jETTEOPE. 101 



Stfr, D. Ueber das Niveau der in der XJmgegend von Rakonitz ab- 

 gebauten Flotze. [Horizon of the worked-out seams in the neigh- 

 bourhood of Rakonitz.] Yerh. k.-k. geol. Eeichs. p. 267. 



• . Neue Aufschliisse im Lunzer Sandstein bei Lunz, und 



ein neuer Fundort von Wenger-Schiefer im Polzberg zwischen 

 Lunzersee und Gaming. [New exposures of the Lunz Sandstone 

 at Lunz, and a new locality for the Wenger beds in Polzberg 

 between the Lunzer See and Gaming.] Yerh. k.-k. geol. Reichs. 

 pp. 271-273. 



. Neue Anfschliisse in Seegengottes bei Rossitz, und Sendung 



von Pflanzenresten aus dem liegendsten Flotze von Herrn H. 

 Rittler. [New exposures in Seegengottes, near Rossitz, and a col- 

 lection of plant-remains from the lowest beds, by Herr H. Rittler.] 

 Yerh. k.-k. geol. Reichs. pp. 396-399. 



Taramelli, T. Stratigrafia deUe serie paleozoica neUe Alpi Carniche. 

 [Stratigraphy of the Palaeozoic Series of the Camic Alps.] Me- 

 morie del R, Istituto Yeneto, vol. xviii. 



Tardy, A. Sur des traces de glaciers quaternaires dans les mon- 

 tagnes de la Madelaine. [Traces of Quaternary glaciers in the 

 Madelaine hills.] Bull. Soc. Geol. France, 3 ser. t. i. pp. 414, 415. 



Announces discoveries of striated bonlders of Carboniferous conglo- 

 merate. 



. Age, Origine, Climat des Glaciers Miocenes. [Age, origin, 



and climate of the Miocene glaciers.] Bull. Soc. Geol. France, 

 3 ser. t. ii. pp. 453-457. 

 Suggests the correlation of the Miocene deposits of the Turin hill 

 (believed by Gastaldi and by himself to be glacial) with the HelicC' 

 liamondi conglomerate of Dijon (believed by M. Martin to be of glacial 

 origin), and with the sands and conglomerates of the forest of Orleans. 

 The climate of the period is compared to that of New Zealand. 



G. A. L. 



Coupe de la Bresse, a propos de la communication de M. do 



Saporta sur les tufs de Meximieux. [Section across the Bresse, 



with reference to M. de Saporta's communication on the tuffs of 



Meximieux.] Compt. Rend. 2 sess. Assoc. Frang. pp. 382, 383. 



Subdivides the divisions E and C of M. Benoit [BuU. Soc. Geol, 



France, t. xv.] into several zones. G. A. L. 



ToMBECK, — . Note sur I'Oxfordien et le Corallien de la Haute Marno. 



[Oxfordian and Corallian of the Haute Marno.] Bull. Soc. Geol. 



France, 3 ser. t. ii. pp. 13-21, 1 fig. in text. 



This paper refers to part of a fine section between Yilliers-sur-Marno 



and Roocourt. The following divisions are determined: — 1. Astarte 



Limestone. 2. Oolite of La Mothe. 3. Upper compact Coralline 



Oolite. 4. Oolite of Soncourt. 5. Lower compact Coralline Oolite. 



6. Upper marl without fossils. 7. Oolite with Dicerates, and lumpy 



