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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 />

Himachal Pradesh were dated. The age range covered by these pr<strong>of</strong>iles span entire Late<br />

Quaternary Period. The pollen analytical investigations in the sediment pr<strong>of</strong>ile <strong>of</strong> Sithikhar<br />

swamp, Spiti Valley, Himachal Pradesh indicate cold-arid climatB before 1,900 yrs but later<br />

the climate became colder as evidenced by decline in the frequencies <strong>of</strong> most plant taxa in<br />

younger sediments. The samples from Takche, Spiti Valley were found to be palynologically<br />

barren.<br />

Charcoal samples (6) relating to archaeobotanical studies from the Harappan site<br />

in Dholavira, Kutch, Gujarat were dated. The calibrated C-14 ages <strong>of</strong> the samples lead to<br />

the inference that the Harappan Civilization was flourishing in this locality for a much<br />

longer period (2,660 to 1,<strong>95</strong>0 B.C.) than at other sites excavated so far.<br />

For a collaborative programme (with the Geology Depattment, Kumaon University)<br />

on neotectonic studies in Himalayas, sediment samples from Pithoragarh were dated.<br />

The ages <strong>of</strong> two samples differ widely 30,000 yrs in one case and 2,000 yrs in the other.<br />

Dating <strong>of</strong> systematically eolleeted pr<strong>of</strong>ile samples is in progress. Samples <strong>of</strong> peat from<br />

Nilgiris were dated for a collaboration programme with the Indian <strong>Institute</strong> <strong>of</strong> Science,<br />

Bangalore in continuation <strong>of</strong> earlier studies on palaeoelimate <strong>of</strong> southern India.<br />

The C-14 dating <strong>of</strong> shell and kankar samples (8) in Gangetic alluvium was continued<br />

for understanding the development <strong>of</strong> alluvial deposits and climate changes in Holocene<br />

in the Indo-Gangetie Plain.<br />

Five peat samples from West Bengal were dated on payment for Centre for Study <strong>of</strong><br />

Man and Environment, Caleutta to reconstlUct palaeoclimate and environment and their<br />

changes during the Quaternat·y <strong>of</strong> lower Bengal delta in a precise geochronological framework.<br />

Six sample~ <strong>of</strong> coral, sediment and wood were dated for Jadavpur University on<br />

payment for studies relating to past sea level and palaeoclimate. One charcoal sample was<br />

dated for Lumbini Development Trust, His Majesty's Government, Nepal from a site in<br />

Lord Buddha's birth place, Lumbini in Nepal.<br />

Five samples <strong>of</strong>bmnt wood, sediment and ehat·eoal were dated as palt <strong>of</strong> a programme<br />

relating to the investigations by NGRI <strong>of</strong> 1993 eaIth quake in Latoor, MahaI·ashtra.<br />

G. Rajagopalan<br />

For the reconstruetion <strong>of</strong> past trophic conditions around Didwana Lake, Rajasthan<br />

on the basis <strong>of</strong> elemental analysis, phospholUS eoncentrations (authigenic phospholUs passes<br />

to the sediments primarily through biotic cycling) at different depths <strong>of</strong> trial trench were<br />

measured. This is in addition to the measurements <strong>of</strong> elemental, organic and mineral eontents<br />

carried out earlier in these sediments, which covers a time span <strong>of</strong> 8, 100 yrs BP. Five<br />

samples were analysed for measuring authigenic phospholUs concentrations using Spectrophotometer.<br />

We concentrations range from 7,880-1,8250 ppm . Conclusions derived are<br />

in agreement with those on the basis <strong>of</strong> other elemental, organic and mineral content data.<br />

G. Rajagopalan & B. SekaI·<br />

Programme 8.3 Potassium-Argon dating <strong>of</strong> sedimentary and igneous<br />

rocks<br />

119

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