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CHAP. XXII.] MOLLUSCA. 537<br />

Family 20.—GASTEOCH^NID^. (5 Genera, 40 Species.)<br />

DiSTKiBUTiON.—Temperate and warm seas. Aspergillum ranges<br />

from the Eed Sea to New Zealand. There are 35 fossil species,<br />

ranging back to the Lower Oolite.<br />

Family 21.—PHOLADID^. (4 Genera, 81 Species.)<br />

Distribution.—These burrowing molluscs inhabit all Tempe-<br />

rate and warm seas from Norway to New Zealand. There are<br />

about 50 fossil species, ranging back to the epoch of the Lias.<br />

General Remarks on the Distribution of the Marine Mollusca.<br />

The marine Mollusca are remarkable for their usually wide<br />

distribution. About 48 of the families are cosmopolitan, rang-<br />

ing over both hemispheres, and in cold as well as warm seas.<br />

About 15 are restricted to the warmer seas of the globe ; but<br />

several of these extend from Norway to New Zealand, a distri-<br />

bution which may be called universal, and only 2 or 3 are<br />

absolutely confined to Tropical seas. Two small families only,<br />

are confined to the Pacific and Indian Oceans. Marine fishes,<br />

on the other hand, have a much less cosmopolitan character, no<br />

less than 30 families having a limited distribution, while 50<br />

are universal. Some of these 30 families are confined to the<br />

Northern seas, some to the Atlantic and Mediterranean, and a<br />

considerable number to the Indian Ocean and Western Pacific.<br />

Many of these families, it is true, are much smaller than those<br />

of the Mollusca, which seem to possess very few of those small<br />

isolated families of two or three species only, which abound in<br />

all the Vertebrate classes. These differences are no doubt con-<br />

nected with the higher organisation of fishes, which renders them<br />

more susceptible to changed conditions of life ;<br />

and this is indi-<br />

cated by the much less antiquity of existing families of fishes,<br />

the greater part of which do not date back beyond the Cretaceous<br />

epoch, and many of them only to the Eocene. In striking con-<br />

tras-,t we have the vast antiquity of most of the families of Mol-

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