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Annual Report 2011-2012 - Birbal Sahni Institute of Palaeobotany

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EBIRBAL SAHNI INSTITUT<br />

<strong>Annual</strong> <strong>Report</strong> <strong>2011</strong>-<strong>2012</strong><br />

1946<br />

OF PALAEOBOTANY<br />

Thrust Area:<br />

Project 14.1:<br />

FRONTIERS IN PALAEOBOTANICAL RESEARCH (Reconnaissance<br />

Projects to aid in development <strong>of</strong> future research direction)<br />

Carboniferous land plants in the Himalaya (Spiti): Phytogeographic and palaeogeographic<br />

implications<br />

The studied specimens from the Spiti area include<br />

Asterophyllites sp., stems, trace fossils, conifer axes and<br />

Psilophytes axes. The work carried out in this project is<br />

being finalized for publication.<br />

K.J. Singh [& S.K. Parcha (WIHG)]<br />

Project 14.2: Megaflora and palynology <strong>of</strong> the Kargil Molasse<br />

Compiled the palae<strong>of</strong>loral (leaf impressions, sporespollen,<br />

algal and fungal remains) and gyrogonites <strong>of</strong><br />

charophytes records recovered from the Kargil and<br />

Tharumsa formations (Kargil Molasse Group) <strong>of</strong> northwest<br />

Ladakh Himalaya.<br />

R.C. Mehrotra, Madhav Kumar & AK Ghosh<br />

[& Ashok <strong>Sahni</strong> (Chandigarh) & K. Kumar (WIHG)]<br />

Project 14.3:<br />

Chronology, palaeobotany and magnetostratigraphy <strong>of</strong> the Rajmahal volcano-sedimentary<br />

succession<br />

Compiled the palae<strong>of</strong>loral records recovered from<br />

the Intertrappean beds <strong>of</strong> the Rajmahal Basin. The<br />

palyn<strong>of</strong>lora from the bed at Moti Jhama yielded long<br />

ranging taxa (Auracariacites, Callialsporites,<br />

Podocarpidites) occur from Jurassic to Early<br />

Cretaceous. No significant age marker taxa could be<br />

observed. Hence precise age could not be defined.<br />

Archana Tripathi (superannuated w.e.f. 31.07.2009) & B.N.<br />

Jana (superannuated w.e.f. 30.06.2009) [& Kanchan Pande<br />

(IITB) & G.V.R. Prasad (Jammu)]<br />

Project 14.4: Neyveli lignites: Biostratigraphy and palaeoecology<br />

Analysis <strong>of</strong> samples from Neyveli lignite mine,<br />

Tamil Nadu revealed a diversified assemblage <strong>of</strong> algal<br />

and fungal remains, pteridophytic spores and angiosperm<br />

pollen. Significant palynotaxa in the assemblage are:<br />

Proxapertites,<br />

Monocolpopollenites,<br />

Acanthotricolpites, Retipollenites, Tricolpites,<br />

Marginipollis,<br />

Pelliceroipollis,<br />

Dermatobrevicolporites, Lanagiopollis,<br />

Tribrevicolporites, Retitrescolpites, Meliapollis,<br />

Palaeosantalaceaepites,<br />

Rhoipites,<br />

Dipterocarpuspollenites, Cruciferoipollenites,<br />

Verrutricolpites, Ctenolophonidites, Jacobipollenites<br />

and Clavaperiporites. Based on the present day<br />

distribution <strong>of</strong> the families represented (Schizaeaceae,<br />

Cyatheaceae, Gleicheniaceae, Arecaceae, Meliaceae,<br />

Rhizophoraceae, Bombacaceae, Araliaceae and<br />

Caesalpiniaceae), a tropical climate with plenty <strong>of</strong> rainfall<br />

has been inferred during the sedimentation <strong>of</strong> Neyveli<br />

lignite deposits. A good representation <strong>of</strong> tropical rain<br />

forest elements belonging to Alangiaceae and<br />

Ctenolophonaceae with good number <strong>of</strong> pteridophytic<br />

spores indicates tropical climate with plenty <strong>of</strong> rainfall.<br />

The environment <strong>of</strong> deposition has been deduced as<br />

coastal, ranging from back-mangrove to mangrove with<br />

a short transgressive phase before the deposition <strong>of</strong> lignite.<br />

Rahul Garg (superannuated w.e.f. 30.11.2010) &<br />

M.R. Rao & Poonam Verma [& Ashok <strong>Sahni</strong> (Chandigarh) &<br />

R. Nagendra (Anna Univ, Chennai)]<br />

www.bsip.res.in<br />

33

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