134 PROCEEDINGS OF THE NATIONAL MUSEUM. VOL. XXXIV. 
parisiensis. Lamited to shore sands and off-shore deposits in both 
Atlantic and Pacific oceans. Known from the lower Tertiary de- 
posits of Kurope. Identified in material obtained at Station D. 4017. 
CLAVULINA CYLINDRICA Hantken. 
Clavulina cylindrica HANTKEN, Mittheil. Jahrb. ung. geol. Anstalt, IV, 
ISH, 7 IS Ol, i, ies, S, 
With Haplostiche soldanii, which it resembles, this species is 
found in the coral sands of tropical waters. The two are separable 
by their difference in aperture, Clavulina cylindrica always having a 
valvular opening, while the other is always simple or perforate. 
Abundant in the Clavulina-szaboi strata of Hungary and also from 
the Tertiary of Italy. Rather rare in the South Atlantic, less so in 
the North Atlantic, and variously recorded in shoal waters of the 
South Pacific. Rare in the Globigerina ooze of Station D. 4000. 
Subfamily BU LIMININ A. 
Genus BULIMINA. 
BULIMINA AFFINIS d’Orbigny. 
Bulimina affinis D’ORBIGNY, Foram. Cuba, 1839, p. 109, pl. 11, figs. 25, 26. 
Equivalent probably to Reuss’s Bulimina ovulum, described in 
Cretaceous deposits and present in the North and South Pacific 
oceans of to-day. It is separated from B. ovata, which it closely re- 
sembles, only by its acute apical aboral extremity. Some specimens 
obtained from Stations D. 4017, D. 4025, and D. 4174. 
D’Orbigny obtained his types from the shore sands of Cuba. Dis- 
tribution much more limited, however, than that of the types of B. 
ovata and B. pupoides, which it resembles. 
BULIMINA ACULEATA d’Orbigny. 
Bulimina aculeata D’ORBIGNY, Ann. Sci. Nat., VII, No. 7, 1826, p. 269. 
With the smooth upper portion of the test and the lower rough 
spinous portion, the above is one of the peculiar surface ornamenta- 
tion forms found among the Bulimine. The spines often project 
from the edges of the chambers as in B. marginata, but in the former 
they are never lengthened into spines. 
Abundant in the North Atlantic and South Pacific and its 
bathymetric range extends from shallow depths down to 2,740 
fathoms. 
It has been recognized in the glacial clays of Norway. Present 
at Station H. 4567 only. 
