A history of land mammals in the western hemisphereScott, William Berryman
History
A history of land mammals in the western hemisphere
Scott, William Berryman
Mammals; Mammals, Fossil
We have next to inquire what is the nature of the obstacles or barriers
that prevent the indefinite spread of terrestrial mammals, so that the
mammalian fauna of the whole earth, and even of a single continent,
is not uniform, but highly variegated. The rate of multiplication of
animals is so rapid that, under normal conditions, the animal population
is always pressing hard upon the means of subsistence and every species
that is increasing in numbers must constantly extend its range in search
of food. Every species would increase indefinitely, if there were no
countervailing checks. Were all the young to survive and breed in their
turn, “even large and slow-breeding mammals, which only have one at a
birth, but continue to breed from eight to ten successive years, may
increase from a single pair to 10,000,000 in forty years” (Wallace).
Evidently, a species must spread from its place of origin until stopped
by insuperable obstacles, the most obvious of which are wide seas. A few
land mammals are not only excellent swimmers, but will cross straits
without hesitation, as the Guanaco has been seen to swim the Straits
of Magellan; for the great majority, however, a very few miles of sea
form an impassable barrier. As was shown above, a broad or deep river is
sufficient to limit many species, as the Santa Cruz River in Patagonia
marks the southern boundary of the armadillos.
Important geographical changes, such as the joining of lands that before
were separate, or the dividing of continuous lands by transgressions
and incursions of the sea, must necessarily have a profound effect upon
the distribution of land mammals. Separated land-areas, however similar
may have been their faunas at the time of separation, will, through the
operation of the divergent evolutionary process, grow more unlike in
proportion to the length of time that the separation continues. Regions
which have been severed within a short time (in the geological sense of a
short time) are zoölogically very similar or even identical, while those
that have long been isolated are correspondingly peculiar. Attention has
already been called, in another connection, to the contrasted cases of
such great continental islands as Great Britain, Java, Sumatra, etc.,
on the one hand, and Australia, on the other. The continental islands,
which have but lately been detached from the neighbouring main lands,
are hardly more peculiar zoölogically than equal areas of the adjoining
continents, while the long-continued isolation of Australia has made it
the most peculiar region of the earth. Climatic changes, which, as we
saw in Chapter I, have indubitably taken place many times, have also had
a great effect in shifting the distribution of mammals, which in its
present form is the outcome of a very long series of geographical and
climatic changes, on the one hand, and of adaptive changes in the animals
themselves, on the other.
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