210 CRETACEOUS PALEONTOLOGY. 



1905. Nodosaria consobrina var. emaciata Bagg, Bull. U. S. G. 

 S., No. 268, p. 30, pi. 5, fig. 4. 



Description. "Test smooth, greatly elongated, tapering; seg"- 

 ments numerous, short, elongate oval ; similar to Nodosaria con- 

 sobrina, but more elongated and slender; septa somewhat de- 

 pressed, transverse, primordial end rounded; aperture mam- 

 millate, somewhat prolonged into a tube. 



"Length, 2 mm." (Bagg.) 



Formation and locality. Marshalltown clay-marl, Marshall- 

 town (Bagg) ; Vincentown limesand, Vincentown (Bagg). 



Geographic distribution. New Jersey; Eocene of Maryland, 

 Miocene of California. 



Nodosaria farcimen (Soldani). 

 Plate I., Fig. 50. 



1791. Orthoceras farcimen Soldani, Testaceographia, vol. i, pt. 



2, p. 98, pi. cv, fig. o. 

 1861. Dentalina farcimen Reuss, Bull. Acad. Roy. Belgique, 



ser. 2, vol. 15, p. 146, pi. i, fig. 18. 

 1884. Nodosaria farcimen Brady, Challenger Report, vol. 9, 



pp. 498, 499, pi. Ixii, figs, 17, 1 8,' and woodcuts, p. 499. 

 1898. Nodosaria farcimen Bagg, Bull. U. S. Geol. Survey No. 



88, pp. 38, 39. 

 1898. Nodosaria farcimen Bagg, Bull. American Paleont.. vol. 



2, No. 10, pp. 25, 26, pi. i, fig. 2. 

 1900. Nodosaria farcimen Chapman, Pfoc. California Acad. 



Sci., ser. 3, vol. i, No. 8, p. 248, pi. xxix, fig. 13. 

 1905. Nodosaria farcimen Bagg, Bull. U. S. G. S., No. 268, p. 



30, pi. 5, fig. 5. 



Description. "Test arcuate, tapering, with from six to ten 

 inflated segments, separated by deep, straight, transverse sutures. 

 The latter quality separates this species from Nodosaria com- 

 munis, in which the sutures are oblique. There is also an irreg- 

 ularity in the increase of the size of the chambers noticeable in 

 most specimens. The ultimate chamber is prolonged into a round 

 tube which bears the oral opening. 



