1994-95 - Birbal Sahni Institute of Palaeobotany
1994-95 - Birbal Sahni Institute of Palaeobotany
1994-95 - Birbal Sahni Institute of Palaeobotany
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BSIP<br />
Pollen analysis <strong>of</strong>a 1.8 m deep soil pr<strong>of</strong>ile from Dewar Tal has revealed the presencc<br />
<strong>of</strong> chirpine forests in the region around 2,500 years B.P. The broad-leaved taxa, such<br />
as Quercus, Alnus, Rhododendron, etc. were scantily distributed around 2,000 years B.P.<br />
The mixed Chirpine-Oak forests got established as indicated by the increased frequencies<br />
<strong>of</strong> Quercus, Alnus, Rhododendron and shmbby elements <strong>of</strong> Strobilamhes, Oleaceae and<br />
Rosaceae. Thereafter, the decline in these forests and simultaneous improvement in grasses<br />
and other non-arboreals have been witnessed.<br />
Chhaya Sharma & M.S. Chauhan<br />
Pollen analysis <strong>of</strong>24 samples from 1.5 m deep soil pr<strong>of</strong>ile (DT-3) from Deoria Tal,<br />
Garhwal Himalaya has been carried out. Study reveals the dominance <strong>of</strong> non-arboreals over<br />
arboreals. Poaceae followed by Cyperaceae are major constituents. Asteraceae,<br />
Ranunculaceae, Cheno/Ams, Caryophyllaceae, Brassicaceae, Polygonaceae, Lantiaceae and<br />
Urticaceae, etc. are other associates <strong>of</strong> ground cover. Arboreals are poorly represented by<br />
Pinus, Quercus, Alnus, Bewla, Carpinus, Rhododendron, Picea, Abies, Ephedra, Ulmus,<br />
Celtis, Juglans, Myrtaceae, Symplocos, Juniperus and Fabaceae. Fern spores are encountered<br />
in good number reflecting their oligin from local source. The overall vegetation assemblage<br />
depicts that around 2,500 years B.P. the open mixed broad-leaved forest existed in the<br />
region.<br />
Chhaya Sharma & Asha Gupta<br />
Five aeropalynological samples from Chaurangi Khal, Garhwal Himalaya were<br />
pollen analysed .The study reveals the dominance <strong>of</strong> ru·boreals over non-arboreals. Arboreals<br />
show high frequency <strong>of</strong> Pinus followed by Quercus, Carpinus, Betula, Alnus, Corylus,<br />
Ulmus, Celtis, Juglans and Rhododendron. Non-ru·boreals ru·e represented by Poaceae,<br />
Ranunculaceae, Cyperaceae, Cheno/Ams and Brassicaceae, etc. Fungal spores ru·eencountered<br />
in good nUI)1berwhile fern spores occur rarely. TIle composition <strong>of</strong>aerospora more or<br />
less colTesponds with the sUlTounding vegetation in the region, except for the under-representation<br />
<strong>of</strong> fern spores which could be attributed to their restricted verticaltranspOltation.<br />
Programme 7.3<br />
History <strong>of</strong> mangrove vegetation in India<br />
Asha Gupta & Chhaya Shru·ma<br />
Objecti\'e<br />
To study palynostratigraphy and Dispersed Organic· Maller<br />
analysis <strong>of</strong> the sediments from Chilka Lake in Mahanadi<br />
Brahmani-Baitarini delt{/lc region in Orissa<br />
Five samples <strong>of</strong>250 m deep pr<strong>of</strong>ile at the depth between 51-55 m from Sadanandpur<br />
in Mahanadi Delta have been palynologically investigated. The assemblage showed the<br />
preponderance <strong>of</strong> Poaceae, Cyperaceae, Chenopodiaceael Amru·anthaceae, Urlicaceae, Typha,<br />
Leollla, N)'mphoides, Potamogeton, etc. The core-mangrove taxa such as Rhizophora,<br />
Avicennia, Excoecaria, Heritiera and pelipheral mangroves were lowly present. The palynological<br />
;nvestigation has revealed that during this phase the sea regressed leaving the<br />
relics <strong>of</strong> mangrove forest in Mahanadi Della.<br />
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