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 5.2<br />
comparison with Gondwana, Cathaysiall and Allgaran elements<br />
to trace their origin<br />
Several good specimens orthe genus Kall'a~ioph)'I//IIn coli eelcd Ii'omthe DunpaUlri<br />
Member <strong>of</strong> Mama! Formation were sorted, cleaned and photographed. It has been observed<br />
that not a single leafis preserved in a flat position, almost all arc folded. The leaves bave an<br />
incipient parallel venation. Cellulose acelale pulls were made from these specimens for the<br />
recovery <strong>of</strong> cuticles. No cuticle was recovered but the macerate did contain a few monosaccate,<br />
disaccate-nonstriate and disaccate-slriale pollen. These pollen are identifiable up 10generic<br />
level. The genera that have been identified include Cordaililla, POlonieisporites,<br />
IJensipolleniles, Slriomollosacciles, Schellrillgipolleniles, Cedripiles, Prolohaplo~ypilllls,<br />
Slrialiles, Lahiriles, Gondwanipol/elliles, Rhizomaspora and Schizopol/is.<br />
On the basis <strong>of</strong> composilion <strong>of</strong> the megaflora, the Mamal Formation has generally<br />
been equated WiUlthe Karharbari 'Formalion' <strong>of</strong> Gondwana Supergroup <strong>of</strong> the peninsula.<br />
The composilion <strong>of</strong> palyn<strong>of</strong>lora from the I)unpatbri Member, particularly the presence <strong>of</strong><br />
the genus Schi~opol/is suggests that this member may be equivalenl <strong>of</strong> the basal part <strong>of</strong> the<br />
Barakar Formalion. Except for the presence <strong>of</strong> Ulegenus Cordailina, the palyn<strong>of</strong>lora known<br />
so far is Iypically Gondwanan in composition.<br />
H.K. Maheshwati,<br />
Usha l3ajpai [& H.M. Kapoor]<br />
Palynotloras <strong>of</strong> the Tethyan sediments <strong>of</strong> the Himalaya,<br />
their provenance and regional relationship<br />
OlijeClil'e<br />
To search palyn<strong>of</strong>ossils ill the well rla/ed sequence <strong>of</strong> Palaeozoic<br />
and Mesozoic sedimeills <strong>of</strong> Nil; (Spiri), Malia Johar (K(lmaoll)<br />
and Kashmir (Gury(ll ravine and PahalWIOIl)<br />
Qualitalive assessment <strong>of</strong> tbe palynoassemblages recovered Ii'om eight secLions in<br />
Niti area, has been completed. They compare with the Late Permian and Eat'ly Triassic<br />
palynoassemblages <strong>of</strong> peninsular India and establishes correlation between the palynoassemblages<br />
from marine and continental sequences at Permian-Triassic transiLion.<br />
R.S. Tiwat'i, Vijaya l& VD. Mamgain & R.S. Misra, GSI)<br />
Qualitative assessment <strong>of</strong> the spore-pollen taxa recovered from tbe five well-dated<br />
sections in Spiti at'ea has been done. For the lirsl time, l3at'akar. Upper Ranigan) and Lower<br />
Panchel equivalent miolloras at'e identified in these sections. which exhibit close similat·ity<br />
wilh the known palynoassemblages from pellinsulat· India.<br />
Programme 5.3<br />
R.S. Tiwari. Vijaya. Ram-Awatar [& T Singh. WIHG]<br />
Palynostratigraphic studies, evaluation <strong>of</strong> rank and properties<br />
orcoal and associated sediments in eastern Himalaya<br />
Ohjective<br />
To correlate Ihe palyn<strong>of</strong>lora wilh petrography <strong>of</strong> coal and to<br />
compare with the known palyn<strong>of</strong>loras from Ihe peninsular<br />
Gondwana<br />
103