Island Life; Or, The Phenomena and Causes of Insular Faunas and FlorasWallace, Alfred Russel
Science
Island Life; Or, The Phenomena and Causes of Insular Faunas and Floras
Wallace, Alfred Russel
Biogeography; Glacial epoch; Island ecology
Here, too, we obtain a glimpse of the way in which {409} species die out
and are replaced by others, which quite agrees with what the theory of
evolution assures us must have occurred. On a continent, the process of
extinction will generally take effect on the circumference of the area of
distribution, because it is there that the species comes into contact with
such adverse conditions or competing forms as prevent it from advancing
further. A very slight change will evidently turn the scale and cause the
species to contract its range, and this usually goes on till it is reduced
to a very restricted area, and finally becomes extinct. It may conceivably
happen (and almost certainly has sometimes happened) that the process of
restriction of range by adverse conditions may act in one direction only,
and over a limited district, so as ultimately to divide the specific area
into two separated parts, in each of which a portion of the species will
continue to maintain itself. We have seen that there is reason to believe
that this has occurred in a very few cases both in North America and in
Northern Asia. (_See_ pp. 65-68.) But the same thing has certainly occurred
in a considerable number of cases, only it has resulted in the divided
areas being occupied by _representative forms_ instead of by the very same
species. The cause of this is very easy to understand. We have already
shown that there is a large amount of local variation in a considerable
number of species, and we may be sure that were it not for the constant
intermingling and intercrossing of the individuals inhabiting adjacent
localities this tendency to local variation in adaptation to slightly
different conditions, would soon form distinct races. But as soon as the
area is divided into two portions the intercrossing is stopped, and the
usual result is that two closely allied races, classed as representative
species, become formed. Such pairs of allied species on the two sides of a
continent, or in two detached areas, are very numerous; and their existence
is only explicable on the supposition that they are descendants of a parent
form which once occupied an area comprising that of both of them,--that
this area then became discontinuous,--and, lastly, that, as a consequence
of the discontinuity, the two sections of the parent species became
segregated into distinct races or new species. {410}
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