Biostratigraphy and floristic evolution of coal swamp floras of a part of Talcher Basin, India: a window on a Permian temperate ecosystem

The present megafloral assemblage recorded from the Barakar sediments of Dholpahar section along Singda rivulet near Gopal Prasad Village in Talcher Basin comprises of equisetaceous stems, Gangamopteris buriadica , Palaeovittaria kurzii and 19 species of the genus Glossopteris . Record of Gangamopte...

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Veröffentlicht in:Arabian journal of geosciences 2018-09, Vol.11 (17), p.1-14, Article 524
Hauptverfasser: Goswami, Shreerup, Das, Kamaljyoti, Sahoo, Mrutyunjaya, Bal, Soumyaranjan, Pradhan, Sanghamitra, Singh, Kamal Jeet, Saxena, Anju
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Sprache:eng
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Zusammenfassung:The present megafloral assemblage recorded from the Barakar sediments of Dholpahar section along Singda rivulet near Gopal Prasad Village in Talcher Basin comprises of equisetaceous stems, Gangamopteris buriadica , Palaeovittaria kurzii and 19 species of the genus Glossopteris . Record of Gangamopteris , Palaeovittaria and many narrow mesh forms of Glosspteris viz., G. angustifolia , G. churiensis , G. communis , G. recurva , G. spatulata , G. stenoneura , G. tenuifolia , G. vulgaris and G. zeilleri from two older fossiliferous horizons demonstrates that these fossils were preserved during Lower Barakar sedimentation. The report of middle and broad mesh forms of Glossopteris viz., G. barakarensis , G. browniana , G. indica , G. intermittens , G. karharbariensis , G. nakkarea , G. oldhamii , G. taeniensis and G. retifera in the youngest fossiliferous horizons reveals that these fossils were preserved during the deposition of Upper Barakar sediments. The continuation of some of the Karharbari plant fossils in the early phase of Barakar Formation and their disappearance in the flora of Late Barakar suggests a shift in the climatic setup. Palaeoclimate and palaeovegetation of this area are also summarised in this study. Moreover, the fossil assemblages of different fossiliferous beds of Dholpahar section demonstrate the evolution of midrib and meshes in different reticulate leaves.
ISSN:1866-7511
1866-7538
DOI:10.1007/s12517-018-3886-7