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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<strong>1994</strong>--<strong>95</strong><br />
On Independence Day celebrations a baby presenting her song.<br />
Gangapur beds is to be continued for building-up tbe floras tbrough ages. The investigations<br />
will help to understand tbe evolutionary lineages and significance <strong>of</strong> plant fossils in<br />
stratigraphy. The ultrastructural studies <strong>of</strong> plant parts - cuticles, seeds, megaspore, etc.<br />
are also planned which will facilitate tbe taxonomic placement and also tracing tbe affinity<br />
witb tbe parent plant group. The efforts for palynodating <strong>of</strong> coal-bearing sediments in<br />
Rajmahal, Panagarh, Deocha-Pachami areas, Raniganj, Sohagpur, Pali-Parsora, Tatapani<br />
Ramkola, Kotbagudem and Satpura Basin <strong>of</strong> peninsular India are to be made which have a<br />
bearing on coal exploration. Studies on Spiti Himalaya, peri-Gondwana and Arunachal<br />
Pradesh will be carried out to correlate tbe marine and non-marine palynological assemblages<br />
as well as plant megafossils. Such study has immense value for chronostratigraphy<br />
<strong>of</strong> non-marine sequences.<br />
Cenozoic vegetation and plant biogeography are planned to be studied in tbe Deccan<br />
Intertrappean sediments in Madbya Pradesh and also in tbe Tertiary sediments from Assam,<br />
Bihar, Bengal, Kerala, Rajastban, Himachal Pradesh, Uttar Pradesh and Gujarat. Likewise,<br />
the studies <strong>of</strong> micr<strong>of</strong>ossils, Le., phytoplank1on are to be continued for tbeir biostratigraphical<br />
aspects in Cauvery Basin and Andaman and Nicobar islands.<br />
The flora and vegetational pattern in Quaternary sediments will be studied in Silent<br />
Valley, soutb India, Spiti Valley, Himachal Pradesh and Garhwal Himalaya. Studies in tbe<br />
mangrove vegetation from Chilka Lake, Mahanadi delta are to be continued. The efforts<br />
will be made to develop climatically responding tree ring chronologies. Analysis <strong>of</strong> tbe<br />
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