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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 />

107

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