TRIASSIC FLORA OF BALD HILL. 
be present, giving oii forked lateral nerves at an acute angle.” 
Thus, according to that author, both types of venation niav be 
|)resent. 
l)isfril>ution. Ipswich aud Walloon Series of (hieensland (d’rias 
and durassic). Hawkesbury Sandstone and Wdanamatta Shales 
of New South Wales; also at Dubbo, New South Wales; Leigh's 
(Veek, South Australia (Triassic); I’oit Phillip, near (Irice’s (’reek 
and South (lippsland (-lurassie). 
FEHN-MKE PLANTS. INOERTAE SEDfS. 
(lenus TAFLNionunos Krongniart, 1828. 
Taeniopteris wianamattae Peistmantel sp. 
(Plate XIII., fig. 51.) 
}facrotae)iiopferis iviaii/imaflae Feist mantel, 1878, PalaeouTographic'a., 
Suppl. vol. 11!., Lief. 8, Heft 2, p. 107, f)l. XIII., fig 2. Wilkin- 
son, 1870, Ann. Rep. Dept. Mines, N.S. W'ales, p. 215, pi. \^. 
'r. Woods, 1882, Proc. Linn. Soc. N.S. Wales, vol \HIL, |>. 118, 
])1. 10a. Feistmantel, 1800, Mem. (leol. Surv. N.S. Wales, 
Palaeont. No. 2., ]>. 11(5, pi. XXV'IL, figs, 1, 2. Ftheridge, 
jun., 1802, Deol. and Pal. ()ueenslan(l, p. 270. Dun, 1808, 
Austr. Asso(‘. Adv. Sci., vol. VI L. p. 207. 
Taeni.o})teris mreetl Mcl’oy, 1808, Proc. Roy. Soc. Viet., X.S., vol. X., 
pt. IP, p. 285, and text-fig. 
Maerotaeniopferis iroodsi Dun, 18i)8, Austr. Assoc. Adv. Sci., vol. 
VI L, p. 200. 
Taeniopterifi S]). Arber, 1005, (’at. Foss. Phmts (( Jlossopteris Flora), 
Brit. Mus., p. 128. 
Taeniojderis {.Macrotae-iuopferi.s) sp. (’hapman, 1014, Australasian 
Fossils, p. 88. 
Taeniopteris H'lanamaUae Feistm. sj)., W'alkom, 1017, ()ueensland 
(leol. Surv. Pub. No. 257, pt. L, p. 28. 
Taeii/io pterin {Macfotae/niojiteris) manamuttae, Feistm. ( lia})inan, 
1010, \dctoria?i. Naturalist, vol. XXXV., Xo. 10, pp. 140, 150, 
152. 
A’ote the T p pe-speciineii' nf T. Hu'ceti McCop. I have care- 
fully exatnined the type of Taeniopteris Sireeti described (ref. above) 
by McCoy, and find it to be idendical iir all the })reserved cl)aractM's, 
such as width of lamina, and s})acing and forking of secondary 
veins, with T. nnanamattae. This I have already stated in another 
place. In the original descri|)tion McCoy says that the specimeii 
came from the (ranpa.mo pterin Sandstone. The (diai'acter of the 
matrix, however, clearly shows its origin to be from the U{)pei', 
siliceous layer in the trench at Bald Hill (see remarks an, tea, p. 124). 
I 135 ] 
