(332 Transactions of the Society. 



184. Truncatulina culter Parker and Jones sp. 



Planoriulina culter Parker and Jones, 1865, Phil. Trans., vol. civ. p. 421, pi. 



xix. fig. 1 a, b. 

 Anomalina bengalensis Schwager, 1866, Novara. Exped. geol. Theil, vol. ii. 



p. 259, pi. vii. fig. 111. 

 Truncatulina culter (Parker and Jones) Brady, 1884, Foram. ' Challenger,' 



p. 668, pi. xcvi. fig. 3 a, b, c. 



All fossils, and apparently from a clay. The specimens are 

 small compared with recent types. This species has been recorded 

 principally from depths of 1000 to 2000 fathoms, but, according 

 to Brady, Schwager states that his specimens of Anomalina bengal- 

 ensis were from the shores of the Nicobar Islands, which would 

 point to the fact of their living in comparatively shallow water. 



Anomalina d'Orbigny. 

 185. Anomalina ammonoides Keuss sp. 



Bosalina ammonoides Keuss, 1845, Verstein. Buhm. Kreid., pt. i. p. 36, pi. xiii. 



fig. 66, pi. viii. fig. 53. 

 Ditto. Id., 1850, Haidinger's Naturw. Abhandl., vol. iv. p. 36, pi. iv. fig. 2. 

 Planorbuliua ammonoides (Keuss) Parker and Jones, 1865, Phil. Trans., 



vol. civ. p. 379. 

 Anomalina ammonoides (Reuss) Brady, 1884, Foram. ' Challenger,' p. 672, 



pi. xciv. figs. % 3. 



Very fine specimens, which have been derived from several 

 distinct sources, including probably Cretaceous beds and Eocene 

 sands and clays. 



186. Anomalina coronata Parker and Jones. 



Anomalina coronata Parker and Jones, 1857, Ann. and Mag. Nat. Hist., ser. 2, 

 vol. xix. p. 294, pi x. figs. 15, 1 6. 



Ditto. (Parker and Jones) Brady, 1864, Trans. Linn. Soc. Lond., vol. xxiv. 

 p. 469, pi. xlviii. fig. 13 a, b. 



Ditto. (Parker and Jones) Brady, 1884, Foram. ' Challenger,' p. 675, pi. 

 xcvii. figs. 1, 2 



Planorbulina coronata (Parker and Jones) Goiis, 1894, Arctic and Scan- 

 dinavian Foraminifera, p. 90, pi. xv. figs. 781-3. 



A single small, and imperfect example. The shell is in good 

 preservation, and looks like a recent specimen. This is a very 

 common species in some parts of the North Sea and in the Faroe 

 Channel, but it rarely occurs under the 100 fathom line, and we 

 know no previous record of its occurrence in a shore-sand, if our 

 specimen is to be accepted as recent. The species has been re- 

 corded from several Tertiary formations in various parts of the 

 world. 



