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

other. About this same time (but perhaps not contemporaneously)<br />

Madagascar must have been connected with some<br />

portion of Southern Africa, and the whole of the country would<br />

possess no other Primates but Lemuroidea. After the Mada-<br />

gascar territory (very much larger than the existing island)<br />

had been separated, a connection appears to have been long<br />

maintained (probably by a northerly route) between the more<br />

equatorial portions of Asia and Africa ; till those higher forms<br />

had become developed, which were afterwards differentiated into<br />

Simia, Presbytes, and Cijnopithecus, on the one hand, and into<br />

Troglodytes, Colobus, and Cynocephalus, on the other. In ac-<br />

cordance with the principle of competition so well expounded<br />

by Mr. Darwin, we can understand how, in the vast Asiatic and<br />

African area north of the Equator, with a great variety of<br />

physical conditions and the influence of a host of competing<br />

forms of life, higher types were developed than in the less<br />

extensive and long-isolated countries south of the Equator.<br />

In Madagascar, where these less complex conditions prevailed<br />

in a considerable land-area, the lowly organized Lemuroids have<br />

diverged into many specialized forms of their own peculiar type<br />

while on the continents they have, to a great extent, become<br />

exterminated, or have maintained their existence in a few cases,<br />

in islands or in mountain ranges. In Africa the nocturnal and<br />

arboreal Galagos are adapted to a special mode of life, in which<br />

they probably have few competitors.<br />

How and when the ancestors of the Cebidse and Hapalidse<br />

entered the South American continent, it is less easy to conceive.<br />

The only rays of light we yet have on the subject are, the<br />

supposed affinities of the fossil Cmnopithecns of the Swiss, and<br />

the LemuravidsB of the North American Eocene, with both<br />

Cebidae and Lemuroids, and the fact that in Miocene or Eocene<br />

times a mild climate prevailed up to the Arctic circle. The dis-<br />

covery of an undoubted Lemuroid in the Eocene of Europe,<br />

indicates that the great Northern Continent was probably the<br />

birthplace of this low type of mammal, and the source whence<br />

Africa and Southern Asia were peopled with them, as it was,<br />

at a later period, with the higher forms of monkeys and apes.<br />

;

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