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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 />

41

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