Lower Kimerid- 

 gian. 



EUROPE. 49 



Brussels, and which has only been found in Belgium at Viesalm and 

 Angres. G. A. L. 



Bayax, — , Observations sur la coupe des terrains du Bas-Bugey 



donnee par M. Falsan. [On M. Falsan's section of the rocks of 



the Bas-Bugey.] Compt. Rend. 2 sess. Assoc. Fran9. pp. 373-78. 



The conclusions arrived at by a study of M. Falsan's section are 



discussed. In comparing the Upper Jurassic beds, of Bugey with 



Quenstedt's divisions in Wiirtemberg, the equivalence is as follows : — 



Weisser Jura e Bed with coralline f acies 



of Valfin, rEchaillon, &c. 



Weisser Jura d \ Beds of Arinaille. 



r Uppsr j Am.-tenuilobatus 



^jrr . -r \ ZOnO. 



weisser dura y s Middle aiid Am.-bimammatm | Q^ralhan 



y Lower. zone. j 



Weisser Jura /3. G. A. L. 



Berendt, G. Marine Diluvialfauna in Ostpreussen, und zweiter 



Nachtrag zur Diluvialfauna Westpreussensn. [Fauna of the Drift 



in Prussia.] Zeit. deutsch. geol. Gesell. Bd. xxvi. 517-521 



(plate). 



In making the Thurn-and-Insterburg Eailway, the first fossils from 



the drift in East Prussia have been found (6 marine and 1 freshwater). 



Other species are cited from Western Prussia. F. W. R. 



. Anstehender Jura in Yorpommern. Zeit. deutsch. geol. 



Gesell. Bd. xxvi. pp. 823-826. 

 Note on the occurrence of a blue clay of Jurassic age in place near 

 Grimmen in Western Pomerania. It contains Ammonites of the group 

 Falciferi, to which the name of Harpoceras has been given ; and it is 

 placed at the junction of the Lias and Brown Jura, being thus on the 

 lowest geological horizon yet' observed in Pomerania and the neigh- 

 ])ouring countries. Boulders containing similar fossils are found near 

 Hamburg. F. W. R. 



. Bergstrand, C. E. Om den geologiska bildningen af (Eland och dcss 

 forhSllande till dervarande odlade jordarter. [Geological struc- 

 ture of OCland and its relation to the soil.] Geol. foren. Stock- 

 holm Forhandl. bdt. i. pp. 154-102, 1 fig. in text: 

 The rocks consist (in descending order) of: — 1. Silurian light-grey" 

 and reddish limestones (divided into upper Ortlioceratite-'hQdiS and lower 

 (7ercf<o/)?/r/e -limestone) ; 2. Alum-shales, with bands of conerctionary 

 bituminous limestone or stinkstone, and pyritiferous in the lower layers ; 

 3. Clay-slate ; and 4. Grits. General dip E., and not great. G, A. L. 

 Billy, — de. Constitution geologique de la chaine des Aiguilles- 

 Rouges (valleo de Chamounix). [Geology of the Aiguilles- 

 Rouges chain.] Bull. Soc. Geol. France, 3 ser. t. ii. pp. 40-42. 

 An acknowledgment that the foot of the chain of the Aiguilles- 

 Rouges is in part formed of sedimentary metamorphic rbcks, a retracj^ 

 tation of a criticism of M. V. Payot's work x)n the C oology of the neigh- 

 bourliood of Mont-Blanc. . ' ' G. A. L, 



1874. ' .' ■ E 



