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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 />

26

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