1995-96 - Birbal Sahni Institute of Palaeobotany
1995-96 - Birbal Sahni Institute of Palaeobotany
1995-96 - Birbal Sahni Institute of Palaeobotany
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<strong>1995</strong>-<strong>96</strong><br />
Major Achievements<br />
and Activities <strong>of</strong> the <strong>Institute</strong><br />
Research<br />
The <strong>Birbal</strong> <strong>Sahni</strong> <strong>Institute</strong> has commitment to develop scientific knowledge<br />
and expertise in the field <strong>of</strong> <strong>Palaeobotany</strong> and related disciplines. An integrated<br />
and multidisciplinary approach is adopted to complete thc targets <strong>of</strong> different<br />
programmes undertaken for fulfilling the objectives <strong>of</strong> the <strong>Institute</strong>.<br />
During the year <strong>1995</strong>-<strong>96</strong>, some <strong>of</strong> the salient results achieved at the Institu<br />
te are as follows<br />
Early Life<br />
The continued efforts to understand the early life during Precambrian and<br />
Cambrian time have brought significant results. The biota from argillaceous sediments<br />
<strong>of</strong> Rohtas Formation in Bihar, Uttar Pradesh and Madhya Pradesh has<br />
shown presence <strong>of</strong> Chlorophyta even before 1000 Ma years. Maiden record <strong>of</strong><br />
shelly fauna from Sahabad Limestone Formation has been made from Bhima<br />
Basin. From the present state <strong>of</strong> knowledge on organic remains from Bhima Basin<br />
it is concluded that these sediments belong to latest part <strong>of</strong> terminal Proterozoic.<br />
Well developed stromatolites were recorded from the Iron Ore Group representing<br />
Kashia Formation from Barbil-Noamundi area. The inferred environment<br />
<strong>of</strong> deposition for the Kashia Formation is intertidal to subtidal zone. The sandstone<br />
dykes were recorded from Kashia Formation. This is the first record <strong>of</strong> sandstone<br />
dyke from Archaean <strong>of</strong> India.<br />
Gondwana Sequence and associated coals<br />
Studies <strong>of</strong> plant fossil assemblages from Auranga, Jharia, Karanpura and<br />
Hura coalfields and Hinjrida Ghati (Orissa) have been carried out on Permian<br />
(250-280 million years old) sediments. For the first time the male fructification<br />
Nesowalesia is reported from India which is known only from Australia. The assemblage<br />
indicates that very much disturbed conditions prevailed in the<br />
preservational and depositional environment <strong>of</strong> Karanpura and Hura coalfields.<br />
The megafloral assemblage <strong>of</strong> Mesozoic deposits <strong>of</strong> Murlipahar, Balidih<br />
and Sitalpura localities <strong>of</strong> Rajmahal Basin and Gangapur Formation (Pranhita<br />
Godavari Basin) has been analysed. Phyllopteroides laevis-an index Neocomian<br />
species <strong>of</strong> Eastern Australia has been- recorded from Murlipahar <strong>of</strong> RajmahaJ<br />
Basin.<br />
The palynodating apd correlation <strong>of</strong> coal-bearing strata is an important<br />
aspect <strong>of</strong> research at the <strong>Institute</strong>. Palynological investigations are being carried<br />
out on the bore-core materials <strong>of</strong> the drillings made by G.S.I., M.E.C.L. and Singreni<br />
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