STUB— TEKTIARIES OP SCLAVONIC. 23 



Neu-Gradiska, there was observed, in the first place, marine and over- 

 lying white marl. Towards the Diluvial plain of the Save, in the Slobos- 

 tina-Thal, white calc-marl and grey marl were observed near Caje. 

 Under these the Leithakalk appears near Benkovac, and beneath it 

 the clay [Tegel] crops out at the northern end of the district. It 

 contains Vaginella depressa, Daud., very abundantly, together with 

 the following Foraminifera, as determined by Herr F. Karrer : — 



Glanduhna laevigata, 0. r. B. N. Rotalina Boueana, 0. ? (badly pre- 

 Dentalina inornata, 0. r. B. served). 



elegans, 0. c. B. N. G-lobigerina triloba, Ess. c. B. N. 



pauperata, 0. vr. B. buUoides, 0. vc. B. N. 



Vaginuhna Badenensis, 0. c. B. Truncatulina lobatula, 0. vr. N. 



Marginulina, sp. ? Bulimia pupoides, 0. r. N. 



Cristellaria cassis, 0. r. B. pyrula, 0. vr. "N. B. 



, sp. ? Textularia Mayeriana, 0. vr. N. B. 



Robulina Austriaca, 0. c. B. N. articulata, 0. vr. B. 



cultrata, 0. c. B. N. Sphaeroidina Austriaca, 0. vr. N. B. 



, sp.? Bilocuhna lunula, 0. r. B. 



Nonionina bulloides, 0. vr. N. 



[N.=Nussdorf. B.= Baden. c.= common. vc.=very common. r.=rare. 

 vr.= very rare.] 



They show that this clay [Tegel] is equivalent to that of Baden in 

 the Vienna Basin. There are no traces of Gasteropods, Bivalves, or 

 Bryozoa. Cypridce are rare. 



Near Rogolje, the lowest member of the Neogene strata is a grey 

 marly sand, containing no traces of MoUusca, but the following 

 Bryozoa (determined by Herr Stoliczka) and Foraminifera (deter- 

 mined by Herr F. Karrer) : — 



Bryozoa. 

 Crisia Edwardsi, Ess. Scrupocellaria elliptica, Ess. 

 Filisparsa biloba, Ess. Salicornia marginata, G-oldf. (S. crassa, 

 Idmonea foraminosa. Ess. Busk). 

 tenuisulca, Ess. Eschara polystomella. Ess. 



Foraminifera . 



Vaginulina Badenensis, 0. vr. B. G-lobigerina triloba, 0. r. N. B. 



Polystomella Fichtelliana, 0. vr. N. Uvigerina pygmsea, 0. vr. N. B. 



crispa, 0. r. N. B. Globulina gibba, 0. vr. N. B. 



Nonionina granosa, 0. vr. N. tuberculata, 0. (?) vr. B. 



Rotalina Boueana, 0. r. N. B. Textularia Mayeriana, 0. r. N. B. 



Partschiana, 0. vr. N. B. abbreviata, 0. r. B. 



Almeriana, 0. vr. N. deperdita, 0. vr. N. 



Soldanii, 0. vr. N. — — laevigata, 0. vr. N. 



Globigerina bulloides, 0. r. N. B. 



The conclusion to which Herr Karrer arrives is, that these beds 

 are higher than those of Benkovac, somewhat lower than those 

 of Nussdorf, and probably equivalent to those of Ehrenhausen, 

 Porzteich, and Grinzing, in the Vienna Basin. This formation con- 

 tinues in a N.W. direction towards Gomi Caglic, as far as a ridge 

 near the river, when a white sandy marl and calc-marl, containing 

 AmpJiistegina Haueri, Orb., and A. mammillata, Orb., may be seen 

 alternating with Leithakalk full of small Nullipores. At the top of 

 the ridge the white calc-marl sets in, and forms the surface-rock of 

 this and all the higher hilly ground. 



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