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
409. Two inquiries concerning these bones have excited the curiosity
of naturalists; first, to discover among the living tribes at present
inhabiting the earth, those to which the fossil remains may with the
greatest probability be referred; and, secondly, to find out the cause
why these remains exist in such quantities, in countries where the
animals to which they belong, whatever they be, are at present unknown.
The solution of the first of these questions, is much more within our
reach than the second, and at any rate must be first sought for.
On the authority of so eminent a naturalist as Pallas, the bones from
Siberia may safely be referred to the elephant, the rhinoceros, and
buffalo, as mentioned above, though perhaps to varieties of them with
which we are not now acquainted. With respect to the bones of North
America, the question is more doubtful, for they have this particular
circumstance attending them, viz. that along with the thighbones,
tusks, &c. which might be supposed to belong to the elephant, grinders
are always found of a structure and form entirely different from
the grinders of that animal.[216] Some naturalists, particularly M.
DAUBENTON, referred these grinders to the hippopotamus; but Dr W.
HUNTER appears to have proved, in a very satisfactory manner, that they
cannot have belonged to either of the animals just mentioned, but to a
_carnivorous_ animal of enormous size, the race of which, fortunately
for the present inhabitants of the earth, seems now to be entirely
extinct.[217] The foundation of Dr Hunter's opinion is, that in these
grinders the enamel is merely an external covering; whereas, in the
elephant, and other animals destined to live on vegetable food, the
enamel is intermixed with the substance of the tooth.[218]
[Footnote 216: See Mr Collinson's papers, above referred to. Phil.
Trans. vol. lvii.]
[Footnote 217: Phil. Trans. vol. lviii. p. 3, &c.]
[Footnote 218: A fossil grinder in the collection of JOHN MACGOWAN,
Esq. of Edinburgh, answers nearly to Mr Collinson's description, and is
very well represented by the figure which accompanies it. This grinder
weighs four pounds one-fourth avoirdupois; the circumference of the
_corona_ is eighteen inches; the coat of enamel is one-fourth of an
inch thick; there are five double teeth; in Mr Collinson's specimen
there are only four.]
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