The age of the glacial deposits is later than the Glossopteris flora and occurs early in the time of the Gangamopteris flora.
At Bajo de Velis, in San Luis, the plants belong to the " Glossopteris flora," which is so widely spread in South Africa, India and Australia, and the beds are correlated with the Karharbari series of India (Permian or Permo-Carboniferous).
Dvina, Glossopteris, Noeggerathiopsis and other ferns characteristic of the Indian Gondwana beds have been found; and with these are numerous remains of reptiles similar to those which occur in the Indian deposits.
Some of the plants are European forms, others belong to the Glossopteris flora characteristic of India and South Africa.
In Zululand they are chiefly anthracitic. The fossils include several species of Glossopteris among them: Glossopteris ' See C. L.
These include among others, Glossopteris browniana, Gangamopteris cyclopteroides, Sigillaria Brardi, Bothrodendron Leslii, Noeggerathiopsis Hislopi.
They are underlain by Jurassic rocks, from beneath which sandstones and shales yielding Glossopteris browniana var.
It is somewhat remarkable that this characteristically southern flora, known as the Glossopteris Flora (from the name of one of the most characteristic genera), has also been found in the north of Russia.
Plants constitute the chief fossils of the Ecca series; among others they include Glossopteris, Gangamopteris, Phyllotheca.
Among plants Glossopteris occurs for the last time.
These contain reptilian remains, and also clear imprints of leaves of the Glossopteris indica, as well as other indications of an ancient vegetation.
The Glossopteris flora of India and the southern hemisphere, the age of which has been disputed, but is now regarded as for the most part Permo-Carboniferous, is, however, dealt with in the succeeding section, in connexion with the Mesozoic floras.
The extraordinary abundance of Glossopteris in PermoCarboniferous rocks of Australia, and in strata of the same age in India and South Africa, gave rise to the term " Glossopteris flora for the assemblage of plants obtained from southern hemisphere rocks overlying beds containing Devonian and Lower Carboniferous fossils.
The Glossopteris flora of Australia occurs in certain regions in association with deposits which are now recognized as true boulderbeds, formed during widespread glacial conditions.
Similar glacial deposits occur also in South America, and members of the Glossopteris flora have been discovered in Brazil and elsewhere.
In South Africa, Glossopteris, Gangamopteris and other genera, identical with those from Australia and India, are abundantly represented, and here again, as in India and South America, the plants are found in association with extensive deposits of undoubted glacial origin.
To state the case in a few words: there is in South Africa, South America, Australia and India an extensive series of sediments containing Glossopteris, Gangamopteris and other genera, and including beds full of ice scratched boulders.
The most important evidence on which this conclusion is based is afforded by the occurrence of European forms of Carboniferous shells in marine strata in New South Wales, which are intercalated between Coal Measures containing members of the Glossopteris flora, and.
Africa (Eeca boulder-beds), Australia and Tasmania (Bacchus Marsh boulder-beds, &c.), and South America, which are associated with Glossopteris-bearing strata.
On the other hand, the plant-beds of the Permo-Carboniferous age in South Africa, South America, India and Australia demonstrate the existence of a widely distributed vegetation wh i ch agrees in age with the Upper Carboniferous and of the beds in which Glossopteris and other genera make FIG.
- Glossopteris frond, with portion enlarged to show the venation.
It is only recently that undoubted sporangia have been found in close association with Glossopteris leaves.
Associated with Glossopteris occurs another fern, Gangamopteris, usually recognized by the absence of a well marked midrib, though this character does not always afford a satisfactory distinguishing feature.
In view of recent discoveries which have demonstrated the Pteridosperm nature of many supposed ferns of Palaeozoic age, we must admit the possibility that the term fern as applied to Glossopteris and Gangamopteris may be incorrect.
There can be little doubt that the Indian Lower Gondwana rocks, in which the boulder-beds and the Glossopteris flora occur, must be regarded as belonging to a vast continental area of which remnants are preserved in Australia, South Africa and South America.
We may next inquire what types occur in the Glossopteris flora agreeing more or less closely with members of the rich PermoCarboniferous vegetation of the north.
In the Tongking area, therefore, a flora existed during the Rhaetic period consisting in part of genera which are abundant in the older Glossopteris beds of the south, and in part of wellknown constituents of European Rhaetic floras.
- G - G, Glossopteris Flora.
Rhaetic flora of Tongking (Glossopteris, &c.; IX.
Glossopteris, &c., in Permian rocks in prov.
In 1895 Professor Zeiller described several plants from the province of Rio Grande do Sul in South America (Map A, including a few typical members of the Glossopteris flora associated with a European species, Lepidophloios laricinus, one of the characteristic types of the Coal period, and with certain ferns resembling some species from European Permian rocks.
Starting with the Permo-Carboniferous vegetation, and omitting for the moment the Glossopteris flora, we find a comparatively homogeneous flora of wide geographical range, consisting to a large extent of arborescent lycopods, calamites, and other vascular cryptogams, plants which occupied a place comparable with that of Gymnosperms and Angiosperms in our modern forests; with these were other types of the greatest phylogenetic importance, which serve as finger-posts pointing to lines of evolution of which we have but the faintest signs among existing plants.
In the southern hemisphere the Glossopteris flora succeeded a Lower Carboniferous vegetation with a rapidity similar to that which marked the passage in the north from Palaeozoic to Mesozoic floras.
It was from this Glossopteris flora that several types gradually migrated across the equator, where they formed part of the vegetation of more northern regions.
The difference between the Glossopteris flora and those which have left traces in the Upper Gondwana rocks of India, in the Wianamatta and Hawkesbury beds of Australia, and in the Stormberg series of South Africa is much less marked than that between the PermoCarboniferous flora of the northern hemisphere and the succeeding Mesozoic vegetation.
Glossopteris Flora: Blanford, H.
Arber, Catalogue of the Fossil Plants of the Glossopteris Flora in the Department of Geology (British Museum, Nat.
A similar association was found also in Argentine rocks by Kurtz (Map A, G1), and from South Africa Sigillaria Brardi, Psygmophyllum, Bothrodendron and other northern types are recorded in company with Glossopteris, Glangamopteris and Naeggerathiopsis.
In his account of some plants from the Coal Measures of Kansu (Map A, IV.) Dr Krasser has drawn attention to the apparent identity of certain leaf-fragments with those of Naeggerathiopsis Hislopi, a typical member of the Glossopteris flora; but this plant, so far as the evidence of vegetative leaves may be of value, differs in no essential respects from certain species of a European genus Cordaites.
By Professor Zeiller - and this author has recently made important additions to his original account - which demonstrates an admixture of Glossopteris types with others which were recognized as identical with plants characteristic of Rhaetic (After Feistmantel.) FIG.
Species which do not occur in the Glossopteris flora.
These two instances - the Tongking beds of Rhaetic age and the Bunter sandstones of 'the Vosges - afford evidence of a northern extension of Glossopteris types and their association with European species.