Geological Contemporaneity and Persistent Types of LifeHuxley, Thomas Henry
Science
Geological Contemporaneity and Persistent Types of Life
Huxley, Thomas Henry
Fossils; Life (Biology)
It negatives those doctrines; for it either shows us no evidence of any
such modification, or demonstrates it to have been very slight; and as
to the nature of that modification, it yields no evidence whatsoever
that the earlier members of any long-continued group were more
generalized in structure than the later ones. To a certain extent,
indeed, it may be said that imperfect ossification of the vertebral
column is an embryonic character; but, on the other hand, it would be
extremely incorrect to suppose that the vertebral columns of the older
Vertebrata are in any sense embryonic in their whole structure.
Obviously, if the earliest fossiliferous rocks now known are coeval
with the commencement of life, and if their contents give us any just
conception of the nature and the extent of the earliest fauna and flora,
the insignificant amount of modification which can be demonstrated
to have taken place in any one group of animals, or plants, is quite
incompatible with the hypothesis that all living forms are the results
of a necessary process of progressive development, entirely comprised
within the time represented by the fossiliferous rocks.
Contrariwise, any admissible hypothesis of progressive modification must
be compatible with persistence without progression, through indefinite
periods. And should such an hypothesis eventually be proved to be true,
in the only way in which it can be demonstrated, viz. by observation
and experiment upon the existing forms of life, the conclusion will
inevitably present itself, that the Paleozoic, Mesozoic, and Cainozoic
faunae and florae, taken together, bear somewhat the same proportion to
the whole series of living beings which have occupied this globe, as the
existing fauna and flora do to them.
Such are the results of paleontology as they appear, and have for some
years appeared, to the mind of an inquirer who regards that study simply
as one of the applications of the great biological sciences, and who
desires to see it placed upon the same sound basis as other branches of
physical inquiry. If the arguments which have been brought forward are
valid, probably no one, in view of the present state of opinion, will
be inclined to think the time wasted which has been spent upon their
elaboration.
[Footnote 1: The Anniversary Address to the Geological Society for
1862.]
[Footnote 2: "le plus grand service qu'on puisse rendre a la science est
d'y faire place nette avant d'y rien construire."--CUVIER]
[Footnote 3: Anniversary Address for 1851, 'Quart. Journ. Geol. Soc.'
vol. vii.]
[Footnote 4: See Hooker's 'Introductory Essay to the Flora of Tasmania',
p. xxiii.]
[Footnote 5: See the abstract of a Lecture "On the Persistent Types of
Animal Life," in the 'Notices of the Meetings of the Royal Institution
of Great Britain'.--June 3, 1859, vol. iii. p. 151.
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