These wetland areas are generally created by the accumulation of silt in areas with low currents. The silt deposits do happen quickly, which means that in many cases, these marshes are regaining ground from the sea, although the sea level is rising due to global warming.
Vegetation adapted to salty soils and sea spray is developing there. These are so-called halophilic plant species (adapted to salt) such as the Obione false-purslane (Halimione portulacoides, Aelen 1938) or the Salicornia (Salicornia sp.) which are specific to this environment.
Due to the high accumulation of silt, oxygen does not penetrate deep into the silt and plant debris is very little degraded. Thus, ecosystems retain the carbon taken up by plants through the process of photosynthesis.
The work carried out on salt marshes in the Pertuis Charentais (Charente Maritime and Vendée) has shown that these environments have the potential to process up to 8.8 TCO2eq/ha/year, which is the equivalent of the annual carbon footprint of a French person. These environments are therefore classified as carbon sinks, also called "blue carbon ecosystems" referring to the carbon retained by vegetated marine ecosystems.