Becent Foraminifera off the East Coast of Australia. 13 



Beophax guttifera Brady. (PL II, fig. 9.) 



Beophax guttifera Brady, 1881, Quart. Journ. Micr. Sci., vol. xxi, N.S., 



p. 49. 

 B. guttifera Brady, 1884, Chall. Kept., p. 295, pi. xxxi, figs. 10-15. 



Not one of the tests consists of more than four chambers, and 

 they do not show the separation of the chambers to anything 

 approaching the extent figured in the " Challenger " Eeport, but 

 they agree with some of the specimens which Mr. Earland has 

 kindly sent me from the Faroe Channel. 



Beophax distans Brady. 



Beophax distans Brady, 1881, Quart. Journ. Micr. Sci., vol. xxi, N.S., p. 50. 

 B. distans Brady, 1884, Chall. Kept., p. 296, pi. xxxi, figs. 18-22. 



Two fragments. They are built of clear, wdiite sand-grains. 

 The choice of this particular kind of sand-grain, for the formation 

 of tests, is not at all uncommon at this locality. 



Beophax spiculifera Brady. 



Beophax spiculifera Brady, 1879, Quart. Journ. Micr. Sci., vol. xix, N.S., 



p. 54, pi. iv, figs. 10,' 11. 

 B. spiculifera Brady, 1884, Chall. Kept., p. 295, pi. xxxi, figs. 16, 17. 



A few fragments, each consisting of a single chamber. 



Beophax difflugiformis Brady. 



Beophax difflugiformis Brady, 1879, Quart. Journ. Micr. Sci., vol. xix, N.S., 



p. 51, pi. iv, fig. 3, a, h. 

 B. difflugiformis Brady, 1884, Chall. Kept., p. 289, pi. xxx, figs. 1-5. 



A few specimens built of coarse sand-grains, similar to the 

 ■" Challenger " fig. 5. One test is nearly globular, and might be 

 taken for Saccammina sphxrica, but being an odd specimen, found 

 in company with the above, and differing from them in no other 

 respect, it is probably only a more globular form than is usual in 

 this species. When damped, the tests easily disintegrate. They 

 are shaded light brown. 



o 



Haplophragmiuin Reuss. > 



Haplophragmium calcareum Brady. 



Haplophragmium calcareum Brady, 1884, Chall. Rept., p. 302, pi. xxxiii, 

 figs. 5-12. 



Very large specimens occur, built of coarse sand-grains. They are 

 .narrow in comparison with their length, the segments unusually 

 high and depressed at their sutures. The outline is lobulated. 

 They agree with the " Challenger " fig. 7. 



