In wet dune slacks a pioneer situation can exist for a long time. One of the causes for this slow-down of the succession could be the existence of a microbial mat. The upper layer of the mat, consisting of algae and cyanobacteria, develops a tough layer due to excretion of extracellular polymeric substances. Moreover the CO2 fixation and sulfate reduction cause the pH to raise and therefore calcium carbonate is precipitating which strenghtens the top layer still more. Due to respiration of heterotrophic bacteria the oxygen concentration in the soil is diminishing. The redox potential will decrease and sulfate will be used as an electronacceptor. It is then reduced to toxic sulfide. It is assumed that pioneer species can cope better with the...