However, there is still a big gap in understanding the biology of the Gulf. This study
investigates the monthly fluctuations of the phytoplankton communities of the GSV. Biological, chemical and physical properties of the ecosystem were monitored over twelve months in order to assess and explain changes in species composition in relation to environmental conditions. This is the first study of its kind, simultaneously investigating the phytoplankton communities and their environment in this area and is essential to establish a baseline for future studies. This study took place in the vicinity of the recently built desalination plant off Port Stanvac (Figure 1), 30 km south of Adelaide (South Australia), Rucaparib cell line on the coast of
the GSV. The GSV is a large, relatively shallow (<40 m deep) inverse estuary with well mixed dense waters. Its main water circulation moves in a clockwise direction, with most open-ocean water entering through Investigator Strait and being expelled from the Gulf through the Backstairs Passage (Figure 1, Bye & Kämpf 2008). Shallow depths support broad subtidal seagrass meadows, intertidal sandflats, mangrove woodlands, samphire-algal marshes and supratidal Venetoclax OSBPL9 flats (Barnett et al. 1997). Depending on seasonal patterns, wind direction, temperature and salinity gradients, the flushing time of the entire volume of the Gulf is approximately four months (Pattiaratchi et al. 2006, Bye & Kämpf 2008). The GSV has restricted water exchange with the open ocean due to the dense upwelling of shelf waters at the mouth of the Gulf and Kangaroo Island that acts as a physical barrier, protecting the Gulf from high wave action (Middleton &
Bye 2007). Between January and December 2011, monthly samples were taken at the intake pipe (S1) and around the outfall saline concentrate diffusers (S2–S5) of the Adelaide Desalination Plant (ADP), with a total of 5 sites being sampled. The intake pipe and the outfall are located at a depth of 20 m and at a distance of 1300 m and 900 m from the edge of the shore respectively. At each site, samples were collected in triplicate at two depths, sub-surface (i.e. 1 m below the surface) and bottom (i.e. 1 m from the bottom ~ 18–19 m depth depending on weather and tide conditions). Vertical profiles of salinity (Practical Salinity Units, PSU) and temperature [°C] were obtained using a multi-parameter probe (66400-series YSI Australia, Morningside QLD) calibrated to a standard salinity solution before deployment.
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