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Pvn H,i I'UitlS

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12 TEREBRATULID.E.<br />

complete at the lower end : deltidium (or triangular space below<br />

the beak) slight, and divided by the point of the lower<br />

valve: lunge-plate of both valves exceedingly thick, forming<br />

strong supports for the teeth and lamellar processes ; from<br />

these processes extend into the interior two diverging ridges<br />

or septa in the upper valve, and three or more in the lower<br />

valve : teeth of upper valve very strong and projecting towards<br />

each other : sockets in lower valve deep : skeleton consisting<br />

of two thin and elastic blades, which reach within about one-<br />

fourth of the front margin ; they are furnished with upright<br />

spurs at a short distance from the hinge-plate, and have sharp<br />

points. L. 1. B. 0-8.<br />

Yar. oblonga.<br />

Shell much narrower and deeper than usual,<br />

and having the front margin nearly straight.<br />

Habitat :<br />

Rocky and stony ground, from 50 to 90<br />

fathoms, on the north and east coasts of Shetland, but<br />

exceedingly rare in a living state. More than fifty years<br />

ago, when the late Professor Fleming was Minister of<br />

Bressav Island, a stone was brousrht to him by one of<br />

his parishioners, a long-line fisherman, to which three<br />

specimens<br />

of this curious shell were attached. One of<br />

them was sent to Col. Montagu, who described it in the<br />

eleventh volume of the f<br />

Linnean Transactions/ My<br />

late friend Mr. Barlee, as well as myself with Mr. Wal-<br />

ler and Mr. Norman, have lately dredged specimens of<br />

various sizes and ages in the same part of our seas, at<br />

distances from land ranging from one to thirty-five miles.<br />

The locality ("Dublin Bay"), recorded by Dr. Turton<br />

in his (<br />

Conchological Dictionary/ appears to be more<br />

than questionable, especially as he omitted it in his sub-<br />

sequent work on the British bivalves. This species<br />

does not appear to have been found in any of our upper<br />

tertiaries ; but, in all probability, the T. euthyra of Phi-<br />

lippi, a fossil from a corresponding formation in Sicily,<br />

is the same species. T. cranium is rather common on<br />

the Scandinavian coasts; and Dr. Wallich obtained dead

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