NORIC AND RHAEHC. 
107 
Pinacoceras parma Mojs. 
,, post par ma Mojs. 
Jiambanuijites Dieneri Mojs. 
,, Schkujintweiti Mojs. 
Flacites Sakuntala Mojs. 
Paranaudlus bambanagensis Mojs. 
ludonaulilus Kraffti Mojs.^ 
Clydonautilus bianqularis Mojs. 
The Halorites limestone is eminently a cephalopod horizon, in which 
ammonites predominate very considerably among the invertebrate 
fauna. The number of species of Brachiopoda and Lamellibranchiata 
which have been described by Bittner (I.e., p. 72), is very small. He 
mentions the following forms : — 
Rhynchonella bambanagensis Bittn. 
Halobia off. comata Bittn. 
Lima serraticosta Bittn. 
Anodontophora Griesbachi Bittn. 
The lowest noric horizon in Painkhanda is a complex of nodular and 
slaty limestones, from 70 to 100 feet in thickness, which succeeds the 
beds with Halobia comata in the Bambanag section and is overlain imme- 
diately by the fossiltferous layer of the Halorites beds. The small fauna 
consists of badly preserved cephalopoda, of which only a single species 
has been found worthy of a specific name. The rest are indetermin- 
able fragments. 
The following forms have been enumerated by E. v. Mojsisovics : — 
Proclydonautilus Griesbachi Mojs. 
Pinacoceras sp. ind. afj. imperator Mojs. 
Hauerites sp. ind. ( = Metacarnites Dien). 
Arcestes sp. ind. 
Sagenites sp. ind. 
Juvavites sp. itid. 
Parajuvavites sp. ind. afj. Jacquini Mojs. 
sp. ind. 
^ E. V. Mojsisovics, Die Cephalopoden der Hallstaetter Kalke, Abhandl. K. K. 
Geol. ReicJisanst., yi-1, Suijplem., p. 205. 
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