Abstract. Sediments play an important role in organic matter mineralisation
and nutrient recycling, especially in shallow marine systems. Marine
ecosystem models, however, often only include a coarse representation of
processes beneath the sea floor. While these parameterisations may give a
reasonable description of the present ecosystem state, they lack predictive
capacity for possible future changes, which can only be obtained from
mechanistic modelling. This paper describes an integrated benthic–pelagic ecosystem model developed
for the German Exclusive Economic Zone (EEZ) in the western Baltic Sea. The
model is a hybrid of two existing models: the pelagic part of the marine
ecosystem model ERGOM and an early diagenetic model by Reed et al. (2011).
The latter one was extended to include the carbon cycle, a determination of
precipitation and dissolution reactions which accounts for salinity
differences, an explicit description of the adsorption of clay minerals, and an
alternative pyrite formation pathway. We present a one-dimensional
application of the model to seven sites with different sediment types. The
model was calibrated with observed pore water profiles and validated with
results of sediment composition, bioturbation rates and bentho-pelagic fluxes
gathered by in situ incubations of sediments (benthic chambers). The model
results generally give a reasonable fit to the observations, even if some
deviations are observed, e.g. an overestimation of sulfide concentrations in
the sandy sediments. We therefore consider it a good first step towards a
three-dimensional representation of sedimentary processes in coupled
pelagic–benthic ecosystem models of the Baltic Sea.