posed, which incorporates most <strong>of</strong> physical, chemical and petrological factorsrecognized to have induced spontaneous heating process.A rich assemblage <strong>of</strong> leaf-impressions from Arjun Khola were identified andassigned to the genera, viz., Ag/aia, Alstonia, Alsodeia, Anacolosa, Artocarpus,Bridelia, Diospyros, Dracontomelum, Euphoria, Evadea, Filicium, Garcinia, Grewia,Gynocardia, Lagerslroemio, Lepionurus, Miliusa, Mil/ellia, Phyllanthus, Unona, Vitis,etc. <strong>of</strong> the dicotyledonous families. Two fabaceous fruits have been identified wilhthose <strong>of</strong> Butea superb a and Sindora velutina. Fossil woods <strong>of</strong> Dipterocarpus(Dipterocarpaceae), Canarium (Burseraceae), Euphoria, (Sapindaceae), Julbernardia,(Fabaceae), Barringtonia (Leeythidaeeae), Madhuca and Manilkara(Sapotaceae) have been identified from Namsang beds near Deomali, ArunachalPradesh. Of these, Julbernardia is an African genus and suggests phytogeographicallinkage <strong>of</strong> Africa with the Indian subcontinent during Neogene. A leaf <strong>of</strong> Mangi[erarecovered from the Upper Palaeocene sediments near Laitryngew, Khasi Hillssupports the view that the genus Mangi[era appeared first in the Upper Palaeocenein the Indian subcontinent. A fossil wood similar to Grewia (Tiliaceae) with tilecells and radial gum canals has been identified. Woods similar to African generaTrichilia (Meliaceae), Blighia (Sapindaceae) and Erythr01ylon (Erythroxylaceae)were also identified from Nawargaon. The genus Chlorophora <strong>of</strong> the familyMoraceae, a typical African genus, has been recorded for the first time in the IndianNeogene flora <strong>of</strong> western India.Morphotaxonomic study <strong>of</strong> the palyn<strong>of</strong>lora obtained from the Neyveli Mine-lhas been partly done. The assemblage is correia table to the upper zone <strong>of</strong> theNeyveli Formation, viz., Trilatiporites sellingii Cenozone <strong>of</strong> Jayamkondacholapuramarea. Latest Maastrichtian, low latitude calcareous nannoplankton marker speciesMicula prinsii has been reported in this section, terminating in stratigraphic orderat the base <strong>of</strong> the clay layer. An in tegra ted scheme, incorporating din<strong>of</strong>lagellate cyst,calcareous nannoplankton, planktonic foraminifera and geochemical data, is proposedfrom the Langpar Formation exposed along the western bank <strong>of</strong> the UrnSohrengkew River, on the southern slope <strong>of</strong> Cherrapunji Plateau, Khasi Hills.Three new species <strong>of</strong> the genus TrichodiniunJ, viz., T. minulum, T. brevispinosum, T.jainii and a new combination Acanlhaulax magnum (Jain) are described from theGrey Shale Member <strong>of</strong> Dalmiapuram Formation (Lower Albian) together with anew genus Ectodinium and a new species, Callaiosphaeridium tapeum fromTrichinopoly Formation (Turonian-Santonian) <strong>of</strong> Cauvery Basin. A rich din<strong>of</strong>lagellatecyst and acritarch assemblage has been recovered from selected core andcUlling samples <strong>of</strong> a 764.9 meter deep bore hole drilled in Puduvoyal, ChingleputDistrict, Palar Basin, southern India and assigned an Early Cretaceous (Hauterivian-Barremian)age. Middle Miocene diatoms from the 75 meter thick South CoastCliff Seclion <strong>of</strong> Kamorta Island have been detailed out. Palynoassemblages <strong>of</strong> fourmeasured sections, viz., Dali, Khargala, Sair and Kalakot <strong>of</strong> Jammu depict theirclose similarity with those recorded from Kalka-Simla and Banethi-Bagthan areas<strong>of</strong> Himachal Pradesh. Based on this observation a possible sea-link between thesetwo widely separated areas is envisaged during Eocene time. Palynological investigationon the Cretaceous-Tertiary transition in the bore hole core no. CM5 drilledin the Atlantic occan <strong>of</strong>f Senegal Coast, West Africa suggcsts a major change infloral composition marking Krr boundary, characterized by the disappearance <strong>of</strong>(iv)
Maastrichtian marker taxa and presence <strong>of</strong> a fern spike.••Pollen analytical investigation <strong>of</strong> 12 glacier dust samples from Dunagiri Glacier,Garhwal Himalaya revealed presence <strong>of</strong> broad-leaved Quercus, Betula, Alnus, Carpinus,Ulmus and Celtis, Pinus, Abies, Picea and Cedrus in low values. Poaceae,alongwith Cheno/Ams, Ranunculaceae, Asteraceae, Rosaceae, etc. are the prominentherbaceous elements. Palynology <strong>of</strong> 4.30 meter deep pr<strong>of</strong>ile dated 3800 yearsB.P. from Rambha on south east flank <strong>of</strong> Chilka Lake enabled to divide whole timespan into two phases, between 3,800 - 2,000 yrs. B.P. records the existence <strong>of</strong> welldeveloped core-mangrove forest and from 2,000 yrs. B.P. till date records the overalldegradation <strong>of</strong> core- mangrove vis-a-vis uprise in the values <strong>of</strong> hinterland taxa. Treesamples <strong>of</strong> Cedrus deodara from