1996-97 - Birbal Sahni Institute of Palaeobotany
1996-97 - Birbal Sahni Institute of Palaeobotany 1996-97 - Birbal Sahni Institute of Palaeobotany
BSIP Fifty six samples from Umrangso section of Kopili Formation were studied. Only three samples yielded pollen and spores which were assigned to : Striatriletes, Dellsiverllpollenites, Polypodiaceaesporites, MOllolites, Todisporites major, T minor, Diporodicellaesporites and few fungal bodies. A draft manuscript entitled "Palynology of the Kopili Formation (Upper Eocene) in the type area, Khorungma, Assam, India" was finalized. Visited North-Central Hill District, Assam for the collection of samples for palynological studies. Programme 6.10 : Biodiagenesis of Tertiary coals from Nagaland and kerogen study from Tertiary sequence of Assam-Arakan Basin B.K. Misra Fluorescence microscopic investigation on 25 coal samples from four coal seams of Changki Valley Coalfield, Nagaland was carried out. The coals contain high to very high proportions of fluorescing macerals. Of the total fluorescing macerals, perhydrous vitrinite constitutes up to 50 per cent. The liptinite macerals (up to >30%), in order of decreasing abundance, are liptodetrinite, resinite, cutinite, suberinite, sporinite and exsudatinite, besides 'minor amount of alginite (BotryococcllS) and f1uorinite. In petrographic composition, under fluorescence mode, these coals are similar to the other Late Palaeocene and Oligocene coals from Meghalaya, Assam and Arunachal Pradesh. Programme 6.11: Palynostratigraphy and correlation of Tertiary sediments of Meghalaya R.K. Saxena, S.K.M. Tripathi & Vandana Prasad Recovered a rich palynofloral assemblage consisting of dinoflagellate cysts, fungal remains, pteridophytic spores and angiospermic pollen from the Tura Formation (Palaeocene-Eocene) exposed along Tura-Dalu Road Section in West Garo Hills District. Dinoflagellate cysts are represented by Operculodinium spp. and Homotryblium spp. Fungal remains are constituted by spores and fruiting bodies. Angiospermous pollen are the dominant constituents of the assemblage. The palynoflora indicates a tropicalsubtropical climate sustaining wet evergreen forest in the vicinity of the area. Deposition of the studied sequence is inferred to have taken place under shallow marine conditions as the assemblage shows presence of dinocysts. The palynofloral assemblage exhibits a similarity with known Palaeocene-Eocene assemblages recorded from the Cherra and Therria Formations of Meghalaya, Mikir Formation of Assam and Matanomadh Formation of Kutch, Gujarat. Rich palynofloral assemblage has also been recorded from the Rewak Formation exposed along Siju-Baghmara Road in South Garo Hills District. The assemblage consists of dinoflagellate cysts, fungal remains, pteridophytic spores and angiospermic 411
1996-97 pollen. The fungal remains are represented by Illapertisporites, Lirasporis, Parmathyrites and Phragmothyrites. Rich representation of pollen belonging to Alangiaceae, Bombacaceae and Arecaceae suggests existence of thick evergreen forests in the vicinity of the area of deposition. Occurrence of mangrove element, viz., Paleosalltalaceaepites and dinocysts suggests near shore environment of deposition. Abundance of pteridophytic spores and fungal remains indicates a warm-humid (tropicalsubtropical) climate with heavy rainfall. Palynological study of the Tura Formation exposed in Nongwal Bibra area in East Garo Hills District was finalized and submitted for publication. R.K. Saxena & M.R. Rao Samples from the Oligocene-Lower Miocene sediments exposed along Tura Dalu Road Section in West Garo Hills District were investigated. Study of palynoflora recovered from the Kherapara Formation (Oligocene) of this section has been completed. The assemblage is dominated by pteridophytic spores followed by angiospermous and gymnospermous pollen. Dinoflagellate cysts and fungal remains are also present. The assemblage also cqntains reworked Permian and Cretaceous palynofossils, e.g., Parasaccites, Rouseisporites, Callialasporites, Plicatipollellites and Striatopodocarpites. Present day distribution of the families represented in the assemblage, dominance of pteridophytic spores and presence of fungal remains (Phragmothyrites, Trichothyrites, Parmathyrites, Multicellaesporites, etc.) indicate tropical-subtropical (warm and humid) climate. Representation of dinoflagellate