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Mireille Consalvey PhD Thesis - University of St Andrews

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6.1.3. Examining primary productivity on intertidal mudflats<br />

Despite limited periods <strong>of</strong> light exposure (Ser6dio and Catarino 1999)<br />

and highly variable temperature conditions (Blanchard and Guarini 1996;<br />

Ser6dio and Catarino 1999) estuarine microphytobenthos have been recorded to<br />

contribute up to 1/3 <strong>of</strong> the total estuarine carbon budget (Sullivan and Moncrieff<br />

1988; Sundback et al. 1997; see Underwood and Kromkamp 1999 for further<br />

discussion). Guarini et al. (2000) discussed the "vertical scale compression<br />

problem" whereby photosynthetic activity is limited to the upper gm. It is the<br />

problems associated with sampling at this scale that has hindered progress in this<br />

field compared to pelagic systems as well as the daily changes In photon fluence<br />

rates, temperatures and the migration <strong>of</strong> cells in and out <strong>of</strong> the photic zone<br />

(discussed above). Therefore, the inherent variation in microphytobenthic<br />

primary productivity patterns (seasonal and hourly) (Kromkamp et al. 1995;<br />

Barranguet 1997) complicates any extrapolations/estimations.<br />

Guarini et al. (2000) examined the behavioural and physiological<br />

processes that control primary productivity on intertidal mudflats, proposing and<br />

verifying a simple model <strong>of</strong> primary productivity and biomass changes over the<br />

exposure penod. The authors concluded that temperature was the prominent<br />

feature controlling the dynamics <strong>of</strong> benthic primary production, but discussed the<br />

key role <strong>of</strong> light in controlling the migration <strong>of</strong> phototrophs to the sediment<br />

surface. They separated the sediment bi<strong>of</strong>ilm into two compartments: surface and<br />

sub-surface and hypothesised the surface component to be saturated with<br />

biomass and having a continuous light distribution.<br />

Pinckney and Zingmark (1991) attributed daily variations in primary<br />

production to changes in the distribution <strong>of</strong> biomass related to tidal stage and sun<br />

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