Harshil in Uttarka'shi have been dated and a 745yrs long (1243-1987) chronology has been prepared. Another chronology <strong>of</strong> Pinuswallichiana growing in sub-alpine mesic site in Gangotri ranges from 1694 - 1988AD. The occurrence <strong>of</strong> hemplbhang (Cannabis sativa) charcoals from NeolithicChalcolithic site at Senuwar, Rohtas, Bihar (Ca 2000-600 B.C.) suggests the exploitation<strong>of</strong> narcotic properties <strong>of</strong> this plant. The occurrence <strong>of</strong> pomegranate (Punicagranatum) from Rohira, Punjab (ca. 2000 - 1700 B.C.) suggests the cultivation <strong>of</strong>pomegranate in the orchard husbandry <strong>of</strong> Harappans.A core <strong>of</strong> lake deposit from Orissa relating to the study on the evolution <strong>of</strong>mangrove vegetation was dated to 3470 ± 170 yrs at a depth <strong>of</strong> 3.5 m. A carbonaceousocean-sediment core from Andaman Sea was dated using the organic fraction<strong>of</strong> the sediment. The C-14 age at a depth <strong>of</strong> 33 cm is 11850 yrs and at 1.0 m it is21000 yrs. Charcoal samples relating 10 archaeological studies from Mesolithicculture <strong>of</strong> Kerala has been dated for the first time at 2850 ± 80 yrs B.P. Petrifiedwood samples collected from Deccan Intertrappean beds have been dated using theAuto Scan system; the F-T ages <strong>of</strong> petrified woods from different localities nearShahpura in Mandla district, Madhya Pradesh are Ghghua: 57 ± 8 ma, Umaria: 56±7 ma, Silther: 53 ± 9 ma, Parapani: 54 ± 7 ma and Mehdwani: 58 ± 8 ma.The Research Programming and Planning Group consisting <strong>of</strong> Drs H.P. Singh,K.P. Jain, H.K. Maheshwari and R.S. Tiwari helped to prepare this document. DrA Rajanikanth rendered considerable help in bringing out this report. The printing<strong>of</strong> this report has been looked after by Dr J.S. Antal. .(B.S. VENKATACHALA)Director(v)
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- Page 5 and 6: AcknowledgementWe are grateful to t
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- Page 20 and 21: BSIPThe Palaeobotanical Society Int
- Page 22 and 23: BSIPGeneral, Geological Survey of I
- Page 24 and 25: BSlPin Proterozoic succession of Cu
- Page 26 and 27: BSIP";jEuryphy/lum whilt;anum Feist
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- Page 38 and 39: BSIPMARINE SEDIMENTARIES OF INDIA1'
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- Page 50 and 51: BSIPMeghalaya have yielded a rich s
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BSIPThe Auto Scan system for the fi
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BSIPthe Indian Tertiary sedimentsOb
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BSIPM.S. ChauhanPart-7Part-8Part-9P
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BSIPB.K. MisraAnand PrakashG.K.B. N
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BSIPStudied the pollen morphology (
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BSIPremains based on field and herb
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BSIPPapers SubmittedAgarwal, Anil -
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BSIPKapoor, U.M., Maheshwari, U.K.
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BSIPSharma, Chhaya - Palaeoclimatic
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BS!PAbstractsSubmittedAwasthi, N. -
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BSIPPapers PublishedAgarwal, A. 199
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BSIPKar, R.K. 1991. Two new spore g
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BSIPSingh, H.P., Jain, K.P., Mahesh
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BSIPAbstractsPublishedAmbwani, K. &
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BSIPDesikachary, T.V., Shukla, Mano
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BSIPLucknow : 68.Maheshwari, U.K. 1
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BSIPSharma, Mukund, Shukla, Manoj &
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BSIPVenkatachala, B.S., Kar, R.K.,
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BSIPGuleria,J.S.Coringoperation at
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BSIPPapers Presentedat Symposia/Con
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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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BSIPmud bank and Vembanad Lake, Ker
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BSIPTechnical Assistance renderedto
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BSIPHonours and AwardsAsha GuptaMuk
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BSIPI.Archaean and Proterozoic Pala
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BSIPFlorida Museum of Natural Histo
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BSIPType and Figured specimens/slid
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BSIPInstitutionalVisitors1. U.N. Po
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