The Old Red Sandstone; or, New Walks in an Old Field
John Stuart Mill · en
of the chalk, with those of the other later formations, down to the
New Red Sandstone, we find that the skeleton style of preparation
obtains; whereas, in at least three fourths of the ichthyolites of
the Lower Old Red, we find only what we may term the external style.
I had marked, besides, another circumstance in the ichthyolites,
which seemed, like a nice point of circumstantial evidence, to give
testimony in the same line. The tails of all the ichthyolites, whose
vertebral columns and internal rays are wanting, are unequally lobed,
like those of the dog-fish and sturgeon, (both cartilaginous fishes,)
and the body runs on to nearly the termination of the surrounding
rays. The one-sided condition of tail exists, says Cuvier, in no
recent osseous fish known to naturalists, except in the bony pike--a
sauroid fish of the warmer rivers of America. With deference,
however, to so high an authority, it is questionable whether, the
tail of the bony pike should not rather be described as a tail set on
somewhat awry, than as a one-sided tail.
All these peculiarities I could but note as they turned up before me,
and express, in pointing them out to a few friends, a sort of vague,
because hopeless, desire, that good fortune might throw me in the
way of the one man of all the world best qualified to explain the
principle on which they occurred, and to decide whether fishes may be
at once bony and cartilaginous. But that meeting was a contingency
rather to be wished than hoped for--a circumstance within the
bounds of the possible, but beyond those of the probable. Could the
working-man of the north of Scotland have so much as dreamed that he
was yet to enjoy an opportunity of comparing his observations with
those of the naturalist of Neufchatel, and of having his inferences
tested and confirmed?