The effects of rain on the erosion threshold of intertidal cohesive sediments

Intertidal sedimentary environments are complex systems governed by interactions between physical, chemical and biological processes and parameters. Tidally induced flow and wave action are known to be an integral driving force behind the erosion, transport, deposition and consolidation cycle (ETDC) of intertidal sediments. Whilst considerable advances have been made in understanding both the physical and biological processes and their interactions in these systems, it is clear that there are gaps in our understanding. One factor that has been largely ignored to date is that of rain. Visual observations in the field and associated data indicated that rain showers during low tide are correlated with a reduction in the erosion threshold of intertidal cohesive sediments. This paper presents preliminary field and laboratory data showing the importance of rain in reducing the erosion threshold of cohesive intertidal sediments. The implications for our knowledge of, and modelling of the ETDC cycle of cohesive intertidal sediments are discussed.     

Diatom migration and sediment armouring – an example from the Tagus Estuary, Portugal

This study measured sediment stability, colloidal and total carbohydrate and chlorophyll a in the upper 2 mm of the sediment over a whole emersion period (0800–1140) in the Tagus estuary, Portugal on the 18th April 2000. Low-temperature scanning electron microscopy (LTSEM) time series images revealed the migration of microalgae throughout the emersion period, including their appearance at the sediment surface at the beginning of emersion and their subsequent return below the surface at the end of emersion. Different species arrived at the sediment surface at different times and there was a slight lag between the appearance of the first cells and the subsequent increase in sediment stability. Increased chlorophyll a concentration in the surface sediments preceded the increase in sediment stability, whilst colloidal and total carbohydrate concentrations increased afterwards. Sediment water content decreased during the emersion period. Erosion threshold increased shortly after the microalgal cells appeared at the sediment surface, suggesting that the cells themselves act to `armour' the sediment surface, retarding erosion. Lack of correlation between sediment stability and factors traditionally considered to control sediment stability (e.g., water content and carbohydrate content) indicates that an important variable or interaction has yet to be identified. One possibility is that the carbohydrate fraction extracted does not measure accurately the binding effectiveness of the carbohydrates in the sediment. We propose feedback and `critical point' models to explain how the various sediment properties determine sediment stability. The implication is that sediment stability varies in an apparently idiosyncratic and site-specific fashion due to the complex interaction of physical and biological variables. Given the importance of ecological processes in intertidal sediments, the measurement, understanding and modelling of sediment erosion would benefit greatly from the application of ecological methods of experimental design and sampling.     

Hydroelectricity and fish: a synopsis of comprehensive studies of upstream and downstream passage of anadromous wild Atlantic salmon, <Emphasis Type="Italic">Salmo salar</Emphasis>, on the Exploits River,Canada

Microalgal biofilms are associated with considerable variability in the properties of natural sediments, yet little effort has been made to isolate micro-scale spatial and temporal changes in sediment properties caused by the growth of a biofilm. Understanding the changes associated with biofilm growth and quantifying the time scales over which these changes occur is important for developing suitable experimental designs and for understanding how biofilms mediate sediment properties and processes. The development of a microphytobenthic biofilm and associated changes in the sediment was investigated over 45 days in the laboratory. The biogeochemical properties of the sediment: bulk density, water content, chlorophyll a concentration and colloidal carbohydrate concentration were measured on a sub-millimetre scale in the top 2 mm. The erosion threshold was measured with a Cohesive Strength Meter (CSM). Biofilm development was rapid, with changes in the properties occurring after 1 day and a visible film forming after just 3 days. The largest changes in sediment properties tended to occur in the surface 200 μm through time, with some variables also showing a differing response with depth. There were significant changes in water content, chlorophyll a concentration, colloidal carbohydrate concentration and erosion threshold in the surface 2 mm, with a general trend to increase with time. Bulk density was highly variable and did not show a consistent pattern of change with time. Erosion threshold was positively correlated with water content, chlorophyll a and colloidal carbohydrate in the surface 200 μm and these were also positively correlated with each other. Low Temperature Scanning Electron Microscopy (LTSEM) images revealed changes in the surface sediment structure and the formation of a thick multi-layer biofilm. The rapidity of biofilm growth and development and the associated changes to the sediment should be considered when designing experiments that investigate biofilms and properties of sediments and/or that involve biocide treatments or disturbance to the sediment.     

