NO. 2.] STRATIGRAPHIC RESULTS. 129 



Serpula fiaccida Goldf. 

 Macrocephalites Kosttlitzi n. sp. 



sp. 



J * Ishmce var. arctica E. T. Newton. 



* pila Nik. 

 Cadoceras Frearsi (d'Orb.) Nik. 



sp. sp. (?Elatmce Nik.) 

 Belemnites sp. indet. 1. 



The Middle Callovian 

 (= zone of Reineckia anceps, = zone of Cadoceras Milasch&vici). 



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

 of clay-sandstone of the Middle Callovian; 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 Callovian, 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 Callovian. 



The fossils of the Middle Callovian of Cape Flora are: 

 Pseudomonotis sp. (cf. ornati Querist). 

 Pecten Lindstromi Tullberg. 



* cf. demissus E. T. Newton. 

 ? Limea cf. duplicata Goldf. 

 Lima sp. indet. 



Leda cf. nuda Keys. sp. 



Macrodon Schourovski F. Rouill. sp. 



Cadoceras 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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