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Annual Report 2011-2012 - Birbal Sahni Institute of Palaeobotany

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EBIRBAL SAHNI INSTITUT<br />

1946<br />

OF PALAEOBOTANY<br />

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

deposits, indicating that the forest was dominant with<br />

podocarpaceous elements, whereas Pteridophytes were<br />

in paucity.<br />

The morphotaxonomic study <strong>of</strong> plant fossils<br />

collected from various localities, viz. Chandia, Patparha,<br />

Barambaba, Jhala, Praghua and Khareri have been<br />

carried out. The plant fossils are well preserved in<br />

blackish grey–pinkish white shales, embody number <strong>of</strong><br />

species <strong>of</strong> Elatocladus, Brachyphyllum, Pagiophyllum,<br />

Araucarites, Podozamites, Todites, Weichselia,<br />

Gleichenia and Phlebopteris. Branched or unbranched<br />

twigs <strong>of</strong> Gleichenia are commonly found in these<br />

sedimentary deposits. The floral assemblage is dominated<br />

by conifers and pteridophytes. While comparing and<br />

correlating with various Early Cretaceous palae<strong>of</strong>loral<br />

assemblages <strong>of</strong> India this has been observed that the<br />

palae<strong>of</strong>lora is coeval with the floral assemblage <strong>of</strong><br />

Dhrangadra and Himmatnagar formations, where too the<br />

flora is dominated by conifers and pteridophytes. The<br />

present floral assemblage resembles to some extent with<br />

Gangapur floral assemblage <strong>of</strong> Andhra Pradesh, as both<br />

are rich in conifers and pteridophytes, but can easily be<br />

differentiated by the broad-leaved bennettitalean remains<br />

which are prevalent in quite good number in Gangapur<br />

Formation. Studied palae<strong>of</strong>loral assemblage <strong>of</strong> South<br />

Rewa Basin shows close affinity with Floristic<br />

assemblage zone-10 Sukh-Dev (1987), which is also<br />

characterized by occurrence <strong>of</strong> Weichselia, Onychiopsis,<br />

proliferation <strong>of</strong> Gleichenia, Araucaria, Allocladus,<br />

Brachyphyllum and Pagiophyllum and lack <strong>of</strong><br />

cycadophytes and pteridosperms.<br />

Neeru Prakash<br />

Project 2.5:<br />

Palae<strong>of</strong>loristical analysis <strong>of</strong> Mesozoic sedimentary succession <strong>of</strong> western India<br />

Compiled the megafloral assemblage, consisting <strong>of</strong><br />

fossil algal mats, Thallites, Coniopteris, Onychiopsis,<br />

Brachyphyllum, etc., recovered from the Isoetites-rich<br />

locality near Than (Gujarat).<br />

B.N. Jana (superannuated w.e.f. 30.06.2009)<br />

Project 2.6:<br />

Integrated palaeobiology <strong>of</strong> East Coast Cretaceous<br />

Xylotomical studies on the petrified woods <strong>of</strong> the<br />

Krishna-Pranhita-Godavari basins reveal variations within<br />

the wood structure <strong>of</strong> Cretaceous flora. New finds <strong>of</strong><br />

Podocarpean and Araucarian woods along with<br />

Ginkgolean fossil leaves demonstrate their luxuriant<br />

growth. In addition, undertook field excursion to Pranhita-<br />

Krishna-Godavari basins and collected fossil specimens<br />

and sediment samples.<br />

A. Rajanikanth<br />

Project 2.7:<br />

Investigation <strong>of</strong> carbonified/ fusainised plant mes<strong>of</strong>ossils recovered through bulk<br />

maceration <strong>of</strong> Late Triassic and Tertiary sediments <strong>of</strong> India and comparative studies<br />

on selected modern taxa<br />

Cuticle isolated from plant compressions on hand<br />

specimens collected from the Nidhpuri plant-bearing bed<br />

has been described and compiled.<br />

Usha Bajpai (superannuated w.e.f. 31.05.2010)<br />

Gondwana Palynology Group<br />

Project 3.1:<br />

Palynostratigraphy and evolution <strong>of</strong> palyn<strong>of</strong>lora through the Palaeozoic and Mesozoic<br />

sequence in Rajmahal Basin<br />

Compiled the palynological data generated from<br />

coal-bearing horizon encountered in 10 bore-holes <strong>of</strong> the<br />

Rajmahal Basin. The study evidenced definite Late<br />

Permian age for part <strong>of</strong> coal-bearing strata in the basin,<br />

along with the coal seams <strong>of</strong> Early Permian Barakar<br />

Formation.<br />

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

12<br />

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