Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
These species differ from each other in size, the smallest being
scarcely so large as a lamb of three months, and in various
circumstances connected with the form of their teeth, which it would
be too tedious and minute to detail here.
The _Anoplotheria_ have hitherto been discovered nowhere but in
the gypsum quarries of the neighbourhood of Paris. They have two
characters which are observed in no other animal; feet with two
toes, the metacarpal and metatarsal bones of which are separate in
their whole length, and do not unite into a single piece, as in the
ruminantia; and teeth placed in a continuous series without any
interruption. Man alone has the teeth so placed in mutual contiguity,
without any interval. Those of the anaplotheria consist of six
incisors in each jaw, a canine tooth and six grinders on each side,
both above and below; their canine teeth are short and similar to
the outer incisors. The three first grinders are compressed; the
four others are, in the upper jaw, square, with transverse ridges,
and a small cone between them; and, in the lower jaw, in the form of
a double crescent, but without neck at the base. The last has three
crescents. Their head is of an oblong form, and does not indicate
that the muzzle has terminated either in a proboscis or a snout.
This extraordinary genus, which can be compared to nothing in living
nature, is subdivided into three subgenera: the _Anaplotheria_,
properly so called, the anterior molares of which are still pretty
thick, and the posterior ones of the lower jaw have their crescents
with a simple ridge; the _Xiphodons_, of which the anterior molares
are thin and sharp on the edges, and the under posterior, have,
directly opposite the concavity of each of their crescents, a point,
which, on being worn, also assumes the form of a crescent, so that
then the crescents are double as in the ruminantia; lastly, the
_Dichobunes_, the outer crescents of which are also pointed at the
beginning, and which have thus points disposed in pairs upon their
lower posterior grinders.
The most common species in our gypsum quarries (_An. commune_), is
an animal of the height of a boar, but much more elongated, and
furnished with a very long and very thick tail, so that altogether it
has nearly the proportion of the otter, but larger. It is probable
that it was well fitted for swimming, and frequented the lakes in the
bottom of which its bones have been incrusted by the gypsum which was
deposited there. We have one a little smaller, but in other respects
pretty similar (_An. secundarium_.)
We are as yet acquainted with only one _xiphodon_, which, however,
is a very remarkable animal: it is that which I have named _An.
gracile_. It is slender, and delicately formed, like the prettiest
gazelle.
Public-domain text, read in full here on John Shaqi.
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