The Old Red Sandstone; or, New Walks in an Old Field — John Stuart Mill — John Shaqi
The Old Red Sandstone; or, New Walks in an Old Field
John Stuart Mill · en
It requires skill such as that possessed by Agassiz, to determine
that the uncouth _Coccosteus_, or the equally uncouth _Pterichthys_,
of the Old Red Sandstone, with their long articulated tails and
tortoise-like plates, were _bona fide_ fishes; but there is no
possibility of mistaking the _Osteolepis_: it is obvious to the least
practised eye that it must have been a fish, and a handsome one. Even
a cursory examination, however, shows very striking peculiarities,
which are found, on further examination, to characterize not this
family alone, but at least one half the contemporary families
besides. We are accustomed to see vertebrated animals with the bone
uncovered in one part only,--that part the teeth,--and with the rest
of the skeleton wrapped up in flesh and skin. Among the reptiles,
we find a few exceptions; but a creature with a skull as naked as
its teeth,--the bone being merely covered, as in these, by a hard,
shining enamel,--and with toes also of bare enamelled bone, would
be deemed an anomaly in creation. And yet such was the condition
of the _Osteolepis_, and many of its contemporaries. The enamelled
teeth were placed in jaws which presented outside a surface as naked
and as finely enamelled as their own. (See Plate IV., fig. 5.) The
entire head was covered with enamelled osseous plates, furnished
inside like other bones, as shown by their cellular construction,
with their nourishing blood vessels, and perhaps their oil, and
which rested apparently on the cartilaginous box, which must have
enclosed the brain, and connected it with the vertebral column.
I cannot better illustrate the peculiar condition of the fins of
this ichthyolite than by the webbed foot of a water-fowl. The web
or membrane in all the aquatic birds with which we are acquainted
not only connects, but also covers the toes. The web or membrane in
the fins of existing fishes accomplishes a similar purpose; it both
connects and covers the supporting bones or rays. Imagine, however, a
webbed foot in which the toes--connected, but not covered--present,
as in skeletons, an upper and under surface of naked bone; and a very
correct idea may be formed, from such a foot, of the condition of fin
which obtained among at least one half the ichthyolites of the Lower
Old Red Sandstone. The supporting bones or rays seem to have been
connected laterally by the membrane; but on both sides they presented
bony and finely enamelled surfaces. (See Plate IV., fig. 6.) In this
singular class of fish, all was bone without, and all was cartilage
within; and the bone in every instance, whether in the form of jaws
or of plates, of scales or of rays, presented an external surface of
enamel.