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Pontoon Time Series
A time series was taken at the King Harry Pontoon to enable us to look at variability, both temporally and spatially.
Temperature decreases consistently over depth
Dissolved Oxygen is higher on the surface than at depth
pH remains relatively constant through the time series
Salinity increases with depth
The flooding tide brings with it an influx of saltwater which is evident from the more Saline seawater pushing up into the middle and upper layers
Chlorophyll concentrations increase with depth
Estuary
The flow speed is much higher and more turbulent further upstream
The flow speed is relatively low at the mouth of the estuary
Dissolved Oxygen Saturation varies very little between stations
Chlorophyll increases with depth due to a more stratified upper layer and nutricline thus optimal growth being at lower light but higher nutrients
Offshore
Throughout the day the water column remained stratified.
Dissolved oxygen increased rapidly throughout the morning and decreased slowly in the afternoon.
Disparity between deep and shallow silicon and phosphate concentration was greater at the end of the sampling period (at 14:13 UTC) than at the start (08:38).
Negative correlation was found between chlorophyll and silicon concentration.
A deep chlorophyll maximum (DCM) occurred at 30m between 11:48 and 13:05 (UTC).
Thermocline was around 10-
Salinity remained fairly constant with depth.
Dissolved oxygen peaked in the DCM.
Turbidity increased with depth below 20m.
Pseude-
Geophysics
The side-
The closest classification of the habitat type from the grab was ‘Infralittoral coarse sediment’ (SS. SCS. ICS).
The habitat could not be fully identified, as none of the most abundant species were present in the grab.
The most dominant species that were found in this habitat were Crepidula femicata and Echinodesmata Asterias Reubens