no. 16083. FKFORAMINIFERA FROMTHE HAWAITAN ISLANDS— BAGG. 159 
TRUNCATULINA WUELLERSTORFI (Schwager). 
Anomalina wuellerstorfi SCHWAGER, Novara Exped., Geol. Theil, II, 1866, 
> AWS, fol, Wat, SS, WOH, WO 
This species is very abundant in nearly all of the Albatross mate- 
rial examined and is wanting only at Stations D. 4000, D. 4476, H. 
4555, H. 4566, and H. 4579. Its earliest appearance dates back to the 
Cretaceous. 
Genus ANOMALINA. 
ANOMALINA AMMONOIDES (Reuss). 
Rosalina anvmonoides Reuss, Verstein. bohm. Kreid., Pt. 1, 1845, p. 36, pl. 
XI, fig. 60; pl. vit, fig. 53. 
Kasily recognized by its depressed involute nautiloid form with 
rounded margin and median aperture. The species is, however, 
liable to considerable minor varieties. It is chiefly found in the 
South Pacific, and in waters of moderate depths. As a fossil it is 
‘well known in the Cretaceous of both this country and Europe. It 
is not abundant in the material studied but occurs at Stations D. 
4000, D. 4025, D. 4174, H. 4430, H. 4440, H. 4476, H. 4508, H. 4566, 
H. 4567, H. 4579, and H. 4694, and is rather common at D. 4025. 
ANOMALINA ARIMINENSIS (d’Orbigny). 
Planulina ariminensis D’ORBIeNY, Ann. Sci. Nat., VII, 1826, p. 280, pl. v, 
figs. 1-8 bis, modele No. 49. 
Differs from A. ammonoides in the greater compression of the 
test and the more squarely built periphery, together with a stronger 
limbation of the sutures. 
Widely found in the North Atlantic, at moderate depths; rare in 
the South Atlantic, and also the South Pacific; abundant in the Med- 
iterranean. Found also at the Abrohlos Bank from 47 to 940 fathoms, 
and in Hongkong Harbor. In the fossil state it 1s known from 
the Cretaceous, and has been found in the Tertiary and later deposits 
in many localities. Rather rare at Stations H. 4430 and H. 4567. 
ANOMALINA CORONATA Parker and Jones. 
Anomalina coronata PARKER and JONES, Ann. Mag. Nat. Hist., ser. 2, XIX, 
1857, p. 294, pl. X, figs. 15, 16. 
The above species is coarsely constructed, like Anomalina grosseru- 
gosa, but the segments are more or less angular along each side of 
the peripheral border and sharply marked off from the depressed 
umbilici. The perforation of the shell is coarse and the test large. 
Rare within the Tropics but abundant in many temperate zone dredg- 
ings from the North and South Atlantic oceans. Geologically known 
from the Eocene through the later Tertiaries. It is usually found 
