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 />
Lunalisporiles alongwith GUllalisporiles, Lundbladispora and acritarchs at 307.30 m depth.<br />
The composition <strong>of</strong> assemblage from 334.00 m depth shows presence <strong>of</strong> distinct Early<br />
Triassic assemblage.<br />
Archana Tripathi<br />
Samples from bore-holes TP-9 and TP-IO dtilled by MECL have been analysed for<br />
palynodating. The sandy shales and sandstones representing the Supra-Barakars have yielded<br />
Lundbladispora. Lunalisporiles. Playfordiaspora representing Early Triassic assemblage<br />
at 280.50 to 259.50 m (in TP 9) and 352.80 m (in TP 10) depths.<br />
Archana Tripathi & K.L. Meena<br />
The palynological studies <strong>of</strong> samples <strong>of</strong> bore-hole RT-12 from Mand-Raigarh<br />
Coallleid were carried out, in which Karharbari palynoassemblage encountered between<br />
163.00 m to 316.00 m. Barakarpalynoassemblage between 69.15 to 152.00 m and Raniganj<br />
assemblage was found at 35.00 m depths. The genus Parasacciles shows dominance in<br />
Karharbari assemblage. Scheuringipolleniles in Barakar assemblage and the Raniganj assemblage<br />
is characterized by the presence <strong>of</strong> striate and non-striate genera such as Faunipollenites.<br />
Crescentipolleniles. Slrialopodocarpiles and Scheuringipolleniles along with<br />
several trilete genera such as Micr<strong>of</strong>oveolalispora. Microbaculispora, etc.<br />
B.N. Jana<br />
Proloeusaccites gen. nov. from Pali Formation, Sohagpur Coalfield showing character state <strong>of</strong> par·<br />
tially filled saccus ( x 850 ).<br />
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