BSIPIn the light <strong>of</strong> the distribution patterns <strong>of</strong> the modern counterparts <strong>of</strong> fossil leavesa low land mixed broad-leaved mesophytic tropical evergreen to semi-evergreenforest in the area during Siwalik sedimentation has been envisaged. However, anincrease in the deciduous elements towards the upper part <strong>of</strong> the Siwalik sequencerefiects a gradual change in the climatic conditions which could have been causedby the uplift <strong>of</strong> the Himalaya.N. Awasthi and Mahesh PrasadLeaf-impressions from Siwalik sediments <strong>of</strong> Hardwar, Nainital, and fossilwoods from Kalagarh and Hardwar were studied. The fossil woods identified fromKalag~ -h are : Dipterocarpus, Hopea, Sterculia, Bursera, Euphoria, Dialium,Milletlia and Diospyros, while a wood from Hardwar is comparable to Dipterocarpusspeciosus and D. gracilis.MaheshPrasadProgramme 5.7Objective,Palynology, palaeoecology and palaeogeograhy<strong>of</strong> the Tertiary sediments <strong>of</strong> Nepal Himalaya,To study palyn<strong>of</strong>ossils from the Mio-Pliocene sediments,To carry out palynozonation and age determination<strong>of</strong> assemblages loge/her with reflections onthe past vegetation and environment <strong>of</strong> depositionEvidences <strong>of</strong> micro- and megafossils from the Siwalik sediments (Neogene) <strong>of</strong>Surai Khola area, Nepal have been used to reconstruct the vegetation and palaeoenvironmentalconditions. The fossil assemblage mainly consists <strong>of</strong> leaf impressions,carbonised woods, seeds, fruits, pollen and spores representing all majorplant groups.The palaeobotanical evidences suggest existence <strong>of</strong> a lowland mixed mesophytieforest communities <strong>of</strong> broad leaved semi- evergreen to evergreen trees. Anincrease in the "deciduous elements is also noticed. A fresh water swampy environment<strong>of</strong> deposition is interpreted for the older horizons due to the presence <strong>of</strong>algal and other aquatic plants, viz., Azolla, Cera/opteris, Typha, Nymphea, etc.Gradually swampy conditions seem to have changed to a bottomland habitat whichis depicted by the presence <strong>of</strong> a number <strong>of</strong> ferns and other herbaceous clements inthe subsequent younger horizons.S. SarkarPROJECTG,nrOSTRATIGRAPIIY AND PALYNOFACIES OFPETROLIFEROUS BASINS OF EAST INDIAProgramme 6.lObjective34: Tertiary floral history <strong>of</strong> no.·theast India,To study morphotaxollomy <strong>of</strong> megafossils from thePalaeogene and Neogene sediments <strong>of</strong> Assam,Meghalaya and Arullachal Pradesh,To recollstruct Tertiary floral history, palaeoecology
<strong>1991</strong>-<strong>92</strong>A fossil leaf and fruit resemblingMesuQ [urea from Makum CoaJrield,Assam.and phytogeographyFossil woods <strong>of</strong> Dipterocarpus (Dipterocarpaceae), Canarium (Burseraceae),Euphoria, (Sapindaceae), Julbernardia, (Fabaceae), Barringtonia (Lecyihidaceae),Madhuca and Manilkara (Sapotaceae) have been identified from Namsang bedsnear Deomali, Arunachal Pradesh. Of these, Julbernardia is an African genus andsuggests phylOgeographicallinkage <strong>of</strong> Africa with the Indian subcontinent duringNeogene.This genus disappeared from India perhaps at the close <strong>of</strong> Pliocene, like manyother African and Malaysian elements.A fruit <strong>of</strong> the genus Mesua has been identified from Tirap Colliery <strong>of</strong> MakumCoalfield, Assam. It further confirms wider distribution <strong>of</strong> this genus in northeastIndia during Oligocene.From the Upper Palaeocene sediments near Laitryngew, Khasi Hills, a leaf <strong>of</strong>Mangifera has been identified. This supports the view that the genus Mangiferaappeared first in the Upper Palaeocene in the Indian subcontinent.N. Awasthi and R.C. MehrotraProgramme 6.2Objective: Palynostratigraphy <strong>of</strong> sedimentary rocks InTherriaghat Section and its correlation withJaintia and Garo Hills sediments: To work out palynostratigraphy <strong>of</strong> different Tertiaryformations35
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BSIPGuleria,J.S.Coringoperation at
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BSIPgroup, Rohtas, Bihar, India. Bi
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BSIPMaheshwari, ILK. - Provincialis
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BSIPSingh, H.P. - Tertiary palynofo
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BSIPTechnical Assistance renderedto
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