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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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