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157. Modes of distribution.-The means and modes of migration and distribution are obvious in the case of animals that can fly or swim or make long journeys on foot. An island can be visited and become peopled by birds from the nearest mainland. Fishes and marine mammals can travel from ocean to ocean. But many animals have no means of crossing watery barriers. "Oceanic islands, that have been formed de novo in mid-ocean and are not detached portions of pre-existing continents, are almost invariably free from such animals as are incapable of traversing the sea. If sufficiently distant from any continent, oceanic islands are generally without mammals, reptiles, and amphibia, but have both birds and insects and certain other invertebrates which are transported to them by involuntary migration."

As suggested in the last sentence, migration may be passive or involuntary. For example, those minute animals that can become dried up and yet retain the power of renewing their active life under favorable conditions are sometimes carried in the dried mud adhering to the feet of birds, and may thus become widely distributed. Parasites are carried by their hosts in all their wanderings. Some animals, as rats and mice, are carried by ships and railway trains and thus widely distributed.

158. Fauna and faunal areas.—The term fauna is applied to the animals of any region considered collectively. Thus the fauna of Illinois comprises the entire list of animals found naturally in that State. It includes the aboriginal men, the black bear, the fox, and all its animal life down to the Amaba. The relation of the fauna of one region to that of another depends on the ease with which barriers may be crossed. Thus the fauna of Illinois differs little from that of Indiana or Iowa, because the State contains no barriers that animals may not readily pass. On the other hand, the fauna of California or Colorado differs materially from that of adjoining regions, because a moun

tainous country is full of barriers which obstruct the diffusion of life. Distinctness is in direct proportion to isolation. What is true in this regard of the fauna of any region is likewise true of its individual species. The degree of resemblance among individuals is in strict proportion to the freedom of their movements. Variation within the limits of a species is again proportionate to the barriers which prevent equal and free diffusion.

159. Realms of animal life. The various divisions or realms into which the land surface of the earth may be divided on the basis of the character of animal life have their boundary in the obstacles offered to the spread of the average animal. In spite of great inequalities in this regard, we may yet roughly divide the land of the globe into seven principal realms or areas of distribution, each limited by barriers, of which the chief are the presence of the sea and the occurrence of frost. There are the Arctic, North Temperate, South American, Indo-African, Lemurian, Patagonian, and Australian realms.

Of these the Australian

realm alone is sharply defined. Most of the others are surrounded by a broad fringe of debatable ground that forms a transition to some other zone.

The Arctic realm includes all the land area north of the isotherm of 32°. Its southern boundary corresponds closely with the northern limit of trees. The fauna of this region is very homogeneous. It is not rich in species, most of the common types of life of warmer regions being excluded. Among the large animals are the polar bear, the walrus, and certain species of "ice-riding" seals. There are a few species of fishes, mostly trout and sculpins, and a few insects. Some of these, as the mosquito, are excessively numerous in individuals. Reptiles are absent from this region and many of its birds migrate southward in the winter, finding in the arctic only their breeding homes. When we consider the distribution of insects and other small animals of wide diffusion we must add to the arctic realm all high moun

[graphic]

FIG. 177.--The Atlantic walrus (Odobanus rosmarus); animals of the arctic realm.

tains of other realms whose summits rise above the timber line. The characteristic large animals of the arctic, as the polar bear or the musk-ox or the reindeer, are not found there, because barriers shut them off. But the flora of the mountain top, even under the equator, may be characteristically arctic, and with the flowers of the north may be found the northern insects on whose presence the flower depends for its fertilization. So far as climate is concerned high altitude is equivalent to high latitude. On certain mountains the different zones of altitude and the corresponding zones of plant and insect life are very sharply defined (Fig. 178).

The North Temperate realm comprises all the land between the northern limit of trees and the southern limit of frost. It includes, therefore, nearly the whole of Europe, most of Asia, and most of North America. While there are large differences between the fauna of North America and that of Europe and Asia, these differences are of minor importance and are scarcely greater in any case than the difference between the fauna of California and that of our Atlantic coast. The close union of Alaska with Siberia gives the arctic region an almost continuous land area from Greenland to the westward around to Norway. To the south everywhere in the temperate zone realm the species increase in number and variety, and the differences between the fauna of North America and that of Europe are due in part to the northward extension into the one and the other of types originating in the tropics. Especially is this true of certain of the dominant types of singing birds. The group of wood-warblers, tanagers, American orioles, vireos, mocking-birds, with the fly-catchers and humming-birds so characteristic of our forests, are unrepresented in Europe. All of them are apparently immigrants from the neotropical realm where nearly all of them spend the winter. In the same way central Asia has many immigrants from the Indian realm to the southward. With all these variations there

[graphic]

FIG. 178.-Mt. Orizaba, a high mountain rising near the city of Orizaba, Mexico, and showing zones of climate and life from tropical (at base) to arctic (at summit).

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