17; 



Pecten Steivartianus, Lundgren^), but a more exact determination 

 cannot be made. 



According to Lundgren, Feden Stewartianus occurs fairly 

 abundantly in the grey sandstone of Cape Stewart in Jameson's 

 Land which is reckoned by him to be of Callovian age. 



Pecten sp. cf. Johnstrupi. Lundgren. 



1895. Lundgren, В. Anmärkningar om några Jurafossil från Kap Stewart 

 i Ost-Grönland. Medd. om Grönland. Hefte 19, 1896, p. 199, tab. III, 

 flg. 13. 



Part of a ribbed Pecten was found by Hartz on Aug. 11'^ 

 in a block of dark-coloured calcareous sandstone from Varde- 

 klöft. The ears of the shell are wanting, otherwise it is in 

 every other respect identical with Pecten Johnstrupi but is too 

 incomplete to be determined with any certainty. 



Pecten Johnstrupi is, according to Lundgren, one of the 

 very commonest species occurring in the grey sandstone of Cape 

 Stewart in Jameson's Land, which rock is by him referred to 

 the Callovian. 



Pecten sp). cf. Rinki. Lundgren. 



1896. Lundgren, В. Anmärkningar om några Jurafossil från Kap Stewart i 

 Ost-Grönland. Medd. om Grönland. Hefte 19, 1896. p.200, tab. III, fig. 14. 



A smooth cast of a Pecten has been found in a block 

 of coarse-grained sandstone from Vardeklöft. The specimen is 

 about 46°i™ long and 45™°^ wide. It resembles Pecten Rinki 

 but cannot be determined with any certainty. 



Pecten Rinki, as described by Lundgren, occurs in the grey 

 sandstone of Cape Stewart in Jameson's Land, which is referred 

 to the Callovian by Lundgren. 



Pecten sp. 



Pi. VI, fig. 10. 



A cast of a rather finely striated Pecten, which cannot be 

 identified, occurs in the Aucella- ssindsione. The sandstone 



Lundgren, В. 1895, p. 198, pi. HI, fig. 12. 



