Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
The sea which had covered these lands and destroyed their animals,
left large deposits, which still form at the present day, at no great
depth, the basis of our great plains: it had then retired anew, and
left immense surfaces to a new population, whose remains are found in
the sandy and muddy deposits of all countries known.
It is to this deposition from the sea, made in a state of quiet,
that certain fossil cetacea, very much resembling those of our own
days, should, in my opinion, be referred;--a dolphin, allied to
our epaulard[295], and a whale very like our rorquals[296], both
discovered in Lombardy by M. Cortesi; a large head of a whale found
within the very precincts of Paris[297], and described by Lamanon
and Daubenton; and an entirely new genus, which I have discovered
and named _Ziphius_, and which already contains three species. It is
allied to the cachalots and hyperoodons[298].
In the extinct population which fills our alluvial and superficial
strata, and which has lived upon the deposit just alluded to,
there are no longer either palæotheria or anaplotheria, or, in in
fact, any of those singular genera. The pachydermata, however,
still predominate; and these are of a gigantic size, elephants,
rhinoceroses, and hippopotami, accompanied with innumerable horses
and several large ruminantia. Carnivorous animals of the size of
the lion, tiger, and hyena, had desolated this new animal kingdom.
In general, its character, even in the extreme north, and on the
edges of the present frozen ocean, was similar to that which the
torrid zone alone now presents, and yet there was no species in it
absolutely the same as any of those which are found alive at the
present day.
The most remarkable of these animals is the species of elephant named
_mammoth_ by the Russians (the _Elephas primigenius_ of Blumenbach),
which was fifteen or eighteen feet high, and was covered with coarse
red wool, and long, stiff, black hairs, which formed a mane along
its back. Its enormous tusks were implanted in alveolæ longer than
those of the elephants of the present day; but in other respects it
was pretty similar to the Indian elephant[299]. It has left thousands
of its carcases from Spain to the shores of Siberia, and it has been
found in the whole of North America; so that it had been distributed
on both sides of the Atlantic, if, indeed, that ocean had existed
in its time, in the place which it occupies at present. It is well
known that its tusks are still so well preserved in cold countries,
as to be applied to the same uses as fresh ivory; and, as we have
already remarked, individuals of it have been found with their flesh,
skin, and hair, which had remained frozen since the last general
catastrophe. The Tartars and Chinese have imagined it to be an animal
which lives under ground, and perishes whenever it perceives the
light.
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