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Mireille Consalvey PhD Thesis - University of St Andrews

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increasing PPFD; first an apparent decrease in the cross-sectional area <strong>of</strong> the<br />

thylakoid membranes and then a downwards migration at PPFD > 600 ýImol M-2<br />

s-1. The differential responses <strong>of</strong> taxa to high light intensities may lead to<br />

structured bi<strong>of</strong>ilm communities, and may help maintain high primary<br />

productivity rates (for the whole bi<strong>of</strong>ilm), despite potentially damaging light<br />

intensities.<br />

An increase in the surface maxima relative to the downwelling PPFD has<br />

been described by many authors (Lassen et al. 1992; Kiffil et al. 1994,1996) but<br />

was not seen in this study. This may be attributed to the dense bi<strong>of</strong>ilms, sediment<br />

characteristics (see section 6.1) or the sampling technique. Determining the<br />

sediment surface is a key aspect <strong>of</strong> microscale analysis and one that is seldom<br />

discussed in the literature. The LTSEM images demonstrated the highly<br />

heterogeneous nature <strong>of</strong> the sediment/bi<strong>of</strong>ilm. Figure 6.23 shows a Gyrosigma<br />

cell emerging through a naviculoid layer and opens the question where does the<br />

surface start? This question is particularly relevant when considering cells such<br />

as GyrosigmalPleurosigma sp. that are as large as the sampling interval (100<br />

ýjm). In reality sampling will start somewhere between the two extremes and is<br />

not possible to determine without correlative microscopic examination.<br />

Figure 6.23: Gyrosigma Sp. emerging (Arlesford Creek 1999). Scale bar = 50<br />

pm. Arrows indicate possible bi<strong>of</strong>ilm. surface.<br />

185

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