The Student's Elements of GeologyLyell, Charles, Sir
Science
The Student's Elements of Geology
Lyell, Charles, Sir
Geology
We have seen that most of the fossil shells of the Older Pliocene
strata of Suffolk which are of recent species are identical with
testacea now living in British seas, yet some of them belong to
Mediterranean species, and a few even of the genera are those of warmer
climates. We might therefore expect, in studying the fossils of
corresponding age in countries bordering the Mediterranean, to find
among them some species and genera of warmer latitudes. Accordingly, in
the marls belonging to this period at Asti, Parma, Sienna, and parts of
the Tuscan and Roman territories, we observe the genera _Conus, Cypræa,
Strombus, Pyrula, Mitra, Fasciolaria, Sigaretus, Delphinula,
Ancillaria, Oliva, Terebellum, Terebra, Perna, Plicatula,_ and
_Corbis_, some characteristic of tropical seas, others represented by
species more numerous or of larger size than those now proper to the
Mediterranean.
Older Pliocene Flora of Italy.—I have already alluded to the Newer
Pliocene deposits of the Upper Val d’Arno above Florence, and stated
that below those sands and conglomerates, containing the remains of the
_Elephas meridionalis_ and other associated quadrupeds, lie an older
horizontal and conformable series of beds, which may be classed as
Older Pliocene. They consist of blue clays with some subordinate layers
of lignite, and exhibit a richer flora than the overlying Newer
Pliocene beds, and one receding farther from the existing vegetation of
Europe. They also comprise more species common to the antecedent
Miocene period. Among the genera of flowering plants, M. Gaudin
enumerates pine, oak, evergreen oak, plum, plane, alder, elm, fig,
laurel, maple, walnut, birch, buckthorn, hickory, sumach, sarsaparilla,
sassafras, cinnamon, Glyptostrobus, Taxodium, Sequoia, Persea,
Oreodaphne (Fig. 134), Cassia, and Psoralea, and some others. This
assemblage of plants indicates a warm climate, but not so subtropical
an one as that of the Upper Miocene period, which will presently be
considered.
Fig. 134: Creodaphne Heerii. Fig. 135: Liquidambar europæum, var.
trilobatum Fig. 134: _Creodaphne Heerii_.
Leaf[5]
Fig. 135: _Liquidambar europæum_, var. _trilobatum_, A. Br. (sometimes
four-lobed, and more commonly five-lobed).
_a._ Leaf. _b._ Part of same. _c._ Fruit. _d._ Seed Œningen.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account