Microphytobenthos as a biogeomorphological force in intertidal sediment stabilization

The properties and behavior of intertidal marine sediments cannot be understood without taking their biology into account. Biological factors are important for the stability and erosion threshold of intertidal sediments as well as for sediment transport. In this paper I focus on intertidal sediments that are colonized and dominated by phototrophic microorganisms and their impact on the morphodynamics and sediment stabilization. The emphasis is on epipelic diatoms. These organisms exude copious amounts of extracellular polymeric substances (EPS) that may contribute to the stability of the sediment by gluing and binding. I review the factors that lead to the development of such microphytobenthic communities and the processes that lead to the exudation of EPS and its fate in intertidal mudflats. Epipelic diatoms exude EPS partly as the result of unbalanced growth. Extraction of EPS from cultures of epipelic diatoms yields two operational fractions. While one fraction contains largely neutral EPS, which may serve as a carbon- and energy reserve for the organism, the other is acidic and more recalcitrant to degradation. The latter EPS fraction is therefore predominant in the muddy sediment and may be responsible for increasing the erosion threshold. However, since extracted EPS alone is incapable of increasing the erosion threshold, diatoms are apparently actively involved in the structuring of the biofilm matrix. Therefore, sediment stabilization cannot be attributed simply to EPS alone.     

Sediment-benthos relationships as a tool to assist in conservation practices in a coastal lagoon subjected to sediment change

This study explores the relation between sediment composition and intertidal macrobenthos populations in the Zwin nature reserve (Belgium and The Netherlands), a tidal lagoon that is included in the Ramsar list of wetlands of international importance and has been designated as Natura 2000 area, among others due to its function as wintering habitat for shorebirds that feed upon macrobenthic invertebrates. Species response models show highest biomass of these prey species in organically enriched cohesive sediments and a distinct decline in probability of occurrence for most species in coarse sediments. Further, the biomass of macrobenthos declined between 2003 and 2010 in the extensive low intertidal inlet channel concurrent with the coarsening of the sediment over time in this hydrodynamically stressed habitat. In contrast, macrobenthos biomass increased in a sheltered shallow intertidal habitat that acted as a catchment area for finer sediments, therefore facilitating the succession towards a higher elevated habitat with salt marsh vegetation establishment. Hence, spatio-temporal sediment dynamics decreased site quality for intertidal predators due to a reduction in feeding areas over time, and a change in physical sediment properties that alter the macrobenthos species occurrence and population biomass. This study thus illustrates that sediment transport dynamics may affect the functioning of coastal shallow soft-sediment habitats, like coastal lagoons. The presented macrobenthos species response models provide a tool to assist in management actions that enable the conservation of cohesive low intertidal habitats that provide a high food supply to shorebirds, fish and macrocrustaceans.     

Erodibility and erosion patterns of mudflat sediments investigated using an annular flume

Laboratory flume experiments were carried out, to measure the effect of biota on erodibility of mudflat sediments. The experiments sought to reproduce the environment of the lower mudflat at Hythe, Southampton Water, Southern England; this is characterised by fine grain-size and a surface layer of very fluid mud. Natural sediments were used to produce settled beds in the Lab Carousel, an annular flume of 2 m diameter. The following bed conditions were investigated diatom biofilms; the addition of cockles (Cerastoderma edule); and abiotic sediment, obtained by the addition of sodium hypochlorite. The erosion threshold (τ_crit, calculated with the TKE method) was in the range 0.02–0.20 Pa. Bioconsolidation increased τ_crit considerably: compared to the abiotic sediment experiment, τ_crit was 5–10 times higher depending on the biofilm development. The relationship between τ_crit and water content of sediment (the best proxy for sediment compaction) was as good, or better than between τ_crit and chlorophyll a (proxy for biofilm development). When cockles were introduced, τ_crit was significantly lower (reduction by 50–75% compared with the diatom biofilm experiments), reflecting the surface disturbance by the bivalves. The biofilm erosion was characterised by a patchy pattern: the bed surface stayed mainly uneroded and erosion was visible only on a few elongated patches commencing at some weakness points of the biofilm, then progressing downstream. The results illustrate the importance of the surface heterogeneity: the irregularities of a natural bed (weak points of the biofilm, bioturbations, microrelief, larger roughness elements like shells or algae, etc.) have a determinant effect on the erodibility of biofilms. Such characteristics may have more influence than biofilm strength, because the erosion starts from the weaker areas.     

