Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
A second aspect in which such speculations are too partial, is in
the unwarranted use which they make of analogy. It is not unusual to
find such analogies as that between the embryonic development of the
individual animal and the succession of animals in geological time
placed on a level with that reasoning from analogy by which geologists
apply modern causes to explain geological formations. No claim could
be more unfounded. When the geologist studies ancient limestones built
up of the remains of corals, and then applies the phenomena of modern
coral reefs to explain their origin, he brings the latter to bear
on the former by an analogy which includes not merely the apparent
results, but the causes at work, and the conditions of their action,
and it is on this that the validity of his comparison depends, in so
far as it relates to similarity of mode of formation. But when we
compare the development of an animal from an embryo cell with the
progress of animals in time, though we have a curious analogy as to the
steps of the process, the conditions and causes at work are known to
be altogether dissimilar, and therefore we have no evidence whatever
as to identity of cause, and our reasoning becomes at once the most
transparent of fallacies. Further, we have no right here to overlook
the fact that the conditions of the embryo are determined by those of
a previous adult, and that no sooner does this hereditary potentiality
produce a new adult animal, than the terrible external agencies of the
physical world, in presence of which all life exists, begin to tell on
the organism, and after a struggle of longer or shorter duration it
succumbs to death, and its substance returns into inorganic nature, a
law from which even the longer life of the species does not seem to
exempt it. All this is so plain and manifest that it is extraordinary
that evolutionists will continue to use such partial and imperfect
arguments. Another illustration may be taken from that application
of the doctrine of natural selection to explain the introduction of
species in geological time, which is so elaborately discussed by Sir
C. Lyell in the last edition of his "Principles of Geology." The great
geologist evidently leans strongly to the theory, and claims for it
the "highest degree of probability," yet he perceives that there is a
serious gap in it; since no modern fact has ever proved the origin of a
new species by modification. Such a gap, if it existed in those grand
analogies by which he explained geological formations through modern
causes, would be admitted to be fatal.
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