116 POMPECKJ. JURASSIC FAUNA OF CAPE FLORA, [norw. POL. EXP. 



monotis sp. (cf. ornati Quenst. sp.) was proved, must also be designated 

 Middle Callovian. These stone marls do not appear to have been observed in 

 situ. The pieces before me are surrounded by a rusty-bi'own weather-crust; 

 they were found loose on the talus in the locahties 



2. NNW. of Elmwood, 100 ft. above the sea; 

 4. South-western end of Windy Gully, ca. 400 ft. above the sea. 

 Doubtless the pieces have fallen out of layers which are at a greater 

 height than 400 ft. Probably the stone marls with Cadoceras Nanseni are also 

 in situ at a height of 550 ft. I have some pieces of rock before me from 

 this level, which, petrographically, come between the stone-marls and the clay- 

 sandstones. 



In proving the presence of the 

 Lower Callovian at the south-western end of Windy Gully, at ca. 400 ft. 



and the 



Middle Callovian above Elmwood at 550 ft. 



the occurrences of Callovian in the region of Cape Flora are not exhausted. 



On July 12th, 1896, Prof. Nansen collected a large number of fossils 



at locality 3 



"At the margin of the glacier NNW. of Elmwood, 100--200 ft. above the sea", 



at a distance of IV2 kilometres from Elmwood [cf. p. 17. "Doubtful horizon". 



Letter-press Fig. 1, g, h, Fig. 3, h]. These were: 



Cadoceras Frearsi (d'Orb.) Nik.) 



,. , ,., f free, probably from clay. 



Macrocephahtes sp. J 



Cadoceras sp. indet. (casts of 



umbiHci). 



Serpula flaccida Goldf. 



Cadoceras sp. ex. aff. Nanseni 



n. sp. 



Leda cf. nuda Keys. sp. 



Cadoceras Tchefkini d'Orb. sp 



Belemnites m. f. subextensus 



mk.-Panderi d'Orb.i 



Quenstedtoceras verlumnum. 



Sintz. 



in phosphoritic nodules. 



in clay sandstone. 



in gray, hard clay with a brownish 

 weather crust. 



1 Only one specimen of ttiese Belemnites still shows traces of the surrounding clayey 

 rock; all the other numerous pieces were found loose, washed out of the rock. 



