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1991-92 - Birbal Sahni Institute of Palaeobotany

1991-92 - Birbal Sahni Institute of Palaeobotany

1991-92 - Birbal Sahni Institute of Palaeobotany

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<strong>1991</strong>-<strong>92</strong>the tree-dominated autochthonous mangrove-mixed angiospermous vegetationgrowing under moderately per-humid tropical climate. The vegetal accumulationtook place in a rheotrophic peat-swamp on. a lower delta plain in a near-shorelagoon. The affect <strong>of</strong> anaerobic 'degradation under alkaline mileau was morepronounced and resulted in pyrite-rich perhydrous coals by the inOuence <strong>of</strong> putrefactioninstead <strong>of</strong> normal humification. Anaerobic alkaline conditions facilitatingsevere biodegradation <strong>of</strong> organic mailer were not only responsible for the formation<strong>of</strong> fine-grained authigenic partings within the seams as well as ro<strong>of</strong> and Ooor<strong>of</strong> the seams but also for the termination <strong>of</strong> the coal seams.B.K.MisraPROJECT 7Programme 7.1,RECONSTRUCTION OF QUATERNARYVEGETATIONAL PATTERNS, History <strong>of</strong> vegetation and climate in tropicalmontane forests in south IndiaObjective ,To build up a complete palyn<strong>of</strong>loral succession <strong>of</strong>the Shola forest / grassland in Annamalai Hills,Palni Hills and Silent ValleyTen surface samples from Bombay Shola, Palni Hills were pollen analysed andrevealed high yield <strong>of</strong> pollen/spores. The common feature <strong>of</strong> this study is that thesamples collected within the forested zone have recorded higher frequencies forarboreal taxa which decline proportionately in the samples investigated fromoutskirt and away from the forest.1\venty five pr<strong>of</strong>ile samples from Bombay Shola were pollen analysed andrecorded preponderance <strong>of</strong> non-arboreals which is almost matching with composition<strong>of</strong> the surface samples. Allhough shola trees are inadequately present butImpatiens, a close associate <strong>of</strong> shala woods, is regularly present in the samples whichsignifies tile existence <strong>of</strong> silola woods.H.P. Gupta and S.K. BeraPollen morphology <strong>of</strong> 27 modern trees from Silent Valley has been completedunder LM.H.A.KhanProgramme7.2 : Depositional environment andthe Quaternary Period in thepalynological approachclimate duringHimalaya : AObjective,To build up a fine resolution climatic sequence <strong>of</strong>Quaternary Period in tile Himalayan regionPollen analysed 8 samples from 2 meter deep pr<strong>of</strong>ile (GT-l) from Gola Thppar,Dehradun. The study has revealed the occurrence <strong>of</strong> Holoptelea, Bauilinia,Murraya, Ficus, Mallotus and Meliaceae. Strobilantiles, Fabaceae and Urticaceaeare scanly. The ground vegetation is composed <strong>of</strong> grasses, sedges, Chen~/Ams,Brassicaceae, Artemisia, etc. Besides, fungal spores <strong>of</strong> Alternaria, Curvularia,41

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