BSIPStudied the pollen morphology (SEM only) <strong>of</strong> Pseudophoenix -P. ekmanii, P.sargentii and P. vinifer.Studied the pollen morphology and aperture evolution in Agave Linn.(Agavaceae). It is observed that the transition <strong>of</strong> developmental stages in aperture,e.g., monosulcate, bisculate, pont-operculate and anazonosulculate are exhibitedby this single genus.K. Ambwani and Madhav Kumar0, e meter deep sediments from Kathuta Thl, ranging in age between ca 200·400 years B.P., were pollen analysed. The study has exhibited good pollen assemblagealbeit non-arboreals predominated. The arboreal taxa encountered fromsedimcnls are Holoptelea, Acacia, Capparis, Combrctaceac, Myrtaccac, Malvaceac,etc. and their collective frequencies range between 3-15 per cent <strong>of</strong> the totalassemblage. The ground vegetation is largely dominated by grasses and followedby Chenopodiaceae, Asteraceae, Afteman/hera, etc. Polygonum plebejum,Eriocaulon, Cyperaceae, Apiaceae, etc. inhabited the marshy!and along the lakemargins and Lemna, Po/amoge/on, Eichomia, Nymphoea, Nymphoides, etc. inhabitedthe lake water. The study has revealed that tree-less conditions prevailedaround the lake and crop cultivation was on its peak. The lake had wider spread inthe past which was congenial for aquatic and marshy life.M.S. Chauhan, Asha Khandelwal, S.K. Bera and H.P. GuptaThe study reveals high pollen production in Shorea robus/a whereas low percentage<strong>of</strong> sa! pollen is recorded in surface soils within the forest and graduallydeclines across the open land.Yellow spots colle.;ted from plant leaves in Vikas Nagar, Lucknow duringFebruary, 19<strong>92</strong> were pollen ana lysed and found more or less similar pollen compositionas during the previous year. However, several additional taxa belonging toApiaceae and Asteraceae were reported.S.K.BeraAsha Khandelwal and H.P. GuptaOne meter core from Andman Island has been palynologically investigated.Pollen, spores, diatoms and din<strong>of</strong>lagellate cysts have been recorded.H.P. Gupta and Asha KhandelwalSubathu Formation exposed in Koshalia Nala Section <strong>of</strong> Shim!a lesser Himalayahas been studied. Detailed documentation <strong>of</strong> Early Eocene taxa including Krrboundary nann<strong>of</strong>ossil species are recorded.S.A. Jafar and O.P. SinghWorked out 35 rock samples <strong>of</strong> Nupra Shale sequence (Jurassic), Thakkolaarea, Nepal, for din<strong>of</strong>lagellate contents, under the "International Earth ScienceExpedition Lost Ocean]] in the Plate Tectonic suture zone between Nepal andTibet"56
<strong>1991</strong>-<strong>92</strong>K.P. Jain, Rahul Garg and Khowaja-AteequzzamanA well preserved and datable Palaeocene dinonagellate cyst assemblage isdiscovered from an outcropping carbonaceous shale sequence overlying theDeccan Traps near Nareda, south-western Kutch as well as from Lakhpat subcrop.This is extremely significant as age <strong>of</strong> the earliest Palaeogene clastic sequence inKutch has generated much controversy in recenl years because existence <strong>of</strong> Palaeocene- Early Eocene rocks dated earlier on foraminiferal and bivalve evidencehas <strong>of</strong>ten been denied based mainly on a "false identification" criteria.RahulGargThe distribution <strong>of</strong> pteridophytic spores in the Tertiary sediments <strong>of</strong> India hasbeen critically analysed. One hundred and fifty fossil spore genera have beenstudied to understand their morphological range <strong>of</strong> variation. They have beencompared with the spores <strong>of</strong> extant taxa. A range chart <strong>of</strong> pteridophytic sporesincorporating data from the Tertiary strata <strong>of</strong> India has been prepared.SamirSarkarPalynological and palaeoecological study <strong>of</strong> the Kundlu and Nalagarh formationspertaining to Lower Siwalik sediments (Mid- Miocene) exposed in andaround Kundlu has been made. Palynological evidences coupled with plantmegafossil records have been used to reconstruct the history <strong>of</strong> the vegetation <strong>of</strong>this area. Tho distinct palynoassociations have been identified. PalynoassociationI characterises the entire Kundlu Formation which extends into the lower part <strong>of</strong>the younger Nalagarh Formation. It exhibits the excl usive presence <strong>of</strong> Cosmarium,Pediastrum along with high incidence <strong>of</strong> Ceratopteris, Lycopodium and Polypodium.Palynoassociation II is characterised by the presence <strong>of</strong> Pinus, Podocarpus, Acacia,Dipterocarpus, etc. and is confined to the upper part <strong>of</strong> Nalagarh Formation.Angiospcrmous pollen register a dominant position in this assemblage whereas thealgal elements sharply decline. The present palynonora augumented by megafossilevidences brings to ligh t a broad leaf type <strong>of</strong> vegetation conforming to warm humidclimate with tropical to subtropical distribution.Samir Sarkar and H.P. SinghDuring noristic survey <strong>of</strong> Mahuadanr Valley (Chhechari Valley) which is situatedin Chotanagpur plateau region <strong>of</strong> south Bihar in Palamau District, someangiospermic plants have been collected from different localities in the area forreference collection. 