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Pvn H,i I'UitlS

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ARCA. 173<br />

mens obtained by Sars and MfAndrew on the coast of<br />

Finmark at depths of from 20 to 160 fathoms are smaller<br />

than the Greenland shells; bnt those from our own<br />

seas and more southern latitudes dwindle into insigni-<br />

ficant proportions compared with any of the above.<br />

M fAndrew has also dredged this species alive off Gib-<br />

raltar, in 45 fathoms, and Forbes in the iEgean, in<br />

200 fathoms. Two specimens which I procured from<br />

water off the north coast of Shetland were at-<br />

deep<br />

tached bv the bvssus to tubes of Pomatoceros arietinus,<br />

and I kept one of<br />

Muller [Ditrupa subulata, Berkeley) ;<br />

them alive for more than a day. Soon after it was put<br />

into a glass vessel and had a fresh supply of water,<br />

it left<br />

its plug of attachment on the Annelid case, and crawled<br />

away at a fair pace on its narrow foot, the valves of its<br />

shell spread out with the beaks uppermost. The action<br />

appeared<br />

to be similar to that of Galeomma Turtoni.<br />

The shell has all the characteristics of Lamarck's<br />

genus Cucullcsa, the side teeth being nearly parallel<br />

with the hinge-line, and consequently at almost a right<br />

angle<br />

angle<br />

to the central teeth or crenulations. But this<br />

varies in different individuals and at successive<br />

of the side teeth is<br />

periods of growth, and the position<br />

more frequently oblique than horizontal. The central<br />

teeth are often wanting. I therefore abstain from<br />

removing this species from Area,<br />

as well as from offer-<br />

ing any opinion as to the value of Lamarck's genus.<br />

Mr. G. B. Sowerby was the first to notice the inequality<br />

of the valves in Cucullcea.<br />

Dr. Torell called my attention to the probability that<br />

the present species might be identical with the A.<br />

glacialis of Gray. Professor Sars had previously ex-<br />

and in his Report on the so-<br />

pressed the same opinion ;<br />

called glacial formation in the Diocese of Christiania.

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