Fortnightly light and temperature variability in estuarine intertidal sediments and implications for microphytobenthos primary productivity

Photosynthetically active radiation (PAR) and temperature were measured continuously at the surface of estuarine intertidal sediments in the Tagus estuary, Portugal, along two spring-neap tidal cycles. PAR and temperature were strongly conditioned by the periodic tidal inundation, with large and abrupt variations occurring during flooding and ebbing. PAR levels reaching the sediment surface decreased very rapidly to zero or very low values during most of the daytime immersion. Inundation during high tide had the general effect of attenuating the amplitude of daily temperature fluctuation, with the incoming water usually warmer than the sediment during the night or early morning and cooler during the day. The daily progression of tidal emersion resulted in a clear fortnightly variation in total daily PAR reaching the sediment surface, while both daily mean temperature and mean temperature of diurnal low tide periods failed to exhibit a well-defined fortnightly periodicity. The obtained results indicate that the estuarine intertidal environment is dominated, at sub-seasonal time scales, by fortnightly periodicity in irradiance and temperature conditions favourable for benthic photosynthesis.     

Microphytobenthos,their Extracellular Polymeric Substances,and the Morphogenesis of Intertidal Sediments

Intertidal sediments are important areas that separate the land from the sea and form natural coastal defenses. They are known as highly productive ecosystems, fueling the coastal food web. It is also conceived that microphytobenthos contribute to the stability of intertidal sediments by increasing the erosion threshold and that they are major players in coastal morphodynamics. Depending on the sedimentary composition of intertidal flats, different types of microphytobenthos colonize the sediment surface. Fine sand sediment is often colonized by cyanobacteria, prokaryotic algae, which form dense and rigid microbial mats. Mudflats on the other hand are characterized by the development of thin biofilms of epipelic diatoms. Both groups of phototrophic microorganisms excrete extracellular polymeric substances (EPS), but they do so in different ways and for different reasons. Two operationally defined fractions, water- and EDTA-extractable EPS, have been obtained from intertidal diatom biofilms and from cultures. They differ in composition and their production seems to be under different metabolic control. Water-extractable EPS are considered to be closely associated with the diatoms and are rich in neutral sugars, notably glucose. These EPS show a dynamic relationship with the microphytobenthic biomass. EDTA-extractable EPS are tightly bound to the sediment, probably through bridging by divalent ions. This material is rich in uronic acids and other acid sugars and is weakly related to chlorophyll. These EPS have been conceived to be a major factor in the structuring and diagenesis of coastal sediments and essential for increasing the sediment erosion threshold. However, this relationship is now questioned.     

Intra-Annual Variability in Responses of a Canopy Forming Kelp to Cumulative Low Tide Heat Stress: Implications for Populations at the Trailing Range Edge

Anthropogenic climate change is driving the redistribution of species at a global scale. For marine species, populations at trailing edges often live very close to their upper thermal limits and, as such, poleward range contractions are one of the most pervasive effects of ongoing and predicted warming. However, the mechanics of processes driving such contractions are poorly understood. Here, we examined the response of the habitat forming kelp, Laminaria digitata, to realistic terrestrial heatwave simulations akin to those experienced by intertidal populations persisting at the trailing range edge in the northeast Atlantic (SW England). We conducted experiments in both spring and autumn to determine temporal variability in the effects of heatwaves. In spring, heatwave scenarios caused minimal stress to L. digitata but in autumn all scenarios tested resulted in tissue being nonviable by the end of each assay. The effects of heatwave scenarios were only apparent after consecutive exposures, indicating erosion of resilience over time. Monthly field surveys corroborated experimental evidence as the prevalence of bleaching (an indication of physiological stress and tissue damage) in natural populations was greatest in autumn and early winter. Overall, our data showed that L. digitata populations in SW England persist close to their upper physiological limits for emersion stress in autumn. As the intensity of extreme warming events is likely to increase with anthropogenic climate change, thermal conditions experienced during periods of emersion will soon exceed physiological thresholds and will likely induce widespread mortality and consequent changes at the population level.     

