1994-95 - Birbal Sahni Institute of Palaeobotany
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