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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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