146 NEW YORK STATE MUSEUM 



was broii<;lil to the <^iirfaro. and shows in addition to the fossils 

 mentioned beU)w well preserved specimene of Panenka 

 1 i n e k 1 a e n i . For material from this locality T am indebted 

 to Miss I. C. Striokler of Buffalo. 



Still another outcrop of this bed has been observed on the left 

 bank of Ellicott creek near Weude station. Orthoceras 

 e X i 1 e is a common fossil at this place. 



Tlie species identified from this bed at Lancaster are: 



Chonetes mucronatus Hall cc 



Strophalosia truncata {Hall} cc 



Liorh^'nchus limitare (Tanuxetn) c 



Ambocoelia nana Grahau . ec 



Meristella meta Hall rr 



Orthoceras exile Hall rr 



II 6 inches. This bed is made up of large concretions which 

 are confluent or separated by small masses of calcareous shale 

 onl}'. The limestone of which the concretions are composed is 

 similar to that of bed I, but ie finer grained and breaks with a 

 conchoidal fracture. Fossils are less numerous than in bed I, 

 thei'^ being fewer individuals but many more species. Stroph- 

 alosia truncata and Ambocoelia nana are slightly 

 larger than the same species in the underlying bed. The list of 

 fossils is as follows: 



Ohonetes mucronatus Hall c 



C. scitulus Hall rr 



Strophalosia truncata {Hall) cc 



Productella dumosa Hall r 



Liorhynchus limitare (Tamixem) cc 



Ambocoelia nana Grahau ec 



Spirifer (Martinia) subumbona Hall rr 



Palaeoneilo sp. rr 



Lei>todesma marcel lense 77^/77 c 



Pleurotoniaria ityfj Hall r 



P. capillaria var. ruslica Conrad r 



Onychochilus (?j nitidulus Clurk^ rr 



