Ecosystems are complex and often require complex models if their detailed b
ehaviour is to be replicated. However, such complex models are difficult to
analyse due to their nonlinearities and the large number of parameters tha
t most such models have. One approach that allows greater understanding of
basic process is the development of simplified models. We have developed a
series of simple models describing alternative formulations of a coastal ec
osystem, as a tool to aid development and analysis of more sophisticated mo
dels. Sediment biogeochemistry plays a critical role in many coastal ecosys
tems, and much of the nitrogen input load is lost through denitrification,
provided eutrophication has not set in. We have dealt with the sediment and
water column response separately in simple models by exploiting the differ
ent time scales of sediment and water column response. In simple water colu
mn models, we have considered a variety of common formulations of phytoplan
kton-zooplankton interactions, and their implications for the steady-state
response of phytoplankton and nutrients to increased nutrient load. For mos
t formulations, we have derived explicit formulae linking model parameters
to predicted mean, steady-state concentration and biomass. The simple model
results provide considerable insight into the response of the bay to chang
es in nutrient load. In particular, the sediment model identifies a maximum
denitrification capacity for the bay. Once loads exceed this capacity, den
itrification declines, and nutrients are instead lost through export. This
decline in denitrification results in a switch from mesotrophic to eutrophi
c conditions. The water column model analysis confirms the importance of th
e zooplankton mortality formulation in N-P-Z models in determining the depe
ndence of steady-state phytoplankton biomass on nutrient load, and the stab
ility of steady-state solutions. (C) 1999 Elsevier Science B.V. All rights
reserved.