Buffon's Natural History, Volume 01 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &cBuffon, Georges Louis Leclerc, comte de
History
Buffon's Natural History, Volume 01 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &c
Buffon, Georges Louis Leclerc, comte de
Natural history
There are shell-fish which live at the bottom of the sea, and which are
never cast on the shore; authors call them Pelogiæ, to distinguish them
from the others which they call Litterales. It is to be supposed the
cornu ammonis, and some other kinds that are only found in a petrified
state, belong to the former, and that they were filled with the stony
sediment in the very places they are found. There might also have been
certain animals, whose species are perished, and of which number this
shell-fish might be ranked. The extraordinary fossil bones found in
Siberia, Canada, Ireland, and many other places, seem to confirm this
conjecture, for no animal has hitherto been discovered to whom such
bones could belong, as they are, for the most part, of an enormous size.
These shells, according to Woodward, are met with from the top to the
bottom of quarries, pits, and at the bottom of the deepest mines of
Hungary. And Mr. Ray assures us, they are found a thousand feet deep in
the rocks which border the isle of Calda, and in Pembrokeshire in
England.
Shells are not only found in a petrified state, at great depths, and at
the tops of the highest mountains, but there are some met with in their
natural condition, and which have the gloss, colours, and lightness of
sea-shells; and to convince ourselves entirely of this matter, we have
only to compare them with those found on the sea shores. A slight
examination will prove that these fossil and petrified shells are the
same as those of the sea; they are marked with the same articulations
and in the glossopetri, and other teeth of fishes, which are sometimes
found adhering to the jaw-bone, the teeth of the fish are remarked to be
smooth and worn at the extremities, and that they have been made use of
when the animals were alive.
Almost every where on land we meet with fossil-shells, and of those of
the same kind, some are small, others large, some young, others old;
some imperfect, others extremely perfect and we likewise sometimes see
the young ones adhering to the old.
The shell-fish called _purpura_ has a long tongue, the extremity of
which is bony, and so sharp, that it pierces the shells of other fish;
by which means it draws nutriment from them. Shells pierced in this
manner are frequently found in the earth, which is an incontestible
proof that they formerly inclosed living fish, and existed in those
parts where there were the Purpura.
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