The Foot-prints of the Creator : $b or, The Asterolepis of Stromness — John Stuart Mill — John Shaqi
The Foot-prints of the Creator : $b or, The Asterolepis of Stromness
John Stuart Mill · en
of the dorsal vertebræ of a herring into melted wax, and then withdraw
it, we will find it to represent in its crusted state the vertebral
centrum of a Placoid,—soft without, and osseous within; but in order
to represent the placoid skull, we would have first to mould it out of
one unbroken piece of wax, and then to cover it over with a priming of
bone-dust. And such is the effect of this arrangement, that, while the
skull of a Placoid, exposed to a red heat, falls into dust, from the
circumstance that the supporting framework on which the granular bone
was arranged perishes in the fire, the vertebral centrum, whose internal
framework is itself bone, and so _not_ perishable, comes out in a state
of beautiful entireness,—resembling in the thornback a squat sand-glass,
elegantly fenced round by the lateral pillars, (fig. 8, _b_;) and in
the dog-fish (_a_) a more elongated sand-glass, in which the lateral
pillars are wanting. Such are the heads and vertebral joints of the
existing Placoids; and such, reasoning from analogy, seem to have been
the character and construction of the heads and vertebral joints of the
Placoids of the Silurian period,—earliest-born of the Vertebrata.
[Illustration: Fig. 8.
a. _Osseous centrum of Spinax Acanthias._
b. _Osseous centrum of Raja clavata._
(Nat. size.)]
The most ancient brain-bearing craniums that have come down to us
in the fossil state, are those of the Ganoids of the Lower Old Red
Sandstone; and in these fishes the true skull appears to have been
as entirely a simple cartilaginous box, as that of the Placoids of
either the Silurian period or of the present time, or of those existing
Ganoids, the sturgeons. In the Lower Old Red genera _Cheiracanthus_ and
_Diplacanthus_, though the heads are frequently preserved as amorphous
masses of colored matter, we detect no trace of internal bone, save
perhaps in the gill-covers of the first-named genus, which were fringed
by from eighteen to twenty minute osseous rays. The cranium seems to have
been covered, as in the shark family, by skin, and the skin by minute
shagreen-like scales; and all of the interior cerebral framework which
appears underneath exists simply as faint impressions of an undivided
body, covered by what seem to be osseous points,—the bony molecules,
it is probable, which encrusted the cartilage. The jaws, in the better
specimens, are also preserved in the same doubtful style, and this state
of keeping is the common one in deposits in which every true bone,
however delicate, presents an outline as sharp as when it occupied its
place in the living animal. The dermal or skin-skeleton of both genera,
which consisted, as has been shown (pages 55, 56) of shagreen-like
osseous scales and slender spines, both brilliantly enamelled, is
preserved entire; where as the interior framework of the head exists as
mere point speckled impressions; and the inference appears unavoidable
that parts which so invariably differ in their state of keeping now, must