1996-97 - Birbal Sahni Institute of Palaeobotany
1996-97 - Birbal Sahni Institute of Palaeobotany
1996-97 - Birbal Sahni Institute of Palaeobotany
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BSIP<br />
•<br />
A new tetrad pollen from Narcdi<br />
Formation. Early Eocene, Kutch.<br />
B.D. Mandaokar<br />
About 40 samples from bore-hole K-15, drilled by Central Ground Water Board<br />
in Tupni area <strong>of</strong> Jamnagar District were studied. A poor palynoassemblage comprising<br />
bisaccate pollen grains (? Podocarpidites) could be recovered, which does not permit<br />
definite age assignment.<br />
Outcrop samples (40) were collected from Bet Shankhodar, Gujarat.<br />
Palynologically all the samples proved barren. except some samples which have yielded<br />
foraminifera and din<strong>of</strong>lagellate cysts.<br />
Visited Dwarka, Sasangir, Jamnagar, Somnath and Harshad in Gujarat to collect<br />
rock samples for palynological studies.<br />
Programme 3.11: Palynological investigation <strong>of</strong> the Tertiary formations <strong>of</strong><br />
Rajasthan (other than Kapurdi area)<br />
K. Ambwani<br />
Samples from bore-hole RGBH-33!l4, drilled near Raneri Village, Bikaner<br />
District yielded rich and varied spores and pollen assemblage. Association <strong>of</strong><br />
Lycopodiumsporites, Proxapertites, Spinizonocolpites, Lakiapollis,<br />
Matanomadhiasulcites as well as Retitribrevicolporites along with Dandotiaspora (D.<br />
dilata) in the assemblage indicates a Late Palaeocene age for the sediments.<br />
A new genus Clavadiporopollenites raneriensis was instituted while studying<br />
the palynoassemblage. The affinities <strong>of</strong> this pollen grain could not be traced out with<br />
the modern counterpart. However, its typical exine morphology with peculiar fingerlike<br />
processes around the pores signifies an important evolutionary trend in the plant<br />
communities during Early Tertiary Period.<br />
Visited Raneri, Gadala and Bethnok localities <strong>of</strong>Bikaner District for collection<br />
<strong>of</strong> Tertiary rock samples.<br />
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