CLINTON GROUP, 
301 
Genus BEYRICHIA (M‘Coy). 
This fossil body has been very appropriately separated by Mr. M c Coy from Agnostis, to 
which such bodies have heretofore been referred. 
We have three or four species of this in our successive groups, beginning with the Clinton 
group. 
668. 1. BEYRICHIA LATA. 
Pl. ALXVI. Fig. 10 a-e. 
Agnostus latus. Vanuxem, Conrad, Rep. N. Y. Geology. 
Semioval or subreniform, unequally trilobate or trinucleate ; on one valve an oval subcentral 
lobe reaching more than half way across, with a depression on each side, beyond which the 
surface is elevated; ventral margin bordered by a narrow defined rim; on the other valve 
a depression corresponding to the lobe, and the surface elevated on either side; surface 
granulate 1 ? 
We know nothing of this species, except from casts in ferruginous slate and sandstone, or 
equally ill-defined specimens in iron ore. In the best preserved specimens, the surface appears 
to have been granulate or tuberculate. 
Fig. 10 a. A fragment of ferruginous slate, covered with the separate valves of this fossil. 
Fig. 10 i. A valve having a subcentral depression. 
Fig. 10 c. A valve with a subcentral lobe or nucleus. 
Fig. 10 d, e. The interior of the shell, or impression made by the cast. 
Position and locality. In the ferruginous shale associated with the iron ore at Wadsworth’s 
quarries, and in the ferruginous sandstones below, at New-Hartford, Oneida county; in nu¬ 
merous localities in the same position farther west, and in the green shale of the group at 
Sodus and Rochester. 
