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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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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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