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1995-96 - Birbal Sahni Institute of Palaeobotany

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BSIP<br />

Programme 4.3<br />

To carry out stable carbon isotope (C-13) and organic petrographic<br />

studies<br />

To attempt palaeoceanography<br />

modelling<br />

Based on the din<strong>of</strong>lagellate cyst evidence, lower part <strong>of</strong> the Trichinopoly Formation<br />

is dated to be Middle-Upper Turonian in age. A din<strong>of</strong>lagellate cyst biozonation scheme is<br />

proposed. Final plates and charts are prepared and a manuscript is finalised.<br />

Din<strong>of</strong>lagellate cyst, calcareous plankton (foraminifera, nann<strong>of</strong>ossils) and siliceous<br />

plankton (radiolaria) data through Albian-Santonian sequence <strong>of</strong> Cauvery Basin<br />

have been compiled to assess the sequence <strong>of</strong> bioevents having palaeoceanographic implications.<br />

Quantitative analysis <strong>of</strong> various din<strong>of</strong>lagellate cyst groups and palynodebris has<br />

revealed significant palaeoenvironmental signatures.<br />

Stratigraphic frequency distribution <strong>of</strong> Neocomian din<strong>of</strong>lagellate cysts recovered<br />

from subsurface sequence <strong>of</strong> Palar Basin is documented.<br />

K.P. Jain, Rahul Garg & Khowaja-Ateequzarnman<br />

Neogene calcareous nannoplankton palaeoceanography <strong>of</strong><br />

Andaman and Nicobar Islands<br />

Objective To compare Neogene calcareous nannoplankton assemblage<br />

<strong>of</strong> Andaman and Nicobar Islands with that known from nearshore<br />

and high latitude and to select cosmopolitan markers<br />

To integrate calcareous nannoplankton and planktonicforaminiferal<br />

zonations to improve dating resolution<br />

To record palaeoenvironmental events with special reFerence to<br />

Antarctica glaciation event based on plankton assemblage<br />

backed by stable isotope and organic data<br />

Based on data generated during previous years, fresh sampling was done in well<br />

measured sections <strong>of</strong> Car-Nicobar Island, with the aim <strong>of</strong> demarcating MiocenelPliocene<br />

boundary and selecting a suitable section in Sawai Bay area. Several low-latitude marker<br />

species <strong>of</strong> calcareous nann<strong>of</strong>ossils were found to be either missing or displayed diachronous<br />

appearance at MiocenelPliocene transition beds exposed in Sawai Bay region. In this<br />

aspect the vertical distribution <strong>of</strong> dark and birefringent horse-shoe shaped calcareous<br />

nann<strong>of</strong>ossils (ceratoliths) are significant for Indo-Pacific region, demanding more intensive<br />

study and photodocumentation <strong>of</strong> ta;<br />

A draft manuscript "NmUl<strong>of</strong>".·. 'IS from mud-volcanoes <strong>of</strong> Andaman<br />

: global biostratigraphic applicability" was prepared.<br />

Programme 4.4<br />

Objective<br />

Islands, India<br />

S.A. Jafar<br />

Late Cenozoic diatom biostratigraphy <strong>of</strong> Andaman and<br />

Nicobar Islands<br />

To study morphology and taxonomy <strong>of</strong> diatom and silic<strong>of</strong>lagellate<br />

taxa from Late Cenozoic surface and subsurface sections (type<br />

104

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