30 MR. F. CHAPMAN ON FORAMINIFERA FROM 
Invotutina contca, Schlumberger. (PI. 5. figs. 6a, 0.) 
Involutina conica, Schlumberger, 1898, Feuille Jeunes Naturalistes, 
ser. 3, Ann. 28, No. 382, pp. (1, 2), figs. 1-3. 
This species has been lately described from the Great Oolite 
between Villers-sur-Mer and Caen by M. Schlumberger. 
The specimens now before us are, if anything, larger than 
those from France. 
Frequent in the Red Limestone of Nesselsdorf. 
Family TEXTULARIIDA. 
Subfamily TEXTULARIING. 
Vanvuttna, d’Orbigny [1826]. 
VALVULINA CUNEIFORMIS, sp. nov. (PI. 5. figs. 7a, 0.) 
Test conical, flattened on opposite sides; septal face convex, 
with a valve-like aperture. Chambers numerous, narrow, and 
alternate in three series. Length of test <4, inch (‘373 mm.). 
Measurement across the long and short axes of oral face of test 
#. inch (463 mm.) and yz inch ('357 mm.) respectively. 
This species is somewhat like Textularia conica, d’Orbigny *, 
in its general shape. It differs, however, in the numerical 
arrangement of the chambers; the aperture also is characteristic 
of Valvulina. 
Another form which V. cuneiformis resembles is Valvulina 
paleotrochus, var. compressa, Brady 7, from the Carboniferous 
formation, but the latter is strongly concave on the apertural 
face. 
Frequent from the Red Limestone of Nesselsdorf. 
Family LAGENID 2. 
Subfamily NoDOSARIING. 
Lineuina, d’ Orbigny [1826]. 
LINGULINA NoDoSARIA, Reuss. (Pl. 5. figs. 8a, 6.) 
Lingulina nodosaria, Reuss, 1862, Sitzungsb. Ak. Wiss. Wien, vol. xlvi. 
p- 59, pl. v. figs. 12a, 0. 
he specimen here figured consists of two chambers only, and 
* Foram. Cuba, 1839, p. 143, pl. i. figs. 19 & 20. 
+ Carboniferous Foram. (Pal. Soc.), vol. xxx. 1876, p. 89, pl. iv. figs. 5a, 0. 
