TABLE IV. 



The following list includes species quoted by previous authors from the Inferior Oolite, which 

 are not tabulated in this Monograph. 



Actseonina parvula. Homer. 



Alaria subpunctata, Goldfuss. 



Ceritella acuta, Morris and Lycett. 



Cerithium Roissyi, d'Archiac. 



Chemnitzia Wetherellii, Morris and Lycett. 



Cylindrites acutus, Sowerby. 



— brevis ? Morris and Lycett. 

 Delphinula alta, Morris and Lycett. 



— funata, Goldfuss. 

 Emarginula Blotii, Deslongchamps. 



— planicostulata, Deslongchamps. 

 Fusus ? carinatus, Eomer. 



Natica formosa, Morris and Lycett. 



— macrostoma, Eomer. 



— ? neritoidea, Morris and Lycett. 



— Striclclandi, Morris and Lycett. 

 — ■ Verneuili, d'Archiac. 



Nerinpea Bruntriitann, d'Archiac. 



Nerinsea punctata, Voltz. 



— triplicata, Bronn. 



— Voltzii, Deslongchamps. 

 Nerita pulla, Eomer. 



Onustus Burtonensis, Lycett. 



Phasianella conica, Morris and Lycett (=PA. 

 acutiuscula, M. and L.). 



— parvula, Morris and Lycett. 



— tumidula, Morris and Lycett. 

 Pleurotomaria clathrata, Morris and Lycett. 

 Rimula tricarinata, Sowerby. 

 Trochotoma extensa, Morris and Lycett. 



— obtusa, Morris and Lycett. 



— tabulata, Morris and Lycett. 

 Trochiis bigugatus, ? Quenstedt. 



Turbo depauperatus, Lycett. 

 — princeps, Eomer. 



Of the above species, some, such as Cerithium Roissyi and other Bathonian forms, most probably 

 occur in the higher beds, and especially in the Paludina-hed. at Laugton Bridge, which has more of a 

 Great Oolite than an Inferior Oolite fauna. The same may also be said of N^atica Stricklandi (quoted 

 by Witchell from the Clypeus-gvit), and possibly other Bathonian species of Natica. Again, we may 

 regard Nerita pulla as a general term for any small Nerita (Neridomus) , which in the Inferior Oolite 

 may possibly be covered by Nerita tumidula. Delphinula alta, as it occurs in the Lincolnshire Lime- 

 stone, has been split up into two species, each of which differs more or less from the Great Oolite 

 form. 



On the other hand, it seems highly probable that some of the names on the list, such as Natica 

 macrostoma, Turbo princeps, and several more, are the result of incorrect identification. 



