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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<strong>1996</strong>-<strong>97</strong><br />
pollen. The fungal remains are represented by Illapertisporites, Lirasporis,<br />
Parmathyrites and Phragmothyrites. Rich representation <strong>of</strong> pollen belonging to<br />
Alangiaceae, Bombacaceae and Arecaceae suggests existence <strong>of</strong> thick evergreen forests<br />
in the vicinity <strong>of</strong> the area <strong>of</strong> deposition. Occurrence <strong>of</strong> mangrove element, viz.,<br />
Paleosalltalaceaepites and dinocysts suggests near shore environment <strong>of</strong> deposition.<br />
Abundance <strong>of</strong> pteridophytic spores and fungal remains indicates a warm-humid (tropicalsubtropical)<br />
climate with heavy rainfall.<br />
Palynological study <strong>of</strong> the Tura Formation exposed in Nongwal Bibra area in<br />
East Garo Hills District was finalized and submitted for publication.<br />
R.K. Saxena & M.R. Rao<br />
Samples from the Oligocene-Lower Miocene sediments exposed along Tura<br />
Dalu Road Section in West Garo Hills District were investigated. Study <strong>of</strong> palyn<strong>of</strong>lora<br />
recovered from the Kherapara Formation (Oligocene) <strong>of</strong> this section has been completed.<br />
The assemblage is dominated by pteridophytic spores followed by angiospermous and<br />
gymnospermous pollen. Din<strong>of</strong>lagellate cysts and fungal remains are also present. The<br />
assemblage also cqntains reworked Permian and Cretaceous palyn<strong>of</strong>ossils, e.g.,<br />
Parasaccites, Rouseisporites, Callialasporites, Plicatipollellites and<br />
Striatopodocarpites. Present day distribution <strong>of</strong> the families represented in the<br />
assemblage, dominance <strong>of</strong> pteridophytic spores and presence <strong>of</strong> fungal remains<br />
(Phragmothyrites, Trichothyrites, Parmathyrites, Multicellaesporites, etc.) indicate<br />
tropical-subtropical (warm and humid) climate. Representation <strong>of</strong> din<strong>of</strong>lagellate cysts<br />
(Achomosphaera and Spinijerites) mangrove and back-mangrove elements<br />
(Paleosantalaceaepites and Malvacearumpollis) and coastal plants (Spinizonocolpites)<br />
suggests a near-shore environment <strong>of</strong> deposition.<br />
Palyn<strong>of</strong>loral study <strong>of</strong> the Boldamgiri Formation exposed along Adugiri<br />
Purakhasia Road near Boldamgiri in West Garo Hills District was finalized for<br />
publication.<br />
PROJECT 7<br />
Programme' 7.1<br />
RECONSTRUCTION OF QUATERNARY VEGETATIONAL<br />
PATTERNS<br />
History <strong>of</strong> vegetation and climate in tropical montane<br />
forests in south India<br />
H.P. Gupta, S.K. Bera & Anjum Farooqui<br />
Pollen analysed 5 modern surface samples collected from Konalur and Kuntan<br />
Shola, Palni Hills. The vegetational composition has enabled to understand the interplay<br />
<strong>of</strong> pollen/spores and also to interpret the face value <strong>of</strong> the pollen diagram to be<br />
constructed from the area. Pollen analysed two sediment pr<strong>of</strong>iles, one each from Konalur<br />
swamp (2.0 m) and Kuntan Shola (1.5 m) dating back to 4000 yrs BP and 1000 yrs BP,<br />
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