Abstract:In the present paper, we list and document the relevant behavioral and physiological processes controlling primary productivity of epipelic microalgae on intertidal mudflats in order to develop a simplified model. We first propose, in an attempt to characterize the 'photosynthetically active biomass' of the epipelic community, a new approach to describe the photic environment at the sediment surface, by substituting a discrete 2-layer model in place of continuous vertical light distribution. This concept thus … Show more
“…In addition to mobility restrictions, the proportion of silt determines the degree of sediment pore space Wlling, and thus the upper size limits of interstitial species (Schwinghamer, 1981). However, we expect diatom grazers to be mainly active at the sediment surface as a typical mudXat bioWlm is most pronounced near the sediment surface, where diatoms and other phototrophs give rise to an eYcient primary production (e.g., Decho, 2000;Guarini, Blanchard, Gros, Gouleau, & Bacher, 2000). In essence, the feeding eYciency of the two harpacticoid copepod species may be favoured when grain size is increasing, as seen in our experiment.…”
Estuarine soft sediments support a diverse group of eukaryotic and prokaryotic organisms though the role of the sediment per se for the functioning of these organisms remains largely unknown. The present study aimed to test the eVect of sediment grain size on the grazing activities of harpacticoid copepods. In controlled experiments, two common intertidal harpacticoid species (Paramphiascella fulvofasciata and Nitokra spinipes) were each oVered a mix of two benthic diatom species (Navicula phyllepta and Seminavis robusta) in diVerent sedimentary conditions. Several microcosms were created using a variety of sediment types, including Wne silt (<63 m), coarser grained sands (125-250, 250-450, 100-300 m), artiWcial 'sediments' of glass beads (250-500, 2000 m) and even the absence of sediment was tested. The diatoms were enriched in the stable carbon 13 C to facilitate tracing in the harpacticoids. Both copepod species were able to graze on the diatoms with highest uptake when sediment was absent. In contrast, both harpacticoid species showed no uptake in silty conditions. In general, grazing was favoured when mean sediment grain size increased. The strong negative eVect of Wne grains on the grazer's eYciency can be explained by the resulting diVerences in the structure (and accessibility) of the diatom bioWlm on the one hand and the mobility of the grazer on the other hand. In view of the subtle equilibrium between primary producers and grazers, these results might have important implications for the eVect of siltation of tidal Xats due to, e.g., human activities.
“…In addition to mobility restrictions, the proportion of silt determines the degree of sediment pore space Wlling, and thus the upper size limits of interstitial species (Schwinghamer, 1981). However, we expect diatom grazers to be mainly active at the sediment surface as a typical mudXat bioWlm is most pronounced near the sediment surface, where diatoms and other phototrophs give rise to an eYcient primary production (e.g., Decho, 2000;Guarini, Blanchard, Gros, Gouleau, & Bacher, 2000). In essence, the feeding eYciency of the two harpacticoid copepod species may be favoured when grain size is increasing, as seen in our experiment.…”
Estuarine soft sediments support a diverse group of eukaryotic and prokaryotic organisms though the role of the sediment per se for the functioning of these organisms remains largely unknown. The present study aimed to test the eVect of sediment grain size on the grazing activities of harpacticoid copepods. In controlled experiments, two common intertidal harpacticoid species (Paramphiascella fulvofasciata and Nitokra spinipes) were each oVered a mix of two benthic diatom species (Navicula phyllepta and Seminavis robusta) in diVerent sedimentary conditions. Several microcosms were created using a variety of sediment types, including Wne silt (<63 m), coarser grained sands (125-250, 250-450, 100-300 m), artiWcial 'sediments' of glass beads (250-500, 2000 m) and even the absence of sediment was tested. The diatoms were enriched in the stable carbon 13 C to facilitate tracing in the harpacticoids. Both copepod species were able to graze on the diatoms with highest uptake when sediment was absent. In contrast, both harpacticoid species showed no uptake in silty conditions. In general, grazing was favoured when mean sediment grain size increased. The strong negative eVect of Wne grains on the grazer's eYciency can be explained by the resulting diVerences in the structure (and accessibility) of the diatom bioWlm on the one hand and the mobility of the grazer on the other hand. In view of the subtle equilibrium between primary producers and grazers, these results might have important implications for the eVect of siltation of tidal Xats due to, e.g., human activities.
