LAMELLIBRANCHIATA. 497 
Clionychia undata. 
of the shell leaving a distinct depression in the casts. Muscular scars large, situated 
about midway in the postero-car linal half of the valve, the two lobes united by a 
narrow neck, the upper one oval in shape and about one-third as large as the more 
nearly circular lower one. 
The posterior extremity is more produced and more narrowly curved than in the 
other species referred to this genus. 
Formation and locality.—Lower limestone of the Trenton formation at Minneapolis, Minnesota. 
Mus. Reg. No. 5526. 
CLIONYCHIA UNDATA Emmons. 
PLATE XXXV, FIGS. 21 and 22. 
Pterinea undata Emmons, 1842. Geol. Report. New York, p. 395. 
Ambonychia undata HAL, 1847. Pal. New York, vol.i, p. 165. 
Shell subquadrate, cardinal margin long, straight, anterior side straight, nearly 
vertical, curving sharply backward below into the gently convex base, which in its, 
turn curves rapidly upward into the broadly rounded posterior margin; antero- 
cardinal’ angle about 85°, postero-cardinal angle about 115°. Beaks prominent, 
attenuate, slightly incurved, with the umbones strongly convex, the anterior slope 
very abrupt, the rapidity of the descent becoming gradually less in following the 
margin around to the posterior extremity of the hinge, where it is very gentle; 
cardinal slope concave, becoming strongly so and very abrupt in nearing the beaks. 
Surface marked with broad concentric folds, which are strongest on the cardinal 
and umbonal slopes and fade away gradually in curving around to the anterior side. 
Immediately beneath the beaks the anterior side of a good cast of the interior 
presents a sharply defined lunule-like impression, which, having been occupied by 
an internal thickening of the margin of the valves, was scarcely indicated on the 
exterior of the shell. Hinge plate narrow, muscular impressions undetermined. 
The above description is based upon the specimen illustrated on plate xxxv. 
It presents no evidence of distortion and seems to be in every respect in a good 
state of preservation. Comparing this example with Hall’s description and figures 
of the New York types of the species we observe that it differs in several particulars 
that might be regarded as important. The outline is more nearly quadrate, and the 
convexity of the valves less, giving a form that deviates from the figures of the 
New York specimen precisely as C. erecta does from C. lamellesa. Hall also mentions 
the absence of a “definite lunette,’ while such an impression is distinctly present 
in the casts of the Minnesota specimens. Despite these differences [ am almost 
confident of the specific identity of the latter and the types of the species, because | 
am inclined to doubt the actual existence of the discrepancies noticed. 
32— 
