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Annual Report 2011-2012 - Birbal Sahni Institute of Palaeobotany

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EBIRBAL SAHNI INSTITUT<br />

<strong>Annual</strong> <strong>Report</strong> <strong>2011</strong>-<strong>2012</strong><br />

1946<br />

OF PALAEOBOTANY<br />

Project 5.2:<br />

Palynological investigation, facies analysis and palaeoenvironmental interpretations <strong>of</strong><br />

Palaeocene-Eocene sediments in Rajasthan Basin<br />

Palyn<strong>of</strong>ossils from Matasukh lignite mine, Nagaur<br />

district representing Marh Formation have been studied.<br />

The sequence, constituted by carbonaceous shale, siltstone<br />

and lignite, yielded a rich palynological assemblage.<br />

Quantitatively as well as qualitatively, angiosperm pollen<br />

dominates over the pteridophytic spores and fungal<br />

remains. Significant palynotaxa in the assemblage are<br />

assigned different species <strong>of</strong> Lygodiumsporites,<br />

Todisporites, Lycopodiumsporites, Dandotiaspora,<br />

Arecipites, Palmidites, Longapertites, Proxapertites,<br />

Matanomadhiasulcites, Pseudonyssapollenites,<br />

Dermatobrevicolporites, Sastripollenites,<br />

Ratariacolporites and Meliapollis. Based on the<br />

Spini prominatus<br />

Dipterocapus<br />

stratigraphical record <strong>of</strong> palyn<strong>of</strong>ossils in Indian<br />

Palaeogene strata, the investigated sequence is dated as<br />

early Eocene.<br />

S.K.M. Tripathi & Hukam Singh<br />

Project 5.3:<br />

High resolution biostratigraphy <strong>of</strong> Cretaceous-Tertiary sedimentary sections <strong>of</strong> Cauvery<br />

Basin<br />

A manuscript entitled ‘Palynological evidence for<br />

dating <strong>of</strong> Grey Shale, Dalmiapuram Formation, Cauvery<br />

Basin, Tamil Nadu’ has been prepared. Additionally, a<br />

field visit to Ariyalur and adjoining areas, Tamil Nadu has<br />

been undertaken and collected fresh rock samples from<br />

Grey Shale <strong>of</strong> Dalmiapuram Formation [GVKC and<br />

Kallakudi Mine-II, and Ananadawadi (K/T boundary)]<br />

areas for palynological investigation.<br />

M.R. Rao<br />

Project 5.4:<br />

Palynological studies <strong>of</strong> the Late Cretaceous-Early Palaeocene sediments <strong>of</strong> Central<br />

India and the Khasi Hills <strong>of</strong> Meghalaya, India<br />

Myxomycetaceous fossil spores have been<br />

recovered from the Deccan Intertrappean beds <strong>of</strong> Padwar<br />

(MP). These remains are found in association with the<br />

index palynotaxa <strong>of</strong> Maastrichtian age, viz. Azolla<br />

cretacea, Ariadnaesporites ariadnae, Gabonisporites<br />

vigourouxii and Aquillapollenites bengalensis. The<br />

fossil spores, flagellate swarm cells, zygotes and spores<br />

<strong>of</strong> the Myxomycetes are recovered from the highly<br />

carbonaceous lignitic shales <strong>of</strong> the dry dug out well at<br />

Padwar. The well is more than 9 m deep and the basal<br />

and top parts are composed <strong>of</strong> the traps. There is also a<br />

3 m thick volcanic ash bed in between. The samples are<br />

rich in fungal and pteridophytic spores and angiospermic<br />

pollen, out <strong>of</strong> which the myxomycetaceous forms are<br />

Project 5.5:<br />

studied in detail. The myxomycetaceous spores apparently<br />

resemble some pteridophytic spores in the sub-circular<br />

shape and broad reticulation. However, the absence <strong>of</strong><br />

trilete or monolete mark and its dark brown colour, easily<br />

differentiate them from others. Further, 4 types <strong>of</strong> motile<br />

cells are distinguished on the characters <strong>of</strong> flagella– i)<br />

unicellular cells with a posterior whiplash type <strong>of</strong> flagellum,<br />

ii) uniflagellate cells with an anterior tinsel type <strong>of</strong><br />

flagellum, iii) biflagellate cells with one flagellum <strong>of</strong> tinsel<br />

type and the other whiplash type, and iv) both the flagella<br />

are <strong>of</strong> whiplash type. On the basis <strong>of</strong> detailed<br />

morphological characters, the myxomycetaceous forms<br />

are being constituted into new genera and species.<br />

R.S. Singh<br />

Palyn<strong>of</strong>acies analysis and palyno-cyclicity in Palaeogene-Neogene sediments <strong>of</strong> Upper<br />

Assam and Jaintia Hills, northeast India<br />

Finalized palyn<strong>of</strong>loral and palyn<strong>of</strong>acies analyses <strong>of</strong><br />

188 m thick section <strong>of</strong> Tirap colliery <strong>of</strong> Makum coalfields<br />

(Tikak Parbat Formation, Chattian) in Upper Assam. The<br />

studied section provides important insights into the<br />

composition and distribution <strong>of</strong> plant communities in a late<br />

Oligocene tropical delta (palaeolatitude approximately 18°<br />

N). The lower two thirds <strong>of</strong> this section represent lower<br />

delta plain environments with only a small degree <strong>of</strong><br />

www.bsip.res.in<br />

17

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