I 



TYPE SI'E(!IMENS OF INVERTEBRATE FOSSILS. LM)7 



262. Fasciolaria ? ( Cryptorhytis ) flexicostata (Meek and Hay- 

 deu). Holotype and paratypes. 



Fort Pierre (Cret.)- Yellowstone River, near Miles City, 

 Montana. 



Meek, Rept. U. S. Geol. Surv. Terr., IX, 1S76, p. 367, pi. 19, 

 fig. 2. 



See Fusus flexnocostatus. 



287. Fasciolaria ( Piestochilus ? ) galpiniana ( Meek and Hayden) . 



Holotype and paratype. 

 Fox Hills (Cret.). Moreau River, South Dakota. 



Meek, Rept. U. S. Geol. Surv. Terr., IX, 1876, ]). 362, pi. 32, figs. 

 2a, 2b. 



See Fusus galpinianus. 



259. Fasciolaria (Piestochilus) scarboroughi (Meek and Hay- 

 den). Holotype and paratypes. 

 Fox Hills (Cret.). Butte au Gres, Mis.souri River. 



Meek, Rept. U. S. Geol. Surv. Terr., IX, 1S76, p. 359, pi. 32, 

 figs. 4, ^a-d. 



See Fusus (Pleurotoma?) scarboroughi. 



112421. Fasciolaria (sparrowi var?) acuta (Emmons). Plesiotype. 

 Miocene. Natural Well, Duplin County, North Carolina. 



Dall, Trans. Wagner Free lust. Sci. Phila., Ill, Ft. 11, 1892, p. 

 229, pi. 13, fig. 2. 



1 1 1630. Fasciolaria (Lyrosoma) sulcosa (Conrad). Plesiotype. 



Miocene. Jericho, New Jer-se}'. 



Whitfield, Mon. XXIV, U. S. Geol. Surv., 1894, p. 100, pi. 17, 

 figs. 9, 10. 



115482. Fasciolaria textilis Guppy. Holotype. 



Oligocene. Jamaica, British West Indies. 



Guppy, Geol. Mag., London, Dec. II, I, 1874, p. 410, pi. 16, fig. 5. 



112390. Fasciolaria tulipa Linnoeus. Plesiotype. 



135104. Pliocene. Shell Creek, De Soto County, Florida. 



Dall, Trans. Wagner Free Inst. Sci. Phila., Ill, Pt. I, 1890, p. loi, 

 pi. 7, fig. II. 



22922. Fasciolaria? (Cryptorhytis ) utahensis (Meek). Plesiotypes. 



Colorado (Cret.). Poi.son Canyon, Huerfano Park, Colo- 

 rado. 



Stanton, Bull. No. 106, U. S. Geol. Surv., 1S93, p. 153, pi. 32, 

 See Fusus ? utahensis. 



22923. Fasciolaria ? walcotti vStanton. Holotype. 



Colorado (Cret.). Upper Kanab Valley, Utah. 



Stanton, Bull. No. 106, U. S. Geol. Surv., 1893, p. 153, pi. 32, fig. 5. 



