Glossopteris Brcwniana , Bgt., p. 150-51. Jerry’s Plains and Mulu- 
bimba. 
Glossopteris linearis, M‘Coy, p. 151, PI. IX, f. 5, 5a. Wollongong 
and (?) Arowa*. 
Becopteris tenuifolia, M £ Coy, p. 152, PI. IX, f. 0. Clarke’s Hill. 
(A doubtful species.) 
Zeugophy Hites elongates, Morr., p. 152. Mulubimba, New South 
Wales. 
Bhyllotheca australis, Bgt., p. 156. Mulubimba, New South Wales. 
Bhyllotheca ramosa, M £ Coy, p. 156, PI. XI, f. 2, 3. Mulubimba, 
New South 1 ’vales. 
Bhyllotheca Sookeri, M £ Coy, p. 157, PI. XI, f. 4-7. Clarke’s Ilill, 
New South Wales. 
The fossil animals do not concern us here. I shall, therefore, not 
enumerate them. They arc quoted by the Bev. W. B. Clarke in his 
“ Remarks on the Sedimentary Formations of New South Wales,” 1878, 
Appendix XI B, p. 124. 
(6.) 1848. Clarke (Rev. W. B.) Remarks on tlie identity of the Epoch of the Coal-heds 
and Palaeozoic Rocks of New South Wales. Ann. Mag. Nat. Hist, 1848, Vol. il.,p. 206. 
(7.) 1847 Jukes (Prof. J. B.) Notes on the Falaeozoic Formations of New South Wales 
and Van Diemen’s Land. Quart. Joum. G'eol. Soc., Vol. Ill, p. 224, Spc. 
(8.) 1848. Clarke (Rev. W. B.) On the Genera and Distribution of Plants in the Car- 
boniferous System Of New South Wales. Quart. Joum. Geol. Soc., Vol. IV., pp. 50, Sfc. 
In contradiction to Count Strzelecki’s statement of the entire absence 
of the genera Sigillaria, Catamites, and Lcpidodendron, in the Australian 
coal-beds, Mr. Clarke maintains the occurrence of them in these strata. 
He also names various other genera of Carboniferous plants. 
(9.) 1849. Dana (Prof. J. B.) Geology : Wilkes’ United States Exploring Expedition. 
Vol. X. Appendix, p. 714. Ato. Philadelphia, 1819. 
There the following fossils are described : — 
TJrosthencs australis, Dana, a lieterocercal fish, p. 681, &c., Pi. I, 
f. 1. Newcastle. 
Coniferous Stems, p. 714. 
* These two localities require some explanation : — • 
Clarkes’ Hill is in the Wianamatta beds, and not in the Newcastle beds, where Thinnfddia ( Gleichcnites) 
odontopteroides does not occur. 
The position of Al'OWa was uncertain, until I have recognised, from original specimens, forwarded by Mr. 
W. B. Clarke, that Otopteris ovata was the same as Ilhacopteris from the beds at Smith’s Creek, and thus the beds 
at Arowa appear on the same horizon (beds below Lower Marines), but then it would appear doubtful whether 
Glossopteris linearis, quoted by M'Coy from Arowa, really came from that locality. 
