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12-14 September, 2011, Lucknow - Earth Science India

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National Conference on <strong>Science</strong> of Climate Change and <strong>Earth</strong>’s Sustainability: Issues and Challenges ‘A Scientist-People Partnership’<br />

<strong>12</strong>-<strong>14</strong> <strong>September</strong>, <strong>2011</strong>, <strong>Lucknow</strong><br />

INTERPLAY BETWEEN POLLEN AND EXTANT<br />

VEGETATION IN WETLAND ENVIRON OF LOWER<br />

BRAHMAPUTRA FLOODPLAIN OF ASSAM, INDIA<br />

Swati Dixit and S.K. Bera<br />

Birbal Sahni Institute of Palaeobotany, 53, University Road, <strong>Lucknow</strong> 226 007<br />

email: swatidixit26@gmail.com<br />

A total of twenty eight surface samples (9 dry soil samples and 19 mud samples)<br />

were procured from two major wetlands namely Hasila and Deepor beel of Goalpara<br />

and Kamrup Districts of Lower Brahmaputra valley, Assam. The samples were<br />

palynologically analyzed to determine the composition of pollen deposited on the<br />

surface sediments. The study predicts that inspite of partial coherence between modern<br />

pollen rain and extant vegetation due to differential pollen productivity, dispersal and<br />

deposition, pollen frequencies of surface samples somehow portrays the extant floral<br />

distribution in and around the wetland which is well evidenced from our studies where<br />

relative frequency of the assemblage includes local arboreals at the average value of<br />

42.94% and 28.53% at near proximity of forest, 24.27% and 18.97% at upland area and<br />

within 11% at submerged area of Deepor and Hasila wetland respectively. Thus, the<br />

surface samples from near proximity of the woods dominate in the arboreal pollen<br />

percentages which are quite relevant to extant floral composition. However, under<br />

representation of Shorea robusta as a dominant ingredient of nearby forest could be<br />

attributed due to poor preservation of its pollen in sediment despite its high<br />

productivity. Low profile of phytoplankton viz., diatoms/desmids indicates poor water<br />

condition and preservation status in the wetland sediments. The representation of fungal<br />

elements belongs to Deuteromycetes and Ascomycetes (grass pathogen) as evidenced<br />

by degraded pollen and spores are suggestive of biological degradation in wetland<br />

sediments. Therefore, there is a need to precisely observe the behavioural pattern of<br />

modern pollen deposition which could be helpful in inferring past climate and<br />

vegetation in and around the pristine wetland ecosystem.<br />

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