1990
DOI: 10.54991/jop.1990.1699
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Fossil woods of Terminalia and Lagerstroemia from the late cenozoic beds of Mahuadanr, Palamu District, Bihar

Abstract: Two fossil woods belonging to Terminalia tomentosa and Lagerstroemia sp. cf. L. parviflora have been described from the fossiliferous sandstone exposed near Mahuadanr, Palamu District, Bihar. Based on the earlier record of fossil wood of Sindora from this bed a Miocene-Pliocene age has been suggested.

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Cited by 8 publications
(8 citation statements)
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“…The outcrop exposes mostly shale (arenaceous and clayey) and sandstone, while the studied fossil leaves are preserved as impressions and compressions in greyish blue mudstones and light-brown diatomite. Earlier workers (Prakash et al, 1987;Srivastava and Bande, 1992;Hazra et al, 2020a) have considered the age of the Rajdanda Formation to be 'late Tertiary' (Pliocene), but till date no absolute (radiometric) dating has been carried out.…”
Section: Methodsmentioning
confidence: 99%
“…The outcrop exposes mostly shale (arenaceous and clayey) and sandstone, while the studied fossil leaves are preserved as impressions and compressions in greyish blue mudstones and light-brown diatomite. Earlier workers (Prakash et al, 1987;Srivastava and Bande, 1992;Hazra et al, 2020a) have considered the age of the Rajdanda Formation to be 'late Tertiary' (Pliocene), but till date no absolute (radiometric) dating has been carried out.…”
Section: Methodsmentioning
confidence: 99%
“…However, in view of its close lithological and plant fossil similarities with the Sandhan Formation of Kachchh, its age is considered as Plio-Pleistocene till more evidences are obtained (Guleria & Shukla, 2011). Although the two genera being described herein are already known from various Palaeogene and Neogene sediments of India (Prakash, 1966;Prasad, 1989;Guleria, 1990Guleria, , 1991Srivastava & Bande, 1992;Prakash et al, 1994;Tiwari & Mehrotra, 2000), this is their first record from this formation.…”
Section: Introductionmentioning
confidence: 80%
“…The outcrop yields abundant angiosperm leaf remains, carbonised wood fragments, and fruit remains including winged fruits and flowers. The earlier studies (Prakash et al, 1987; Srivastava & Bande, 1992; Singh & Prasad, 2007, 2008, 2009a, 2009b, 2009c, 2010) have considered the age of the studied sedimentary sections to be “late Tertiary” (Pliocene), but no absolute (radiometric) dating has been carried out to date. Additionally, the district resource map published by the Geological Survey of India (GSI) of Palamau, Jharkhand, also assigns a Pliocene age to the sedimentary beds.…”
Section: Methodsmentioning
confidence: 99%