GASTEROPODA. 13 
More fusiform than other known English examples of the genus. 
Geological Position and Locality, The Great Oolite of Minchinhampton, collected by 
Mr. Witchell. 
Nartica Huuiana, Lyc. Tab. XLI, fig. 2. 
Testa ovata, subglobosa levi ;- anfractibus 6 valde convexis, suturis profunde impressis, 
spira elevato, acuto ; apertura oblique ovali, antice rotundata postice angulata ; columella 
callosa, umbilico nullo. 
Shell ovate, subglobose, smooth ; volutions (6) very convex, the sutures deeply impressed; 
the spire is elevated, acute, the last volution being very large; the aperture is ovate, 
oblique, the anterior side rounded, the posterior side acute, the length exceeding a moiety of 
that of the entire shell; the columella is rounded, thickened, and there is no umbilicus. 
Allied to WV. cntermedia, Tab. VI, fig. 1, but with a more elevated acute spire, more 
deeply depressed sutures, and a more globose ultimate volution ; specimens vary somewhat 
in the figure of the last volution, but the acute, elevated, deeply sutured spire will always 
serve to distinguish it. 
Geological Positions and Localities. J have obtained it in the Great Oolite of 
Minechinhampton, and in the Inferior Oolite of the same locality ; Mr. Whiteaves has also 
kindly forwarded to me a specimen from the Great Oolite of Kirklmgton, Oxon; the latter, 
which is a young form, has the last volution slightly more globose than in the other 
examples. 
Eutima? Lavieata, Lyc. Tab. XXXI, fig. 3. 
Testa parva levigata, subulata, acuta, anfractibus (circa 10) planatis, angustis, suturis 
impressis ; apertura suborbiculari obliquo, umbilico nullo. 
Shell small, smooth, elongated, apex acute; volutions (about ten) narrow, their sides 
flattened, the sutures distinct but not constricted ; the aperture is obliquely orbicular ; there 
is no umbilicus. 
The height of each volution slightly exceeds the half of the opposite diameter; length, 
nine lines; diameter of the last volution, three lines. 
Compared with Lima ? communis, the spire is more acute, the volutions more flattened, 
and the sutures are less deeply impressed. 
Geological Position and Locality. \t occurs rarely in the Cornbrash of Scarborough ; 
the example figured is from the collection of J. Leckenby, Esq. 
