70 PALHONTOLOGY OF NEW=-YORK. 
106. 4. STREPTOPLASMA CRASSA (x. sp.). 
Pu. XXV. Figs, 2 a, 6, ¢. 
Obliquely turbinate, slightly curved, gradually expanding upwards from an obtuse point ; 
lamellz about fifty, coarse and strong ; surface marked by longitudinal lines coincident 
with the lamelle ; transverse lines obsolete. 
The whole aspect of this specimen is strong and coarse, differing essentially from the 
last, which presents a neat symmetrical outline and surface. The interior presents some 
apparent irregularity in the lamella, showing a depression toward the more expanded side 
of the coral, somewhat like Canin1a. The structure otherwise, however, is unlike Caninia, 
and, as in STREPTOPLASMA, consists of simple vertical lamelle. 
This species resembles in some degree the one so common in the Black-river and Birdseye 
limestones, but the lamelle are coarser and stronger, and equal in thickness to twice the 
space between them. 
Fig. 2 a. Lateral view of a specimen, the edges somewhat broken. 
Fig. 2 b. Longitudinal section, showing the internal arrangement of the lamelle. 
Fig. 2c. View of the cup, showing imperfectly the meeting of the lamelle in the centre. 
Position and locality. Trenton limestone, near Middleville. Rare. 
107. 5. STREPTOPLASMA MULTILAMELLOSA (n. sp.). 
Pui. XXV. Figs. 3 a, d, ¢. 
Obliquely turbinate, somewhat curved, rapidly enlarging above ; cup moderately deep ; 
lamelle about 120, thin, edges apparently shghtly crenulated ; exterior covering thickened, 
smooth. 
This species somewhat resembles the S. corniculum in form; but it is more robust, the 
lamelle more numerous, and the cup more shallow. The outer edges of the lamella, 
where denuded of their covering, appear to be crenulated or wrinkled, and the spaces 
between them are twice their thickness : this last character alone is probably sufficient to 
distinguish the species from the two preceding. 
Fig. 3 a. Lateral view of a specimen, somewhat shortened from wearing off of the smaller extremity. 
Fig. 3 6. Transverse section, showing the thin lamelle. 
Fig. 3c. An enlarged portion of the denuded outer surface. 
Position and locality. In the grey crystalline part of the Trenton limestone, Watertown, 
Jefferson county; and near Trenton, Oneida county. (State Collection.) 
