International audienceIt is widely recognized that organic carbon exported to the ocean aphotic layer is significantly consumed by heterotrophic organisms such as bacteria and zooplankton in the mesopelagic layer. However, very little is known for the trophic link between bacteria and zooplankton or the function of the microbial loop in this layer. In the northwestern Mediterranean, recent studies have shown that viruses, bacteria, heterotrophic nanoflagellates, and ciliates distribute down to 2000 m with group-specific depth-dependent decreases, and that bacterial production decreases with depth down to 1000 m. Here we show that such data can be analyzed using a simple steady-state food chain model to quantify the carbon flow from bacteria...
The bacterial loop, the consumption of dissolved organic matter (DOM) by bacteria and subsequent tra...
Atmospheric levels of carbon dioxide are tightly linked to the depth at which sinking particulate or...
To understand (1) the role of heterotrophic bacteria in the biogeochemical cycles, (2) the fate of t...
It is widely recognized that organic carbon exported to the ocean aphotic layer is significantly con...
Carbon budgets of the mesopelagic zone are poorly constrained, highlighting our lack of understandin...
In this study, we carried out dilution experiments at the surface and in the mesopelagic and bathype...
The downward flux of particulate organic carbon (POC) decreases significantly in the oceanÂs mesopel...
We have investigated here the structure of the pelagic microbial food web and quantified the carbon ...
Factors controlling the community composition of marine heterotrophic prokaryotes include organic-C,...
Sinking organic particles transfer ∼10 gigatonnes of carbon into the deep ocean each year, keeping t...
In linear food chains, resource and predator control produce positive and negative correlations, res...
International audienceThe microbial food web structure, the carbon flux between mesozooplankton and ...
International audiencePlanktonic microbial communities often appear stable over periods of days and ...
The vast majority of marine dissolved organic carbon (DOC), the largest reservoir of reduced carbon ...
The oceans’ biological pump (BP) exports large amounts of particulate organic carbon (POC) to the me...
The bacterial loop, the consumption of dissolved organic matter (DOM) by bacteria and subsequent tra...
Atmospheric levels of carbon dioxide are tightly linked to the depth at which sinking particulate or...
To understand (1) the role of heterotrophic bacteria in the biogeochemical cycles, (2) the fate of t...
It is widely recognized that organic carbon exported to the ocean aphotic layer is significantly con...
Carbon budgets of the mesopelagic zone are poorly constrained, highlighting our lack of understandin...
In this study, we carried out dilution experiments at the surface and in the mesopelagic and bathype...
The downward flux of particulate organic carbon (POC) decreases significantly in the oceanÂs mesopel...
We have investigated here the structure of the pelagic microbial food web and quantified the carbon ...
Factors controlling the community composition of marine heterotrophic prokaryotes include organic-C,...
Sinking organic particles transfer ∼10 gigatonnes of carbon into the deep ocean each year, keeping t...
In linear food chains, resource and predator control produce positive and negative correlations, res...
International audienceThe microbial food web structure, the carbon flux between mesozooplankton and ...
International audiencePlanktonic microbial communities often appear stable over periods of days and ...
The vast majority of marine dissolved organic carbon (DOC), the largest reservoir of reduced carbon ...
The oceans’ biological pump (BP) exports large amounts of particulate organic carbon (POC) to the me...
The bacterial loop, the consumption of dissolved organic matter (DOM) by bacteria and subsequent tra...
Atmospheric levels of carbon dioxide are tightly linked to the depth at which sinking particulate or...
To understand (1) the role of heterotrophic bacteria in the biogeochemical cycles, (2) the fate of t...