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Two accounts of plant-remains from the Early Palaeozoic rocks of Victoria have been given recently. The more critical as to the age of the plants (Lang and Cookson, 1935) dealt with a small flora found in beds of mudstone containing graptolites. The latter, from two of the localities (Alexandra and Yarra Track), were determined by Dr. G. L. Elles and established the age of the beds as Lower Ludlow. The flora is thus certainly of this age in these two cases, but, since some of the beds in which it occurs are regarded as Middle Silurian by Australian geologists, the age was stated generally as “not younger than Lower Ludlow.” There is no doubt as to these vascular or land-plants being Silurian.

IV—On plant-remains from the Silurian of Victoria, Australia, that extend and connect floras hitherto described