1994-95 - Birbal Sahni Institute of Palaeobotany
1994-95 - Birbal Sahni Institute of Palaeobotany
1994-95 - Birbal Sahni Institute of Palaeobotany
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
<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