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." — John Shaqi
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
Fig. 9. Sections of a pyritous cast of an Ammonite, showing the
sinuous edges of the septa.
[Illustration: Plate LXI.]
PLATE LXI.
Fossil Cephalopoda, &c.
Fig. 1. Part of the cast of a species of Hamite (_Hamites
intermedius_, of Sowerby), from the Gait of Folkstone. The
name _Hamites_ was employed by Mr. Parkinson to designate
a genus of chambered shells, in which the direction of the
spire, instead of being straight, as in _Baculites_, or
discoidal, as in _Ammonites_, was bent like a hook beyond
the inner reflected part. All the specimens here figured are
but fragments.[55]
[Footnote 55: Medals of Creation, vol. ii. p. 500.]
Figs. 2, & 5. Portions of _Hamites intermedius_, of Sowerby.
Fig. 3. _Hamites plicatilis_, of Sowerby.
Fig. 4. A fragment of _Hamites rotundus_, of Sowerby.
Figs. 6, & 7. Two views of a species of an extinct genus, the
shells of which, though not chambered, are supposed to have
been inhabited by Cephalopoda, like the recent Argonaut. The
specimen (_Bellerophon costatus_, of Sowerby) is from the
Mountain limestone of Derbyshire.[56]
[Footnote 56: Ibid p. 477.]
Figs. 8, & 9. An Ammonite with a contracted aperture, and three
deep constrictions across the disk. From the Inferior oolite
of Normandy.
Figs. 10, & 11. Two specimens of "_Scaphites_, or Boat-like
Ammonite," of Mr. Parkinson. A remarkable cretaceous genus
of extinct cephalopoda. The specimens figured are from the
Lower chalk of Sussex (_Scaphites costatus_, of Mantell; _S.
equalis_, of Sowerby).
Fig. 12. Cast of a spiral chambered shell, called _Turrilite_, of
which many species occur in the lower cretaceous strata
(_Turrilites costatus_, of Langius). The quarries of lower
chalk at St. Catharine's Mount, near Rouen, in Normandy,
have long been celebrated for the number and perfection of
specimens of this elegant type of cephalopodous shells.
The first known English examples of this genus, as well as
of Scaphites, were discovered by me in the chalk marl, at
Hamsey, near Lewes, in Sussex, in 1810. Several very fine
specimens of a large species (_Turrilites tuberculatus_),
some of which are more than two feet in length, have
been obtained from the same strata. The tubercles on the
casts of this species are the bases of strong spines. The
siphunculus, in the state of a pyritous cast, is preserved
in some examples.
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