80 Proceedings of the Royal Society of Victoria. 



Werrikooian. 



Limestone Creek. 



Kalimna7i. 



Jimmy's Point, Gippslancl. Upper beds of the JNlurray River 

 Clifls. Upper beds at Aldinga. Upper beds at Muddy Creek. 

 Upper beds at Shelford. With these we would associate the 

 Marine Sands of the Dry Creek and Croydon bores, South 

 Australia, which were regarded by Prof. Tate as intermediate in 

 age betsveen the Limestone Creek and the Jimmy's Point beds. 

 To this series we also refer the Upper beds at Beaumaris, which 

 were correlated by Professor Tate with the Spring Creek series, 

 the latter being, in our opinion, older than Balcombian. 



Bakonibian. 



Balcombe's Bay and Grice's Creek, Mornington. Lake 

 Connewarre. Southern Moorabool Valley. Upper beds at 

 Maude. Altona Bay. Gellil)iand. Camperdown. INIurgheboluc. 

 Shelford, lower beds. Bairnsdale. Corio Bay. Curlewis. 

 Belmont. Fishing Point, Aire River. 



Jail Jitciaii. 



Spring Creek. Table Cape, Tasmania. Waurn Ponds. With 

 these we include the lower beds at Maude, which Professor Tate 

 and Mr. Dennant considered to show nmch closer relationship to 

 the lower beds of Muddy Creek. We also refer to the same 

 series the lower {i.e. " Eocene ") beds at Aldinga, the Aire Coastal 

 series and the Cape Otway beds. In the association of the 

 Aldinga, Aire Coastal and Cape Otway beds together we are 

 apparently in agreement with the views of Messrs. Tate and 

 Dennant, but, as will be seen on referring to the earliest parts of 

 this paper, their association with the Spring Creek and Table 

 Cape series is strongly opposed to the view of the same authors. 

 But as has been already pointed out the correctness of all the 

 details of this correlation is not a necessary preHminary to the 

 use of the terms suggested. It is open to those who differ to 

 separate any of the members, and, where possible, to group them 

 similarly under other appropriate names. 



