IN JOHAN KI.KI!. [SEC. ARCT. EXP. FRAM 



/1,-jfflrodns xtrifjnfiix ' KVKN. Possibly they are teeth of the Glyptolepis 

 I'.inn described liere. 



M\ material also contain'- a fragment of a jaw with remains of 

 h- th. |S. I. i)|. unfortunately badly preserved (PI. Vlll. fig. 5). At the 

 left we see a numher of -mall marginal teeth, and inside remain- 

 M| the large teeth. The form of the teeth cannot he seen, hut the si/r 

 indicated that they helong to a Holo}>fiichiux form, which must he 

 a-.-umed to lie ]/<>lo]>lt/cliii<s Xcltrii new species. 



llori/. on. The fish hori/.on of Skrap Valley. 



Rhizodontidae. 



Tooth with rhizodont structure. 

 |P1. Vlll. fig. lii. 



My collection contains one tooth showing another structure to that 

 dr-crihed. The tooth, (S. I. 4) appears to have heen ahout \^ mm. long. 

 and ."i mm. hroad. It is hent slightly concave. The upper part of the 

 tonlh i- quite smooth, and at the base we see distinct, coarse ril. 

 The structure must he assumed to be rhizodont. hut I cannot venture 

 to -tale to what species the specimen belong-. 



Horizon. From the light, hard sandstone at S. 0. Haken. on the 

 easl >ide of Goose Fiord. 



Osteolepidcie. 

 Osteolopis sp. 



My material also contains a few small, rhombic scales, which appear 

 to belong to an Ostfiolepis form. The upper surface shows the -aim 

 extremely fine pores that characterise Ostrolepis. The microscopic 

 structure al.-o agrees. I have also other parts of skeleton forms that 

 appear to helong to the same species. 



Mori/, on. The lish hori/. ..... if Skrap Valley. 



Stratigraphic Results of Series E. 

 Distribution of the Fauna in the Fossiliferous Horizons. 



Tin- remain- of the fauna \\hich are de.-crihed in the precedin 

 page- ace thus di-lrihnlrd in the Sandstone series D.; 



