1996-97 - Birbal Sahni Institute of Palaeobotany
1996-97 - Birbal Sahni Institute of Palaeobotany
1996-97 - Birbal Sahni Institute of Palaeobotany
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
<strong>1996</strong>-<strong>97</strong><br />
A total <strong>of</strong> 90 samples were processed, <strong>of</strong> which 64 samples were dated. Some<br />
<strong>of</strong> the results are as follows:<br />
Sediment samples from Sat-Tal, Dharali and one sediment sample from Chharka<br />
Tal, Uttar Kashi (U.P.) have been dated to understand the depositional environment<br />
and climate during the Quaternary Period in Himalaya. The base <strong>of</strong> Dharali sediments<br />
was dated as 1240 ± 90 yrs BP. The C-14 date <strong>of</strong> Chharka Tal sediment at 3.65-3.75 m<br />
depth comes out to be 2090 ± 140 yrs BP.<br />
Two peat samples from Konalur River Basin, Kodaikanal have been dated to<br />
work out the history <strong>of</strong> vegetation and climate in tropical montane forest in south<br />
India. The C-14 date at base (140-150 cm) is 3360 ± 110 yrs BP. Peat samples from<br />
Wadda Lake, Pithoragarh have also been dated and the rate <strong>of</strong> sedimentation works out<br />
to 34 cm!1 000 yrs. Two peat samples from Paradise Lake, Selapass, Kameng, Arunachal<br />
Pradesh have been dated to understand climatic change in the eastern Himalayan region.<br />
The C-14 date at 1.0 m is 1650 ± 140 yrs BP.<br />
Three charcoal samples from Raja-Nal-Ka-Tila near Ram Garh (U.P.) have<br />
been dated to reconstruct regional models <strong>of</strong> agriculture and economic exploitation <strong>of</strong><br />
plants in the prehistoric past for the Vindhyan plateau region. At the depth <strong>of</strong> 3.15-3.2<br />
m, C-14 date is 2830 ± 100 yrs BP.<br />
Installation <strong>of</strong> Ultra Low Background Liquid Scintillation Counter is being<br />
carried out. Fabrication <strong>of</strong> high vacuum system for synthesizing low volume Benzene<br />
samples has been done and some trial syntheses <strong>of</strong> low volume Benzene samples have<br />
been started. Microwave samples preparation system using microwave digestion method<br />
for chemical analysis has been installed. Atomic absorption spectrometer has also been<br />
installed and test measurements have commenced.<br />
Thirty-nine samples have been dated as a part <strong>of</strong> consultancy services <strong>of</strong>fered<br />
by the <strong>Institute</strong>.<br />
G. Rajagopalan & B. Sekar<br />
Interpreted the past climatic changes around Tsokar Lake, Ladakh; Didwana<br />
Lake, Rajasthan and Paradip River delta core on the basis <strong>of</strong> elemental analysis,<br />
authigenic phosphorus concentrations. The results were presented in the IGBP<br />
Symposium held at Bhubaneshwar.<br />
Visited Kalpi and adjoining areas and collected shell and kankar samples for<br />
I4C dating <strong>of</strong> Quaternary history <strong>of</strong> Gangetic alluvium.<br />
Programme 8.3 : Potassium-Argon dating <strong>of</strong> sedimentary and igneous<br />
rocks<br />
C.M.<br />
Nautiyal<br />
A set <strong>of</strong> new Saes getters was fixed. The gettering action <strong>of</strong> the Ti-Zr as well as<br />
Saes getters was monitored with temperature variation. Six thin sections <strong>of</strong> trap<br />
specimens and four <strong>of</strong> the fossil wood were made. Modification in the MS control unit<br />
47