OAttNiC STAGE. 
8d 
Trachysagenites galeatus Dien. 
Discotropites sp. ind. aff. Plinii Mojs. 
Anatomites cf. Bacchus Mojs. 
Joviles spectabilis Dien. 
,, cf. siculus Gemm. 
Sandlingites nov. sp. aff. Reyeri Mojs. 
< „ nov. sp. aff. Castellii Mojs. 
Clionites heracUtiformis Dien. 
Proarcestes cf. Gaylani Klipst.i 
Grey shaly limestones and calcareous shales continue with the same 
lithological characters for the next 200 feet. Seventy feet above the 
nodular limestone a specimen of Jovites spectahilis Dien. was discovered 
by A. V. Krafit, who consequently includes the entire series following 
above the concretionary limestone with Cephalopoda in his " Tropites 
beds. " 
The next overlying bed is a dolomitic limestone, whose thickness 
amounts to 300 feet. It has yielded few and badly preserved fossils, 
with carnic affinities, among them 
Dielasma julicum Bittn. 
Terebraiula sp. ind. aff. piriformis Suess. 
Spiriferina sp. ind. aff. shalshalensis Bittn. 
Lima cf. austriaca Bittn. 
Halobia aff. superba Mojs. ' ^ 
Daonella aff. styriaca Mojs. 
With this complex of dolomitic limestones the carnic stage comes to 
a close. Its entire thickness in the section of Lilang amounts to at 
least 1,600 feet. 
In Painkhauda the development of the carnic stage is more uni- 
form. 
In the Bambanag and Shalshal cliffs the lowest cephalopod horizon 
of this stage was discovered by Diener in the grey "Traumatocrinus 
limestone," which, according to A. v. Krafft, is separated from 
the Ptychites beds of the Upper Muschelkalk by an insignificant 
To this list Oriesbachites MedUyanus Stol. must probably be added. Stolicz- 
ka's type-specimen, which was found loose in the Pin valley near Kuling, is re- 
ferred to the Tropites beds by A. v. Krafft. A similar remark applies to Para- 
cladiscites indicus Mojs. from the same locality. 
( 290 ) 
