256 
Aug, F. Foerste 
railroad bridge, about a mile east of Pulaski, a species of Lingula 
(plate III, Fig. 13) occurs which is distinct from Lingula recti- 
lateralis. It is smaller and slightly less quadrangular. If lines 
are drawn from the beak to the anterodateral angles, the concen- 
tric lines are much more conspicuous on the lateral parts of the 
shell than on the intermediate portions. The shell is very thin 
and there is no indication of longitudinal radiating striae along 
the middle parts of the shell, either on the exterior or interior 
surfaces. The shell apparently belongs to the group with a long 
median septum and with concrete laterals, such as are figured 
by Plall, in his monograph on Palaeozoic Brachiopoda, Plate I, 
Fig. 7, under the name Lingula procteri. 
The following species were associated with the Lingula at the 
Trinucleus horizon, east of Pulaski: Plectamhonites , Dalmanella, 
Rafinesquina alternata of very flat form, Schizocrania filosa, 
Byssonychia radiata, Modiolopsis modiolaris, Colpomya pusilla, 
Cuneaniya, Clidophorus planulatus, Archinacella pulaskiensis , 
Cornulites of straight free form like Tentaculites, Calymene, and 
Trinucleus. 
At the bridge south of Allandale, west of the mouth of the 
Lorraine gorge, the following species occur in the black shale 
commonly identified as Utica: Glossograptus quadrimucronatus, 
near mutation postremus, Climacograptus typicalis, Mastigograp- 
tus resembling tenuiramosus, Schizocrania filosa, Leptoholus in- 
signis, Zygospira of modesta type, Orthoceras, Triarthrus heckii, 
and Trinucleus. This is the fauna usually identified as Utica in 
these more western areas, and it may be followed up stream into 
the mouth of the ^^Gulf. The graptolites were identified by 
Dr. Ruedemann. 
3. Pholidops subtruncata, Hall 
Pholidops subtruncata was figured by Hall from the expo- 
sures at Lorraine, New York. It occurs also east of Lorraine, 
where the road to Worthville crosses the creek, 2 miles west of the 
latter village; also northeast of Lorraine, along the creek within 
the limits of Barnes Corners. It is found also along the river 
about half a mile below Salmon Falls, a short distance below the 
level of the base of the Falls. 
The name of the species is based upon the straightened anterior 
margin of the shell in the case of the type specimens. Speci- 
