2 
UTICA SLATE AND HUDSON-RIVER GROUP. 309 
CEPHALOPODA OF THE UTICA SLATE AND HUDSON-RIVER GROUP. 
Prares LXXXV., LXXXVI. & LXXXVII. 
The rocks of this group furnish few species of CepHaLopopa in addition to those already 
described. The Orrnocerata are usually found in fragments, entirely denuded of the 
shell, and so much compressed as to render it difficult to identify them. Several species, 
apparently identical with those previously described, are found ranging through the group. 
Among these, the young shells of Endoceras proteiforme are the most abundant, particularly 
in the Utica slate. Two or three previously unknown forms appear in the higher part of 
the group, where some of the strata are calcareous; but these are often obscure, and their 
determination unsatisfactory. 
In the western extension of the group, in Ohio and Indiana, I have observed several 
species of OrtHocERAS, but have not yet determined whether they are identical with those 
here described or not. 
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249, 1. TROCHOLITES AMMONIUS. 
Pu. LXXXIV. Figs. 2 a, b,c. 
Reference pag. 192, pl. 40, figs. 4 a-—k, of this volume. 
Trocholites rugosus. ConrApin MS. State Collection. 
Trocholites, Utica trocholite. VanuxEem, Geol. Report, 1842, pag. 57, fig. 3. 
This fossil is clearly identical with T. ammonius of the Trenton limestone, the difference 
observable in some specimens being due to the character of the enclosing shale, or to the 
partial exfoliation of the shell. Its appearance in this position shows that it continued to 
exist in considerable numbers after the cessation of the calcareous deposits below ; and, on 
this account, we may look for its occurrence in the shales of the Hudson-river group. 
Fig. 2 a. A small specimen, partially preserving the shell in some parts, and showing the septa in 
others. 
Fig. 2 6. An enlarged portion of the surface, which is partially exfoliated, and slightly different from 
similar magnified parts of those in the Trenton Jimestone, where the shell is well preserved. 
Fig. 2 c. Mould of a large specimen, in the black slate. 
Position and locality. This species occurs in the Utica slate on East-Canada creek, at 
Canajoharie ; Cold-spring, on the Erie canal ; and in other places, associated with Calymene 
beckit. 
