The Foot-prints of the Creator : $b or, The Asterolepis of Stromness
John Stuart Mill · en
[22] “Mr. Phillips proceeded to describe some remains of a small fish,
resembling the _Cheiracanthus_ of the Old Red Sandstone, scales and
spines of which he had found in a quarry at Hales End, on the western
side of the Malverns. The section presented beds of the Old Red Sandstone
inclined to the west; beneath these were arenaceous beds of a lighter
color, forming the junction with Silurian shales; these, again, passing
on to calcareous beds in the lower part of the quarry, containing the
corals and shells of the Aymestry Limestone, of their agreement with
which stronger evidence might be obtained elsewhere. He had found none
of these scales in the junction beds or in the Upper Ludlow Shales; but
about sixty or one hundred feet lower, just above the Aymestry Limestone,
his attention had been attracted to discolored spots on the _surface_ of
the beds, which, upon microscopic examination, proved to be the minute
scales and spines before mentioned. These remains were only apparent
on the surface, whilst the ‘fish-bed’ of the Upper Ludlow rock, as it
usually occurred, was an inch thick, consisting of innumerable small
teeth and spines.”—_Report, in “Athenæum” for 1842, of the Proceedings of
the Twelfth Meeting of British Association, (Manchester.)_
[23] “This is the lowest position” (that of the Onondago Limestone) “in
the State of New York in which any remains have been found higher in
the scale of organized beings than _Crustacea_, with the exception of
an imperfectly preserved fish-bone discovered by Hall in the Oriskany
Sandstone. That specimen, together with the defensive fish-bone found in
this part of the New York system, furnishes evidences of the existence of
animals belonging to the class _vertebrata_ during the deposition of the
middle part of the protozoic strata.”—_American Journal of Science and
Arts for 1846_, p. 63.
[24] “The shales _alternating_ with the Wenlock Limestone.” (_Edinburgh
Review._)
[25] The Silurian Placoids are most adequately represented by the
_Cestracion_ of the southern hemisphere; but I know not that of the
peculiar character and instincts of this interesting Placoid,—the last of
its race,—there is any thing known. For its form and general appearance
see fig. 49, page 177.
[26] Such as the dog-fishes, picked and spotted.
[27] The twelfth in _Spinax Acanthius_, and the fourteenth in _Scyllium
Stellare_.