The area of salt marshes does no longer increase. The recent erosion c
oincides with a rise on MHT-level in the last 25 years. Despite the de
crease in area, sedimentation continues, especially in the lower salt
marsh, which acts as a sink of nitrogen. Assimilation and mineralizati
on of nitrogen are in balance in most plant communities along the grad
ient from lower to higher salt marshes. Mineralization of nitrogen inc
reases towards the higher salt marsh, whereas the above-ground product
ion and the mean nitrogen content of plants decrease. There is a posit
ive correlation between quality of food plants in salt marshes and bre
eding success of Brent geese in the arctic tundra.Sedimentation on mai
nland salt marshes can compensate for the expected sea level rise. Thi
s is not the case for island salt marshes, if the relative sea level r
ise is more than 0.5-1.0 cm yr-1. The natural succession on salt marsh
es results in an accumulation of organic material, which is related to
the dominance of single plant species. It is not clear to which exten
t this process is enhanced by eutrophication from acid deposition and
seawater. Human exploitation of unprotected salt marshes is old and he
avy in the system of mound settlements. Reclamation rates by dikes in
the last centuries were higher than the rate of area increase.Grazing
by cattle as a management practice results in both a higher plant spec
ies-richness and community diversity than abandoning; hay-making is in
termediate, but shows less structural diversity than grazing with low
stocking density. The invertebrate fauna is favoured by a short period
of abandoning, but eventually characteristic salt marsh invertebrates
are replaced by inland species. Many bird species prefer grazed salt
marshes.The final section gives some perspectives. Provided that no fu
rther embankments take place the optimal nature management option for
plants and animals is a vegetation pattern, which includes areas with
a low canopy (grazed) and areas with a tall canopy.