180 FORAMINIFERA OF THE CRAG. 



Lagena apiculata, Terquem, 1870. Mem. Acad. Imp. Metz, vol. li,p. 350, pi. xxv, 



figs. 22, 23. 



— — Hantken [1876], 1881. Mitth. Jahrb. TJngar. Geol. Anst., 



vol. iv, p. 22, pi. xii, fig. 7 (1876 

 in Hungary). 



— CAnDATA, Bradi/ and Rolertson, 187G. Eep. Brit. Assoc, for 1875, p. 190. 



— MAXIMA, DunikowsM, 1879. Kosmoa (Lemberg), vol. iv, p. 105, fig. 3. 



— APICULATA, Butschli, 1880. Bronn'e Klassen, &c., p. 197, pi. vii, fig. 3. 



— — Brady, 1884. Eeport ' Challenger,' pp. 444, 453, pi. ivi, 



figs. 4, 15—18. 



— — Sherborn and Chapman, 1886. Journ. Eoy. Micr. Soc.,8er. 2, 



vol. vi, p. 744, pi. xiv, fig. 14. 



— — Terquem, 1886. Mem. Soc. Geol. France, ser. 3, vol. iv, p. 6, 



pi. i, fig. 5. 



— — Raeusler, 1887. Neues Jaiirb. f. Min., &c., for 1887, part 1, 



p. 182, pi. iv, figs. 19—30; and pi. v, 

 figs. 36, 37. 



— — Terrigi, 1889. Mem. E. Accad. Lincei, ser. 4, vol. vi,p. Ill, 



pi. V, fig. 11. 



— — Mariani, 1889. Boll. Soc. Geol. Ital., vol. vii, p. 285, pi. x, 



fig. 5. 



— — B., S., and B., 1890. Journ. E. Micr. Soc, p. 555, pi. is, 



figs. 6, 7, 9—11. 



— — var. ODONTOSTOMA, de Amicis, 1893. Ibid., vol. xii, fasc. 3, 



p. 352, pi. iii, figs. 9 a, b. 



— — Egger, 1893. Abhandl. Bayer. Ak. Wiss., vol. xviii, part 2, 



pp. 321, 324, pi. X, fig. 8. 



— — Chapman, 1893. Journ. E. Microsc. Soc. for 1893, p. 581, 



pi. viii, figs. 2 a, b, and figs. 3 a, b. 

 [Elongate and globose forms.] 



— — var. EMACIATA, Idem, 1893. Ibid., figs. 4 and 7. 



— — Idem, 1894. Quart. Journ. Geol. Soc, vol. 1, p. 705. 



— — Ooiis, 1894. K. Sv. Vet.-Akad. Handl., vol. xxv. No. 9, p. 80, 



pi. xiii, fig. 747. 



Characters. — Entosolenian and otherwise, also like L. ijlohosa, but pointed, 

 instead of round, at the base. 



Occurrence. — Lagena apiculata is a cosmopolitan form, found in all latitudes, 

 and at all depths from the httoral zone to 2750 fathoms. As a fossil it is also 

 very widely distributed. It has been recorded from the Lias ; from the 

 Neocomian Beds of Surrey ; from the Gault of Folkestone ; from the Eocene, 

 London Clay ; from the Oligocene of Elsass ; from the Miocene of Messina ; and 

 from the Pliocene of Italy and St. Erth. In the Coralline Crag it has been met 

 with at Sutton only. 



