CHAZY LIMESTONE. 35 
61. 5. ORTHOCERAS TENUISEPTUM. 
Pu. VI. Fig. 6. 
Cylindrical, gradually tapering, straight; surface smooth ; section cylindrical ; septa 
very thin, gently arched, approximate, about ,); the diameter ; siphuncle small ? 
Only fragments of this shell have been found in this limestone, and therefore all its 
characters cannot be ascertained. It corresponds in many respects with O. primigenium of 
VanuxemM (PI. ii. fig. 11); but the specimens of that fossil attain only a small size, while 
this one is very large. Another difference will be observed in the concavity of the septa, 
which are less arched in the specimen under consideration. 
Position and locality. Chazy, Clinton county, in the dark limestone, associated with 
Maclurea magna. The specimens appear on the surface of the strata, and are all more or 
less weathered. (State Collection.) 
62. 6. ORTHOCERAS BILINEATUM. 
Pu. VII. Figs. 4, 4 a. 
For description, see OrTHocERATA of Trenton limestone. 
An examination of this specimen, since the plate was engraved, convinces me that it is 
identical with O. bilineatum of the Trenton limestone. The specimen was given me by 
Dr. Emmons, as coming from the Calciferous sandstone, at a locality two miles east of the 
city of Albany. An examination of the spot has convinced me that the rock in question is 
the Trenton limestone, thrust up through the Hudson-river slates. The association of fossils, 
as well as all other circumstances, prohibit its reference to the Calciferous sandrock. 
63. 7. ORTHOCERAS MONILIFORME. 
Pr. VIL. Fig. 5. 
Elongated, cylindrical, gradually tapering ; surface smooth, or with only fine strie ; 
septa very slightly arched, distant about 4 the diameter ; siphuncle moniliform, contracted 
at the point of contact with the septa. 
The siphuncle is but little expanded between the septa, which latter, being distant, give 
an elongated moniliform appearance. The apparent contraction towards the base is owing 
to the wearing, in an oblique direction, of the surface of the stone in which it is imbedded. 
In describing many of this family of fossils in the older rocks, it will be necessary to rely 
upon the internal arrangement of the parts, as these are often presented in natural sections, 
while the external surface is obscure or inaccessible. 
Position and locality. Chazy, Clinton county, in limestone, with Maclurea magna. 
5* 