Conditional Responses of Benthic Communities to Interference from an Intertidal Bivalve

Habitat-modifying organisms that impact other organisms and local functioning are important in determining ecosystem resilience. However, it is often unclear how the outcome of interactions performed by key species varies depending on the spatial and temporal disturbance context which makes the prediction of disturbance-driven regime shifts difficult. We investigated the strength and generality of effects of the filter feeding cockle Cerastoderma edule on its ambient intertidal benthic physical and biological environment. By comparing the magnitude of the effect of experimental cockle removal between a non-cohesive and a sheltered cohesive sediment in two different periods of the year, we show that the outcome of cockle interference effects relates to differences in physical disturbance, and to temporal changes in suspended sediment load and ontogenetic changes in organism traits. Interference effects were only present in the cohesive sediments, though the effects varied seasonally. Cockle presence decreased only the density of surface-dwelling species suggesting that interference effects were particularly mediated by bioturbation of the surface sediments. Furthermore, density reductions in the presence of cockles were most pronounced during the season when larvae and juveniles were present, suggesting that these life history stages are most vulnerable to interference competition. We further illustrate that cockles may enhance benthic microalgal biomass, most likely through the reduction of surface-dwelling grazing species, especially in periods with high sediment load and supposedly also high bioturbation rates. Our results emphasize that the physical disturbance of the sediment may obliterate biotic interactions, and that temporal changes in environmental stressors, such as suspended sediments, may affect the outcome of key species interference effects at the local scale. Consequently, natural processes and anthropogenic activities that change bed shear stress and sediment dynamics in coastal soft-sediment systems will affect cockle-mediated influences on ecosystem properties and therefore the resilience of these systems to environmental change.     

土壤可蚀性研究述评

土壤可蚀性是土壤对侵蚀营力分散和搬运作用的抵抗能力,是建立土壤流失方程和侵蚀模型的必要参数.土壤可蚀性研究是认识土壤侵蚀机理的一个重要环节.本研究基于土壤可蚀性已有成果,总结评述了土壤可蚀性的相关研究进展.其中,土壤可蚀性的相关指标有土壤抗冲抗蚀性、K因子等;土壤可蚀性包括水蚀可蚀性、风蚀可蚀性、重力可蚀性和冻融可蚀性等不同类型;其评价指标体系可以分为基于土壤内在性质和外在侵蚀营力的两类评价指标体系;土壤理化性质测定法、仪器测定法、小区测定法、数学模型和图解法、水动力学模型求解法是目前常用的5种土壤可蚀性测定和估算方法;土壤可蚀性具有明显的时空分异特征,其影响因素主要包括土壤性质、气候、植被、地形和土地利用等不同方面.在土壤可蚀性的进一步研究中,应注重土壤可蚀性概念的界定、评价指标体系的规范统一、土壤可蚀性估算模型的区域适用性、土壤可蚀性动态变化作用机理等方面.     

The influence of benthic microalgae on the stability of a subtidal sediment

The relationship between benthic microalgae and the stabilisation of sediment was studied using a straight-channel laboratory flume tank. To establish different densities of microalgal biomass, sieved sediment collected from a shallow bay was kept in a laboratory flow-through aquarium either in darkness or with a 16/8 light/dark cycle. The relation between shear velocities causing sediment transport (u_*(crit)) and chlorophyll a content, content of colloidal polysaccharides, biomass and composition of microalgae in the top 5 mm of the sediment were studied. Microalgal samples were also collected using the cover-glass technique. Erosion tests were also made on undisturbed field samples. The investigation showed that the stabilizing effect of microalgae, previously reported for intertidal areas, may also apply for shallow-water sediments lacking regular tidal emersion. Initially, sieving decreased sediment stability by destroying consolidating structures. Within 5 days, however, values of u_*(crit) approached those of the undisturbed field samples (2.8 cm · s⁻¹). The sediment that was exposed to light, became more stable against erosion (higher u_*(crit)) than sediment kept in darkness. This difference is suggested to be caused by different densities of microalgae, as several sediment variables related to algae (content of chlorophyll a, polysaccharide content and algal biomass caught on cover glasses) were significantly different in light and dark treatments. The increased stability was mainly induced by the increased biovolume of motile diatoms within the size groups 20–40 μm and > 100 μm, as well as by filamentous cyanobacteria. Only the biovolume of algae trapped on cover glasses correlated significantly with critical shear velocity, while chlorophyll a, polysaccharides and biovolume in core samples showed positive, but non-significant correlations with critical shear velocity. Although the cover glasses harvested only a minor portion (5–10%) of the algal biovolume in the top 5 mm sediment, at least the motile diatom flora was better assessed by the cover-glass technique. Consequently, this appears to be a better indicator of sediment stability than total biomass or chlorophyll a content in the lop 5 mm sediment. Although there is a methodological uncertainty as to what components the variable “polysaccharides” include, polysaccharide content can be used to give at least a qualitative prediction of sediment stability. It is doubtful, however, whether any reasonable specific quantitative prediction about sediment stability can be made without an extensive knowledge about several factors, such as sediment structure, the quantity and the quality, as well as the physiological status of the organisms.     

