Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
It is not the least remarkable circumstance connected with these
bones, that they are in such a high state of preservation as to
present all the lines and impressions of the parts which had been
attached to them in the recent state. Indeed, if we examine them
as compared with the bones of an animal from which all the softer
parts have been separated by maceration, the only perceptible
differences in their physical properties are, that they are a
little heavier, a degree harder, that their surface is brown, and
that they all, with the exception of the horns, present a polished
appearance, which is owing to the periosteum having been preserved,
and still remaining to cover them, as was discovered when they were
chemically examined.
The existence of fat or adipocire in the shaft of one of the
bones mentioned by Archdeacon Maunsell, and which I saw in his
possession, is a thing for which it is extremely difficult to
account, as it occurred but in one solitary instance, and it did
not appear that this bone was at all differently circumstanced from
the rest. Those which I had an opportunity of examining, by boring
holes in them, were hollow, and contained, for the most part, only
a small quantity of black animal earth.
Mr Stokes found, in a rib of this animal,
Animal matter, 42.87
Phosphates with some Fluates, 43.45
Carb., Lime 9.14
Oxides, 1.02
Silica, 1.14
Water and loss, 2.38
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100.00
Dr Apjohn of Dublin made the following observations with regard to
the animal matter in the bones:
‘The bone was subjected for two days to the action of dilute
muriatic acid. When examined at the end of this period, it had
become as flexible as a recent bone submitted to the action of
the same solvent. The periosteum was in some parts puffed out by
carbonic acid gas, disengaged from the bone, and appeared to be in
a state of perfect soundness.
‘To a portion of the solution of the bone in the muriatic acid some
infusion of galls was added, which caused a copious precipitate of
a dun colour. This proved to be tannate of gelatine, mixed with a
small portion of the tannate and gallate of iron.
‘The cartilage and gelatine, therefore, so far from being
destroyed, had not been perceptibly altered by time.’”
Public-domain text, read in full here on John Shaqi.
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