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- W2323494627 abstract "THE great continent of Gondwanaland existed in the late Palæozoic in the southern hemisphere and persisted through a long period of geological time with little modification. The deposits formed on it are found in Australia, India, South Africa, South America, and Antarctica, where beds of glacial origin generally occur at the base of the series. The fossilised remains of the flora which flourished on the continent in its early stages are found sometimes in, and generally above, the glacial horizon. Characteristic plants are species of Gangamopteris and Glossopteris. The whole floral assemblage is very different from that yielded by the Upper Carboniferous and Permian continental deposits of the northern hemisphere, in which the Pteridosperms (e.g. Alethopteris), Lycopodiales (e.g. Lepidodendron), Equisetales (e.g. Calamites), and Cordaitales (e.g. Cordaites) predominate." @default.
- W2323494627 created "2016-06-24" @default.
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- W2323494627 date "1929-06-01" @default.
- W2323494627 modified "2023-09-26" @default.
- W2323494627 title "The Late Palæozoic Glaciation" @default.
- W2323494627 doi "https://doi.org/10.1038/123946a0" @default.
- W2323494627 hasPublicationYear "1929" @default.
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