217 
to the characters of the Middle Devonian C. sweeti , from Queensland 1 ; 
and in the absence of the entire corallum, or of isolated specimens, it is 
here referred provisionally to that species. 
Favosites multitabulata , Eth. hi. Plate XXX., Figs. 4 and 5. 
Favosites multitabulata , Etheridge. Jun., 1899, Rec. Geoi. Surv., 
New South Wales, Vol. VI., 1899, p. 168, PI. XVIII., Fig. 6; PI. 
XXVI. 
The dimensions of the calices and the spacing of the tabulae of the 
above species, as given by Mr. Etheridge (loc. cit .), exactly agrees with 
our specimen. The double series of mural pores is also present. There 
is no doubt that the Limestone Creek example belongs to this species, 
which I have already met with in the Middle Devonian of Bindi. 
Etheridge’s original specimens came from Boodle’s Freehold, near Moonbi, 
north-east of Tamworth, New South Wales. 
Explanation of Plates. 
Plate XXIX. 
Fig. 1.—Brecciated limestone; showing the fragments invested with a 
layer of clastic material, consisting of quartz grains and a chloritic sub¬ 
stance. Stony Creek, Limestone Creek, Benambra. No. 272 (Slide 1101). 
X 7 *. 
Fig. 2.—Transverse section of part of corallum of Cyathophyllum 
( ?)sweeti, Eth. hi. Showing the relation of the primary and secondary 
septa, and the curved and oblique dissepiments. Stony Creek, Benambra. 
No. 274 (Slide 1103). x 10. 
Fig. 3.—Transverse section of a small portion of the corallum of 
Cyathophyllum (t)sweeti, Eth fil. Showing strongly convex dissepiments. 
Stony Creek, Benambra. No. 275 (Slide 1099). x 6. 
Plate XXX. 
Fig. 4 .—Favosites multitabulata , Eth. fil. Transverse section of coral¬ 
lum. Stony Creek, Benambra. No. 276 (Slide 1104). x 7. 
Fig. 5.— F. multitabulata , Eth. fil. Vertical section. Stony Creek. 
No. 276 (Slide 1105). x 7. 
Plate XXXI. 
Fig. 6.—Crinoidal limestone. Stony Creek. Rock very little altered. 
No. 277 (Slide 1100). x 7. 
Fig. 7.—Recrystallized crinoidal limestone. Stony Creek. No. 278 
(Slide 1106). x 28. 
Plate XXXII. 
Fig. 8.—Stromatoporoid limestone with dolomitized layers. Glen 
Wills, Wombat Creek. No. 1460 (Slide 1112). x 7. 
Fig. 9.—Stromatoporoid limestone with dolomitized layers. The 
organic portion better preserved. Glen Wills, Wombat Creek. No. 1460 
(Slide 1112 bis.), x 7. 
[Report sent in 26.4.10.\ 
r Cyathophyllum sp. ind. Etheridge, jnr., Geology and Palaeontology of Queensland and New Guinea 
(Etheridge and Jack), 1892, p. 59, PI. III. Figs. 11 and 12. C. sweeti, Eth. fil. Proc. Linn. Soc. of New South 
Wales, Vol. IX. Pc. 3,1S95, p. 52, PI. XL. Figs. 3, 4 ; PI. XLI. Fig. 1. 