The role of niche measures in explaining the abundance–distribution relationship in tropical lotic chironomids

In situ measurements of both community metabolism (primary production and respiration) and PAM fluorometry were conducted during emersion on intertidal sediments in the Mont Saint-Michel Bay, in areas where oysters and mussels were cultivated. Results highlighted a low benthic metabolism compared to other intertidal areas previously investigated with the same methods. Comparisons between gross community primary production and relative electron transport rates confirmed this statement. More specifically, primary productivity remained very low all over the year, whereas the associated microalgal biomass was estimated to be high. We suggest that the microphytobenthic community studied was characterized by a self-limitation of its primary productivity by its own biomass, as previously shown in Marennes-Oléron Bay for example. The almost permanent high biomass would represent a limiting factor for micromigration processes within the first millimetres of the sediment. This could be explained by very low resuspension processes occurring in the western part of the bay, enhanced by the occurrence of numerous aquaculture structures that could decrease tidal currents in the benthic boundary layer. Handling editor: N. Desroy     

Effects of burial and erosion on the seagrass Zostera noltii

The effects of experimental burial and erosion on the seagrass Zostera noltii were assessed through in situ manipulation of the sediment level (− 2 cm, 0 cm, + 2 cm, + 4 cm, + 8 cm and + 16 cm). Shoot density, leaf and sheath length, internode length, C and N content and carbohydrates of leaves and rhizomes were examined 1, 2, 4 and 8 weeks after disturbance. Both burial and erosion resulted in the decrease of shoot density for all the sediment levels. The threshold for total shoot loss was between 4 cm and 8 cm of burial, particularly during the 2nd week. A laboratory experiment confirmed that shoots did not survive more than 2 weeks under complete burial. There was no evidence of induced flowering by burial or erosion. As well, no clear evidence was found of sediment level effects on leaf and sheath length. Longer rhizome internodes were observed as a response to both burial and erosion, suggesting a plant attempt to relocate the leaf-producing meristems closer to sediment surface or in search of new sediment avoiding the eroded area. The C content of leaves and rhizomes, as well as the non-structural carbohydrates (mainly the starch in rhizomes), decreased significantly along the experimental period, indicating the internal mobilization of carbon to meet the plant demands as a consequence of light deprivation. The significant decrease of N content in leaves, and its simultaneous increase in rhizomes, suggests the internal translocation of nitrogen from leaves to rhizomes. About 50% of the N lost by the leaves was recovered by the rhizomes. Our results indicated that Z. noltii has a high sensitivity to burial and erosion disturbance, which should be considered in the management of coastal activities.     

The consequences of changes in abundance of <Emphasis Type="Italic">Callianassa subterranea</Emphasis> and <Emphasis Type="Italic">Amphiura filiformis</Emphasis> on sediment erosion at the Frisian Front (south-eastern North Sea)

In the early 1990’s a conspicuous shift took place in the density of two key macrofauna species at the Frisian Front (SE North Sea). The density of the formerly dominant brittlestar Amphiura filiformis showed tenfold reduction and remained low throughout the observation period (1986–2000). In the same period, the burrowing mud shrimp Callianassa subterranea showed a fourfold increase in density. Since the Frisian Front is a transition area where tidal currents fall just below the erosion threshold of silt and bioturbating mud shrimps can potentially affect the sediment erosion threshold, we examined the effects of the species on sediment erodibility. Two experiments were conducted in laboratory annular flumes. In the first experiment we compared the effects of pre-shift and post-shift combinations of the two species on the erodibility of Frisian Front sediment. The results indicated that the erosion was facilitated by a combination of high densities of C. subterranea and low densities of A. filiformis, representing the situation in the late 1990s. The difference in erodibility was already apparent at velocities equal to the critical near-bed current speed measured at the Frisian Front. In the second experiment the effects of pre- and post-shift densities of A. filiformis on sediment erodibility were compared. This showed that low A. filiformis densities as found in the late 1990’s facilitate erosion, but the effect is only significant at velocities above the critical near-bed velocity in the field. At the latter velocity, no significant difference in erodibility was found between the two A. filiformis densities. This implies that the difference in turbidity in the first experiment was mainly due to the activity of C. subterranea. The experimental results indicate that resuspension at the Frisian Front may occur more frequently as a result of the shift towards a Callianassa dominated community. More frequent resuspension of bottom sediment, most likely amplified by the climate induced increase of wind strength in the North Sea, may hamper the recovery of the A. filiformis adult population. Handling editor: K. Martens     

