740 
APPENDIX IV. 
ORGANIC REMAINS, EIGHT-MILE PLAINS, NEAR BRISBANE. 
In stating (p. 608) that remains of the Extinct Mammalia had been discorered in this 
locality. I was under the impression that Mr. C. W. De Vis had obtained among_ others, 
remains of an extinct Species of Wombat, but Mr. De Vis informs me that I was mistaken 
The only organic remains from the Eight-Mile Plains yet identified are those of Ceratedus 
Fosteri and Pallimnarchis pollem-s. fish and a reptile, both of living species. The case, then, 
still stands thus, that the known remains of extinct mammalia have all been derived from 
comparatively high levels, whatever significance the fact may have. ^ 
APPENDIX V, 
EOCENE BEDS IN VICTORIA. 
The following should have been added as a footnote alter the word “ Miocene, p. 575, 
“ Professor E. Tate, on the other hand, regards the fossils from the Schnapper Point 
clays. Port Phillip, as of Eocene age. Journ. E. Soc. N. S. Wales for 1888 [1889], xvii., p. 242. 
In a paragraph on p. 
overflow as 50,000 gallons. 
APPENDIX VI. 
DARR RIVER DOWNS BORE No. 3. 
424. the depth of this bore is given as 2,700 feet, and the daily 
The bore lias since been continued to 3,530 feet, and is therefore 
ihe deepest in the Australian Colonies. {See “ Muckadilla Bore,” p. 428.) Mr. Fiskin, one of 
the owners of the Station, states that the “ bottom ” is sandstone, that the daily overflow is 
500,000 gallons, and that the temperature of the water is 172° Fahr. 
APPENDIX VII. 
LACERTILIAN REMAINS ON SUTTOR RIVER. 
An additional locality for remains of the extinct Lacertilia has been furnished by Mr. 
De Vis, who informs me that a Vertebra of Meffalania, from black sod on tlie bank of a lagoon 
at Mount Lookout, near the head of the Suttor Elver, was sent to him by Mr. Peter Mur y 
about twelve years ago, and is now in the Queensland Museum. 
APPENDIX VIII. 
LIST OF FOSSILS OF THE BURRUM BEDS, WITH THEIR SYSTEMATIC POSITIONS. 
In consequence of the introduction of PhjUopteris Feistmanteli into my Colleague’s List 
after Chapter XXIII. was in type, the following corrections are necessary : _ _ 
Page 311. After the paragraph on Taniopteris {AngioptervEum) Daintreei, insert. 
“ Oenus-PHYLLOTHECA, Saporta. 
-(Ip 
' “ PiiYLLopiEEis Feistmanteli, 7®^- 
“ Loc. Styx Coal Field (Burrum Bed s). Occurs also at Stewart’s Creek, Eockhampton 
swiohBeds).” 
Page 312. In the Synopsis, after Aletlioplei is australis, Morr., insert . 
“ * Phylhpteris Feistmanteli, Eth. Cl.” 
And the last two lines should read 
“ Of the thirteen species above named, five are common 
the remaining eight are peculiar to the Burrum Formation.” 
to the Ipswich Formation, and 
J. 
