CONICET | Buscador de Institutos y Recursos Humanos

The underwater light climate has important effects on primary producers. The aim of this research was to evaluate its variability in a turbid river-floodplain system. Photosynthetically active radiation (PAR) was measured in the Middle Paraná River during different hydrological phases to (a) analyse the photosynthetically active radiation attenuation coefficient (k) and euphotic depth (Z eu ) as well as their associations with optically active components and (b) develop and evaluate indices and regression models based on Secchi disc (SD) measurements to estimate k and Z eu . Values of k were higher in the fluvial system than in the floodplain and during low-water stage than high-water stage. Particulate components controlled the light climate variability. Chromophoric dissolved organic matter and chlorophyll-a had significant effects during floods. The estimation of k and Z eu was sensitive to temporal but not to spatial variations. The highest prediction accuracy was observed when using specific non-linear regressions for each hydrological phase, especially for Z eu estimation (low stage: k = 1.76 × SD −0.80 , Z eu = 2.62 × 1/SD −0.80 ; high stage: k = 2.04 × SD −0.53 , Z eu = 2.26 × 1/SD −0.53 ). The indices k × SD and Z eu /SD were significantly different from those proposed for clear water environments. It is concluded that temporal variations should be considered when estimating k and Z eu in turbid river-floodplain systems because of the temporal heterogeneity in optically active components. Considering that ecological implication of the light climate depends on Z eu :depth ratio, we propose to estimate Z eu instead of k. Finally, indices proposed for clear water environments are not recommended to be applied to turbid environments.

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