Half Hours With Modern Scientists: Lectures and EssaysTyndall, John
Philosophy
Half Hours With Modern Scientists: Lectures and Essays
Tyndall, John
Science
The theory of homologous groups furnishes important evidence in
favor of derivation. Many orders of animals (probably all, when we
come to know them) are divisible into two or more sections, which I
have called _homologous_. These are series of genera or families,
which differ from each other by some marked character, but whose
contained genera or families differ from each other in the same
points of detail, and in fact correspond exactly. So striking is
this correspondence that were it not for the general and common
character separating the homologous series, they would be regarded
as the same, each to each. Now it is remarkable that where studied
the difference common to all the terms of two homologous groups is
found to be one of _inexact parallelism_, which has been shown above
to be evidence of descent. Homologous groups always occupy different
geographical areas on the earth’s surface, and their relation is
precisely that which holds between successive groups of life in the
periods of geologic time.
In a word, we learn from this source that distinct geologic epochs
coexist at the same time on the earth. I have been forced to this
conclusion[47] by a study of the structure of terrestrial life, and
it has been remarkably confirmed by the results of recent deep-sea
dredgings made by the United States Coast Survey in the Gulf Stream,
and by the British naturalists in the North Atlantic. These have
brought to light types of Tertiary life, and of even the still more
ancient Cretaceous periods, living at the present day. That this
discovery invalidates in any wise the conclusions of geology
respecting lapse of time is an unwarranted assumption that some are
forward to make. If it changes the views of some respecting the
parallelism or coëxistence of faunæ in different regions of the
earth, it is only the anti-developmentalists whose position must be
changed.
Footnote 47:
_Origin of Genera_, pages 70, 77, 79.
For, if we find distinct geologic faunæ, or epochs defined by faunæ,
coëxisting during the present period, and fading or emerging into
one another as they do at their geographical boundaries, it is proof
positive that the geologic epochs and periods of past ages had in
like manner no trenchant boundaries, but also passed the one into
the other. The assumption that the apparent interruptions are the
result of transfer of life rather than destruction, or of want of
opportunities of preservation, is no doubt the true one.
δ. Rationale of Development.
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