Search

Abstract: Resuspension of microphytobenthic biomass that builds up during low tide has been acknowledged as a major driver of the highly productive food web of intertidal mudflats. Yet, little is known about the contribution to pelagic food web of the resuspension of other microorganisms such as viruses, picoeukaryotes, cyanobacteria, bacteria, nanoflagellates, and ciliates, living in biofilms associated with microphytobenthos and surficial sediment. In the present study, a novel approach that involves simultaneous Lagrangian and Eulerian surveys enabled to disentangle the effects of resuspension and mixing with offshore waters on the dynamics of water column microorganisms during a rising tide in the presence of waves. Temporal changes in the concentration of microorganisms present in the water column were recorded along a 3km cross-shore transect and at a fixed subtidal location. In both surveys, physical and biological processes were separated by comparing the time-evolution of sedimentary particles and microorganism concentrations. During a rising tide, sediment erosion under wave action occurred over the lower and upper parts of the mudflat, where erodibility was highest. Although erosion was expected to enrich the water column with the most abundant benthic microorganisms, such as diatoms, bacteria and viruses, enrichment was only observed for nanoflagellates and ciliates. Grazing probably overwhelmed erosion transfer for diatoms and bacteria, while adsorption on clayed particles may have masked the expected water column enrichment in free viruses due to resuspension. Ciliate enrichment could not be attributed to resuspension as those organisms were absent from the sediment. Wave agitation during the water flow on the mudflat likely dispersed gregarious ciliates over the entire water column. During the rising tide, offshore waters imported more autotrophic, mainly cyanobacteria genus Synechococcus sp. than heterotrophic microorganisms, but this import was also heavily grazed. Finally, the water column became a less heterotrophic structure in the subtidal part of the semi-enclosed bay, where mixing with offshore waters occurs (50% decrease), compared to the intertidal mudflat, when resuspension occurs. The present study suggests that this differential evolution resulted predominantly from dilution with offshore waters less rich in heterotrophic microorganisms. Indeed, any input of microorganisms accompanying physical transfers due to bed erosion or offshore water mixing was immediately buffered, probably to the benefit of grazers. [Copyright &y& Elsevier]

Abstract: A one-dimensional vertical unsteady numerical model for diffusion-consumption of dissolved oxygen (DO) above and below the sediment–water interface was developed to investigate DO profile dynamics under wind waves and sea swell (high-frequency oscillatory flows with periods ranging from 2 to 30s). We tested a new approach to modelling DO profiles that coupled an oscillatory turbulent bottom boundary layer model with a Michaelis–Menten based consumption model. The flow regime controls both the mean value and the fluctuations of the oxygen mass transfer efficiency during a wave cycle, as expressed by the non-dimensional Sherwood number defined with the maximum shear velocity (Sh). The Sherwood number was found to be non-dependent on the sediment biogeochemical activity (μ). In the laminar regime, both cycle-averaged and variance of the Sherwood number are very low . In the turbulent regime, the cycle-averaged Sherwood number is larger . The Sherwood number also has intra-wave cycle fluctuations that increase with the wave Reynolds number (VAR(Sh) up to 30%). Our computations show that DO mass transfer efficiency under high-frequency oscillatory flows in the turbulent regime are water-side controlled by: (a) the diffusion time across the diffusive boundary layer and (b) diffusive boundary layer dynamics during a wave cycle. As a result of these two processes, when the wave period decreases, the Sh minimum increases and the Sh maximum decreases. values vary little, ranging from 0.17 to 0.23. For periods up to 30s, oxygen penetration depth into the sediment did not show any intra-wave fluctuations. Values for the laminar regime are small (≤1mm for μ =2000gm−3 d−1) and decrease when the flow period increases. In the turbulent regime, the oxygen penetration depth reaches values up to five times larger than those in the laminar regime, becoming asymptotic as the maximum shear velocity increases. [Copyright &y& Elsevier]

Abstract: Experimental and field studies were carried out to quantify the hydrodynamic mobility under swells of a circalittoral epifauna species. The spatial distribution and structure of one population (NW Mediterranean) of the serpulid polychaete Ditrupa arietina was assessed before and after a moderate swell event in late winter 2006 with the two readings separated by a seven-week interval. The overall density in the bay did not change significantly. However, in certain locations, significant but heterogeneous changes occurred: at some stations, D. arietina disappeared, at others it appeared with high densities while at others, densities remained fairly constant, although in this third case, the population size structure was different. In addition, no trend was observed along a cross-shore gradient. Experimental studies were conducted to determine bed friction velocity thresholds for incipient motion, bed load transport and suspension transport for different sizes of D. arietina. The minimum friction velocity required to transport D. arietina as bed load over a smooth rigid bed ranged from 1.5 to for tube lengths ranging from 6 to 25mm. Thus, calcified worms (more than 6mm long) cannot be destabilized by ordinary currents. Conversely, during the moderate swell event, the maximum bed friction was large enough to mobilize D. arietina, making probably all sizes available for bed load transport, while only worms with a tube length of less than 12mm were transported in suspension at 27m water depth. Wave statistics in Banyuls Bay indicate that D. arietina transport under moderate swell events should not be a rare phenomenon (28 days per year at 20m water depth). Thus, the spatial scale for population dynamics studies should account for the extent of D. arietina spatial redistribution by the hydrodynamics. It is also recommended D. arietina be discarded from biotic quality index computations as this species is sensitive to natural hydrodynamic conditions. [Copyright &y& Elsevier]

The Mediterranean Sea hosts 5.6% of the world benthic invertebrate species on 0.82% of the ocean surface. Mediterranean ecosystems are also characterized by low densities (and biomasses) compared to other oceanic ecosystems, a feature often attributed to their oligotrophic environment. Oligotrophic conditions can induce lower growth rates and higher mortality rates, and a stronger competition for food between individuals. A theoretical model was developed in order to study the diversity vs. density patterns in coastal benthic invertebrate species. This model describes their minimal population dynamics including basic processes (growth, mortality, reproduction and effects of competitive interactions between individuals) and incorporating fluxes of larvae (finally recruited as juveniles) between a mosaic of local habitats. Populations are therefore structured in a metacommunity. The connectivity between local communities is ensured by passive pelagic larval dispersal. In the Mediterranean Sea, because of the microtidal regime, the connectivity between coastal habitats is lower and more variable than in macrotidal basins. Mathematical properties of the model revealed that competitive interactions (intra- and interspecific competitions) have a stabilizing effect on interacting organisms when gains by recruitment are higher than losses by mortality. In addition, low mortality rates and low connectivity which decreases negative local interactions maintains high regional species diversity with low local densities. This property suggested that oligotrophy cannot be the only factor leading to the high diversity–low density pattern observed in the Mediterranean Sea. [Copyright &y& Elsevier]