A Pictorial Atlas of Fossil Remains, consisting of coloured illustrations selected from Parkinson's "Organic remains of a former world," and Artis's "Antediluvian phytology."Mantell, Gideon Algernon
Science
A Pictorial Atlas of Fossil Remains, consisting of coloured illustrations selected from Parkinson's "Organic remains of a former world," and Artis's "Antediluvian phytology."
Mantell, Gideon Algernon
Paleontology
Figs. 14, & 15, are the anchylosed caudal vertebræ of the tails of
fishes. From the London clay, Isle of Sheppey.
Fig. 16. "A small oyster with a spathose structure."--_Mr.
Parkinson._ This shell is probably the flat valve of a
species of _Dianchora_, of Sowerby; from the Chalk.
[Illustration: Plate LXVI.]
PLATE LXVI.
Fossil Bivalve Shells.
Fig. 1. A fossil Oyster (_Ostrea Marshii_, of Sowerby), from the
Cornbrash of the Oolite, Wiltshire.
Fig. 2. The fossil Cockscomb Oyster, (_Ostrea carinata_, of
Lamarck,) from the Lower chalk, Havre, France.
Fig. 3. The elegant fossil shell here figured is a peculiar and
most abundant species in the Lias formation; specimens
are not uncommon, in which every part of the shell is as
perfect as if just thrown up on the sea-shore. It belongs
to the genus Gryphites (_Gryphea incurva_, of Sowerby,)
the shells of which are nearly related to the oysters, but
are distinguished by the deep concave under-valve, and its
curved beak, and the almost flat upper shell. The testaceous
substance is of a finer laminated structure than in the
Ostrea, and the hinge-ligament is inserted in an elongated
curved groove.[61]
[Footnote 61: Medals of Creation, vol. i. p. 387.]
Fig. 4. "_Ostrea vel frons folium._"--_Mr. Parkinson._ This
species appears to be the _Ostrea gregarea_ (?) of Sowerby,
which occurs in the chlorite marl or firestone of the Lower
chalk in Sussex and Kent.
Fig. 5. The fossil is the cast of an oyster-like bivalve, called
Perna, (_Perna quadrata_, of Sowerby,) which is easily
recognisable, even in casts, by the line of distinct
teeth which compose the hinge. This species is abundant
in the Portland limestone, particularly in the quarries
around Swindon, in Wiltshire; but from the close adhesion
of the outer surface of the shell to the surrounding
stone, they can seldom be extracted, the casts only being
readily obtainable. In the Kimmeridge clay, which lies
above the Portland rock, the shells may be met with in
great perfection. The best locality is near Hartwell, in
Buckinghamshire, where the clay is extensively dug for the
brick manufactures.
Figs. 6, & 7. Two views of a small shell of the genus _Crenatula_,
from Bedfordshire.
Fig. 8. Portion of a very large species of Perna (_Perna
maxillata_, of Sowerby), from tertiary strata. Piedmont. The
figure shows the inner surface of the shell with part of the
broad crenulated hinge.
[Illustration: Plate LXVII.]
PLATE LXVII.
Fossil Shells of Brachiopoda, &c.
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