Illustrations of the Huttonian Theory of the EarthPlayfair, John
Science
Illustrations of the Huttonian Theory of the Earth
Playfair, John
Geology; Hutton, James, 1726-1797. Theory of the earth
417. The presence of petrified marine objects in places where some of
the fossil bones are found, is no proof that the latter have come from
the sea, though it is produced as such both by Pallas himself, and
afterwards by Kirwan. These marine bodies are the shells and corals
that have been parts of calcareous rocks, from which being detached
by the ordinary progress of disintegration, they are now contained in
the beds of sand or gravel where the animal remains are buried. They
have nothing in common with these remains; they are real stones, and
belong to another, and a far more remote epochs. Such objects being
found in the same place where the bones lie, argues only that the
strata in the higher grounds, from which the gravel has come, are
calcareous; and nothing can show in a stronger light the necessity of
distinguishing the different condition of fossil bodies, united by the
mere circumstance of contiguity, before we draw any inference as to
their having a common origin. If the marine remains were in the same
condition with the bones; if they were in no respect mineralized; then
the conclusion, that both had been imported by the sea, would have
great probability; but without that, their present union must be held
as casual, and can give no insight into the origin of either.
418. On the whole, therefore, no conclusion remains, but that these
bones have belonged to species of elephants, rhinoceros, &c. which
inhabited the very countries where their remains are now buried, and
which could endure the severity of the Siberian climate. The rhinoceros
of the Wilui certainly lived on the confines of the Polar Circle, and
was exposed to the same cold while alive, by which, when dead, its body
has been so long, and so curiously preserved.
These animals may also have lived occasionally farther to the south,
among the valleys between the great ranges of mountains that bound
Siberia on that side. Fossil bones are but rarely found in these
valleys, probably because they have been washed down from thence into
the plains. We must observe, too, that those animals may have migrated
with the seasons, and by that means avoided the rigorous winter of the
high latitudes. The dominion of man, by rendering such migration to
the larger animals difficult or impossible, must have greatly changed
the economy of all those tribes, and narrowed the circle of their
enjoyments and existence. The heaps in which the fossil bones appear to
be accumulated in particular places, especially in North America, have
a great appearance of being connected with the migrations of animals,
and the accidents that might bring multitudes of them into the same
spot.
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