“…However, this suggests a close coupling between water content and cyanobacterial movements. Similarly, migration of benthic diatoms in tidal sediment is strongly influenced by the tide level [13,26], but the causes of the rhythm are not yet clearly understood [13]. The upward migration in the presence of water could simply be a relaxation of a tightly bound population that initiates a random walk; thus part of it reaches the surface in the absence of stimulus.…”
We studied the migration of cyanobacteria in desert crusts from Las Bárdenas Reales (Spain). The crusts were almost exclusively colonized by the filamentous cyanobacterium Oscillatoria, which formed a dense layer approximately 600 lm thick located between 1.5 and 2.1 mm deep. Laboratory and field experiments showed that saturation of the crust with liquid water induced a migration of the cyanobacteria leading to a significant greening of the surface within a few minutes. Under light and rapid evaporation, the green color rapidly disappeared and the crust surface was completely devoid of filaments within 60 min. In contrast, 260 min was required to recover the original white color of the crust when slow evaporation was experimentally imposed. The up and down migration following wetting and drying occurred also in the dark. This demonstrates that light was not a required stimulus. Addition of ATP synthesis inhibitors prevented the cyanobacterium from migrating down into the crust, with filaments remaining on the surface. Therefore, the disappearance of the green color observed during desiccation can only be attributed to an active cyanobacterial motility response to the decrease in the water content. The simplest explanation that can account for the evidence gathered is the presence of a mechanism that links, directly or indirectly, these motility responses to gradients in water content, namely a form of hydrotaxis.
“…The vertical migratory behaviour of benthic microalgae also has ecological importance, as the large changes in microalgal biomass in the photic zone of sediments are a major factor in controlling short-term variation in biofilm-level photosynthetic rates (Pinckney & Zingmark, 1991;Guarini et al, 2000;Seroˆdio et al, 2001). Moreover, migratory rhythms cause changes in the photophysiology of the cells, which affects the photosynthetic efficiency of biofilms (Forster & Kromkamp, 2004;Seroˆdio, 2004;Seroˆdio et al, 2005;Perkins et al, 2010).…”
The vertical migratory behaviour of estuarine microphytobenthos, i.e. the biofilm-forming microalgae inhabiting intertidal sediments, is probably a significant factor for their success in this extreme and unstable environment. The present work aimed to assess the relative role of endogenous versus environmental control of benthic microalgal vertical migratory behaviour. This was done by comparing the patterns of vertical migration in undisturbed sediment samples kept under constant conditions of darkness and low light with those in ambient light conditions, by measuring the changes in the surface microalgal biomass during daytime low-tide periods. The results showed that the formation of a biofilm was a two-phase process. It began with a relatively small accumulation of cells at the surface, starting hours before the beginning of the light period and endogenously driven. However, the full formation of the biofilm required exposure to light by the expected beginning of the photoperiod, which further promoted upward migration and accelerated the cell accumulation at the surface. In the absence of light, upward migration was interrupted and the incipient biofilm began to disaggregate. The relative importance of the endogenously controlled behaviour varied during the spring-neap tidal cycle, reaching a maximum on those days when low tide occurred in the middle of the day, suggesting its entrainment by the duration of light exposure on previous days. The regulation of the surface cell concentration during daytime low tides was found to be strongly dependent on exogenous factors, particularly irradiance. The spontaneous disaggregation of the biofilm shortly before the end of the low-tide period (due to tidal flood or sunset), both under constant as well as ambient light conditions, suggested the presence of an endogenously controlled positive geotaxis.
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