NO. 2.] STRATIGRAPHIC RESULTS. 129 



Serpula flaccida Goldf. 

 Macrocephalites KcettUtzi n. sp. 



n sp. 



^* n Ishmoe var. arctica E. T. Newton. 



* „ pito Nik. 



Gadoceras Frearsi (d'Orb.) Nik. 



„ sp. sp. (?Elatmoe Nik.) 



Belemnites sp. indet. 1. 



The Middle Gallovian 

 (= zone of BeinecMa anceps, = zone of Gadoceras Milaschewici). 

 Above Elmwood, at a height of 500—550 feet above the sea, lie beds 

 of clay-sandstone of the Middle Gallovian; and at the same locality, loose 

 pieces of a clay of the same age were found. Pieces of clay-sandstone, clay 

 and stone marl, which, judging from the fossils they contain, belong to the 

 Middle Gallovian, were moreover found loose at various heights, in several 

 parts of the talus heaps. The occurrences of "cone-in-cone" may also be 

 reckoned as belonging to the Middle Gallovian. 



The fossils of the Middle Gallovian of Gape Flora are: 

 Pseudomonotis sp. (cf. ornati Quenst). 

 Pecten Lindstromi Tullberg. 



* „ cf. demissus E. T. Newton. 

 ? lAmea cf. duplicata Goldf. 

 Lima sp. indet. 



Leda cf. nuda Keys. sp. 



Macrodon Schourovski F. Rouill. sp. 



Gadoceras Tchefkini d'Orb. sp. 



* „ stenolobum (Keys.) Nik. 

 „ Nanseni n. sp. 



„ sp. ex. aff. Nanseni n. sp. 



„ sp. indet. 



Belemnites m. f. subextensus Nik. — Panderi d'Orb. 



1 The fossils marked by an asterisk are taken from the (revised) descriptions by 

 E. T. Newton. 



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