Darwiniana : Essays — Volume 02Huxley, Thomas Henry
Science
Darwiniana : Essays — Volume 02
Huxley, Thomas Henry
Darwin, Charles, 1809-1882; Evolution (Biology)
Yet another product of investigation has largely contributed to the removal
of the objections to the doctrine of evolution current in 1859. It is the
proof afforded by successive discoveries that Mr. Darwin did not
over-estimate the imperfection of the geological record. No more striking
illustration of this is needed than a comparison of our knowledge of the
mammalian fauna of the Tertiary epoch in 1859 with its present condition.
M. Gaudry's researches on the fossils of Pikermi were published in 1868,
those of Messrs. Leidy, Marsh, and Cope, on the fossils of the Western
Territories of America, have appeared almost wholly since 1870, those of M.
Filhol on the phosphorites of Quercy in 1878. The general effect of these
investigations has been to introduce to us a multitude of extinct animals,
the existence of which was previously hardly suspected; just as if
zoologists were to become acquainted with a country, hitherto unknown, as
rich in novel forms of life as Brazil or South Africa once were to
Europeans. Indeed, the fossil fauna of the Western Territories of America
bid fair to exceed in interest and importance all other known Tertiary
deposits put together; and yet, with the exception of the case of the
American tertiaries, these investigations have extended over very limited
areas; and, at Pikermi, were confined to an extremely small space.
Such appear to me to be the chief events in the history of the progress of
knowledge during the last twenty years, which account for the changed
feeling with which the doctrine of evolution is at present regarded by
those who have followed the advance of biological science, in respect of
those problems which bear indirectly upon that doctrine.
But all this remains mere secondary evidence. It may remove dissent, but it
does not compel assent. Primary and direct evidence in favour of evolution
can be furnished only by palæontology. The geological record, so soon as it
approaches completeness, must, when properly questioned, yield either an
affirmative or a negative answer: if evolution has taken place, there will
its mark be left; if it has not taken place, there will lie its refutation.
What was the state of matters in 1859? Let us hear Mr. Darwin, who may be
trusted always to state the case against himself as strongly as possible.
"On this doctrine of the extermination of an infinitude of connecting links
between the living and extinct inhabitants of the world, and at each
successive period between the extinct and still older species, why is not
every geological formation charged with such links? Why does not every
collection of fossil remains afford plain evidence of the gradation and
mutation of the forms of life? We meet with no such evidence, and this is
the most obvious and plausible of the many objections which may be urged
against my theory." [Footnote: _Origin of Species_, ed. 1, p. 463.]
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