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School of Engineering and Science - Jacobs University

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CHAPTER III<br />

Data analysis<br />

To monitor possible negative effects <strong>of</strong> our set-up technique on abundances we<br />

statistically compared microzooplankton communities at the start <strong>of</strong> the experiments in<br />

the mesocosms with the communities in the experimental bottles (t-tests) for<br />

differences. Insignificance was a requirement to apply the results <strong>of</strong> the experiments to<br />

the mesocosms. Regression analyses for the determination <strong>of</strong> k <strong>and</strong> g were conducted<br />

using “SigmaPlot 9.0” (SYSTAT S<strong>of</strong>tware); further statistical analyses were conducted<br />

using the s<strong>of</strong>tware “Statistica 7.1” (StatS<strong>of</strong>t), both at significance levels <strong>of</strong> 0.05. Values<br />

<strong>of</strong> g <strong>and</strong> k, F, I <strong>and</strong> E* obtained in the T. longicornis grazing experiments were tested<br />

against zero using two-tailed t-tests (Köhler et al., 1995).<br />

RESULTS<br />

Bloom dynamics in the laboratory <strong>and</strong> in the field<br />

The mesocosms were filled with water from the open North Sea at Helgol<strong>and</strong> Roads.<br />

On the 20.03.09 an inflow <strong>of</strong> nutrient-rich coastal water was detected in the field as seen<br />

by a decrease in salinity <strong>and</strong> increased SiO 2 <strong>and</strong> DIN (Figure 2a+b). Chlorophyll a<br />

concentration is measured via in situ fluorescence on a work-daily basis at the<br />

“Kabeltonne” station in the field (Wiltshire et al., 2008). When comparing field values<br />

to those in the mesocosms (Figure 2c), both blooms showed a similar development<br />

particularly at the beginning <strong>and</strong> during the last two weeks <strong>of</strong> the experiment when<br />

salinity reached the highest values. During the detection <strong>of</strong> a nutrient-rich waterbody <strong>of</strong><br />

lower salinity (20.-27.03.09) phytoplankton biomass in the field (“Kabeltonne”) showed<br />

values twice as high as in the mesocosms.<br />

Developments in the mesocosms<br />

Nutrients<br />

Within the first four days <strong>of</strong> bloom development phosphate (start 0.36 µmol L -1 ) <strong>and</strong><br />

silicate (start 4.75 µmol L -1 ) decreased rapidly to values below detection limit (< 0.01<br />

µmol L -1 ) <strong>and</strong> no remarkable relaxation from nutrient limitation could be observed<br />

during the course <strong>of</strong> the experiment. Dissolved inorganic nitrogen (DIN) dropped from<br />

around 14 µmol L -1 to around 7 µmol L -1 after the first week <strong>and</strong> remained at a level<br />

between 5 <strong>and</strong> 7 µmol L -1 during the rest <strong>of</strong> the experiment.<br />

72

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