INVERTEBRATA. 325 



St. Aubin, Hauterive, and Ste. Croix ; H. Latreillei and Prosopon Cam- 

 dicJiei, same formation, Ste. Croix. 



A catalogue of all the Cretaceous Macrurous, and Anomurous De- 

 capoda concludes the paper. G. A. L. 



Tribolet, Maurice de. Notes . . . Paleontologiques sur le Jura 

 neuchatelois, see p. 104. 



Tute, S. J. Organisms in Carboniferous Flint or Chert. Science 



Gossip, No. 116, p. 188, woodcut; see also p. 217. 

 The specimens are from the Yoredale series, and are thought to be 

 Foraminiferous. 



Vanden Broeck, Ernest. Quelques considerations sur la decouverte 

 dans le calcaire carbonifere de Namur d'un fossile microscopique^ 

 nouveau appartenant au genre Nummulite. [Discovery of a Num- 

 mulite in the Carboniferous Limestone* of Namur.] Ann. Soc. 

 geol. Belg. t. i. Mem. pp. 16-27. 

 Chiefly an account of Mr. H. B. Brady's researches respecting Carbo- 

 niferous Foraminifera, with an abstract of his paper on Nummulina 

 pristina (see p. 288). G. A. L, 



YiLANOVA T Peira, Juan. Estructura de las rocas Serpentinosas y 

 el Eozoon Canadense. Soc. Espan. Hist. Nat. vol. iii. parts 2, 3. 



States reasons for considering the Eozoon Canadense no organism 

 whatever, and asserts that what has been accepted as the remains of 

 a Foraminiferous animal is merely the peculiar mineralogical structure 

 of Serpentine and other allied rocks. J. M'P. 



Vincent, ^— . Deux Gasteropodes nouveaux pour la faune bruxel- 



lienne. [Two Gasteropoda new to the Bruxellian.J Ann. Soc. 



Mai. Belg. t. viii. Bull. p. x. 



The shells are Phurotoma clavicularis^ var. B., and Voluta athleta. 



Both come from the Rostellaria-ampla and Venus-suherycindides zone in 



the BruxeUian at Uccle near Brussels. G. A. L. 



"Ward, Dr. Oojer. On some Forms of Cuttle-fishes or Cephalopoda, 

 Recent and Fossil. Papers Eastbourne Nat. Hist. Soc. 1873-4, 

 pp. 21, 22. 



Thinks that the shells of some of the Ammonitidse may have been 

 internal. 



Waters, A. W. Remarks on Fossils from Oberburg, Styria. Quart. 

 Journ. Geol. Soc. vol. xxx. pp. 339-341. 



By means of fossils from the Eocene beds of Oberburg and Neustift. 

 several species are added to the list published by Stur (Geologie der 

 Steiermark). H. A. N. 



Wetherell, John W. On some Fossils from the Margate Chalk. 



Proc. Geol. Assoc, vol. iii. no. 5, pp. 192-197. 

 The fossils were got from the bottom part of the cliff, of which a 

 general section is given (woodcut). The list is followed by some ob- 



