674 G. M. MURGOCI 



From the marly-sandy layers of the Stupinita ravine Dr. Redlich 

 cited: 



Inoceramus Cripsii. Pecten inversum Nils. 



Orbitoides Faujasi Brown. Actinacis Haueri Rs. 



Orbitoides secans Leym. Avellana sp. 



Astrocoenia sp. Bacidites anceps Lam. 



Serpula filiformia Sow. Anisoceras cf. siibeonopresum Forb. 



He found in the blocks of a white, grayish, or reddish limestone, 

 with red veins, a numerous fauna, among which are: 



Hippurites I.apeirousei Goldf. Lima divaricata Duj. 

 Hippurites colliciatus Woodw. var. romanica. Lima inversum Nils. 



Orbitoides gensacica Leym. Gryphaea vesicularis Lamk. 



Orbitoides secans Leym. Exogyra sp. 



Lithothamnium cj. turonicum Roth. etc., etc., etc. 



Terebr alula carnea Sow. And two new species: 



Terebratula biplicata Brocc. Terebratella Mrazeki. 



Lima tecta D'Orb. Waldheimia Pascuensis. 



Dr. Redlich, considering that the conglomerates which contain 

 these certainly Senonian limestone blocks underlie the above- 

 mentioned Senonian marls and sandstones, expresses his opinion that 

 these blocks are destruction products of a bank of Hippurites lime- 

 stone which was formed within the conglomerates. But the con- 

 glomerate layers with these interesting blocks overlie the marls and 

 sandstones with Inoceramus Cripsii, 1 and I think I am making no 

 mistake in saying that they are an Eocene formation. 



Besides the Nummulites indicated by Redlich in the lower strata, 

 with Orbitoides, of this complex, I adduce the identity in constitu- 

 tion and the continuity with the strata from the Titesti Basin, 

 where in layers immediately on those banks of conglomerates Sabba 

 Stefanescu and K. Redlich have collected abundant Middle Eocene 

 fossils. 



Such blocks of Hippurites and Coral limestone are very frequent, 

 not only in the Brezoi-Titesti Basin, but also in the Eocene conglom- 

 erates, which form a zone from Arifu (Arges valley) at Salatrucu, 

 Calimanesti, up to Cheia (Valcea). In the coarse conglomerates 

 Sabba and Gr. Stefanescu have found also numerous Middle Eocene 

 fossils. At Calimanesti-Salatrucu the conglomerates are overlain by 



1 Loc. cit. (footnotes 2 and 3, p. 672). 



