OF DF.NISON UNIVERSITY. 93 



lected in the free-stone of middle Waverly at Granville. The types 

 were from the Goniatite bed of the Kinderhook group, a zone certain- 

 ly embraced within the limits of our Waverly. 



Another and apparently distinct species is characteristic ot the 

 upper layers of division III. See Plate VII, Fig. 27. 



Conularia neii'herryi, Winchell. 

 (Plate VI, Fig. 13; Plate VIII, Fig. 9; Plate II, Fig. iS?) 



This species as quoted by Meek (O. Pal. Vol. II, p. 316), was 

 wrongly attributed to Hall. It was described by Winchell. [ Proc. 

 American Philos. Soc, July, 1865, p. 130.] The original description 

 was written from a small fragment and gives an imperfect idea of the 

 species as a description of a specimen merely always does. 



"Shell very small, in the form of a quadrangular pyramid. The 

 pyramid is inclined over one of the angles. Angles of the pyramid 

 slightly rounded and marked by a shallow groove running longitudi- 

 nally. Each side is marked by sharp raised transverse lines, which 

 instead of running direcdy across, are angulated in the middle, so that 

 at this point they are nearer the base of the shell by a distance equal 

 to once and a half the distance between two lines. The distance be- 

 tween the lines increases from above downwards and is everywhere 

 equal to about one nmth of the width of the side. These transverse 

 lines have the appearance of the projecting edges of septa, and are 

 continuous from the middle of one of the shorter sides of the pyra- 

 mid around to the same point, though the ends do not join, but are al- 

 ternate in position. The sides of the pyramid are inclined at an angle 

 of about 30°." The fragment, about one-half inch long, had a basal 

 diameter of .17. Cuyahoga Falls, O, in water limestone, below the 

 conglomerate Prof. Winchell reidentirles this species from bed 4. 

 Sciotoville, O. [Proc. Am. Philos, Soc, \'ol. XII, Jan. 4, 1870, p. 

 258.] " The species appears to have been at least three or four inches 

 in length ; the septa range from 17-44 ^^^ ^^^^ ^"^■''' J ^^ bears a V-shai)ed 

 furrow along each of the angles, within this furrow the septa are de- 

 flected abruptly toward the base of the shell, so that they meet from 

 opposite sides about at a right angle ; the septa also sweep towanl the 

 base wiih a gentle curve in their extension across the side of the pyra- 

 mid, by which their centres are about two intervals lower than the per- 



