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Pvn H,i I'UitlS

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ASTARTE. 313<br />

upper tertiary strata up to the Red Crag, the variety<br />

elliptica being the more usual form in glacial deposits.<br />

This form has not been found south of Great Britain ;<br />

but the variety hicrassata has a wide range in that<br />

direction, throughout<br />

the Mediterranean and Helles-<br />

pont to the Canaries. Northward this species reaches<br />

Iceland, Upper Norway, and the White Sea, as well as<br />

North America (and the variety elliptica as far as Spitzbergen),<br />

at depths varying from 3 to 160 fathoms. All<br />

the other varieties which I have specified come from the<br />

Hebrides and Shetland.<br />

The animal is very inactive ;<br />

and when buried in mud<br />

the shell is often incrusted with a mineral coat like<br />

tar. Specimens living in tenacious and fetid soil have<br />

the beaks and umbonal area more or less eroded. Thev<br />

are now and then distorted; and I found a large and<br />

malformed pearl in one. The ribs are less numerous<br />

and developed in southern examples of the typical form<br />

than in those from more northern parts.<br />

The inside is<br />

sometimes of a lovely salmoncolour. In specimens<br />

from the Northumberland coast and Skye the front<br />

margin is plain<br />

and the sides are crenulated. The<br />

larger kinds of Asterias are said by M. Gay to prey upon<br />

A. incrassata.<br />

I have failed to separate intermediate forms from<br />

either the typical species or the variety elliptica. They<br />

may belong to one or the other. Particular specimens,<br />

and indeed the bulk of them, may be readily distin-<br />

guished ; but although it may not be agreeable to the<br />

mere collector, whose object is to get as many species<br />

as he can, I must regard the Crassina elliptica of Brown<br />

as only a variety and northern form of this most incon-<br />

stant species. I have never in the course of my dredging-<br />

experience found them in company on the<br />

p<br />

same

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