A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological MonumentsLyell, Charles, Sir
Science
A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological Monuments
Lyell, Charles, Sir
Geology
At some points, as at Louans, south of Tours, the shells are stained of a
ferruginous colour, not unlike that of the red crag of Suffolk. The species
are, for the most part, marine, but a few of them belong to land and
fluviatile genera. Among the former, _Helix turonensis_ (fig. 45. p. 30.)
is the most abundant. Remains of terrestrial quadrupeds are here and there
intermixed, belonging to the genera Deinotherium, Mastodon, Rhinoceros,
Hippopotamus, Chaeropotamus, Dichobune, Deer, and others, and these are
accompanied by cetacea, such as the Lamantine, Morse, Sea-calf, and
Dolphin, all of extinct species.
Professor E. Forbes, after studying the fossil testacea which I obtained
from these beds; informs me that he has no doubt they were formed partly on
the shore itself at the level of low water, and partly at very moderate
depths, not exceeding 10 fathoms below that level. The molluscous fauna of
the "faluns" is on the whole much more littoral than that of the red and
coralline crag of Suffolk, and implies a shallower sea. It is, moreover,
contrasted with the Suffolk crag by the indications it affords of an
extra-European climate. Thus it contains seven species of _Cypraea_, some
larger than any existing cowry of the Mediterranean, several species of
_Oliva_, _Ancillaria_, _Mitra_, _Terebra_, _Pyrula_, _Fasciolaria_, and
_Conus_. Of the cones there are no less than eight species, some very
large, whereas the only European cone is of diminutive size. The genus
_Nerita_, and many others, are also represented by individuals of a type
now characteristic of equatorial seas, and wholly unlike any Mediterranean
forms. These proofs of a more elevated temperature seem to imply the higher
antiquity of the faluns as compared with the Suffolk crag, and are in
perfect accordance with the fact of the smaller proportion of testacea of
recent species found in the faluns.
Out of 290 species of shells, collected by myself, in 1840, at
Pontlevoy, Louans, Bossee, and other villages 20 miles south of Tours;
and at Savigne, about 15 miles north-west of that place; 72 only could
be identified with recent species, which is in the proportion of 25 per
cent. A large number of the 290 species are common to all the
localities, those peculiar to each not being more numerous than we might
expect to find in different bays of the same sea.
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