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anglicky - Institute of Hydrobiology

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seasonal selection <strong>of</strong> taxa within the mixed reservoir species pool, is substantially<br />

strengthened by the presence <strong>of</strong> spatially heterogeneous egg banks.<br />

3.9 Spatial heterogeneity and seasonal succession <strong>of</strong> phytoplankton along the<br />

longitudinal gradient in the Římov Reservoir<br />

In order to evaluate the effects <strong>of</strong> contrasting hydrological scenarios on the spatial and<br />

temporal heterogeneity <strong>of</strong> phytoplankton in a reservoir, P. Rychtecký<br />

(rychtecky.pavel@post.cz) and P. Znachor studied seasonal changes in various parameters<br />

along the longitudinal axis <strong>of</strong> the canyon-shaped, eutrophic Římov Reservoir (Czech<br />

Republic) at 1–2 week intervals from April to October 2007. Vertical chlorophyll and<br />

temperature pr<strong>of</strong>iles were measured and functional classification <strong>of</strong> phytoplankton was<br />

applied.<br />

Fig. 3: Temporal variation in vertical pr<strong>of</strong>iles <strong>of</strong> chlorophyll a (mg l –1 , obtained with a submersible<br />

fluorescence probe) at SITE 4 (upper panel) and DAM (lower panel) representing typical<br />

transition and lacustrine parts <strong>of</strong> the Římov Reservoir, respectively. Arrows indicate temporal<br />

dominance <strong>of</strong> a particular functional group in the phytoplankton.<br />

At the river inflow, phytoplankton markedly differed from the rest <strong>of</strong> the reservoir, being<br />

dominated by functional groups D and J (pennate diatoms and chlorococcal algae) without a<br />

clear seasonal pattern. From April to mid-June, groups Y and P (large cryptophytes and<br />

colonial diatoms) prevailed in the whole reservoir (Fig. 3). Phytoplankton spatial<br />

heterogeneity was most apparent during the summer, reflecting a pronounced gradient <strong>of</strong><br />

environmental parameters from the river inflow to the dam (e.g., decreasing nutrients,<br />

increasing light availability, etc.). A dense cyanobacterial bloom (groups H1 and M)<br />

developed in the nutrient-rich transition zone, while functional Group N (desmids) dominated<br />

the phytoplankton at the same time at the dam area (Fig. 3).<br />

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