Annual Report 2011-2012 - Birbal Sahni Institute of Palaeobotany
Annual Report 2011-2012 - Birbal Sahni Institute of Palaeobotany
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 />
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