Organisational Structure - Birbal Sahni Institute of Palaeobotany
Organisational Structure - Birbal Sahni Institute of Palaeobotany
Organisational Structure - Birbal Sahni Institute of Palaeobotany
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<strong>Birbal</strong> <strong>Sahni</strong> <strong>Institute</strong> <strong>of</strong> <strong>Palaeobotany</strong><br />
Accumulation <strong>of</strong> these in plants was also analysed.<br />
The palynostratigraphical records show occurrence<br />
<strong>of</strong> mangrove forest during Early Holocene in the<br />
estuary that declined during Late Holocene. The<br />
anthropogenic pressure from Chennai city is fast<br />
deteriorating the aesthetic value <strong>of</strong> the estuary.<br />
Palynostratigraphical studies from Kolleru Lake (AP)<br />
indicates the shrinking <strong>of</strong> lake in the present day due<br />
to pressure <strong>of</strong> aquacultutre and pisciculture practiced<br />
in large scale decreasing the biodiversity in the area.<br />
Preliminary analysis shows high concentration <strong>of</strong><br />
heavy metals (arsenic, lead, and copper) in surface<br />
soil and sedimentary soil pr<strong>of</strong>ile studied from<br />
Pichavaram (TN). High concentration <strong>of</strong> these was<br />
observed in the leaves <strong>of</strong> mangroves.<br />
A. Farooqui<br />
Component 3: Studies <strong>of</strong> lake sediments in Rajasthan desert proxy climate signals<br />
Carried out LM and SEM studies <strong>of</strong> palyno taxa<br />
<strong>of</strong> families Malvaceae, Capparidaceae and<br />
Sterculiaceae collected from Rajasthan in order to<br />
facilitate the specific identification <strong>of</strong> the recovered<br />
fossil pollen and to ascertain the affinities <strong>of</strong> the<br />
genera and species to determine possible evolutionary<br />
trends in these families. Completed the pollen<br />
analytical investigations <strong>of</strong> 1.40 m deep sedimentary<br />
pr<strong>of</strong>ile from Pachpadra, an extinct salt lake in Barmer<br />
district. The pollen diagram has been divided into<br />
three zones; each prefixed by the abbreviations PP,<br />
signifying the investigated site. Pollen zone PP-I<br />
(125-140 cm) is palynologically barren and is mainly<br />
comprised <strong>of</strong> sandy material with very little clay. PP-<br />
II (70-125 cm) reflects poor occurrence <strong>of</strong> Poaceae,<br />
Cyperaceae, Tubulifloreae, etc. comprising sandy<br />
surface and with little clay. Pollen zone PP-III (0-70<br />
cm) revealed good frequency <strong>of</strong> palyno-taxa, viz.<br />
Poaceae, Cyperaceae, Tubulifloreae, Brassicaceae,<br />
Convolvulaceae, Portulaca sp., Solanum<br />
xanthocarpum amongst non-arboreal and Mimosa sp.,<br />
Syzyzium sp., Holoptelea, Ephedra sp., etc. <strong>of</strong><br />
arboreal. Pollen <strong>of</strong> Pinus roxburghii, transported to<br />
the site has also been recorded. Pollen <strong>of</strong> Dendropthoe<br />
falcata, the epiphyte Loranthaceae has also been<br />
recovered. Completed pollen analytical investigation<br />
<strong>of</strong> 4.00 m deep sedimentary pr<strong>of</strong>ile from Bagundi,<br />
another extinct salt lake, situated 30 km from<br />
Pachpadra town towards Barmer. Studies have<br />
revealed the dominance <strong>of</strong> non-arboreal over arboreal<br />
as witnessed in Pachpadra pr<strong>of</strong>ile. Most <strong>of</strong> the<br />
samples turned out non-productive, except for the<br />
upper part (0-90 cm) with blackish clay sediment.<br />
Finalized manuscript based on the studies <strong>of</strong> surface<br />
samples from Bagundi.<br />
C. Sharma & C. Srivastava<br />
Component 4 :Palaeomangroves and palaeoclimate in Andaman and Nicobar Islands during<br />
Quaternary Period<br />
Pollen analysis in ten samples (nos. 11-20) <strong>of</strong><br />
Quaternary section (BS-1595; 36,550 ±870 yr. BP)<br />
from R.K. Puram, Little Andaman was done. The<br />
palynodebris exhibited poor assemblage <strong>of</strong> pollen<br />
grains, fungal spores, fern spores, micr<strong>of</strong>oraminifera,<br />
etc. The pollen <strong>of</strong> Poaceae, Urticaceae, Acanthaceae,<br />
Fabaceae, Asteraceae, Cyperaceae, Oleaceae along<br />
with mangrove constituents (Rhizophora,<br />
Excoecaria, Heritiera) have been encountered in<br />
varying frequencies. Trilete and monolete fern spores<br />
were found in great abundance in some <strong>of</strong> the<br />
samples. Reworked striate, disaccate pollen <strong>of</strong> older<br />
horizons were also encountered.<br />
A. Khandelwal<br />
Pollen <strong>of</strong> Holoptelea integrifolia X 1000<br />
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