CANADIAN PLEISTOCENE ELORA AND FAUNA. 



The most easterly of the localities in the related deposits is ^Montreal. 

 The majority of the specimens recovered at this point represent drift 

 material brought down hy tributary rivers, but the great abundance of 

 Zoalera marina and the occurrence of Algae show that some of the plants 

 at least were deposited in place. The matrix is a blue clay. Seven 

 species in nil hnvo been recovered from this locality, and they are all 



