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Pvn H,i I'UitlS

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at the height (accurately ascertained)<br />

DONAX. 405<br />

of from 1330 to<br />

1360 feet above the present level of the sea, together<br />

with about fifty other species of shells mostly of an arctic<br />

character ! (Darbishire) ; Mammalian Crag, Bramerton<br />

(S. Wood) ; Sicilian tertiaries (Philippi). M fAndrew has<br />

taken it on the coasts of Upper Norway in 3-25 fathoms ;<br />

I noticed specimens from Jutland in the Royal Museum<br />

at Copenhagen; and southwards it occurs from Schel-<br />

ling on the Dutch coast to Vigo, as well as in the Mediterranean,<br />

iEgean, and Black Sea.<br />

Marvellous accounts have been given of the agility of<br />

this little shell-fish, one of them being that when it is<br />

taken out of the sand it will endeavour to regain the sea<br />

bv a succession of well-directed leaps.<br />

It certainly can<br />

twist itself about almost as actively as Nassa neritea<br />

does in the lagun.es of Venice ; and that is saying a good<br />

deal for it. The fry have triangular shells, with the<br />

posterior end more rounded and the beaks prominent ;<br />

in this stage of growth it is the D. rubra of Turton. A<br />

specimen in my cabinet is inequivalve,<br />

overlapping and partly enveloping the other,<br />

the left valve<br />

as in Cor-<br />

bula. The colours of this shell do not soon fade; they<br />

are, as Tennyson says, of the kind<br />

"That keep the wear and polish of the ware."<br />

This is the D. trunculus of Linne, although<br />

his re-<br />

ferences to the works of Adanson, Buonanni, Klein, and<br />

Argenville belong to an allied species which now generally<br />

bears that name. His descriptions in the ' Fauna<br />

Suecica' as well as in the tenth and twelfth editions<br />

of the '<br />

Systema<br />

Naturae '<br />

exactly apply to the present<br />

species ; and the first authority which he cites is Lis-<br />

ter's f<br />

Treatises on English Animals/ Da Costa finds<br />

fault with these inconsistent references ; but he seems

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