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Abstract of Palaeobotanist-61(1) - Birbal Sahni Institute of ...

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The <strong>Palaeobotanist</strong> <strong>61</strong>(2012): 131-138<br />

0031-0174/2012 $2.00<br />

A basal Gondwana palyn<strong>of</strong>lora from the glacigene<br />

sediments <strong>of</strong> Tatapani-Ramkola Coalfield, India<br />

RATAN KAR<br />

<strong>Birbal</strong> <strong>Sahni</strong> <strong>Institute</strong> <strong>of</strong> Palaeobotany, 53 University Road, Lucknow 226 007, India.<br />

Corresponding author: ratankar@yahoo.com<br />

(Received 16 January, 2012; revised version accepted 23 February, 2012)<br />

ABSTRACT<br />

Kar R 2012. A basal Gondwana palyn<strong>of</strong>lora from the glacigene sediments <strong>of</strong> Tatapani-Ramkola Coalfield, India.<br />

The <strong>Palaeobotanist</strong> <strong>61</strong>(1): 131-138.<br />

Palynological studies were undertaken on the sediments <strong>of</strong> Talchir Formation exposed along a stream cutting in the<br />

Tatapani-Ramkola Coalfield, Chhattisgarh State, India. The glacigenic nature <strong>of</strong> the Talchir Formation is evident, as<br />

manifested by the presence <strong>of</strong> lithified tillites, varves and rafted boulders. The varve clays have yielded a well preserved<br />

assemblage rich in radial monosaccates. The assemblage is dominated by Plicatipollenites (26-31%) with a sub-dominance<br />

<strong>of</strong> Parasaccites (8-22%). Potonieisporites, Virkkipollenites, Caheniasaccites and <strong>Sahni</strong>tes are the other important<br />

constituents. The recovered palyn<strong>of</strong>lora is characteristic <strong>of</strong> Plicatipollenites-Parasaccites palynoassemblage, which<br />

represents Lower Talchir palynozone and is <strong>of</strong> early Permian age.<br />

Key-words—Gondwana, Palynology, Talchir Formation, Early Permian, Tatapani-Ramkola Coalfield.<br />

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