1996-97 - Birbal Sahni Institute of Palaeobotany
1996-97 - Birbal Sahni Institute of Palaeobotany
1996-97 - Birbal Sahni Institute of Palaeobotany
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BSIP<br />
Samampollenites, Brachysaccus, Callialasporites and equates with the Late Triassic<br />
palyn<strong>of</strong>lora.<br />
Archana Tripathi & K.L. Meena<br />
The bore cores <strong>of</strong> Bore hole TCP-39, TCP-41 and TNA-7 from Talcher Coalfield<br />
were palynologically studied. The qualitative assessment <strong>of</strong> spore-pollen in TCP-39<br />
(depth 381.70 m) and TCP-41 (470.25 m) shows palynocomposition typical <strong>of</strong> Late<br />
Permian palyn<strong>of</strong>lora having dominance <strong>of</strong> striate bisaccates and Weylandites,<br />
Cu"ulapolieniles, Kamthisacciles, Densipolieniles spp. and stray occurrence <strong>of</strong><br />
Arcualipolieniles. In the bore-hole TNA-7 the samples investigated at 27.20 to 87.25<br />
m shows the composition similar to that from TCP-39 and TCP-41 in addition to<br />
Striatosporites, Quadrisporites and Leiosphaeridia.<br />
K.L.<br />
Meena<br />
The palynodata <strong>of</strong> bore-hole IBSH-6 from Ib-River Coalfield, Orissa was<br />
studied. The age <strong>of</strong> bore core sediments compares to Raniganj. Processing <strong>of</strong> samples<br />
from bore-holes IBT-2, IBT-3 and IBT-6 for palynodating have been completed.<br />
Visited Geological Survey <strong>of</strong> India, Calcutta for scientific discussion and<br />
consultation <strong>of</strong> library. Visited Sohagpur Coalfield (M.P.) and collected the bore core<br />
as well as outcrop samples for palynological analysis.<br />
Programme 2.5 :<br />
Morphological study <strong>of</strong> plant megafossils from Raniganj,<br />
Karanpura and RajmahaI Coalfields and ultrastructure<br />
<strong>of</strong> megaspores, cuticles, seeds and in situ pollen/spores<br />
H.K. Maheshwari & Usha Bajpai<br />
Further investigated the ultrastructure <strong>of</strong> the cuticular membrane recovered from<br />
healthy and fungi-infected leaves <strong>of</strong> Thinnfeldia indica Feistmantel, in order to<br />
understand the nature <strong>of</strong> changes brought about in the cuticular membrane by the fungi<br />
and how cuticle is lost from the compression fossils. In general, the structural<br />
configuration <strong>of</strong> both cuticular membranes is similar. In the infected leaf, precursors<br />
<strong>of</strong> cutin accretions are irregularly present at the sub-cuticular surface. These accretions<br />
are interpreted as possible result <strong>of</strong> breakdown <strong>of</strong> cutin due to the secretion <strong>of</strong> an<br />
enzyme by the fungi infecting the leaf. The study on the cuticular membrane <strong>of</strong> infected<br />
leaf <strong>of</strong> Thinnfeldia indica under Transmission Electron Microscope shows various<br />
stages <strong>of</strong> degradation <strong>of</strong> amorphous matrix by the release <strong>of</strong> enzyme (cutinase). The<br />
upper portion <strong>of</strong> cuticular membrane is completely intact. It thus seems that fungi,<br />
besides edaphic factors, do playa role in the break-down <strong>of</strong> the cutin and thus constrain<br />
the preservation <strong>of</strong> the cuticular membranes.<br />
Transmission electron micrographs <strong>of</strong> the cuticular membrane <strong>of</strong> Dicroidium<br />
sp., a Late Triassic leaf collected from the Tiki Formation <strong>of</strong> Madhya Pradesh, exhibit<br />
a 'herring bone' structure which possibly is an indicator <strong>of</strong> environmental stress. On<br />
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