GASTEKOPODA. 125 



Distr., 4 sp. Britain, Norway, N. America, Icy sea to Kamtschatka. 

 Living on stones near low water, and ranging to 30 fms. 



Fossil, 3 sp. Miocene — . Brit. 



Suh-gemis. Otina (Gray). V. otis. Shell minute, ear shaped. Animal 

 like velutina, but with a simple mantle, and very short tentacles. W. and 

 S. W. Brit, coast ; inhabiting chinks of rocks, between tide-marks (Forbes). 



FAMILY II. Pyramidellid^. 



Shell spiral, turreted ; nucleus minute, sinistral ; aperture small ; columella 

 sometimes with one or more prominent plaits. Operculum homy, imbricated, 

 nuclus internal. 



Animal with broad ear-shaped tentacles, often connate ; eyes behind the 

 tentacles, at their bases ; proboscis retractile ; foot truncated in front ; ton- 

 gue unarmed. Species all marine. 



Several genera of fossil shells are provisionally placed in this order, from 

 their resemblance to eulima and chemnltzia* Tornatella, usually placed in or 

 near this family, is ojpistho-branchiate. 



Pyramid ELLA, Lam. 



Etym., dimunitive of pyramis, a pyramid. 



Syn., obeUscus, Humph. (P. dolabrata. PI. VIII., fig. 11.) 



Type, P. am-is-cati. PI. VIIL, fig. 10. 



Shell slender, pointed, vnih. numerous plaited or level whirls ; apex sinis- 

 tral ; columella Avith several plaits ; lip sometimes furrowed internally. Operc. 

 indented on the inner side to adapt it to the columeUar plaits. The sheU of 

 the typical pjTamideUse bears some resemblance to cancellaria. 



Distr., 11 sp. W. Indies, Mauritius, Australia. 



lossil, 12 sp. Chalk ?— . France, Brit. 



Odostomia, Fleming, 1824. 



Etijm.., odous, a tooth, and stoma, mouth. 



Type, 0. pUcata, PI. VIIL, fig. 12. 



Shell subulate or ovate, smooth ; apex sinistral ; aperture ovate ; peristome 

 not continuous ; columella A\ith a single tooth-like fold ; lip thin ; operculum 

 horny, indented on the inner side. 



Distr., sp. Brit., Medit., Red Sea, Australia. 



Fossil, 15 sp.? Eocene — . Brit., France. 



Very minute and smooth shells, ha\ang the habit of rissoce, and Hke them 

 sometimes found in brackish water. They range from low water to 40 fms. 

 The animal is undistingtdshable from chemnitzia. 



* '•' The PyramidellidcB present subjects of much interest to the student of extinct 

 moUusca; numerous forms, bearing all the aspect of being members of this family, 

 occur among the fossils of even the oldest stratified rocks. Many of them are gigantic 

 compared with existing species, and the group, as a whole, may be regarded, rather 

 as appertaining to past ages than the present epoch." (Forbes.) 



