Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
Our gypsum quarries in the neighbourhood of Paris are full of them.
Bones of seven distinct species are found there. The first (_P.
magnum_) is as large as a horse. The three next are of the size of a
hog, but one of them (_P. medium_) has narrow and long feet, another
(_P. crassum_) has the feet broader, and a third (_P. latum_) has
them still broader, and especially shorter. The fifth species (_P.
curtum_), which is of the size of a sheep, is much lower, and has
the feet still broader and shorter in proportion than the last. The
sixth (_P. minus_) is of the size of a small sheep, and has long and
slender feet, the lateral toes of which are shorter than the rest.
The seventh (_P. minimum_), which is not larger than a hare, has also
the feet slender[268].
Palæotheria have also been found in other districts of France: at Puy
in Valey, in strata of gypseous marl, a species (_P. velaunum_)[269],
much resembling (_P. medium_), but differing from it in the form of
its lower jaw; in the neighbourhood of Orleans, in strata of marly
rock, a species (_P. aurelianense_)[270], which is distinguished from
the others by having the re-entering angle of the crescent of its
lower grinders split into a double point, and by some differences
in the necks of the upper grinders; near Issel, in a bed of gravel
or molasse, along the declivities of the Black Mountain, a species
(_P. isselanum_)[271], which has the same characters as the Orleans
species, but is of smaller size. It is more particularly, however, in
the molasse of the Department of the Dordogne, that the palæotherium
occurs not less abundantly than in our gypsum deposits in the
neighbourhood of Paris.
The Duke Decaze has discovered in the quarries of a single field,
bones of three species which appear different from all those of our
neighbourhood[272].
The _Lophiodons_ approach still somewhat nearer to the tapirs than
the palæotheria do, inasmuch as their lower false grinders have
transverse necks like those of the tapirs.
They differ, however, from these latter, in having the fore ones more
simple, the backmost of all with three necks, and the upper ones
rhomboidal, and marked with ridges very much resembling those of the
rhinoceros.
We are still ignorant what the form of their snout, and the number
of their toes, may have been. I have discovered not less than twelve
species of this genus, all in France, deposited in marly rocks of
fresh-water formation, and filled with lymneæ and planorbes, which
are shells peculiar to pools and marshes.
The largest species is found near Orleans, in the same quarry as the
palæotheria; it approaches the rhinoceros.
There is a smaller species in the same place; a third occurs at
Montpellier; a fourth near Laon; two near Buchsweiler in Alsace;
five near Argenton in Berry; and one of the three occurs again near
Issel, where there are also two others. There is also a large one
near Gannat[273].
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