土壤可蚀性研究述评

土壤可蚀性是土壤对侵蚀营力分散和搬运作用的抵抗能力,是建立土壤流失方程和侵蚀模型的必要参数.土壤可蚀性研究是认识土壤侵蚀机理的一个重要环节.本研究基于土壤可蚀性已有成果,总结评述了土壤可蚀性的相关研究进展.其中,土壤可蚀性的相关指标有土壤抗冲抗蚀性、K因子等;土壤可蚀性包括水蚀可蚀性、风蚀可蚀性、重力可蚀性和冻融可蚀性等不同类型;其评价指标体系可以分为基于土壤内在性质和外在侵蚀营力的两类评价指标体系;土壤理化性质测定法、仪器测定法、小区测定法、数学模型和图解法、水动力学模型求解法是目前常用的5种土壤可蚀性测定和估算方法;土壤可蚀性具有明显的时空分异特征,其影响因素主要包括土壤性质、气候、植被、地形和土地利用等不同方面.在土壤可蚀性的进一步研究中,应注重土壤可蚀性概念的界定、评价指标体系的规范统一、土壤可蚀性估算模型的区域适用性、土壤可蚀性动态变化作用机理等方面.     

Variability in thermal and UV-B energy fluxes through time and their influence on plant diversity and speciation

Throughout Earth's history there have been temporal and spatial variations in the amount of visible and ultraviolet radiation received by ecosystems. This paper examines if temporal changes in these forms of energy receipt could have influenced the tempo and mode of plant diversity and speciation, focusing in particular upon Cenozoic time-scales. Evidence for changing patterns of plant diversity and speciation apparent in various fossil records and molecular phylogenies are considered alongside calculated changes in thermal and solar ultraviolet energy (specifically UV-B) over the past 50 Myr. We suggest that changes in thermal energy influx (amount and variability) affected the tempo of evolution through its influence upon community dynamics (e.g. population size, diversity, turnover, extinctions). It was not only the amount of thermal energy but also variability in its flux that may have influenced these processes, and ultimately the rate of diversification. We suggest that variations in UV-B would have influenced the mode and tempo of speciation through changes to genome stability during intervals of elevated UV-B. We argue, therefore, that although variability in thermal energy and UV-B fluxes through time may lead to the same end-point (changing the rate of diversification), the processes responsible are very different and both need to be considered when linking evolutionary processes to energy flux.     

The surf zone: a semi-permeable barrier to onshore recruitment of invertebrate larvae?

The supply of larvae to the shore is important for population replenishment and intertidal community dynamics but its variability at most scales is not well understood. We tested the relationship between nearshore mussel larval abundance and intertidal settlement rates over several years at multiple spatiotemporal scales in Oregon and New Zealand. Abundance of competent larvae nearshore and intertidal recruitment rates were simultaneously quantified using collectors mounted at different depths on moorings 50-1100 m from shore, and at adjacent rocky intertidal sites. Total mussel larval abundance and oceanographic conditions were also measured in some locations. At all scales, abundance of nearshore mussel larvae was unrelated to intertidal recruitment rates. In the intertidal, patterns of mussel recruitment were persistent in space, with sites of consistently high or low recruitment. In contrast, nearshore competent larval abundance showed generally similar abundances among sites except for a high, and spatially-inconsistent, variability in Oregon during 1998 only. On moorings, recruitment tended to be greater on midwater collectors than shallower or deeper. Finally, on moorings larval abundance in traps and recruitment on collectors was unrelated. These results suggest that (1) among sites, the size of the nearshore larval pool is relatively uniform while onshore recruitment varies and is unrelated to larval abundance, (2) temporal variability in nearshore larval availability is not strongly expressed onshore, (3) vertical stratification of competent larvae nearshore is strong and may influence transport and recruitment, and (4) within-coast variability in onshore recruitment is strongly driven by processes occurring locally within the surf zone that need to be studied to understand coastal recruitment dynamics.     

