74 Cincinnati Society of Natural History. 
In addition to the fossils in the list on pages 68 and 69, the 
following are found in the upper Utica: 
BRYOZOA. 
Amplexopora septosa (Ulrich). Constellaria constellata - promi- 
Arthropora shafferi-cleavelandi nens Ulrich. 
(James). Crepipora simulans Ulrich. 
Atactopora hirsuta Ulrich. Dekayella obscura Ulrich. 
Batostoma jamesi (Nicholson). (c) e ulrichi (Nicholson).(c) 
Berenicea vesiculosa Ulrich. . ulrichi-robusta Foord. 
Bythopora parvula James. Dekayia maculata (James). 
Callopora nodulosa (Nicholson). Escharopora falciformis (Nichol- 
Ceramoporella granulosa Ulrich, son), variety. 
variety. Phylloporina variolata (Ulrich). 
Ceramoporella granulosa - mil- Stomatopora arachnoidea- tenuis- 
fordensis (James). sima Ulrich. 
Coeloclemaalternatum(James).(c) 
GASTROPODA. 
Bellerophon capax Ulrich. 
CRUSTACEA. 
Ctenobolbina alata Ulrich. Ctenobolbina ciliata-curta Ulrich. 
- bispinosa Ulrich. 
POSITION UNCERTAIN. 
Rusophycus pudicum Hall. 
Protostigma sigillaroides Lesquereux. 
The Lorraine Group. 
The Lorraine at Cincinnati as compared with the under- 
lying Utica contains much less shale and more limestone. 
The shales are bluish or yellowish, and often marly. The 
limestones are even-bedded, on an average four or five inches 
thick, and bluish in color. No markedly waved layers have 
been observed in the Lorraine. All the higher strata at Cin- 
cinnati belong to the Lorraine, and for twenty or thirty miles 
around the city the streams expose these strata. The Lor- 
raine is also found in Kentucky and Tennessee. Mt. Par- 
nassus at Columbia, Tennessee, is a noted locality for Lor- 
raine fossils. 
26 
