330 
Transactions of the Societi/. 
This is well known from the Chalk, also recorded from the Red 
Chalk of Speeton (Burrows, Sherhorn, and Bailey), and from the 
Planermergel of Luschitz, Bohemia (Reuss). Zone i., specimen a, 
very rare; zone v., common; zone viii., rare; zone x., very rare; 
zone xi., 55 ft. from the top, rare ; 50 ft., frequent ; 45 ft., common ; 
40 ft., frequent ; 35 ft., frequent; 30 ft., frequent. 
Verneuilina variahilis Brady, plate VI. figs. 25 a and h. 
Verneuilina variahilis Brady, 1884, Chall. Rep., vol. ix. p. 385, 
pi. xlvii. figs. 21-24. 
In the Gault series of Foraminifera there are many specimens 
which agree almost minutely with Dr. Brady’s species, and which 
appear to be depauperated and coarsely constructed (as regards the 
test) varieties of the typical V. triqnetra. Hitherto this form has 
not been found as a fossil. Zone x., very rare ; zone xi., 50 ft. from 
the top, very rare; 35 ft., frequent; 30 ft., very rare. 
