The Geographical Distribution of Animals, Volume 1: With a study of the relations of living and extinct faunas as elucidating the past changes of the Earth's surfaceWallace, Alfred Russel
Science
The Geographical Distribution of Animals, Volume 1: With a study of the relations of living and extinct faunas as elucidating the past changes of the Earth's surface
Wallace, Alfred Russel
Paleontology; Zoogeography
_Order of Succession of the Regions._--We may here explain the reason for
taking the several regions in a different succession from that in which
they appear in the tabular or diagrammatic headings to each family, in the
Fourth, and concluding part of this work. It will have been seen, by our
examination of extinct animals (and it will be made still clearer during
our study of the several regions) that all the chief types of animal life
appear to have originated in the great north temperate or northern
continents; while the southern continents--now represented by {174}South
America, Australia, and South Africa with Madagascar--have been more or
less completely isolated, during long periods, both from the northern
continent and from each other. These latter countries have, however, been
subject to more or less immigration from the north during rare epochs of
approximation to, or partial union with it. In the northern, more
extensive, and probably more ancient land, the process of development has
been more rapid, and has resulted in more varied and higher types; while
the southern lands, for the most part, seem to have produced numerous
diverging modifications of the lower grades of organization, the original
types of which they derived either from the north, or from some of the
ancient continents in Mesozoic or Palæozoic times. Hence those curious
resemblances in the fauna of South America, Australia, and, to a less
extent, Madagascar, which have led to a somewhat general belief that these
distant countries must at one time or other have been united; a belief
which, after a careful examination of all the facts, does not seem to the
author of this work to be well founded. On the other hand, there is the
most satisfactory evidence that each southern region has been more or less
closely united (during the tertiary or later secondary epoch) with the
great northern continents, leading to numerous resemblances and affinities
in their productions.
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