180 
Macro teen lop ter is Feddeni, Eeistm. Middle Gondwana, India. 
Woodwardites microlobus, Schenk. Bhaetic, in Europe. 
Folypodites Fnchsi, Zcillcr. 
DiclyopInjUam acutilobum, Sclienk. Erequcnt in Bhsetic beds, in 
Europe. 
Clcithropteris plcityphylla, Brongt. TMuetic, in Europe. 
Plerophyllum cequale, Nath. Bhsetic, in Europe. 
Pterozcimites Miinsteri, Scliimp. Bhsetic, Europe. 
Anomo zconiles inconstans, Scliimp. IMuctic, Europe. 
Nilssonict polymorpha, Schenk, Bhsetic, Europe. 
Otozamites rarinervis, Eeistm. Upper Gondwanas, India. 
Podozainites disians, Braun. Bhsetic, Europe. 
Nogycralhiopsis Hislopi, Bunh. sp. -Middle and Lower Gondwanas, 
India. 
Cycaditcs Salcidini, Zcillcr. 
There are, therefore, nine species of Gondwana plants (various horizons) 
found, together with ten species of Pdiaetic plants of Europe and elsewhere. 
Mr. Zcillcr considers this flora to be of Bhaetic age, and to occupy besides, a 
position between the Upper and Middle Gondwana of India, which again 
shows that the position I assigned to the Damuda-Pancliet Series was correct. 
These arc about all the various formations and systems of interest to 
be compared with the Australian rock groups. 
SUMMARY. 
If we now sum up we may draw the following conclusions : — 
1. In Australia, India, South Africa, Tonkin, and also in Afghanistan 
there appear to have prevailed towards the close of the Carboniferous Epoch 
different relations from those in Europe, at least with regard to the plant 
remains. 
2. In Australia there occurs in strata belonging to the series of marine 
beds of the Middle and Upper Carboniferous age, a flora containing the 
genera Glossopteris, FlnjUothcca, and Noggeratliiopsis, which hereafter in 
