Inland dunes in northwestern Europe support a number of dry vegetation
types. These ecosystems are poor in nutrients and it has been suggest
ed that accumulation of nutrients triggers succession in such systems.
We studied the accumulation of organic matter and N and P over a 30 m
onths period in two adjacent ecosystems, the Spergulo-Corynephoretum a
nd the Genisto-Callunetum. Amounts of plant matter and soil organic ma
tter significantly accumulated during the sampling period in the Genis
to-Callunetum but not in the Spergulo-Corynephoretum. While nutrient c
oncentrations of live and dead phytomass in the Spergulo-Corynephoretu
m were significantly higher than in the Genisto-Callunetum, total nutr
ient contents in the systems showed the opposite pattern. N and P conc
entrations in litter were relatively high compared with the other frac
tions of plant matter and the amount of N significantly increased in b
oth ecosystems during the sampling period. Soil moisture contents show
ed a seasonal pattern. It was highest in the top soil layer and higher
in the Genisto-Callunetum than in the Spergulo-Corynephoretum. The es
timated annual increase of total N in these two ecosystems was consist
ent with rates of atmospheric N deposition (wet fall + dry fall) measu
red in comparable Dutch sites.