﻿20 Bulletin 18 46 



more perfect material is obtained from the 

 Lake Charnplain Caleiferous that this species 

 may prove to be D. macleodi. This is, how- 

 ever, doubtful. 



Syntrophia palmata Cleland 



Am. Pal., Vol. 3, Bull. 13, 1900, p. 18, pi. 17, figs. 14 to 17. 



.5. palmata is confined to the Ft. Hunter-Tribes Hill region so 

 far as our present knowledge goes. 



BRYOZOA (?) 



Stromatopora (?) 



Beds of limestone and chert from a few inches to a foot or 

 more in thickness full of Stromatopora (?) occur at Little Falls, 

 St. Johnsville, and elsewhere in the Mohawk Valley. No 

 attempt at a specific determination was made. 



Bchinodermata 



CRINOIDEA 



Crinoid stems and plates 



Well preserved plates apparently identical with those figured 

 by Vauuxem in the Geological Report of the Third District of 

 New York, were among the commonest fossils on weathered 

 surfaces. 



Distribution.— -The distribution is the same as for Pleurotomaria 

 hunterensis. 



Coelenterata 

 GRAPTOLITES 



Callograptus salteri (?) Hall Pi. 4, Fig. 4. 



Geol. of the Quebec Group, p. 135, pi, 19. 



Three specimens of this graptolite, in a poor state of preserva- 

 tion, were found in bed A 3 at Tribes Hill. They were referred 

 to Dr. Ruedeman who identified them as C. salteri (?). This 

 species was not found in any other place. 



