The Doctrine of Evolution: Its Basis and Its ScopeCrampton, Henry Edward
Science
The Doctrine of Evolution: Its Basis and Its Scope
Crampton, Henry Edward
Evolution
Mainly through the influence of the renowned English man of science,
Charles Lyell, the students of the earth came to the conclusion that its
manifold structures had developed by a slow and orderly process that was
entirely natural; for they found no evidence of any sudden and drastic
world-wide remodeling such as that postulated by the Cuvierian hypothesis
of catastrophe. The battle waged for many years; but now naturalists
believe that the forces, of nature, whose workings may be seen on all
sides at the present time, have reconstructed the continents and ocean
beds in the past in the same way that they work to-day. The long name of
"uniformitarianism" is given to Lyell's doctrine, which has exerted an
influence upon knowledge far outside the department of geology. Darwin
tells us how much he himself was impressed by it, and how it led him to
study the factors at work upon organic things to see if he could discern
evidence of a biological uniformitarianism, according to which the past
history of living things might be interpreted through an understanding of
their present lives.
* * * * *
What, now, are the reasons why the palaeontological evidence is not
complete and why it cannot be? In the first place the seeker after fossil
remains finds about three fifths of the earth's surface under water so
that he cannot explore vast areas of the present ocean beds which were
formerly dry land and the homes of now extinct animals. Thus the field of
investigation is seriously restricted at the outset, but the naturalist
finds his work still more limited, in so far as much of the dry land
itself is not accessible. The perennial snows of the Arctic region render
it impossible to make a thorough search in the frigid zone, and there are
many portions of the temperate and torrid zones that are equally
unapproachable for other reasons. But even where exploration is possible,
the surface rocks are the only ones from which remains can be readily
obtained, for the layers formed in earlier ages are buried so deeply that
their contents must remain forever unknown in their entirety. Only a few
scratches upon the earth's hard crust have been made here and there, so it
is small wonder that the complete series of extinct organisms has not been
produced by the palaeontologist.
Public-domain text, read in full here on John Shaqi.
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