TIBETAN PACIES OF THE HIMALAYAN TRIAS. 
137 
Pinacoceras sp. ind. afj. rex. Mojs. 
Flacites cf. perauctus Mojs. 
Biscolropites cf. sandlim/ensis Hau. 
Tropites cf. subbullatus Hau. 
,, sp. ind. afj. acutangulo Mojs. 
„ sp. ind. afj. Wodani Mojs. 
Anatropites cf. spinosus Mojs. 
,, Pikjrimii Dien. 
Margarites irregularicostatus Dien. 
Jovites cf. spectabilis Dien. 
daciformis Dien. 
Juvavites Kraffti Dien. 
,, dogranus Dien. 
,, nov. sp. ind. afj. subinterrupto Mojs. 
Griesbachites pseudomedleyanus Dien. 
cf. Kastneri Mojs. 
Anatomites sp. ind. aff. Camilli Mojs. 
„ „ Henrici Mojs. 
„ „ „ crasseplicato Mojs. 
Gonionotites cf. italicus Gemm. 
Tibetites bhotensis Dien. 
Loxonema {Polygirina) cf. elegans Hoern. 
Sagana cf. geometrica Kok. 
Capulus {Phryx) joharensis Dien. 
Naticopsis sp. ind. aff. obvallato) Kok. 
This fauna has intimate relations both with the julic (middle carnic) 
and tuvalic (upper carnic) faunae of the Alpine Hallstatt limestone. 
There is an assemblage of species indicating nearly equal affinities with 
the zones of Trachyceras aonoides and of Tropites subbullatus. The red 
marble of the exotic block No. 2 must therefore be considered as a 
homotaxial equivalent of both the middle and upper carnic substages. 
The carnic stage, as represented in the exotic blocks Nos. 2 and 5, 
exhibits very important lithological differences from the dark shales 
and limestones of the beds with Halobia comata or the Grey beds and 
Tropites shales of the main region of the Himalayas. On the other hand, 
its lithological resemblance to the carnic Hallstatt limestone of the 
Roethelstein near Aussee is so great that it is no easy matter to distin- 
guish rock specimens or fossils from those two localities without a close 
( 338 ) 