Neutral processes and species sorting in benthic microalgal community assembly: effects of tidal resuspension

Benthic microalgae (BMA) provide vital food resources for heterotrophs and stabilize sediments with their extracellular secretions. A central goal in ecology is to understand how processes such as species interactions and dispersal, contribute to observed patterns of species abundance and distribution. Our objectives were to assess the effects of sediment resuspension on microalgal community structure. We tested whether taxa‐abundance distributions could be predicted using neutral community models (NCMs) and also specific hypotheses about passive migration: (i) As migration decreases in sediment patches, BMA α‐diversity will decrease, and (ii) As migration decreases, BMA community dissimilarity (β‐diversity) will increase. Co‐occurrence indices (checkerboard score and variance ratio) were also computed to test for deterministic factors, such as competition and niche differentiation, in shaping communities. Two intertidal sites (mudflat and sand bar) differing in resuspension regime were sampled throughout the tidal cycle. Fluorometry and denaturing gradient gel electrophoresis were utilized to investigate diatom community structure. Observed taxa‐abundances fit those predicted from NCMs reasonably well (R² of 0.68–0.93), although comparisons of observed local communities to artificial randomly assembled communities rejected the null hypothesis that diatom communities were assembled solely by stochastic processes. No co‐occurrence tests indicated a significant role for competitive exclusion or niche partitioning in microalgal community assembly. In general, predictions about relationships between migration and species diversity were supported for local community dynamics. BMA at low tide (lowest migration) exhibited reduced α‐diversity as compared to periods of immersion at both mudflat and sand bar sites. β‐diversity was higher during low tide emersion on the mudflat, but did not differ temporally at the sand bar site. In between‐site metacommunity comparisons, low‐ and high‐resuspension sites exhibited distinct community compositions while the low‐energy mudflats contained higher microalgal biomass and greater α‐diversity. To our knowledge this is the first study to test the relevance of neutral processes in structuring marine microalgal communities. Our results demonstrate a prominent role for stochastic factors in structuring local BMA community assembly, although unidentified nonrandom processes also appear to play some role. High passive migration, in particular, appears to help maintain species diversity and structure communities in both sand and muddy habitats.     

Role of climate and agricultural practice in determining matter discharge into large,shallow Lake Võrtsjärv,Estonia

Understanding the dynamics of fine sediment transport across the upper intertidal zone is critical in managing the erosion and accretion of intertidal areas, and in managed realignment/estuarine habitat recreation strategies. This paper examines the transfer of sediments between salt marsh and mudflat environments in two contrasting macrotidal estuaries: the Seine (France) and the Medway (UK), using data collected during two joint field seasons undertaken by the Anglo-French RIMEW project (Rives-Manche Estuary Watch). High-resolution ADCP, Altimeter, OBS and ASM measurements from mudflat and marsh surface environments have been combined with sediment trap data to examine short-term sediment transport processes under spring tide and storm flow conditions. In addition, the longer-term accumulation of sediment in each salt marsh system has been examined via radiometric dating of sediment cores. In the Seine, rapid sediment accumulation and expansion of salt marsh areas, and subsequent loss of open intertidal mudflats, is a major problem, and the data collected here indicate a distinct net landward flux of sediments into the marsh interior. Suspended sediment fluxes are much higher than in the Medway estuary (averaging 0.09 g/m³/s), and vertical accumulation rates at the salt marsh/mudflat boundary exceed 3 cm/y. Suspended sediment data collected during storm surge conditions indicate that significant in-wash of fine sediments into the marsh interior can occur during (and following) these high-magnitude events. In contrast to the Seine, the Medway is undergoing erosion and general loss of salt marsh areas. Suspended sediment fluxes are of the order of 0.03 g/m³/s, and the marsh system here has much lower rates of vertical accretion (sediment accumulation rates are ca. 4 mm/y). Current velocity data for the Medway site indicate higher velocities on the ebb tide than occur on the flood tide, which may be sufficient to remobilise sediments deposited on the previous tide and so force net removal of material from the marsh.