The Testimony of the Rocks: or, Geology in Its Bearings on the Two Theologies, Natural and Revealed
John Stuart Mill · en
No trace of the family has yet been detected in even
the Tertiary rocks.
[Illustration: Fig. 57
PTERICHTHYS OBLONGUS.
(One half nat. size.)]
Of the ganoids of the second age of vertebrate existence,--that of the
Old Red Sandstone,--some were remarkable for the strangeness of their
forms, and some for constituting links of connection which no longer
exist in nature, between the ganoid and placoid orders. The Acanth
family, which ceased with the Coal Measures, was characterized,
especially in its Old Red species, by a combination of traits common to
both orders; and among the extremer forms, in which Palæontologists for
a time failed to detect that of the fish at all, we reckon those of the
genera Coccosteus, Pterichthys, and Cephalaspis. The more aberrant
genera, however, even while they consisted each of several species, were
comparatively short lived. The Coccosteus and Cephalaspis were
restricted to but one formation apiece; while the Pterichthys, which
appears for the first time in the lower deposits of the Old Red
Sandstone, becomes extinct at its close. On the other hand, some of the
genera that exemplified the general type of their class were extremely
long lived. The Celacanths were reproduced in many various species, from
the times of the Lower Old Red Sandstone to those of the Chalk; and the
Cestracions, which appear in the Upper Ludlow Rocks as the oldest of
fishes, continue in at least one species to exist still. It would
almost seem as if some such law influenced the destiny of genera in this
ichthyic class, as that which we find so often exemplified in our
species. The dwarf, or giant, or deformed person, is seldom a long
liver;--all the more remarkable instances of longevity have been
furnished by individuals cast in the ordinary mould and proportions of
the species. Not a few of these primordial ganoids wore, however, of the
highest rank and standing ever exemplified by their class; and we find
Agassiz boldly assigning a reason for their superiority to their
successors, important for the fact which it embodies, and worthy, as
coming from him, of our most respectful attention. "It is plain," we
find him saying, "that before the class of reptiles was introduced upon
our globe, the fishes, being then the only representatives of the type
of vertebrata, were invested with the characters of a higher order,
embodying, as it were, a prospective view of a higher development in
another class, which was introduced as a distinct type only at a later
period; and from that time the reptilian character, which had been so
prominent in the oldest fishes, was gradually reduced, till in more
recent periods, and in the present creation, the fishes lost all this
herpetological relationship, and were at last endowed with characters
which contrast as much, when compared with those of reptiles, as they
agreed closely in the beginning. Lepidosteus alone reminds us in our
time of these old-fashioned characters of the class of fishes as it was