of the sea. The low country<br />

of Nicaragua was probably the part submerged, leaving the<br />

highlands of Mexico and Guatemala still united with the North

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