158 
Martiniopsis ? sulradiata, G. B. Sby. 
Sirophalosia Gerardi, King. 
„ Clarkei, Etli. 
Modiomorpka mytiliformis, Etli. iil. 
Qlimnomya Etheridgei, Be Konincis. 
0. carinata, Etli. fil. 
Mourlonia ? coniformis, Etb. fil. 
Eellerophon stanvellensis, Etli. fil. 
PorcelUa Pearsi, Etli. fil. s . 1 , -n ^ar.n 
From Cracow Creek (south of Boolburra, Central Kailway) on the Dawson 
Eiver Mr. R. Etheridge, E.R.8., described* Oho7ietes cracoioenm, Etfi., and 
Eth. The beds yielding these fossils may be 
nrpsiiined to belone to the Middle Formation. 1 • i t 
From a locality described as “ Weelwondongara Creek, Nogoa River, w ic 
unable to identify, but which is probably on Wealwandangie mg block south 0 
Springsure, the same Author described t Productus or SlropUloHia (PL 18, • 
Z) (Sirophalosia Clarkei, Eth.) This Brachiopod, as has already been seen, is very 
characteristic of the Middle or Marino Formation. _ -uu^^vT^pnrl of 
Mr. Smith, shortly before his death, forwarded, from neighbomhood 
Springsure, some Crinoid stems, and undoubted specimens of f 
latter, as has already been seen, being a characteristic fossil of the Middle Forma _ 
Mr. Rands records in his “Report on Clermont” that, 
forty miles north-north-east of Clermont, on the range west of Mount Eankm M • 
RogLs-Harrison found Cyaihophyllim (two species), 4dj^ 
probably P. hrachythwrus, anA Area r' Probably these bods belong to the Mid 
^“Ddntree’s Paper on the “ Geology of Queensland ” J contains a E^ °f fossils 
identified by Mr. R. Etheridge. F.K.S., “from the head of Roper Creek aaid the Bowe 
River,” all characteristic of the Middle Bowen River Beds. It is stra-nge that Daintree 
of all men, should have mixed up fossils from different localities so that it is impos.u 
to say which was which ; but we may take it for granted that somewhere in the neig ' 
bourhood of Gordon Downs representatives of the Middle Bowen Series occur. 
Roper Creek referred to is probably “ Little Roper’s Creek ” ^t^^^^ary of Sandy 0 
Campbell’s Creek, which will be found on the map between the 22nd and 23id - 
of Latitude and tbe Meridians of 148 and 149. Daintree’s Paper also contains (P- ^ 
a list of apparently Cretaceous fossils from “Gordon Downs, at the head of Rop 
Creek,” sent by the Revd. W. B. Clarke to Mr. R. Etheridge, F.R.S. The words at t 
head of Roper Creek ” are here probably inserted by mistake. There is a station nam 
Gordon Downs near Roma, which is a Cretaceous locality. 
J. 
* Quart. Journ. Geol. Soc. Lend., xxviii., pp. 330, 337. 
f Tyoc. cii., p. 334. 
J Quart, Journ. Geol. Soc., xxviii., i>. 28(). 
