1994-95 - Birbal Sahni Institute of Palaeobotany
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 />
Eight samples <strong>of</strong> Dangmal prol1le collected from thickets <strong>of</strong> mangrove forest at<br />
Bhitarkanika, Baitarni Della, Orissa have been palynologically investigated. The samples<br />
showed good assemblage <strong>of</strong> pollen grains, fungal spores, din<strong>of</strong>lagellate cysts, micr<strong>of</strong>oraminifera,<br />
Pediastrum, fern spores and Pseudoscltizea. The dominance <strong>of</strong> Rltizopltora,<br />
Sonneratia, Avicennia, Excoecaria, etc. were recorded. The other peripheral mangroves<br />
and hinterland taxa encountered in varying frequencies are Pandanus, Acacia, Aegialitis,<br />
Heritiera, Xylocarpus, Emblica, Xantltium, Brownlowia, Justicia, Casuarina, Poaceae,<br />
Rubiaceae, Lythraceae, Myrtaceae, Fabaceae, Urticaceae, Chenopodiaceael AmaranUlaceae,<br />
etc. The study reflects the existence <strong>of</strong> mangrove throve as Ule area enjoyed consistent<br />
marine" incursions.<br />
H.P. Gupta & Asha Khandelwal<br />
Nine samples numbering 166, 180, 184, 194, 197,201,206,208,210,218 from<br />
250 m deep pr<strong>of</strong>ile fTOmSadanandpur were pollen analysed. The samples are rich both<br />
quantitatively and qualitatively. The important mangrove constituents are represented by<br />
the members <strong>of</strong> Rhizophoraceae, Avicennia, Sonnera(ia, Excoecaria, Nypa and Brownlowia.<br />
The study has revealed the existence <strong>of</strong> constant depths <strong>of</strong> sea water leading to luxuriant<br />
mangrove throve.<br />
H.P. Gupta & R.R. Yadav<br />
Programme 7.4<br />
Objecrive<br />
Dendrochronology <strong>of</strong> temperate and tropical trees and seasonality<br />
<strong>of</strong> cambium activity<br />
To recollstruct climate (temperature alld precipitation) from<br />
free rings<br />
To study environmental factors determilling tlte seasonality <strong>of</strong><br />
cambium activity<br />
Ring widths <strong>of</strong> dated tree ring sequences <strong>of</strong> Abies pindrow collected from Dwali near<br />
Pindari glacier were measured. Tree growth has shown highly individualistic growth pattern<br />
which could be due to inter-tree competition and stand phase disturbances. Tree ring<br />
chronology further needs to be updated with more replication <strong>of</strong> samples from the area for<br />
climatic reconstluction.<br />
Tree ring samples <strong>of</strong> teak (Tectona grandis) collected from KOI-Li,Andhra Pradesh<br />
were dated and ling widths measured. A master chronology (1872-1989 AD) was prepared<br />
from nine samples. Tree growth and climate relationship using response function analysis<br />
has shown very good correlation between tree growth and summer precipitation.<br />
Fifteen u·cc core samples <strong>of</strong> spluce collected from Dodital in Uttarkashi were dated<br />
using Skeleton plot method. Trees have been found 10 be around 300 years in age. Tree core<br />
samples <strong>of</strong> deodar collected from different areas around Gangotri were also dated. Age <strong>of</strong><br />
trees has been found to be around 500 years in Gangotri.<br />
R. R. Yadav & Amalava Bhattacharyya<br />
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