Vol. 50.] ME. F. CHAPMAN ON THE BAEGATE BEDS OF SEEEEr. 703 



p. 40, pi. iv. figs. 7, 8 ; Chapman, Journ. Roy. Micr. Soc. 1892, 

 p. 754, pi. xii. fig. 3. 



The specimens from the Bargate Beds closely resemble the Gault 

 specimens. 



One specimen from siliceous residue of Bargate limestone, Little- 

 ton ; two from Bargate Pebble-beds, Littleton ; one from Pebble- 

 beds, Halfpenny Lane ; and one from Bargate Beds, Holloway Hill. 



39. Belihiha. Peesli, Reuss. 



B. Presli, Reuss, ' Verstein. bohm. ;Kreid.' pt. i. (1845) p. 38, 

 pi. xiii. fig. 72. 



This species is the largest of the BuKmince from the Bargate 

 series, the specimens measuring J^ inch (0*63 mm.) in length. 

 This form is also found in the Gault of Folkestone (where it attains 

 the same size) and in other Cretaceous strata. 



Two specimens from Bargate Pebble-beds, Littleton. 



40. Belimina obtesa, d'Orbigny. 



B. obtusa, d'Orbigny, Mem. Soc. geol. Prance, vol. iv. (1840) 

 p. 39, pi. iv. figs. 5, 6. 



This species, which is already known from the Gault and Chalk, 

 was found in the Pebble-beds, Littleton (three specimens) ; in the 

 siliceous residue of the Bargate Stone, Halfpenny Lane, Chilworth 

 (one) ; and in the Bargate Beds, Holloway Hill (one). 



41. Beximina Meechisontana, d'Orbigny. 



B. Murchisoniana, d'Orbigny, Mem. Soc. geol. France, vol. iv. 

 (1840) p. 41, pi. iv. figs. 15, 16. 



Two specimens from the Pebble-beds, Littleton. 



42. Beeimtna beevis, d'Orbigny. 



B. brevis, d'Orbigny, Mem. Soc. geol. Prance, vol. [iv. (1840) 

 p. 41, pi. iv. figs. 13, 14. 



This species was previously known as peculiar to Cretaceous 

 strata, occurring in the Gault and Chalk. 



Nine specimens from Bargate Pebble-beds, Littleton ; one from 

 Pebble-beds, Halfpenny Lane ; one from Bargate Beds, Holloway 

 Hill ; and two from beds below Folkestone series, Horsham Road, 

 Dorking. 



Viegelina, d'Orbigny. 



43. VlEGCTLINA SEBSQEAMOSA, Egger. 



V. subsquamosa, Egger, Neues Jahrb. 1857, p. 295, pi. xii. 

 figs. 19-21. 



Previously recorded from Miocene and later deposits, this form 

 occurs in the Bargate Pebble-beds, Littleton (three specimens) ; and 

 in the Bargate Beds, Holloway Hill (one). 



