Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
Thirdly, This more complete action is also more easily ascertained.
It is more easy to demonstrate its effects, because, the number of
quadrupeds being limited, and the greater part of their species, at
least the large ones, being known, we have more means of determining
whether fossil bones belong to them, or to a species that is now
lost. As, on the other hand, we are very far from being acquainted
with all the testaceous animals and fishes which inhabit the sea,
and as we are still probably ignorant of the greater number of those
which live in deep water, it is impossible to know with certainty,
whether a species which occurs in a fossil state, may not still exist
somewhere alive. And hence, we see naturalists persisting in giving
the name of pelagic shells, that is to say, shells inhabiting the
open sea, to the belemnites, cornua-ammonis, and other testaceous
remains, which have hitherto been found only in the older strata;
meaning by this, that if they have not yet been discovered in a
living state, it is because they inhabit the depths of the sea, far
beyond the reach of our nets.
_Small probability of discovering New Species of large Quadrupeds._
Naturalists, certainly, have not yet explored all the continents, nor
do they even know all the quadrupeds which inhabit the countries that
they have explored. New species of this class are discovered from
time to time; and those who have not examined with attention all the
circumstances belonging to these discoveries, might also imagine that
the unknown quadrupeds, whose bones are found in our strata, may
remain to this day concealed, in some islands not yet discovered by
navigators, or in some of the vast deserts which occupy the middle of
Asia, Africa, the two Americas, and New Holland.
However, if we carefully examine what kinds of quadrupeds have been
recently discovered, and in what circumstances they have been found,
we shall see that there is little hope of our ever finding alive
those which have hitherto been observed only in a fossil state.
Islands of moderate extent, and at a considerable distance from
the continents or large islands, possess very few quadrupeds, and
these, for the greater part, of diminutive size. When they happen
to contain any of the larger species, these must have been carried
to them from other countries. Bougainville and Cook found no other
large quadrupeds than hogs and dogs in the South Sea Islands; and the
largest species of the West India Islands was the _agouti_.
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