l888.] NEW-YORK MICROSCOPICAL SOCIETY. 65 



Cornet, M. F. L. Quelques mots sur certaines assises cr6ta- 

 cees du bassin de Mens. Ann. de la Soc. Geol. de Beige., 

 vol. ix, pp. 184 266, 1881-82. 



Dewalque, G. Sur I'extension verticale de quelques fossiles 

 d^vonieus reputes caracteristiques. (Vertical range of some 

 reputed Devonian fossils.) Ann. Soc. Gdol. Beige., vol. i, 

 Bull. pp. 62, 63, 1874. 

 Recepiaculites Neptuni, Defr. 



DiTTMAR, . Die Contortazone und ihre organischen Ein 



schliisse. Miinchen, 3 pis., 1864. 

 Not seen. 



Drvgalski, E. von, Murray, John, et Renard, A. Notice 

 sur la classification le mode de formation et la distribution 

 g^ographique des sediments de mer profonde. Bull. Mus. 

 Roy. Hist. Nat. Belg., 1884, vol. iii, pp. 25-62. Neues Jahr- 

 buch fiir Min., vol. iii, pp. 228-232, 1886. 

 Review. 



DuNiKOwsKi, E. Die Spongien, Radiolarien und Foraminiferen 

 der unterliassischen schichten vom Schafberg bei Salzburg, 

 Denkschr. d. Mathemat. Nat. Cl. d. K. Akad. d. Wiss., vol. 

 xlv, pp. 34, 6 plates, 1882. 



D'Urban, W. S. M. The Zoology of Barents Sea. Ann. and 

 Mag., Nat. Hist. ser. 5, vol. vi, pp. 253-277, 1880. 



Ehrenberg, Berichte iiber die zur Bekanntmach. geeignet. 

 Verhandl. der konigl. preuss. Akademie. der Wissenschaften, 

 1842. 



FoLiN, M. de. On a new locality containing the nummulitic 

 formation, 1886. 

 Not seen. 



FucHs, Th. Zur Bildung der Terra Rossa. [On Terra Rossa.] 

 Verh. K. K. geol. Reichs.\>\). 194-196. 1875. 



Supplementary to Prof. Neumayr's paper ; notices its large develop- 

 ment in Greece, where it is derived from freshwater limestones. Hence 

 it is always due to Globigerina remains, and the climate of the country 

 has more to do with its formation than the nature of the limestone. (E. 

 B. T., Geol. Rec. p. 65.) 



FucHS, Th. Ueber den sogenannten " Badner Tegel" auf 

 Malta. (So-called Baden Clay of Malta.) Sitz. K. Ak. 

 Wiss. Wien. Math. Cl. Abth. i, vol. Ixxiii, pp. 67-84, i 

 plate, 1876. ^ 



