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
The opportunity did occur. The working-man did meet with Agassiz; and
many a query had he to put to him; and never, surely, was inquirer
more courteously entreated, or his doubts more satisfactorily
resolved. The reply to almost my first question solved the enigma of
nearly ten years' standing. And finely characteristic was that reply
of the frankness and candor of a great mind, that can afford to make
it no secret, that, in its onward advances on knowledge, it may know
to-day what it did not know yesterday, and that it is content to
"gain by degrees upon the darkness." "Had you asked me the question
a fortnight ago," said Agassiz, "I could not have replied to it.
Since then, however, I have examined an ichthyolite of the Old Red
Sandstone in which the vertebral joints are fortunately impressed
on the stone, though the joints themselves have disappeared, and
which, exactly resembling the vertebra? of the shark, must have
been cartilaginous." In a subsequent conversation, the writer
was gratified by finding most of his other facts and inferences
authenticated and confirmed by those of the naturalist. I shall
attempt introducing to the reader the peculiarities, general and
specific, of the ichthyolites to which these facts and observations
mainly referred, by describing such of the families as are most
abundant in the formation, and the points in which they either
resemble or differ from the existing fish of our seas.
[Illustration: _PLATE IV._]
Of these ancient families, the _Osteolepis_, or bony-scale,
(see Plate IV., fig. 1,) may be regarded as illustrative of the
general type. It was one of the first discovered of the Caithness
fishes, and received its name in the days of Cuvier, from the
osseous character of its scales, ere it was ascertained that it
had numerous contemporaries, and that to all and each of these the
same description applied. The scales of the fishes of the Lower
Old Red Sandstone, like the plates and detached prickles of the
purely cartilaginous fishes, were composed of a bony, not of a
horny, substance, and were all coated externally with enamel. The
circumstance is one of interest.