EUROPE, X17 



aud 5 subdivisions. Albian, 1 division {Belemnites minimus and Am^ 

 monites auritus zone). Neocomian, 3 divisions and 7 subdivisions. 

 Each number is described separately, G. A. L. 



Toula, Dr. Franz. Geologische Untersuchungen im westlicben 

 Theilc des Balkan's und in den angrenzenden Gebieten. I. Kurze 

 Uebersicht, &c. [Geological Researches in the \V. Balkans, &c.] 

 Sitz, l\ Ak. Wlss. Wien, math.-nat. CI. Abth. I. Bd. Ixxii. Heft 4, 

 pp. 488-498. 

 An account of routes, with geological results. Among the crystal- 

 line rocks met with were granite, gabbro, diorite-porphyry, &c. Of 

 sedimentary rocks are chiefly mentioned : — Coal Measures, Dyas, Trias, 

 Jurassic (including Tithonian, ct;c.), Cretaceous sandstones, Miocene, 

 lignites, &c., &c. The district examined was about 180 German 

 square miles. E. B. T, 



[Geology of the Balkans.] N. Jahrh. Heft i. pp. 44, 45,_ 



[See the above.] 



Ein Beitrag zur Kenntniss des Scmmeringgcbirges. [Geology 



of the Semmering Mountains.] Verh. Tc.-h. geoh lieiclis. p. 334. 

 Eine geologische Eeise in den westlichen Balkan und in dio 



benachbarten Gebiete. Pp. 128, map. 8vo. Vienna. 



Tournouer, — . Note sur quelques fossiles d'eau douce recueilh's 

 dans le forage d'un puits au fort de Vancia, pres de Lyon. [Fresh- 

 water Fossils from a Well at the Fort of Yancia, near Lyons.] 

 Bull. Soc. Geol. France^ 3 ser. t. iii. pp. 741-748, part of pi. xxviii. 

 The list includes the three new forms Planorhis Gimudus, Paludina 

 ( Vivipara) Dresseli, and Vcdvata Vmiciana, which are described and 

 figured. These fossils come from greyish marly bods intercalated in 

 the Glacial or ancient alluvia which spread over the Bressan plateau 

 above the Pliocene sands of Trevoux. G. A. L, 



Tribolet, Dr. Maurice de. Sur les terrains jurassiques supe'rieurs de 

 la Haute-Marne compares ii ceux du Jura suisse et francjais. [The 

 U. Jurassic of Haute-Marne compared with that of the French 

 and Swiss Jura.] Ball. Soc. Geol. France, 3 ser. t. iv. pp. 259-285. 



Compares the horizons of the series as exhibited in England, the 

 Boulonnais, Bray, Mouse, Haute-Marne, Yonne, Cote-d'or, Haute- 

 Saone, and Jura. Gives the following classification : — Purbeckian 

 (with Portlandian dolomites), Cyrena nujosa zone ; Portlandiau, Am- 

 monites c/igas and Cyprina Brongniarti zone ; Yirgulian, Amm. Cale- 

 tanus zone ; Ptcrocerian, Amm. orihoceras zone ; Upper Soquanian, 

 Astarte limestones and oolite of La Mothe ; Lower Sequanian, compact 

 corallian ; Upper liauracian, Doulaincourt oolite or grey marls ; 

 Lower liauracian, rubbly coralline limestones or grey marls ; Phola- 

 domyan, Belemnites Royeri zone ; zone of hydraulic limestones, Amm. 

 Babeanus zone ; Spongitian, Amm. Marfelli zone. G. A. L. 



L 



