EUROPE. 53 



An account of the stratigraphical relations of the Devonian deposits 

 of the vicinity of Gratz. The beds are divided into groups. 



Clae, Dr. C. Neue Beobachtungen aus der Gegend von Gleichen- 



berg. [New observations in the neighbourhood of Gleichenberg.] 



Yerh. k.-k. geol. Eeichs. p. 91. 

 Clemens, Prof. Jos. Beitriige zur Kenntniss des alteren Tertiar in 



Oberen Gran-Thale. [Contributions to a knowledge of the older 



Tertiaries of the Upper Gran valley.] Verb. k.-k. geol. lleichs. 



pp. 332-334. 

 Cleve, p. T. Fynd af ett siluriskt lager i Bohusliins skargSrd. 



[Discoveiy of Silurian beds in the Bohuslans rock-district.] Geol. 



fbren. Stockholm Forhandl. bd. i. pp. 28, 29. 

 An announcement of the discovery. 

 CoGELS, P. Note sur un gisement de Terebratules aux environs 



d'Anvers. [Terehratul a -hed near Antwerp.] Proc.-Yerb. Soc. 



Mai. Belg. t. iii. pp. xviii-xxi. 

 Proves that the green sand with Terebratula grandis of Dejardin is 

 really in the Diestian series. Details of section given, and notes of 

 other fossils fouud. G. A. L. 



■ Seconde note sur le gisement de la Terebratula grandis avec 



quelques observations a ce sujet. [Second note on the Terebratula- 



grandis bed.] Proc.-Verb. Soc. Mai. Belg. t. iii. pp. xxxviii-xlv. 



Concludes that Terehratulce have not been found in place above the 



green Diestian sands. The relations of these sands to the crag gns and 



other associated beds are considered, and Dejardin's classification is 



criticsied. G. A. L. 



-. Nouvelle note sur le gisement de la Terebratula grandis. 



[New note on the T.-grandis bed.] Proc.-Yerb. Soc. Mai. Belg. 



t. iii. pp. Ixix-lxxxvi. 

 Rejoinder to M. Mourlon's criticisms (see p. 84). The author's final 

 views are as follow : — That the Terebratula green sand and a certain 

 coral-bed are both in the series known as the grey sands ; that the 

 zone in which the Terebratulce are found entire and in place belong 

 to the Diestian system ; that above this zone is a line of rolled debris 

 with signs of denudation ; that the corals are later than the rolled 

 debris ; that currents afterwards caused a mixture of the fossils ; and 

 that this Terebratula has only hitherto been found at one horizon, 

 which is Diestian and not Scaldisian. G. A. L. 



Note sur un gisement d^Ostrea cochlear aux environs d'Anvers. 



[Bed with 0. cochlear near Antwerp.] Proc.-Yerb. Soc. Mai. Belg. 

 t. iii. pp. o-ciii. 

 Description of a measured section through Tertiary beds near the 

 Porte Leopold. 



CoQUAND, If. De I'ngo et de la position des marbres blancs statuaires 

 des Pyrenees ct des Alpes apuennes en Toscane. [Age and posi- 



