Remarks on the Eocene Rocks of Victoria. 



157 



This, however, is not the case. The forms that now appear for 

 the first time, or are common instead of rare as in the lower zone, 

 are typical eocene species, which are common at such beds as 

 Mornington. From this horizon we note eleven species recorded 

 for the first time from Spring Creek section, which are common 

 at Mornington, and four which, though previously i-ecorded for 

 the lower beds, are uncommon or even I'are, while occurring 

 frequently in what we regard as higher beds elsewhei-e. 



A recent visit to Maude has enabled us to increase our list of 

 species from the lower beds, and the decided affinity of the fauna 

 to that of Spring Creek will be seen on examination of the table 

 showing the occurrence of the fossils at Spring Creek, Muddy 

 Creek, and Mornington. 



Table Showing the Occurrence of Lower Maude Fossils 

 AT OTHER Localities. 



