TRENTON LIMESTONE. 205 
270. 23. ORTHOCERAS AMPLICAMERATUM (x. sp.). 
Pu. LI. Figs. 1 a-g. 
Teretely cylindrical, extremely elongated, very gradually tapering ; outer chamber 
profound ; septa distant about one third the diameter, very convex; siphuncle excentric, 
small ; surface? section circular. 
The peculiarities of this species are its great length, and very gradual diminution from 
the larger extremity, and the distant and very convex septa, which seem sufficient to 
distinguish it from all other species known in this rock. 
In all the specimens examined, there is no enlargement of the siphuncle sufficient to 
admit the development of embryo tubes, unless they are mainly confined to the outer 
chamber, a longitudinal section of which does not reveal any thing of that kind. 
Fig. 1 a, 6. Parts of the same individual, preserving a large portion of the outer chamber, with an equal 
length of the septate part of the tube. 
Fig. 1c. A transverse section of the specimen, at the upper extremity of 1 a, showing the excentric 
position of the siphuncle. 
Fig. 1 d,e. A fragment of another specimen, showing the same distance of the septa and excentric 
position of the siphuncle. 
Fig. 1 f A fragment of the septate portion of a much larger specimen. 
Fig. 1 g. Transverse section of the same, showing the position of the siphuncle. 
Position and locality. This species is found in the central and higher part of the Trenton 
limestone at Middleville. (State Collection.) 
271. 24. ORTHOCERAS STRIGATUM (ux. sp.). 
Pu. LVI. Figs. 1 a, 0, ¢, d. 
Compare O. lineatum, UtstncER, pag. 29, pl. 9, fig. 6. 
Elongated, teretely cylindrical, gradually tapering ; outer chamber large ; septa distant 
about one fifth the diameter of the shell, very convex ; siphuncle small, central ; surface 
marked by flexuous elevated longitudinal lines, which are indistinctly visible on the cast. 
In the comparative distance of the septa, this species approaches some of the varieties of 
Endoceras proteiforme ; but the septa are more convex, and the siphuncle always central. 
The longitudinal striz differ essentially from the ridges in the next species, and are more 
distinct than in any of the species without annulations. The transverse striz, if any exist, 
are much finer, and not preserved where the shell is exfoliated. 
This species approaches in character to the O. lineatum of HistnceEr ; but the longitudinal 
strie are stronger than in that species, judging from the character of the surface, which is 
imperfectly preserved in our specimens. 
