60 GLOSSOrTERIS. 



V. 7231. A nearly perfect frond, apparently of the narrow- 

 leaved type of G. Browniana, rather more than 9 cm. long and 

 2 cm. hroad. The nervation is very acute. 



Port Stephens. Odinheimer Coll. 



V. 10,648. A number of fragments of fair- sized fronds, some 

 showing the nervation clearly. 



Newcastle. Keene Coll. 



V. 10,649. Two specimens with fragments of fronds of a narrower 

 or more linear type. The nervation is seen here and there. 



Tomago Colliery (at a depth of 342 feet), Hunter River. 



Keene Coll. 



Other specimens : — 53,562 and 53,564 (Australia), 32,447 

 (three specimens from the Hunter River, near Coal-mines ; pres. by 

 Sir E. Home, 1853), 39,148 (Port Stephens; pres. by K.S. Wales 

 Geol. Surv. and litis., 1859), 39,189 and 39,191 (Newcastle 

 Coalfield ; pres. by Sir E. Home, 1859), 40,942 (three specimens from 

 the Newcastle Coalfield; pres. by Sir F. Home, 1860), V. 2109 

 (Australia; pres. by Sir C. Pardon Clarke, 1889), V. 2753 (Cullen 

 Bullen; pres. by W. H. Shrubsole, Esq., 1892), V. 4282 (Australia ; 

 pres. by W. H. Shrubsole, Esq., 1892), V. 6250tf, V. 6250^, and 

 V. 7204 (Port Stephens ; Odinheimer Coll.), V. 7282 (?N.S. Wales), 

 V. 7292 (Port Stephens; Odinheimer Coll.), V. 9366 and V. 9367 

 (Cullen Bullen; pres. by H. F. Collins, Esq., 1903), V. 10,646 

 and V. 10,647 (Tomago Colliery, Hunter River; Keene Coll.). 



Fronds of Glossopteris Broicni ana from Queensland. 



V. 4200. A small fragment with a very oblique network almost 

 at right angles to the midrib. 



Bowen River. 



V. 4201c. A small portion of a frond with the typical nervation 

 of this species. 



V. 4201ff. A median portion of a frond. The midrib is very 

 thick, but the lateral nervation is not very clear. 



V. 4201&. A fragment similar to the above, 12 cm. long, with 

 a very broad midrib, and fairly acute lateral nervation. 



Other specimens : — V. 4201 (several fragments), V. 5952, V. 5953. 



Note. — The specimens registered as V. 4200-1 are possibly those 

 described by Carruthers in 1880 — see Carruthers (72) and (80) — 

 but there is no record to this effect. 



