590 THE PALEONTOLOGY OF MINNESOTA. 
[Ctenodonta longa. 
anterior extremity. Posterior end long, subtriangular in outline, with the extremity, 
subacute and the dorsal side almost straight (faintly convex) from the beaks backward; 
ventral margin broadly rounded, semielliptical; anterior margin nicely rounded. 
Post-cardinal side thick, with a large, sharply defined and slightly concave area 
reaching from the beaks to near the posterior extremity of the shell. Surface gently 
convex, scarcely sloping toward the postero-cardinal area, marked with exceedingly 
fine concentric strize and a few stronger lines of growth. Hinge plate strong, 
abruptly bent, the posterior part nearly twice as long as the anterior, the two 
parts forming an angle of about 105°; denticles very little curved, in two distinct 
series, those in each row sét transversely on the hinge plate, about eleven in the 
anterior series and nineteen or twenty in the posterior series. Muscular impressions 
very deep, bordered on their inner sides by strong ridges and set into the wide exca- 
vated ends of the hinge plate; pallial line simple, faint, submarginal. 
The interior of this strongly marked species proves to be quite different from 
what I expected when I described it from the exterior alone. Instead of showing 
relations to C. /evata, excellent valves since obtained prove the species to be nearer 
C. gibberula and C. contracta, Still, C. planodorsata occupies a somewhat isolated posi- 
tion. Inthe first place, casts of the interior, with their very prominent muscular scars, 
remind at once of the present section of the genus. The hinge, however, is very 
different from that of the typical members of the section, the plate being widest 
under the beaks instead of much the narrowest, and the series of denticles very 
abruptly divided into two sets, the whole hinge, therefore, being much more as in 
the C. recurva section. C. longa has similar characters, as appears to be the case 
also with an undescribed species from the Trenton of Tennessee, so that it might 
have been well to institute another section of the genus. But as these sections are 
merely temporary natural groupings of the species, pending a more thorough study 
of the whole family, the ommission cannot be of much consequence. 
The species is so easily recognized by the flat dorsum that comparisons are quite 
unnecessary. : 
Formation and locality.—In the upper part of the middle third of the Trenton shales at severa 
localities in Goodhue county, Minnesota. 
Crenoponta Lonea Ulrich. 
PLATE XXXVII, FIGS. 30 and 31. 
Tellinomya longa ULRIcH, 1892. Amer, Geol., vol, x, p. 103. 
Shell small, compressed, elongate-elliptical, the length equalling a little more 
than twice the greatest hight. Beaks small, situated about one-fourth of the entire 
length from the anterior extremity. Cardinal line, on the whole, very slightly 
