The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic RemainsMantell, Gideon Algernon
Science
The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic Remains
Mantell, Gideon Algernon
Geology -- England -- Guidebooks; Paleontology
When a bone is too imperfect to be united as a whole, it may be
imbedded in Roman cement, or plaster of Paris, which when dry may be
coloured of the prevailing tint of the rock. For large heavy specimens,
the cement is preferable; it is of easy application, and the fissures
and cracks of the bones may be filled up with it, taking care first to
cover the parts with thin hot glue, or the cement, when it dries, will
shrink and fall out. A thin coating of mastic varnish will restore the
colour, and by excluding the air, tend to preserve the specimens.
The teeth have generally undergone the same changes as the bones with
which they are associated. The teeth of elephants or mammoths that are
imbedded in loose calcareous earth, like the loam and chalk-rubble of
Brighton cliffs, and of Walton in Essex, are friable, and apt to split
and separate in the direction of the vertical plates of dentine and
bone: the pieces should be glued together, and when set, the tooth be
thoroughly saturated with thin glue, used very hot, and the superfluous
cement removed with a sponge wrung out as dry as possible from boiling
water. If there be any portion of the jaw attached to the teeth, it
must be carefully preserved; and search should be made for fragments of
the articulations, or parts of the joints and sockets.
In argillaceous strata, as the Lias-shale, London Clay, &c., the
fossils are frequently saturated with brilliant pyrites, or sulphuret
of iron; a mineral which decomposes upon exposure to the atmosphere,
and occasions the destruction of the specimens. The fossils of the Isle
of Sheppey are peculiarly obnoxious to this change.
[Sidenote: FOSSIL ANIMAL REMAINS.]
The remains of vertebrated animals in the Lias, very often occur
as skeletons more or less perfect, the entire configuration of
the original being preserved in many instances (_Bd._ pl. 7.
_Petrifactions_, p. 340). But the deposit in which they lie is
generally laminated, and the shale flakes off without great care; much
time, labour, and practice are therefore required, to obtain specimens
of any considerable size. To the late Miss Mary Anning, of Lyme Regis,
the merit is due, of having first accomplished this difficult task;
Mr. Hawkins has subsequently carried the art to perfection, as may be
seen in the marvellous examples of Ichthyosauri and Plesiosauri, in the
British Museum.[34]
[34] Petrifactions, Room IV. chap. iv. pp. 341, 376.
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