Three humus profiles were sampled in moist grasslands on loamy sand, repres
enting a chronosequence of an acidifying ecosystem. Over the chronosequence
, earthworm activity decreased, from high activity to complete absence of e
arthworms. We studied the organic matter at three observation levels: the h
umus-profile, the aggregate and the soil organic matter (SOM)-fraction leve
l. With decreasing earthworm activity a trend in separation of organic and
mineral elements can be discerned. Humus forms changed from Vermimull via V
ermic Rhizomull to Rhizic Mullmoder. With decreasing earthworm activity, pa
rticulate organic matter (POM) first changes from intra- to extra-aggregate
POM, and accumulates completely on top of the mineral soil in the absence
of earthworms. The trend in vegetation that follows this changes in organic
matter morphology indicates that less nutrients become available with incr
easing acidification. The decrease in earthworm activity thus seems to be r
elated with an overall decrease of SOM and nutrient dynamics.