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Hypotheses:
1)
Increase in hydrostatic pressure conditions alters bacterial
mineralization rates and slows down the decomposition of particle during
their fall throughout the water column. This affects (a) the quality of
DOM released into the seawater, thus modifying the growth of pelagic
bacteria, and (b) the dissolution rate of mineral ballasts (silicate,
carbonate and dust). Dissolution of mineral ballast would affect the
sinking rate of particles.
2)
Hydrostatic pressure condition alters the species composition of
prokaryotes communities associated with
sinking particles. This succession in microbial communities alters
biogeochemical processes exerted by prokaryotes on the particles. This
affects mineralization processes throughout intermediate and deep-sea
water masses, and the pelagic-benthos coupling, and thus the flux and the
quality of organic inputs for intermediate, deep-sea and benthic microbial
communities.
Objectives:
1)
To quantify effects of increasing hydrostatic pressure on microbiological
processes of organic matter mineralization (POC
DOC transformation) and regeneration of
biogenic elements (silicates, carbonates) within intermediate and deep-sea
waters. These biogeochemical processes affect organic inputs throughout
the intermediate and deep-sea water masses and the coupling between
the pelagic zone and the benthos.
2)
To determine effects of hydrostatic pressure on prokaryotic species
composition ( Bacteria and
Archaea) using DGGE (or
T-RFLP) and
FISH during sinking simulation experiments and in "neutrally buoyant
floc" (atmospheric pressure) experiments.
3)
To study effects of hydrostatic pressure on the dynamics of prokaryotic
community composition and activities. The microbial "black box"
should not be regarded as homogeneous. Micro-FISH method breaks down this
black box with fluorescent 16S rRNA probes and simultaneously determines
DOM uptake by each prokaryotic subgroup.
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