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1994-95 - Birbal Sahni Institute of Palaeobotany

1994-95 - Birbal Sahni Institute of Palaeobotany

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<strong>1994</strong>-<strong>95</strong><br />

Programme 2.15<br />

Palynostratigraphy <strong>of</strong> Gondwana sequence in Tatapani­<br />

Ramkola Coalfield, Madhya Pradesh<br />

Objective<br />

To develop lithostratigraphic<br />

subsurface sequences<br />

set up from various surface and<br />

To reconstmct standard palynological succession, age determination<br />

and correlation with special reference to coal-bearing<br />

horizons<br />

To recognise range <strong>of</strong> stratigraphically significant taxa and<br />

evolutionary trends <strong>of</strong> various palyn<strong>of</strong>loras<br />

To demarcate time boundaries<br />

bow,dQlY<br />

with special reference to PITr<br />

To document phytogeographic and palaeoenvironmelllal events<br />

Quantitative palynological invcstigations <strong>of</strong> bore-holes TRP-6. TRM-l. TRM-2<br />

and TRS-12. have been completed. Bore-hole TRP-6 contains Talchir palynoOora<br />

(Parasaccites-Plicatipollenites assemblage) at the base and is succeeded by Lower Karharbari<br />

palynollora (CallulI/ispora-Jayantisporites assemblage) in the younger part <strong>of</strong> the Qorecore.<br />

Three palynoassemblage zones have been demarcated in bore-hole TRM- I. The<br />

oldest assemblage is represenled by Scheuringipollenites barakarensis assemblage zone<br />

(Lower Barakar) and is succeeded by the dominance <strong>of</strong> striate bisaccate pollen. chieOy<br />

Striatopodocarpites, Hindipollenites, Verticipollenites, Faunipollenites. Striatites. ell'. representing<br />

Upper Barakar. The youngest assemblage is represented by Densipollenites indicus<br />

and Densipollenites invisus in association with striate bisaccate pollen representing Kulli<br />

pal ynozone.<br />

In bore-holes TRM-2 and TRS-12. the palynoassemblages compare with the<br />

Scheuringipollenites barakarensis assemblage zone representing Lower Barakar. The palynological<br />

rep0l1s <strong>of</strong> these bore-holes have been sent to the Coal Wing. Geological Survey<br />

<strong>of</strong> India.<br />

Processing <strong>of</strong> samples collected from surface exposures is continued. Sediments<br />

from Uro Naja have yielded rich Talchir palynoOora dominated by radial monosaccates<br />

(Plicatipollenites-Parasaccites assemblage). Carbonaceous shale and coal samples from<br />

Banki River section have yielded Late Permian (Raniganj) palynoOora. having a dominance<br />

<strong>of</strong> striate bisaeeates.<br />

Suresh C. Srivastava & Ratan Kar<br />

Programme 2.16 Palynological investigation <strong>of</strong> coal-bearing sequence in<br />

Deocha-Pachami area <strong>of</strong> Birbhum District, West Bengal<br />

93

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