A guide to the shell and starfish galleries : $b (Mollusca, Polyzoa, Brachiopoda, Tunicata, Echinoderma, and Worms)British Museum (Natural History). Department of Zoology
Science
A guide to the shell and starfish galleries : $b (Mollusca, Polyzoa, Brachiopoda, Tunicata, Echinoderma, and Worms)
British Museum (Natural History). Department of Zoology
Echinodermata; Mollusks; Worms
_Lingula_ occurs in the Indo-Pacific, Australia, China, Japan, and the
Pacific Islands. _Glottidia_, a smaller form, with two small curved
plates on the brachial and a ridge on the peduncle valve, is found on
the American coast of the Pacific, and in the Atlantic.
[Illustration:
Fig. 5.
_Lingula anatina_, removed from shell, mantle reflected, coiled arms
separated slightly; _a_, mouth. (Marginal setæ omitted.) Ventral
aspect, three-quarter face.
]
[Illustration:
Fig. 16.
_Lingula anatina._ Interior of valves showing muscle scars.
V. Peduncle valve, D. Brachial valve.
]
Order 2.—NEOTREMATA. The _Discinidæ_ includes two genera, _Discina_ and
_Discinisca_ (Fig. 7), with orbicular conical shells, of horny
calcareous composition; both valves are conical in the former genus, but
in the latter the peduncle valve is flattened. Sometimes the embryos
settle down on the parent shells, and we see a mass of shells in various
stages of growth, as in the specimen of _Discinisca lamellosa_ from
Peru.
[Illustration:
Fig. 7.
_Discinisca lamellosa._ Peru. (After G. Sowerby.)
A group of old and young specimens; largest showing foramen in
peduncle valve, the rest showing brachial valves.
]
[Illustration:
Fig. 8.
Three specimens of _Crania anomala_ on a stone. Loch Fyne.
]
The _Craniidæ_ form small limpet-like shells (Fig. 8) closely adherent
to the rocks by the whole surface of the peduncle valve; although this
valve is so named, no peduncle or foramen is found in this family. The
Neotremata, like the _Lingulidæ_, are remarkable examples of persistence
of type, since forms very similar to the present day _Discinas_ and
_Cranias_ occur in the Palæozoic, Ordovician and Silurian strata.
A piece of rock, with several specimens of _Crania anomala_ attached, is
exhibited.
Section II.—ARTICULATA.
Order 3. PROTREMATA.—This group, formerly very abundant, is now almost
extinct, the Family _Thecidiidæ_ representing the Order at the present
day. _Thecidium mediterraneum_ (Fig. 9) forms little oval boxes about a
third of an inch in length, shaped somewhat like a pear cut in half
(peduncle valve), and with a semicircular lid (brachial valve) working
on a hinge on the upper flat surface. The foramen and peduncle are
absent; but between the pointed end of the peduncle valve and the hinge
is an area filled in by a calcareous plate characteristic of the
Protremata.
[Illustration:
Fig. 9.
_Thecidium mediterraneum._ A, natural size. B, section through shell.
Magnified.
]
The brachial valve opens like the lid of a snuff-box, and shuts down on
the least alarm with the rapidity of lightning. The peduncle valve is
fixed on the rocks by its convex surface. The species is common in the
Mediterranean in from 30 to 300 fathoms, and is also found in the West
Indies.
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