The Student's Elements of GeologyLyell, Charles, Sir
Science
The Student's Elements of Geology
Lyell, Charles, Sir
Geology
M. Gaudin, jointly with the Marquis Strozzi, has thrown much light on
the botany of beds of the same age in another part of Tuscany, at a
place called Montajone, between the rivers Elsa and Evola, where, among
other plants, is found the _Oreodaphne Heerii_, Gaud. (see Fig. 134),
which is probably only a variety of _Oreodaphne foetens_, or the laurel
called the Til in Madeira, where, as in the Canaries, it constitutes a
large portion of the native woods, but cannot now endure the climate of
Europe. In the fossil specimens the same glands or protuberances are
preserved[6] (see Fig. 134) as those which are seen in the axils of the
primary veins of the leaves in the recent Til. Another plant also
indicating a warmer climate is the _ Liquidambar europæum_, Brong. (see
Fig. 135), a species nearly allied to _L. styracifluum_, L., which
flourishes in most places in the Southern States of North America, on
the borders of the Gulf of Mexico.
[1] See Antiquity of Man, chap. xiv.
[2] Ehrenberg proposed in 1831 the term _ Bryozoum_, or “Moss-animal,”
for the molluscous or ascidian form of polyp, characterised by having
two openings to the digestive sack, as in _Eschara, Flustra,
Retepora,_ and other zoophytes popularly included in the corals, but
now classed by naturalists as mollusca. The term _Polyzoum,_
synonymous with _ Bryozoum,_ was, it seems, proposed in 1830, or the
year before, by Mr. J. O. Thompson.
[3] E. Forbes Mem. Geol. Survey of Gt. Brit., vol. i, p. 386.
[4] See a Memoir on the Lavas and Mode of Origin of Mount Etna by the
Author in Phil. Trans., 1858.
[5] Feuilles fossiles de la Toscane.
[6] Contributions à la Flore fossile Italienne. Gaudin and Strozzi.
Plate 11, Fig. 3. Gaudin, p. 22.
CHAPTER XIV.
MIOCENE PERIOD—UPPER MIOCENE.
Upper Miocene Strata of France—Faluns of Touraine. — Tropical Climate
implied by Testacea. — Proportion of recent Species of Shells. — faluns
more ancient than the Suffolk Crag. — Upper Miocene of Bordeaux and the
South of France. — Upper Miocene of Œningen, in Switzerland. — Plants
of the Upper Fresh-water Molasse. — Fossil Fruit and Flowers as well as
Leaves. — Insects of the Upper Molasse. — Middle or Marine Molasse of
Switzerland. — Upper Miocene Beds of the Bolderberg, in Belgium. —
Vienna Basin. — Upper Miocene of Italy and Greece. — Upper Miocene of
India; Siwalik Hills. — Older Pliocene and Miocene of the United
States.
Upper Miocene Strata of France—Faluns of Touraine.—The strata which we
meet with next in the descending order are those called by many
geologists “Middle Tertiary,” for which in 1833 I proposed the name of
Miocene, selecting the “faluns” of the valley of the Loire, in France,
as my example or type. I shall now call these falunian deposits Upper
Miocene, to distinguish them from others to which the name of Lower
Miocene will be given.
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