NO. 2.] FACIES, FAUNISTIC CHARACTERS ETC. I39 



It is very remarkable that there is scarcely any faunistic affinity between 

 the fauna of the Callovian of Cape Flora and that of the Callovian of Gape 

 Stewart in East Greenland. Among the numerous Lamellibranchs, which 

 Lundgreen describes from this place, Peden Rinki Lundgr. is perhaps near 

 to our Peden Lindstromi TuUbg. Otherwise, I find no species in the fauna 

 of Cape Steward, which even approximately corresponds to any of the spe- 

 cies from the Callovian of Cape Flora. 



As far as we can tell from our present knowledge, the very same words 

 apply to the Callovian of Cape Flora as those with which Trautschold^ 

 characterised the affinity of the Aucella strata of Novaja Semlja to the Rus- 

 sian Jura. He says: "Generally speaking there is no doubt that the Jura- 

 facies of the northern islands are the same as those of the Russian Jura, 

 and that this northern Jura is nearest to that of the Petschora and Wyt- 

 schegda, which is also very natural". 



This can naturally, only apply here in the restricted sense of our Cal- 

 lovian. 



' S. A. Tullberg, 'Ueber Versteinerungen aus den Aucellen-Schichten Novaja-Semljas', 

 Bihang t. K. Svensk. Vet. Ak. Handl., vol. VI, No. 3, 1881, p. 5. 



