The Testimony of the Rocks: or, Geology in Its Bearings on the Two Theologies, Natural and Revealed
John Stuart Mill · en
The articulata of the Silurian period bore a still more peculiar
character. They consisted mainly of the Trilobites,--a family in whose
nicely-jointed shells the armorer of the middle ages might have found
almost all the contrivances of his craft, anticipated, with not a few
besides which he had failed to discover; and which, after receiving so
immense a development during the middle and later times of the Silurian
period, that whole rocks were formed almost exclusively of their
remains, gradually died out in the times of the Old Red Sandstone, and
disappeared for ever from creation after the Carboniferous Limestone had
been deposited. The Palæontologist knows no more unique family than that
of the Trilobites, or a family more unlike any which now exists, or a
family which marks with more certainty the early rocks in which they
occur. And yet, though formed in a fashion that perished myriads of
ages ago, how admirably does it not exhibit the articulated type of
being, and illustrate that unity of design which, amid endless
diversity, pervades all nature. The mollusca of the Silurians ranged
from the high cephalopoda, represented in our existing seas by the
nautili and the cuttle-fishes, to the low brachipods, some of whose
congeners may still be detected in the terebratula of our Highland lochs
and bays, and some in the lingulæ of the southern hemisphere. The
cephalopods of the system are all of an obsolete type, that disappeared
myriads of ages ago,--a remark which, with the exceptions just
intimated, and perhaps one or two others, applies equally to its
brachipods; but of at least two of its intermediate families,--the
gasteropoda and lamellibranchiata,--several of the forms resemble those
of recent shells of the temperate latitudes. In its general aspect,
however, the Silurian fauna, antiquely fashioned, as I have said, as
became its place in the primeval ages of existence, was unlike any other
which the world ever saw; and the absence of the vertebrata, or at least
the inconspicuous place which they occupied if they were at all present,
must have imparted to the whole, as a group, a humble and mediocre
character. It seems to have been for many ages together a creation of
molluscs, corals, and Crustacea. At length, in an upper bed of the
system, immediately under the base of the Old Red Sandstone, the remains
of the earliest known fishes appear, blent with what also appears for
the first time,--the fragmentary remains of a terrestrial vegetation.
The rocks beneath this ancient bone-bed have yielded, as I have already
said, no trace of any plant higher than the Thallogens, or at least not
higher than the Zosteracea,--plants whose proper habitat is the sea;
but, through an apparently simultaneous advance of the two kingdoms,
animal and vegetable,--though of course the simultaneousness may be but
merely apparent,--the first land plants and the first vertebrates
appear together in the same deposit.