NO. 2.] STRATIGRAPHIC RESULTS. 113 



Cadoceras Nanseni n. sp., and 

 Pseudomonotis sp. (cf. ornati Quenst. sp.) 



There are no fragments of Macrocephalites in this rock. 



The pieces of this marl have rolled down from above, and are 

 surrounded with a red weather-crust (Hydroxide of iron). They certainly do 

 not come fi-om the same height as Macrocephalites Koettlitzi; they have 

 rather fallen from a greater height. Very similar, only more sandy rocks 

 have been found in situ in locality 5, near the lower limit of the basalt, at 

 a height of 500 — 550 ft. above the sea. Cadoceras Nanseni n. sp., — as 

 will be seen below — also points to a more recent faunistic horizon than 

 that of the Lower Callovian.] 



The next locality where rocks and fossils were observed in situ is 5. 



Watercourse helotv the basalt, just above (N. of) Elmwood — 500 — 550 ft. 

 [cf. p. 14. "Upper horizon" Letter-press Fig. 1, d, fig. 3, d.] 

 This is the locality which, in the report of the Jackson-Harmsworth Ex- 

 pedition, is mentioned as "a watercourse at the back of Elmwood" i. 



According to Prof. Nansen, rocks in situ, clay-sandstone and hard, 

 finely-grained stone marl were found in this locality at a height of circ. 

 550 ft. above the sea — according to the report of the Jackson-Harmsworth 

 Expedition, 50 ft. below the basalt. 



From the various, partly coarse-grained, partly more compact, less sandy 

 pieces of clay-sandstone, more like the stone-marl (p. 47), of which only 

 some were found in situ, some loose, weathered out of the rock, the follow- 

 ing fossils are before me: 



Pseudomonotis sp. (cf. ornati Quenst. sp.) 

 Pecten Lindstromi Tullbg. 

 ?Limea cf. duplicata Goldf. 

 Lima sp. indet. 



Macrodon Schourovski F. Rouill. sp. 

 Cadoceras Nanseni n. sp. 

 „ sp. indet. 



1 E T Newton and J. J. H. Teall, 1. c p. 496. Under "3 Elmwood" two localities are 

 comprehended. Only the one under the above mentioned designation is identical with 

 our locality 5. The locality of Cadocwas Tchefkini (? d'Orb.), mentioned 1. c. as 

 "the side of the glacier at the western end of Cape Flora," according to Professor 

 Nansen, is our locality 3, I'/j kilometre north-west of Elmwood. 



15 



