Palynology and detrital zircon geochronology of the Carboniferous Fenestella Shale Formation of the Tethyan realm in Kashmir Himalaya: Implications for global correlation and floristic evolution

• Published in: Journal of Asian earth sciences Vol. 157; pp. 348 - 359
• Main Authors: Agnihotri, Deepa, Pandita, Sundeep K., Tewari, Rajni, Ram-Awatar, Linnemann, Ulf, Pillai, S. Suresh K., Joshi, Arun, Gautam, Saurabh, Kumar, Kamlesh
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 15.05.2018
• Subjects: Fenestella Shale Formation; India; Jammu and Kashmir; Palynology; U–Pb zircon age; U–Pb zircon age; Palynology; Fenestella Shale Formation; Jammu and Kashmir; India
• ISSN: 1367-9120; 1878-5786
• DOI: 10.1016/j.jseaes.2017.09.003

[Display omitted] •Palynomorphs from the Carboniferous Fenestella Shale Formation, Kashmir have been recorded for the first time.•Maximum age of deposition provided by the youngest detrital zircon is 329±16Ma.•On the basis of general similarity, palynomorphs have been correlated with those of other Gondwana countries.•Warm, temperate and arid climate has been inferred for the Fenestella Shale Formation. First palynological data, supplemented by detrital zircon U–Pb ages, from the Fenestella Shale Formation near the Gund Village in the Banihal area of Jammu and Kashmir State, India, provide new insights into the floristic evolution of Gondwana during the Late Palaeozoic, especially in India, from where the Carboniferous–Permian macro- and microfloral records are impoverished. We also present a first approach to the palynological correlation of the Carboniferous–Permian palynoassemblages described from the various Gondwana countries. The palynomorphs from the Fenestella Shale Formation are fairly well preserved and diversified and include 11 genera and 18 species. While the trilete spores and striate bisaccate pollen grains are scarce, monosaccate pollen taxa mainly – Parasaccites, Plicatipollenites and Potonieisporites are dominant. The assemblage is most similar to the Parasaccites korbaensis palynozone of the Lower Gondwana basins of the Indian peninsula and the Stage 2 palynozone of the late Carboniferous of east Australia. Besides, it is comparable with the known Carboniferous assemblages of Pakistan, Yemen and South America; Carboniferous-early Permian assemblages of South Africa and Permian assemblages of Antarctica. The sediment source of the siliciclastic shelf and delta deposits intercalated in the Fenestella Shale Formation is a hinterland in which Precambrian rocks dominantly were exposed and the Th–U ratios of detrital zircons suggest, that most rocks exposed on the erosion level in the hinterland had a felsic composition. The youngest U–Pb zircon age of the investigated fossiliferous strata is 329±16Ma (late Visean to early Serpukhovian), providing a maximum age of deposition of the studied succession. Based on the affinities of the palynofloral assemblage and earlier palaeontological records, a warm, temperate and arid climate has been inferred for the Fenestella Shale Formation.