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Mireille Consalvey PhD Thesis - University of St Andrews

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v vs. 11011-IT . ratory hiolilms<br />

-Mm-'ratol<br />

seem that the microphytobenthic assemblage samples were less migratory than<br />

those seen previously. This may reflect a shift in species and would require<br />

further investigation, but at this stage the hypothesis 7 must be rejected.<br />

The light utilisation efficiencies <strong>of</strong> natural and artificial b1<strong>of</strong>ilms<br />

significantly declined after 90 min <strong>of</strong> treatment. However, there was evidence <strong>of</strong><br />

recovery in the natural bi<strong>of</strong>ilms during a 15 min dark adaptation period in<br />

samples from the low and medium light condition. This was not found in the<br />

high light condition and therefore light history did significantly affect the light<br />

utilisation efficiency. In artificial bi<strong>of</strong>ilms cells from the medium and high light<br />

conditions did not recover and this may reflect the inability <strong>of</strong> cells to migrate<br />

into the sediment, therefore cells in the artificial bi<strong>of</strong>ilm were receiving more<br />

light than cells in the sediment bi<strong>of</strong>ilm.<br />

Hypothesis 8: 15 min <strong>of</strong> dark adaptation will lead to a significant decrease in the<br />

minimum fluorescence yield and significant increases in the maximum<br />

fluorescence yield and light utilisation efficiencies<br />

No decline in the minimum fluorescence yield was found in the artificial<br />

bi<strong>of</strong>ilm but there was a significant decrease in sediment cores, suggesting QA<br />

oxidation or migration. As no decline was seen in ar-tificial bi<strong>of</strong>ilms, migration<br />

may be implicated as the most probable reason, but further investigation is<br />

necessary. There was an increase in the maximum fluorescence yield in the<br />

artificial bi<strong>of</strong>ilm but no change was seen during 15 min <strong>of</strong> dark adaptation in the<br />

sediment cores. It is possible that migration was occurring in the sediment cores,<br />

therefore obscuring any increase associated with NPQ reversal. Regardless, in<br />

223

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