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Inshore
Friday 5th July
We spent the 
day on the RV Falcon Spirit 
collecting oxygen, salinity, and 
temperature, as well as zooplankton and 
phytoplankton. The data collected was
then analysed in a wet lab session the 
following day.

All opinions expressed are of our own, and not of the University of Southampton

Introduction

Seven stations were sampled on the lower part of the Tamar Estuary.


The River Tamar’s source is at Woolley Moor which is located 6km from the north Cornish coast, the River, however, flows South for 98km before reaching the coast at Plymouth. The River Tavy and Lynher River flow into the River Tamar close to the estuary. The Tamar estuary is a ria estuary, with its upper parts having a very well developed salinity gradient, making it a very good example of changing estuarine communities with changing salinity regime. It is also one of the few estuaries where zonation of intertidal and subtidal rocky habitats can be observed along an estuarine gradient.


The fieldwork was conducted on an ebb tide stating after high tide of 5.31m at 07.35 UTC and finished before low tide at 13.44 UTC of 0.79m. There was a wind force of 2 in an ESE direction with good visibility.




At the first station, two niskin bottles were fired from a CTD-  these came from the surface and near the seabed as bottle use was limited. Beyond this station, the triggering mechanism failed so a single surface water sample for each station was taken from the inline water pump onboard the vessel. Samples were used for silicate, phosphate, nitrate/nitrite, and chlorophyll measurements. A single phytoplankton sample was taken from the first niskin bottle samples but no further phytoplankton sampling could be continued once the CTD failed. Oxygen was also unable to be taken due to the CTD issues.


Silicate, Phosphate, Nitrate/Nitrite

Water samples were filtered and syringed into bottles for lab analysis. Samples were auto-analysed in a QuAAtro39 machine in order to get concentrations for silicate, phosphate and nitrate/nitrite. Standard protocol was followed from Grasshoff et al., 1983 to add reagents to create colorimetric complexes; Nitrite and total nitrite (nitrite and reduced nitrate) formed purple complexes, phosphate and silicate formed blue complexes. These were measured at the appropriate wavelengths. (Grasshoff, et al 1983).


Chlorophyll

3x50ml samples from each niskin bottle were filtered simultaneously on a filtering rig. Filter paper was collected and stored in acetone. These bottles were labelled and stored in a freezer in the lab overnight, with the freezer acting as a sonicator. This bursts the phytoplankton cells which are adhering to the filter paper causing the chlorophyll to be released into the acetone solution. The test tubes are then removed from the freezer, and then filter paper is removed as there should be no more chlorophyll attached to it. For each sample, the acetone solution must be placed into a new test tube, and this test tube is then placed into the fluorometer. The lid is then placed on, and the test is run. The chlorophyll concentration is then given in µg/L. This must then be converted to the total chlorophyll concentration at each site by the following equation:










Methodology

Encyclopedia Britannica. (2019). River Tamar | river, England, United Kingdom. [online] Available at: https://www.britannica.com/place/River-Tamar-England [Accessed 10 Jul. 2019].


Sac.jncc.gov.uk. (2019). Plymouth Sound and Estuaries - Special Areas of Conservation. [online] Available at: https://sac.jncc.gov.uk/site/UK0013111 [Accessed 10 Jul. 2019].

Tidetimes.org.uk. (2019). Plymouth (Devonport) Tide Times for 5th July 2019 |

TideTimes.org.uk. [online] Available at: https://www.tidetimes.org.uk/plymouth-devonport-tide-times-20190705 [Accessed 11 Jul. 2019].



The samples were then transferred to the waste bucket after use.


Phytoplankton

The collected sample was not analysed as it gave no meaningful context as a standalone sample for the whole river transect.