The successional stages of Baltic Sea zoobenthos were analysed along a
south/north transect (Belt Sea, northern Danish straits to the Bothni
an Sea) in relation to a proposed conceptual model of succession. The
model predicts five successional stages ranging from diverse communiti
es to dead bottoms. Stage I: 'climax community' dominated by deep-burr
owing species, and a deep RPD-layer, II: first signs of stress, strong
fluctuations, decreasing species richness, increased biomass/producti
on, and an elevated RPD-layer, III: dominated by small polychaete worm
s (or their ecological equivalents), and the RPD-layer close to the se
diment/water boundary layer, periods of hypoxia, IV: long periods of h
ypoxia and formation of bacterial mars (Beggiatoa spp.) at the sedimen
t surface, no permanent benthic macrofauna, V: complete break-down of
benthic communities due to long-term anoxia, lamination of sediments.
Differences in successional sequences between basins and vertical zone
s (supra- and sub-halocline) are documented, and general trends are di
scussed in relation to changes on a geological time-scale.