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Transactions of the Society. 
Romer from the Chalk of North Germany, and by Reuss from the 
Upper Chalk and Wealden beds of Westphalia, and also from 
the Hils-thon near Brunswick and Speeton-clay between Grunen- 
plan and Escherhausen. It is found in the Gault in zone i., 
specimen b, very rare ; zone ii., specimen a, frequent ; zone ii., 
specimen b, frequent ; zone ii., specimen c, rare ; zone iii., very com- 
mon ; zone iv., very common ; zone vi., very rare ; zone vii., very rare ; 
zone x., rare ; zone xi., 6 ft. from the top, very rare. 
Haplophragmium agglutinans d’Orbigny sp., plate V. fig. 14. 
Spirolina agglutinans d’Orbigny, 1846, For. Foss. Vien., p. 137, 
plate vii. figs. 10-12. 
The range of this species in time is very extensive, making its first 
appearance in the Lower Carboniferous rocks of Yorkshire, occurring 
again in the Lias, Gault, Lower Tertiaries, Miocene, and also in recent 
deposits. In the Gault it is found in zone ii., specimen c, very rare ; 
zone iii., very rare ; zone xi., 45 ft. from the top, very rare ; 35 ft., 
very rare ; 12 ft., very rare. 
Haplophragmium nanum Brady, plate Y. figs. 15 a, b, c. 
Haplophragmium nanum Brady, 1881, Quart. Journ. Micr. Sci., 
vol. xxi. n.s., p. 50. H. nanum Brady, 1881, Denkschr. d. Ak. 
Wiss. Wien, vol. xliii. p. 99, plate ii. fig. 1 a-c. 
An inequilateral form found in deep-sea deposits. The Gault 
specimens are almost identical with the figures of the recent ones. 
Zone i., specimen b, very rare ; zone ii., specimen c, very rare ; zone 
iii., rare ; zone xi., 6 ft. from the top, very rare. 
Haplophragmium globigeriniforme Parker and Jones sp., plate Y. 
fig. 16. 
Lituola nautiloidea var. globigeriniformis Parker and Jones, 1865, 
Phil. Trans., vol. civ. p. 407, plate xv. figs. 46, 47. Haplophragmium 
globigeriniforme Parker and Jones sp., Brady, 1884, Chall. Rep., 
vol. ix. p. 312, plate xxxv. figs. 10, 11. 
This is recorded by Dr. Brady as an essentially deep-water 
form. The only record of its occurrence as fossil is by Terrigi from 
the Upper Pliocene Sands of Rome. It is found in the Gault in 
zone iii., rare ; zone v., very rare ; zone vii., very rare ; zone ix., very 
rare ; zone xi., 35 ft. from the top, very rare ; 12 ft., very rare. 
Placopsilina d’Orbigny [1850). 
Placopsilina Cenomana d’Orbigny, plate VI. fig. 4. 
Placopsilina Cenomana d’Orbigny, 1850, Prodr. Paleont., vol. ii. 
p. 185, No. 758. P. Cenomana Reuss, 1854, Denkschr. d. k. Ak. 
Wiss. Wien, vol. vii. p. 71, plate xxviii. figs. 4, 5. 