94 species have been identified. Leaf impressions <strong>of</strong> eachspecies have been prepared in order to understand the morphology <strong>of</strong> fossil plantleaves. The vegetation <strong>of</strong> the area is tropical deciduous type. Sal is the dominantspecies in the forest.The study <strong>of</strong> sedge nora has long been neglected possibly because <strong>of</strong> its minutegrass-like appearance and complicated noral morphology. There are some membersin the family Cyperaceae which play major role in soil reclamation andprevention <strong>of</strong> soil erosion. 96 species belonging to 8 genera <strong>of</strong> Cyperaceae familyhave been collected from eastern Uttar Pradesh. The area includes the districts <strong>of</strong>Bahraich, Gonda, Basti, Gorakhpur and Deoria. A key for identification <strong>of</strong> plant57
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Birbal Sahni (1891-1949)ANNUAL REPO
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AcknowledgementWe are grateful to t
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To coordinate with other knowledge
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posed, which incorporates most of p
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1991-92BIRBAL SAHNIBIRTH CENTENARY
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BSIP-----Dr B. S. Venkatachala welc
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BSIPDr A. P. Mitra opening the Exhi
- Page 18 and 19: BSIPDelegates of the Symposium - Ev
- 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
- Page 28 and 29: BSIPin Mahanadi Valley in compariso
- Page 30 and 31: BSIP----Au st raIia----
- Page 32 and 33: BSIPbeen observed tijat the coals a
- Page 34 and 35: BSIPTransverse Section of a monocot
- Page 36 and 37: BSIPular fruit of euphorbiaceousaff
- Page 38 and 39: BSIPMARINE SEDIMENTARIES OF INDIA1'
- Page 40 and 41: BSIPH10~mTrichodinium brel'ispillos
- Page 42 and 43: BSIPand time boundaries: To integra
- Page 44 and 45: BSIPmarine innuence during Karharba
- Page 46 and 47: BSIPIn the light of the distributio
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- Page 50 and 51: BSIPMeghalaya have yielded a rich s
- Page 52 and 53: BSIPbetween 1002-944 m show an almo
- Page 54 and 55: BSIPTetraploa and Microthyriaceaear
- Page 56 and 57: BSIPand a 745 year long (1,243-1,98
- Page 58 and 59: BSIPclinicalimplicationsObjective ,
- Page 60 and 61: BSIPThe Auto Scan system for the fi
- Page 62 and 63: BSIPthe Indian Tertiary sedimentsOb
- Page 64 and 65: BSIPM.S. ChauhanPart-7Part-8Part-9P
- Page 66 and 67: BSIPB.K. MisraAnand PrakashG.K.B. N
- Page 70 and 71: BSIPremains based on field and herb
- Page 72 and 73: BSIPPapers SubmittedAgarwal, Anil -
- Page 74 and 75: BSIPKapoor, U.M., Maheshwari, U.K.
- Page 76 and 77: BSIPSharma, Chhaya - Palaeoclimatic
- Page 78 and 79: BS!PAbstractsSubmittedAwasthi, N. -
- Page 80 and 81: BSIPPapers PublishedAgarwal, A. 199
- Page 82 and 83: BSIPKar, R.K. 1991. Two new spore g
- Page 84 and 85: BSIPSingh, H.P., Jain, K.P., Mahesh
- Page 86 and 87: BSIPAbstractsPublishedAmbwani, K. &
- Page 88 and 89: BSIPDesikachary, T.V., Shukla, Mano
- Page 90 and 91: BSIPLucknow : 68.Maheshwari, U.K. 1
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- Page 116 and 117: BSIPHonours and AwardsAsha GuptaMuk
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BSIPI.Archaean and Proterozoic Pala
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BSIPJawaharlal Nehru University, Ne
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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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BSIP22. Henri J. RakotoariveloPalae
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BS!PNeerja Jha, Ph.D. (w.e.f. 01.04
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BSIPTechnical and Administrative Pe
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BSIPKunwarDriversHanuman PrasadLall
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BSIPPromotionsPromotions and Appoin
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BSIPOrganisationalGoverningStructur
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BSIPChief Engineer, U.P.P.W.D. or h
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BSIPInternal Committees1. Research
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BSIPAuditorsto theReportGoverning B
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BSIPBIRBAL SAHNI INSTITUTEOFBalance
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1991-92COMMENTS TO BE READ WITH REF