“…Our fine-scale analysis of the vertical distribution of sediment chl a (Fig. 1) is in qualitative agreement with similar high resolution measurements from coastal marine environments that show a maximum chl a concentration in the surface 1 mm of sediment with continuously decreasing or reduced but constant chl a concentrations with increasing sediment depth below 1 mm to 5 or 10 mm (MacIntyre and Cullen, 1995;Herlory et al, 2004;Cartaxana et al, 2006). A chl a maximum in surficial marine sediment may be attributed to settling of suspended material from overlying water prior to core processing (MacIntyre and Cullen, 1995).…”
“…Our fine-scale analysis of the vertical distribution of sediment chl a (Fig. 1) is in qualitative agreement with similar high resolution measurements from coastal marine environments that show a maximum chl a concentration in the surface 1 mm of sediment with continuously decreasing or reduced but constant chl a concentrations with increasing sediment depth below 1 mm to 5 or 10 mm (MacIntyre and Cullen, 1995;Herlory et al, 2004;Cartaxana et al, 2006). A chl a maximum in surficial marine sediment may be attributed to settling of suspended material from overlying water prior to core processing (MacIntyre and Cullen, 1995).…”
“…We estimated that an average of 125,000 diatom cells/copepod would correspond to food limitation, so there was suYcient food available in our experimental units. There were no data on diatom concentration in the Weld situation, however it is well known that diatom bioWlms are well-established on intertidal mudXats (e.g., Bellinger, Abdullahi, Gretz, & Underwood, 2005;Decho, 2000;Herlory, Guarini, Richard, & Blanchard, 2004) though these bioWlms are very variable depending on light conditions (pers. observ.…”
Section: Discussionmentioning
confidence: 99%
“…The EPS matrix of bioWlm forms sticky coatings on individual sediment particles and detrital surfaces, which act as a stabilizing anchor to buVer cells and their extracellular processes during frequent physical stresses (e.g., changes in salinity and temperature, UV irradiation, desiccation) (Decho, 2000). Especially intertidal mudXats, where the test harpacticoid species were collected from, are known for these extended bioWlms of microphytobenthos (e.g., Bellinger et al, 2005Decho, 2000Herlory et al, 2004).…”
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.
“…This rhythmic behaviour has been considered a key adaptation to the sedimentary intertidal habitat (Seroˆdio & Catarino, 2000;Mitbavkar & Anil, 2004). Upward migration allows the microalgae to reach the illuminated layers of the sediment and photosynthesize, which is of crucial importance because of the periodic disturbance caused by tidal resuspension and subsequent burial in aphotic layers of the sediment (Herlory et al, 2004;ChulHwan et al, 2006;Mitbavkar & Anil, 2006). On the other hand, downward migration may help microalgae to avoid grazers (Buffan-Dubau & Carman, 2000), minimize resuspension into the water column (Kingston, 1999b), promote access to carbon or nutrients Kromkamp et al, 1998;Kingston, 1999bKingston, , 2002, or facilitate sexual reproduction (Saburova & Polikarpov, 2003).…”
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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