468 THE JOURNAL OF GEOLOGY. 
Two specimens of this species were found, one of which, after 
breaking away the outer whorl, furnished a specimen two inches 
in greater diameter. The edges of the septa are distinct and 
show the characteristic curves. It has also the closed umbilicus 
and narrower ventral margin and outline of JV. vofa, but is rather 
narrower and has not the surface markings. The larger specimen 
resembles WV. fexanus (?), (Shum), Gabb. It is possible that 
this species of Gabb will eventually prove to be identical with 
NV. rota, Blanford. 
Gyrodes pansus, stol.; (Eret. Gastr., Inds.305, ple 22: 
Six specimens of this fossil were found all in fair preservation 
and two of which were exceptionally good. The characteristic 
markings, low spire and outline all indicate that there can be no 
doubt of its proper identification. 
Aucula muda, Forbes; Urans."Geolt Soc. onde Vil basucie: 
Releon lindi4oAe pli72 4 
Six specimens were collected of this shell which show clearly 
all the characteristic features of the species. The fossils are all 
well preserved. 
Inoceramus labtatus, Schloch; Bronn’s Jahrb., VII., 93; Proc. 
Acady sce Rhiky ns57, 01945 Can. Mes oss: wl joant 357 ocnmOr 
S. Geol sur Bulle 100.777 .pl auAe 
Ten quite perfect half-shells, besides a large number of frag- 
ments of this species were obtained. The shells agree so well 
with Meek’s description that there can be no room for any other 
rererence: 
Pectunculus sagittata (?), Gabb; Cal. Pal., I., 197, pl. 131; U. 
SiGeol sur Bulle No.5 a3: 
A number of specimens of this shell were found in very good 
preservation, which resemble very closely P. subplantata, Stol., 
but being uncertain as to their identity with this species, I have 
preferred to refer them to P. sagittata, Gabb, in view of what has 
been said by Professor White as to the absence of the sagittate 
markings. F. M. ANDERSON. 
STANFORD UNIVERSITY, 
California, May 8, 1895. 