cysts (Achomosphaera and Spinijerites) mangrove and back-mangrove elements (Paleosantalaceaepites and Malvacearumpollis) and coastal plants (Spinizonocolpites) suggests a near-shore environment of deposition. Palynofloral study of the Boldamgiri Formation exposed along Adugiri Purakhasia Road near Boldamgiri in West Garo Hills District was finalized for publication. PROJECT 7 Programme' 7.1 RECONSTRUCTION OF QUATERNARY VEGETATIONAL PATTERNS History of vegetation and climate in tropical montane forests in south India H.P. Gupta, S.K. Bera & Anjum Farooqui Pollen analysed 5 modern surface samples collected from Konalur and Kuntan Shola, Palni Hills. The vegetational composition has enabled to understand the interplay of pollen/spores and also to interpret the face value of the pollen diagram to be constructed from the area. Pollen analysed two sediment profiles, one each from Konalur swamp (2.0 m) and Kuntan Shola (1.5 m) dating back to 4000 yrs BP and 1000 yrs BP, 41
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BSIP<br />
Fifty six samples from Umrangso section <strong>of</strong> Kopili Formation were studied.<br />
Only three samples yielded pollen and spores which were assigned to : Striatriletes,<br />
Dellsiverllpollenites, Polypodiaceaesporites, MOllolites, Todisporites major, T minor,<br />
Diporodicellaesporites and few fungal bodies.<br />
A draft manuscript entitled "Palynology <strong>of</strong> the Kopili Formation (Upper Eocene)<br />
in the type area, Khorungma, Assam, India" was finalized.<br />
Visited North-Central Hill District, Assam for the collection <strong>of</strong> samples for<br />
palynological studies.<br />
Programme 6.10 :<br />
Biodiagenesis <strong>of</strong> Tertiary coals from Nagaland and kerogen<br />
study from Tertiary sequence <strong>of</strong> Assam-Arakan<br />
Basin<br />
B.K.<br />
Misra<br />
Fluorescence microscopic investigation on 25 coal samples from four coal seams<br />
<strong>of</strong> Changki Valley Coalfield, Nagaland was carried out. The coals contain high to very<br />
high proportions <strong>of</strong> fluorescing macerals. Of the total fluorescing macerals, perhydrous<br />
vitrinite constitutes up to 50 per cent. The liptinite macerals (up to >30%), in order <strong>of</strong><br />
decreasing abundance, are liptodetrinite, resinite, cutinite, suberinite, sporinite and<br />
exsudatinite, besides 'minor amount <strong>of</strong> alginite (BotryococcllS) and f1uorinite. In<br />
petrographic composition, under fluorescence mode, these coals are similar to the other<br />
Late Palaeocene and Oligocene coals from Meghalaya, Assam and Arunachal Pradesh.<br />
Programme 6.11: Palynostratigraphy and correlation <strong>of</strong> Tertiary sediments<br />
<strong>of</strong> Meghalaya<br />
R.K. Saxena, S.K.M. Tripathi & Vandana Prasad<br />
Recovered a rich palyn<strong>of</strong>loral assemblage consisting <strong>of</strong> din<strong>of</strong>lagellate cysts,<br />
fungal remains, pteridophytic spores and angiospermic pollen from the Tura Formation<br />
(Palaeocene-Eocene) exposed along Tura-Dalu Road Section in West Garo Hills District.<br />
Din<strong>of</strong>lagellate cysts are represented by Operculodinium spp. and Homotryblium spp.<br />
Fungal remains are constituted by spores and fruiting bodies. Angiospermous pollen<br />
are the dominant constituents <strong>of</strong> the assemblage. The palyn<strong>of</strong>lora indicates a tropicalsubtropical<br />
climate sustaining wet evergreen forest in the vicinity <strong>of</strong> the area. Deposition<br />
<strong>of</strong> the studied sequence is inferred to have taken place under shallow marine conditions<br />
as the assemblage shows presence <strong>of</strong> dinocysts. The palyn<strong>of</strong>loral assemblage exhibits<br />
a similarity with known Palaeocene-Eocene assemblages recorded from the Cherra<br />
and Therria Formations <strong>of</strong> Meghalaya, Mikir Formation <strong>of</strong> Assam and Matanomadh<br />
Formation <strong>of</strong> Kutch, Gujarat.<br />
Rich palyn<strong>of</strong>loral assemblage has also been recorded from the Rewak Formation<br />
exposed along Siju-Baghmara Road in South Garo Hills District. The assemblage<br />
consists <strong>of</strong> din<strong>of</strong>lagellate cysts, fungal remains, pteridophytic spores and angiospermic<br />
411