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DIENER: TRIAS OF THE HIMALAYAS. 
Between 200 and 300 feet above the base of the system the following 
species were found by A. v. Krafft : — 
Spirigern Noetlingi Bittn. 
Sfiriferina cf. Haueri Suess. 
Lima cumaunica Bittn. 
Pecten chabrangensis Dien. 
Sf. ind. aff. Landrano Bittn. 
Entolium cf. suhdemissum Muenst. 
Megalodon ladaJchensis Bittn. 
Fig. 8. — Section between Kibber and Ki (from A . v. Krafft' s diary). 
7- Megalodon limestone. 
6. Juvavites shales. 
5. Dolomites with Lirna cf. austriaca. 
4. Tropites shales. 
3. Grey Beds. 
2. Daonella and Halobia limestone. 
1. Daonella shales. 
It is evident from this faunula that, notwithstanding the scarcity of 
fossils, the beds including it are still equivalent to the Upper Trias. 
About 400 feet above the base of the system a white, dolomitic band, 
30 feet in thickness, was observed in several sections by A. v. Krafft, 
but has not yielded any fossils. Beds with rhsetic types are entirely 
absent. 
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