Phytoplankton are unicellular
photosynthetic plants that exist as single motile and non-motile
cells or as chains of cells and are important ecologically and economically.
Small-scale distribution of species is primarily determined by physical
and chemical environmental factors. They form the basis of most
marine food webs and have significant influence on nutrient cycling
and hence water quality. Phytoplankton generally go unnoticed until
a 'bloom' occurs, when physical conditions concentrate cells to
very high levels or increased light and/or nutrient availability
allows the dense growth of a single species resulting in water discolouration
and a decline in ecosystem health may occur. Nutrient and light
availability are "bottom-up' controls on phytoplankton productivity
and biomass.
To date 145 phytoplankton species have been reported from Moreton
Bay, including diatoms (Bacillariophyta), dinoflagellates (Dinophyta)
and cyanobacteria (Cyanophyta), as well as other small flagellate
groups (Cryptophyta, Chlorophyta and Euglenophyta).
These groups are typical of variable salinity estuarine environments.
Zooplankton are non-photosynthetic protist or animal plankton which
have heterotrophic nutrition (i.e., they require carbon already
fixed into organic molecules). Although capable of swimming movement
their large-scale distribution is dictated by water motion. Zooplankton
includes protists (unicellular organism), microscopic animals (copepods),
jellyfish and larvae of fish and shellfish, which spend only a part
of their life in the water column as plankton. Zooplankton graze
on phytoplankton providing a 'top-down' control on phytoplankton
biomass, an interaction that varies according to the dominance of
the controlling bottom-up mechanisms of light and nutrients.
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