OF DENISON 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 of the 
upper layers of division III. See Plate VII, Fig. 27. 
Conularia newherryi, Winchell. 
(Plate VI, Fig. 13; Plate VIII, Fig. 9; Plate II, Fig. 18?) 
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 directly 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 ninth 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 reidentifies this species from bed 4. 
Sciotoville, O. [Proc. Am. Philos. Soc., Vol. 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 to the inch; it bears a V-shaped 
•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 toward the 
base with a gentle curve in their extension across the side of the pyra- 
mid, by which their centres are about two intervals lower than the por- 
