FOSSIL FLORA OF EASTERN AUSTRALIA AND TASMANIA, 107 
3. Upper Paleozoic. Under this heading Mr. Clarke comprised 
several groups :— 
a, Upper Coal Measures or Glossopteris beds, also “Newcastle 
beds.” Thea e beds were by Professor Moy considered 
bette considerin: 
stones, and caught all means as older than the indian 8 § 
beds (Damuda series). The Rey. W. B. Clarke considered 
them palzozoic, and so does Mr. C. 8. Wilkinson, to which 
The best bevmed aes where fossils from these beds were 
collected are Blackman’s Swamp, Bowenfels, Guntawang, Mudgee, 
Illawarra, Mulubimba, aii Wollongong. 
The sani hitherto known ar 
Fishes : Urosthenes A emer Dana (a heterocercal fish). 
Plants : Phyllotheca Australis, M‘Coy (and two other species 
which I think do not differ from this one); Vertebraria 
Australis, MCoy ; Sphenopteris lobifolia, Morr. ; alata, 
; , ¥; germana, 
M'Co lumosa, M‘Coy; flexuosa, M‘Coy. 
Clieioytirte ‘Pcianl: Bgt; Hnearis, Mt wibeiek ; ampla, Dana; 
reticulum, Dana; cordata, Dana; teroides, Feistm. ; 
Wilkinsoni, Feistm. ; parallela, Feistn 
Gangamopteris angustifolia, Moy; Gang. Ci larkeana, Feistm. ; 
Caulopteris(?) A 
Zeugophyllites elongatus, Morr.; Viggerathiopeis spathulata, 
sp. ‘fean stm.); ogg. media, Dana, sp. (Fstm.) 
_Brachyphyilum Australe, sce scales of conifers. 
b. Upper wee beds ; beds with marine animals. 
e. ne al measures ; beds with coal seams and flora, below 
din i animals. Th 
are in so 
Hb dees Glossopteris, and Néggerathiopsis, appear to 
take their origin. 
Acco ccording to ea eek received from the late Mr. Clarke, 
it appears that two dyin | in these may be distin, separ- 
ated had lower marine bed Se ice 
a, higher Levitin arind portion , @ 
look Socal thar Hill, and Wagmond Terrace, &c., 
with the following fossils :-—Phyllotheca, sp., Glossopteria 
