INVESTIGATION ON THE PHYSIOLOGICAL ECOLOGY OF PHYTOPLANKTON IN THE SUNDERBAN MANGROVE ENVIRONMENT, NW COAST OF BAY OF BENGAL
Man
Power:
1 Research Fellow and 1 Field Asst.
Tenure: 3 Years
Objectives:
i.
To study the effect of changes in external forcing and boundary
conditions on the blooming condition of different species of phytoplankton.
ii.
To study the exchanges of gases i.e. CO2, CH4, NOx
between air and coastal water during succession and blooming of different
phytoplankton species and estimation of their net fluxes
iii.
To study the impact of eutrophication on phytoplankton productivity.
iv.
To determine the conditions for maximum species diversity of
phytoplankton to occur and its relation to pollution index.
v.
To critically examine the availability of Fe, Mn, Al etc. thorough the
complexation with naturally occurring ligands such as humic acids and its
relation to eutrophication.
vi.
To study the number of types of organisms which are able to survive in
eutrophic system and consider predator – prey model.
vii.
Application of model to explain the CO2 exchange flux in the
air water interface.
Findings:
i.
Maximum number of phytoplanktons were observed during blooming time
(February)
ii.
Net negative flux of CO2 was also observed during monsoon at
Jambu and Thakuran
iii.
Emission rate of CO2 and
CH4 showed a considerable diurnal variations and between the Lothian
Island the atmosphere were found to be 113.06 and 1.51 kg/d respectively.
iv.
Average primary productivity was found to be 32-83 mg C m –2
h –1 .
Publications:
i.
Impact of Sunderban Mangrove biosphere on the Carbon dioxide and methane
mixing ratios at the NE coast of Bay of Bengal, India, Atmospheric Environment,
Elsevier Publication.
ii.
Biogenic controls on the air-water carbon dioxide exchange in the
Sunderban mangrove environment, NE coast of Bay of Bengal, India. Limnology and
Oceanography, 2004(49):95-101.
Benefits:
This
finding would help to find answer of the basic question that “ Are the
world’s coastal oceans being changed from systems with predominantly internal
cycles of production and consumption to systems which are based more on external
inputs of organic carbon”.