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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 />

der 10 recognise Iheir ecological imporlance and 10trace evolUlionary<br />

lineage<br />

To deduce palaeoclimme and depositional environmenl prevalem<br />

al the time <strong>of</strong> deposition<br />

Palyn<strong>of</strong>ossils from rock samples collected along the road sections <strong>of</strong> Will iam Nagar<br />

- Nongwalbibra were studied. The palynoassemblage includes fungi (5%) and pteridophytic<br />

spores (30%), while among the angiosperms, monocots form 20 per cent and the dicottaxa<br />

are represented by 40 per cent <strong>of</strong> the assemblage. Occurrence <strong>of</strong> Laricoidites is indicative <strong>of</strong><br />

the sediments being younger in age than lower part <strong>of</strong> Palaeogene and is comparable to the<br />

assemblage recorded from the top seam in Rekmangiri area. The important palynotaxa<br />

recorded from the sediments comprise Lycopodiumsporites speciosus, Cyathidiles minor,<br />

Diclyophyllidites dulcis, Dandoliaspora telonala, D. dilma, Matanomadhiasulciles maximus,<br />

Droseridites major, Kielmeyerapolleniles syncolporatus, Relitribrevicolporites rubra,<br />

Tricolpites sp., Psilastephanocolpites psilmus, Margocolporites sallllii, Palmidiles plicatus,<br />

Spinizonocolpites echinalUs, Proxapertiles operculmus, Laricoidites magnus, etc. For the<br />

detailed morphological studies SEM examination was also calTied oul.<br />

K. Ambwani<br />

Programme 6.4<br />

Palynological investigation <strong>of</strong> the Tertiary sediments <strong>of</strong><br />

Jaintia and Cachar Hills<br />

Objeclive<br />

To study morphotaxonomy<br />

and affinity <strong>of</strong> palyn<strong>of</strong>ossils<br />

To selecI ecologically and slratigraphically important<br />

palynolaxafor biostraligraphic zonmion, correlation and dating<br />

and environment <strong>of</strong> deposilion <strong>of</strong> sedi­<br />

To infer palaeoclimale<br />

ments<br />

Disang assemblage recorded from Silchar-Haflong Road section was compared<br />

with the Palaeocene-Eocene llora <strong>of</strong> Meghalaya, Bengal Basin and Kutch Basin. Though<br />

few laxa, like Palmidiles, Spinizonocolpiles, Slrialriletes, Tricolporopililes and PellicieroipoUis<br />

are common between the assemblages. Disang assemblage is poor in val'iety and<br />

number. Nevertheless, the assemblage is identical with Disang assemblage <strong>of</strong> Upper Assam.<br />

J.P. MandaI<br />

Programme 6.5<br />

Objective<br />

Palynological studies <strong>of</strong> Khasi (Late Cretaceous) and Garo<br />

(Late Tertiary) groups in the South-Shillong front,<br />

Meghalaya<br />

To establish palynological zonmion for correlation and daling<br />

<strong>of</strong> each unit <strong>of</strong> rocks<br />

To infer palaeoclimale and depositional environment<br />

109

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