An appraisal of the Permian palaeobiodiversity and geology of the Ib-River Basin, eastern coastal area, India

• Published in: Journal of Asian earth sciences Vol. 157; pp. 283 - 301
• Main Authors: Goswami, Shreerup, Saxena, Anju, Singh, Kamal Jeet, Chandra, Shaila, Cleal, Christopher J.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 15.05.2018
• Subjects: Ib-River Basin; Ichnology; Marine incursion; Palaeoclimate; Palaeovegetation; Vegetational reconstruction; Ichnology; Palaeovegetation; Marine incursion; Ib-River Basin; Palaeoclimate; Vegetational reconstruction
• ISSN: 1367-9120; 1878-5786
• DOI: 10.1016/j.jseaes.2017.09.006

[Display omitted] •Permian palaeoclimate, palaeoenvironment and biostrtaigraphy of Ib-Basin deduced.•Reconstructed Permian vegetation during Barakar and Lower Kamthi formations.•Redefined the stratigraphic status of unclassified Barakar and Kamthi formations.•Marine incursions and marine marginal environment during Permian are summarized. The Ib-River Basin situated in the east coastal area of India, in Odisha State is a south-eastern part of the Mahanadi Master Basin. A large number of plant macrofossils belonging to the Glossopteris flora were described and documented between 2006 and 2010 from various localities of the Barakar and Lower Kamthi formations of this basin. The floral components representing leaves, roots and fructifications in these assemblages belong to the Lycopodiales, Equisetales, Sphenophyllales, Filicales, Cordaitales, Cycadales, Ginkgoales, Coniferales and Glossopteridales. In the present study, all the available data pertaining to the biological remains, petrological analyses as well as the geology of this basin are reviewed and analyzed to deduce and reconstruct the biostratigraphy, palaeoclimate, palaeoenvironment and the landscape of this basin during Permian time in general and during the deposition of Barakar (Artinskian - Kungurian) and Lower Kamthi (Lopingian) formations in particular. The floral composition suggests the prevalence of a temperate climate with a slight change from warm moist to warm dry conditions during the deposition of the Barakar Formation and warm and humid during the deposition of Lower Kamthi sediments. Distribution of various plant groups in the Barakar and Lower Kamthi formations have been shown to depict the biodiversity trends. Vegetational reconstructions during the deposition of the Barakar and Lower Kamthi formations around the Ib-River Basin have also been attempted based on all the fossil records from this area. The status of unclassified Barakar and Kamthi formations has been redefined. Apart from megafloristics, the palynology of the basin is also discussed. Possible marine incursions and marine marginal environment in the Ib-Basin during Permian are overtly summarized on the basis of records of acritarchs, typical marine ichnofossils and evidences of wave activity in Lower Gondwana sediments of this Basin.