BIVALVIA. 5 



far beyond the preceding, that the new border composed of the outer layer, is simply 

 joined on to the margin of the former one, so that the successive formations of the 

 outer layer scarcely underlie each other. But when the animal has arrived at its full 

 growth, the new laminae cease to project beyond the old, and as each is composed of 

 a marginal band of the external substance attached to the edge of an entire lamina of 

 the inner, these bands must now underlie each other, being either quite free as in 

 Ostrea, or closely united to each other as in Unio, and most other Bivalves ; and the 

 additions to the shells of the Gasteropoda are made upon the same plan, although it 

 has commonly been supposed that they are only attached to the edge of the old shell, 

 instead of being continued over its entire surface." 



The figure and size of the foot materially influences the form of the anterior part 

 of the shell, while the posterior depends upon the modification of the siphons. 

 The degree of development of the nervous system is said to be very variable in 

 these animals, and the organs of sense dependant thereon variously distributed, im- 

 perfect organs of sight are present in some species, and rudimentary organs of hearing 

 have been detected in others, and are possibly present in all : while in some, the sexes 

 are separate and distinct, in others they are united or hermaphrodite, microscopic 

 animals and plants constitute their principal food. 



Species of this class have been found in the seas of every clime, and inhabit the 

 waters of all depths, some few are left dry by the retiring tide, while others frequent 

 the bottom of seas, to the depth of 200 fathoms ; and the vertical range of many 

 species is so extensive, as to render doubtful the allocation of strata from the presence 

 of a few fossil forms, with whose habits we are but indifi'erently acquainted ; more- 

 over, the habits of all recent species are not, perhaps, necessarily the same as those 

 of their prototypes that lived in times long past, and probably, under different 

 conditions. 



The authors of the beautiful work upon the 'British Mollusca,' now in the course of 

 pubhcation, have given many interesting details respecting the range in depth at 

 which most of these animals have been obtained, and occasionally, the nature of the 

 ground they had selected for their habitation ; tiie generality of species prefer clear 

 water and a sandy bottom, but others are frequenters of mud. The bottoms of the 

 Crag Seas, judging from the deposits now remaining upon the Eastern Coasts of 

 England, appear to have been principally of sand or gravel, with comminuted frag- 

 ments of shells ; that of the Coralline Crag Sea being generally fine in its particles, 

 formed at a depth varying, perhaps, from 20 to as much as 40 fathoms, if the habits of 

 the then existing animals were the same as their homologues of the present day. The 

 Red Crag Sea appears to have been subject to greater agitation, and was probably 

 less in depth, while much of its bottom was of a gravelly character, or of coarser sand. 

 The deposits of the Mammahferous Crag Period present us with characters rather 

 more variable : that which is found near Norwich, being what is called Fluvio-marine, 

 formed probably, in a shallow estuary, and composed of sand, gravel, and shells, 



