Page:Quarterly Journal of the Geological Society of London, vol. 35.djvu/67

Rh the changed conditions of the land would no longer permit the spread of East-Australian forms of vegetation into the newly-emerged tract, but that it would be occupied by Victorian forms. The geologist of that time would then meet with a somewhat parallel case to that now seen in the difference between the Miocene fossil flora of Bacchus Marsh and the recent flora of Victoria.