Emiliania huxleyi (Lohmann) Hay et Mohler is represented as a state va
riable in a general phytoplankton model that also includes one diatom
group and one phytoplankton group encompassing the 'other flagellates'
than E. huxleyi. Furthermore, three nutrient variables (nitrogen-, ph
osphorus-, and silicon-nutrients) are included. The main features of t
he model are that E. huxleyi has been given a higher growth affinity f
or orthophosphate than the two other groups, and that diatoms, besides
being dependent on silicon, have been given a higher maximal growth r
ate than the two flagellate groups. The output from the simulation mod
el is compared with observations made in mesocosm experiments loaded w
ith different amounts of nitrate and orthophosphate. The simulated E.
huxleyi is not able to grow as well as the real E. huxleyi, and this a
pplies especially to the experiments low in orthophosphate. It is diff
icult to account for the high observed numbers of E. huxleyi in terms
of the available inorganic othophosphate in these experiments. The lit
erature, however, gives some evidence that E. huxleyi is able to utili
se organic phosphorous sources. By assuming an organic phosphorus sour
ce that adds phosphorus to the orthophosphate pool, however, the fit b
etween the model and the observations is improved. Furthermore, simula
tions indicate that the phosphorus originating from organic substances
should be more available for the E. huxleyi than for the other groups
. In simulation models this is achieved by defining a higher E. huxley
i uptake affinity for orthophosphate, but it may also be assumed that
the orthophosphate originating by enzymatic activity on organic substa
nces are spatially (at the scale of the uptake process) more close to
the E. huxleyi cell than to the other phytoplankters present in the wa
ter body.