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Pvn H,i I'UitlS

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224 kelliidtE.<br />

and the Sphariidce possess the peculiarity of their tube<br />

or tubes being situate at the shorter and smaller side of<br />

the shell, which may therefore be considered the posterior<br />

end, the ligament being situate at the other end.<br />

Philippi described the present genus<br />

under the name<br />

of Bornia, though not without some suspicion of its being<br />

identical with Kellia. He remarks that he had no<br />

means of seeing Turton's work on the British bivalves.<br />

One character of his genus he conceives to be of very<br />

great importance; and that is the absence of any mark<br />

of a fold of the mantle—" sinus palliaris nullus." There<br />

must be some mistake in this. The character exists in<br />

Mediterranean as well as in British examples of the<br />

typical species. Perhaps Philippi meant to say that the<br />

pallial scar in Kellia is not sinuated as in the Veneriche<br />

and allied families.<br />

It may be well here to say that, in describing the right<br />

and left valves, I have followed the rule laid down in<br />

Dr. Gray's " Conchological Observations" (Zool. Journ.<br />

i. p. 208), viz., "When a bivalve shell is placed on its<br />

basal margin, with the ligament towards the observer,<br />

the right and left valve will correspond with his own<br />

sides." Some rule of this kind is indispensable, in<br />

order to ensure a uniform method of description \<br />

but it<br />

appears of late years to have been left to the caprice of<br />

every author.<br />

Many species<br />

of Kellia are known in a recent and<br />

fossil state. During the formation of the Crag strata,<br />

within the area which is bounded on the west by the<br />

counties of Norfolk, Suffolk, and the adjacent comer of<br />

Essex, several kinds flourished ;<br />

but of these one only is<br />

known to have survived, and still exists in the British<br />

seas.

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