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 />
Programme 5.5<br />
Objective<br />
Maceration<br />
To develop information on phytogeography and understanding<br />
<strong>of</strong> the orogeny <strong>of</strong> Himalaya<br />
Morphotaxonomic study <strong>of</strong> the recovered palyn<strong>of</strong>ossils from the Tattapani and<br />
Metka coal mines were carried out. Photodocumentation <strong>of</strong> the selected palynotaxa was<br />
made. Data interpretation <strong>of</strong> the recorded palyn<strong>of</strong>lora from Beragua and Kalakot coal mine<br />
areas was done. Three distinct palyn<strong>of</strong>loral associations have been recognised in the<br />
Subathu succession <strong>of</strong> Tattapani and its adjoining areas. A comparison <strong>of</strong> the present<br />
dinocyst association with the one recorded earlier from Shimla hills <strong>of</strong> Himachal Pradesh<br />
reveals close similarity. Palyn<strong>of</strong>loral composition dominated by dinocysts confirms a shallow<br />
water nearshore marine environment <strong>of</strong> deposition for the Subathu Formation. A<br />
paper entitled "Palyn<strong>of</strong>ossils from the Subathu Formation (Eocene) <strong>of</strong> Jammu and their<br />
palaeoenvironmental significance" was finalized.<br />
Palyn<strong>of</strong>ossils have been recorded at several stratigraphic levels <strong>of</strong> Siwalik succession<br />
in Mansar and Uttarbani areas <strong>of</strong> Jammu. Qualitatively as well as quantitatively they<br />
are very poorly represented. Detailed morphotaxonomic study is in progress.<br />
Samir Sarkar<br />
ductive.<br />
Programme 5.6<br />
Palynostratigraphy <strong>of</strong> the Tertiary sediments<br />
Ladakh Himalaya<br />
To systematically<br />
To establish palynozonation<br />
study spores and pollen<br />
<strong>of</strong> Kargil Basin,<br />
To reconstruct the past vegetation. environment <strong>of</strong> deposition<br />
and palaeogeography<br />
<strong>of</strong> samples collected last year was done but the samples proved unpro-<br />
R.K. Saxena & Samir Sarkar<br />
Neogene Himalaya : floristics, evolntionary patterns and<br />
climate<br />
Objective To undertake extensive study <strong>of</strong> fossil plants from Neogene<br />
sediments <strong>of</strong> different regions <strong>of</strong> the Himalaya<br />
To build up floral successionfor interpreting palaeoecology, phytogeographyand<br />
evolution <strong>of</strong> the Himalayan/lora<br />
Leaf-impressions from the Kasauli Formation were sorted, cleared and photographed.<br />
Out <strong>of</strong> the specimens investigated, a frond has been identified as Acrostichum, a<br />
coastal fern from near Daghota, Kalka-Shimla Road. Tlus fem is <strong>of</strong> special significance as<br />
it indicates persistence <strong>of</strong> coastal envirolUnent in the vicinity <strong>of</strong> Kasauli-Kumarhatti during<br />
Lower Miocene.<br />
N. Awasthi, J.S. Guleria, M. Prasad & Raslmu Srivastava<br />
Morphotaxonomical study <strong>of</strong> plant remains including woods, leaves, fmits and<br />
seeds from Siwalik sedin,ents <strong>of</strong> Arjunkhola, Suraikhola and Rehr has been carried out.<br />
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