15 
Genus — NODOSAPIA, Lamarck. 
NODOSARIA PERMIAN A, Spandel, S]). 
(Plate II, Pigs. G, 8a, b.) 
Orthocerina permiana , Spandel, 1898, Die Foram deutschen Zechsteins, p. 7 
(Author’s Copy), Fig. 2. 
Observations. — The specimens before us, and also those figured, seem 
to be merely irregularly grown Nodosarines. It is unnecessary to retain 
Orthocerina in any restricted sense, as the specimens on which the genus 
was originally founded are included in other genera as Rhabdogonium. Spandel 
records this species from the Zechstein of Germany. 
Occurrence. — In the decomposed limestone of Wollong. Occasional. 
Nodosaria (Dentalina), cf. farcimen, Reuss (after Soldani). 
(Plate II, Fig. 11.) 
Orthoceras farcimen , Soldani, 1791, Testaceographia, vol. 1, pt. 2, p. 98, PI. CV, Fig. O. 
Dentalina farcimen , Reuss, Bull, de l’Acad. Roy. Belg., ser. 2, vol. XV, p. 146, 
PI. 1, Fig. 18. 
Nodosaria ( Dentalina ) farcimen, Soldani sp., Brady, 1884, Rep. Chall., vol. IX, 
p. 498, PI. LX II, Figs. 17, 18 ; woodcuts, Figs. 13 a-c. 
Observations. — This species seems to be represented in the present 
series by two segments of a subovate-chambered Nodosaria. N. farcimen 
is already familiar to us as a Permian fossil. 
Occurrence . — In the decomposed limestone of Wollong, New South 
Wales. 
Nodosaria (Dentalina) ? bradyi, Spandel, sp. 
(Plate II, Fig. 12.) 
Dentalina bradyi , Spandel, 1901, Abhandl. der Naturhist, Gesellsch. in Niirnberg, 
p. 16 (author’s copy), Fig. 9. 
The original description of N. (D) bradyi was based on a specimen seen 
in a thin rock-slice of the Kansas Permo-Carboniferous limestone. Allowing 
for a certain range of variation, the specimen before us, although not so 
slender, nor so bulbous at the commencement, probably belongs to the same 
species. The aperture in the Australian specimen shows a modified stellate 
condition. 
Occurrence . — In the decomposed limestone of Wollong, New South 
Wales. 
