Contributions to the Theory of Natural Selection: A Series of EssaysWallace, Alfred Russel
Science
Contributions to the Theory of Natural Selection: A Series of Essays
Wallace, Alfred Russel
Natural selection
The facts proved by geology are briefly these:--That during an immense,
but unknown period, the surface of the earth has undergone successive
changes; land has sunk beneath the ocean, while fresh land has risen up
from it; mountain chains have been elevated; islands have been formed
into continents, and continents submerged till they have become islands;
and these changes have taken place, not once merely, but perhaps
hundreds, perhaps thousands of times:--That all these operations have
been more or less continuous, but unequal in their progress, and during
the whole series the organic life of the earth has undergone a
corresponding alteration. This alteration also has been gradual, but
complete; after a certain interval not a single species existing which
had lived at the commencement of the period. This complete renewal of
the forms of life also appears to have occurred several times:--That
from the last of the geological epochs to the present or historical
epoch, the change of organic life has been gradual: the first appearance
of animals now existing can in many cases be traced, their numbers
gradually increasing in the more recent formations, while other species
continually die out and disappear, so that the present condition of the
organic world is clearly derived by a natural process of gradual
extinction and creation of species from that of the latest geological
periods. We may therefore safely infer a like gradation and natural
sequence from one geological epoch to another.
Now, taking this as a fair statement of the results of geological
inquiry, we see that the present geographical distribution of life upon
the earth must be the result of all the previous changes, both of the
surface of the earth itself and of its inhabitants. Many causes, no
doubt, have operated of which we must ever remain in ignorance, and we
may, therefore, expect to find many details very difficult of
explanation, and in attempting to give one, must allow ourselves to call
into our service geological changes which it is highly probable may have
occurred, though we have no direct evidence of their individual
operation.
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