This
project concerns the role of marine micro-organisms in the mineralization
of particulate (POM) and dissolved (DOM) organic matter and on the
regeneration of biogenic compounds (silicates, carbonates) in the meso-
and bathypelagic zones of the oceans. Actually, most of the information
concerning these processes comes from the epi-pelagic zone and/or does not
take into account the effect of increasing pressure with depth. Yet, it is
essential to integrate this process (as well as the associated decrease in
temperature) when studying oceanic organic matter (OM) mineralization.
The
LMGEM has not only a thorough knowledge but also the required equipment (hyperbaric
bottles and samplers, sinking particles simulator) developed in
collaboration with a private society (Métro-Mesures SA) that make it one
of the international leader laboratories on high-pressure studies in
microbial ecology.
A
double and innovative approach based on laboratory experiments and in situ
studies (ANTARES and DYFAMED sites, Mediterranean sea) will allow to
determine the effect of pressure on prokaryotes (e.g. community
structure), and on their activity (transformation and mineralization of
OM). Due to the high inputs of anthropic OM to the oceans (wind inputs,
rain falls, maritime transport), we will focus on the fate of both
biogenic and anthropic OM. In this context, petroleum hydrocarbons will be
considered as a model, as their fate in the meso- and bathypelagic zones
remain actually unknown.
The
proposed experiments will specifically allow to characterize and quantify
the effects of an increase in hydrostatic pressure and a decrease in
temperature on :
(i)
processes of OM mineralization (transformation of POC into DOC,
respiration, hydrocarbon biodegradation) and on the regeneration of
biogenic compounds (silicates, carbonates) in intermediary and deep
oceanic waters ;
(ii)
the structural ((phylo)genetic) and functional (activities) dynamics of
prokaryotic communities ;
(iii)
the flux of POM in the water column and the kinetic of particles
transformation in the mesopelagic zone ; these information will be
incorporated into a model describing the transformation of particles by
micro-organisms in the entire water column.