14 FORAMINIFERA OF THE CRAG. 
7. QuinqueLocuLiIna Broneniartiu, D’Orbigny, Plate IIT, figs. 41,42; Plate LV, fig. 2. 
PoLLONTES VESICULARIS, Montfort, 1808. Conch. Syst., vol. i, p. 246. 
ADELOSINA STRIATA (young Q. Brongniartii), D'Orb., 1826. Modéle No. 18 (“young”), 
No. 97 (“adult”) ; Ann. Se. Nat., vol. vii, p. 304, No. 2. 
Tritocuttina Bronentarti, D’Ord., 1826. Ann. Se. Nat., vol. vii, p. 300, No. 23; 
Soldani, Testac. Zooph., vol. iii, p. 229, pl. 154, figs. 4, 
ce, dd, ee, ff, 9g. 
— —_ Id., 1839. Foram. Cuba, p. 176, pl. 10, figs. 6—8. 
QuINQuELocuLINA Guancna, Id., 1839. Foram. Canaries, p. 143, pl. 3, figs. 34—36. 
— Partscuil, Id. 1846. For. Fos. Vien., p. 293, pl. 19, figs. 4—5. 
~~ Bovtana, Jd., 1846. Ibid., p- 293, pl. 19, figs. 7—9. 
—_ Dutemp.et, Id., 1846. Tbid., p- 294, pl. 19, figs. 10—12. 
— NussporrigEnsts, Id., 1846. Ibid., p. 295, pl. 19, figs. 13—15. 
TRILOCULINA DIcHoTOMA, Feuss, 1850. Denks. Akad. Wien., vol. i, p. 383, pl. 49, fig. 12. 
QUINQUELOCULINA stTrIonaTA, Id., 1850. Ibid., vol. i, p. 385, pl. 50, fig. 10. 
ADELOSINA CRETACEA, Id., 1851. Hiding. Naturw. Abhandl., vol. iv, p. 46, pl. 5, fig. 15. 
QuINQUELOcULINA BroneniartiI, Parker and Jones, 1860. Ann. Nat. Hist., ser. 3, vol. vi, 
p. 344. 
Characters.—Shell having a surface-ornamentation of delicate, parallel, longitudinal 
strie. Segments arranged as in the other Quinqueloculine Aole. Colour white to 
yellowish. Length, jth to th inch. 
The finely striated A/cdole included under this sub-varietal term may be found in 
every condition, from that approaching the common smooth unornamented shell, in which 
but a few short lines appear at the base of the penultimate chamber, as in Plate IV, fig. 2 
(a condition represented to some extent in D’Orbigny’s ‘ Modéles’ Nos. 18 and 97), to 
that in which the whole of the surface is covered by delicate hair-like markings. 
Mr. Wood’s collection contains but a few specimens from Sutton, and we have not 
noticed the variety in the other Crag deposits. We have never seen examples having 
precisely the characters of Q. Brongniartiz from our own coast, though we have a fair 
approach to it im some specimens ef Q. dzcornis, in which, though the marking is analogous, 
the shape of the shell is sufficiently distinct to justify separation. We find it occasionally 
in the Mediterranean, and in most shallow-water-dredgings from tropical seas. In the 
Tertiary clays of the North of Italy, in the Miocene of the Vienna Basin, and in the 
Eocene of the Paris Basin, it is also sparingly found. 
