1995-96 - Birbal Sahni Institute of Palaeobotany
1995-96 - Birbal Sahni Institute of Palaeobotany
1995-96 - Birbal Sahni Institute of Palaeobotany
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<strong>1995</strong>-<strong>96</strong><br />
Carboniscd wood <strong>of</strong> Chrysophyllum roxbllrghii, an evergreen clement, from Nepal Siwaliks; I, cross<br />
section (X 80); 2, tangential longitudinal secliol1.<br />
Six fossil woods collected from Siwalik sediments <strong>of</strong> Tanakpur have been studied<br />
and tentatively identified with extant taxa Cassia and Ormosia <strong>of</strong> the family Fabaceae,<br />
'l'erminalia <strong>of</strong> Combretaceae and a lauraceous wood. Twenty fossil woods collected from<br />
Siwalik sediments <strong>of</strong> Kalagarh area in Pauri Garhwal District <strong>of</strong> Uttar Pradesh have been<br />
studied. Of these. two fossil woods seem to be new belonging to the genus Dalbergia anu<br />
Bi"ch<strong>of</strong>ia <strong>of</strong> the, families Fabaeeae and Euphorbiaceae, respectively.<br />
A number <strong>of</strong> leaf-impressions recovered from Siwalik sediments <strong>of</strong> eastcrn Nepal<br />
have been investigated and identified with the extant genus Bambllsa <strong>of</strong> Poaceae,<br />
Dipterocarp"s and Hopea <strong>of</strong> Dipterocarpaceae, Leea <strong>of</strong> Ampelidaceae, Ardisia <strong>of</strong><br />
Myrsinaceae and Diospyros <strong>of</strong> Ebenaceae. A draft manuscript "Observations on the plant<br />
fossils from the Siwalik sediments <strong>of</strong> eastern Nepal" was prcpared.<br />
The overall study on plant megafossils from the Siwalik sediments suggcsts the<br />
cxistence <strong>of</strong> a tropical forest all along the Himalayan foot-hills during deposition. On the<br />
basis <strong>of</strong> habit and habitat <strong>of</strong> modem equivalents as well as physiognomic characters <strong>of</strong> the<br />
fossils existence <strong>of</strong> tropical climate during Siwalik period has been suggested.<br />
M. Prasad<br />
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