NORIC AND RHAETIC. 
95 
Paratibetites Tornquisti Mojs. 
,, sp. ind. (iff. Wheeler i Dien. 
Juvavites angulatus Dien. 
,, Sf. ind. aff. Ehrlichii Hau. 
Anatomites sp. ind. aff. Melchioris Mojs. 
„ sp. ind. aff. Caroli Mojs. 
,, sp. ind. aff. Alphonsi Mojs. 
Dielasma aff. julico Bittn. 
Halohia sp. ind. aff. fascigeroe Bittn. 
Pecton (Amusium) margarito costatus Dien. 
Pecten sp. ind. aff. monilifero Muenst. 
Lima cf. serraticosta Bittn. 
Homomya sp. ind. aff. larianoe Stopp. 
Mytilus sp. ind. aff. rugoso Roem. 
Mysidioptera sp. ind. 
The Juvavites shales become calcareous in the upper portions and 
pass into concretionary limestones, which resemble gradually the con- 
cretionary limestone of the Muschelkalk in their lithological characters. 
Near the top of the series some beds of calcareous sandstones with 
plant remains have been noticed by A. v. Krafft. 
The calcareous sandstones with plant remains form the base of ths 
next rock-group, A. v. Krafft 's "Coral limestone." It is a mass of grey 
limestone, about 100 feet in thickness. In the section of Lilang it is 
a true organogenic limestone in which remains of crinoids and corals 
abound. But in the section of Kaga corals occur rather rarely, and 
none at all have been found W. of Chabrang. Otherwise the coral 
limestone is very poor in well-preserved fossils. Only two species of 
brachiopods are known from it, namely : — 
Spiriferina Griesbachi Bittn. 
Rhynchonella bambanagensis Bittn. 
The coral limestone is overlain by flaggy sandstones alternating with 
black, splintery shaly limestones and sandy shales. The thickness of 
this series, which lithologically recalls the Juvavites beds, is about 30 
feet. 
V 290 ) 
