Assessment of benthic environmental disturbance in the Ba Lai estuary using the nematode biomass spectra

The researchs on the biomass spectra - a functional characteristic of biotic communities is still limited. In this study, the nematode biomass spectra in the bottom of Ba Lai estuary was investigated at six subtidal stations from the sea toward the upstream. The result showed that nematode biomass spectra ranged between -8 and 1 being significantly different between stations, and the lowest biomass of those spectras was in station BL4 (< 2 µg) which is upwardly closed to the Ba Lai dam. BL4 was also characterized by the lowest nematode abundance in the studied area. In addition, station BL3 downwardly closed to the dam exhibited low number of individuals. The heterogeneity in the nematode biomass spectra of BL3 and BL4 might due to the disturbance in the sedimentary environment of Ba Lai estuary related to the dam impact. This research again supports the important role of biomass spectra as bioindicator tool for biomonitoring and environmental quality assessment. Therefore, applying nematode biomass spectra is recommended for environmental assessment due to their advantages such as timesaving, not taxonomical expertise-requirement.

Assessment of the Effect of Al2O3 and TiO2 Nanoparticles on Orange Peel Biomass and its Application for Cd (II) and Ni (II) Uptake

In recent years, nanotechnology has been used to synthesize novel materials with several applications, such as wastewater treatment, medicine, and packaging. In this study, titanium dioxide (TiO2) and alumina (Al2O3) nanoparticles were synthesized and used to modify orange peel (OP) biomass. The resulting materials (OP-TiO2 and OP-Al2O3) were applied as biosorbents for removing nickel and cadmium from an aqueous solution. FT-IR, SEM-EDS, and XRD analyses were carried out to determine functional groups of biomass, morphology and elemental composition of the biosorbent, and average particle size, respectively. The presence of hydroxyl, carboxyl, and amine groups in the biomass spectra contributed to the adsorption process. Successful synthesis of the biosorbents due to the presence of aluminum and titanium elements was confirmed by energy dispersive x-ray spectroscopy (EDS). The average particle size was calculated as 19.13 ±4.1 nm and 58.56 ±12.64 nm for TiO2 and Al2O3, respectively. The solution pH significantly affected the adsorption process, and pH of 4 to 6 was selected as a suitable range. The highest removal yields of 87.85% and 95.6% were achieved using OP-Al2O3 for nickel and cadmium uptake, respectively. These results revealed an improvement in adsorption properties after loading the orange peel biomass with nanoparticles. Keywords: Biosorbent, Heavy metals, Nanomaterials, Wastewater treatment.

Nematode morphometry and biomass in the Saigon River harbours in relation to antifouling contaminants

Morphometry and biomass of nematode communities in different harbours of the Saigon River were investigated in the dry and wet seasons in relation to environmental variables such as total organic carbon, pH, conductivity, salinity and oxygen redox potential, in addition to concentrations of different butyltin compounds. The results indicated that nematodes in contaminated sediments from the Saigon River harbours were mainly characterised by slender morphotypes, whilst very few thin and stout nematodes were observed. Individual nematode biomass was generally low, especially in the wet season. There was no significant correlation between butyltin compounds and nematode morphometrics in the dry season but significant correlations were found for the wet season. Although significant correlations were observed for the wet season, the strong seasonal differences in nematode biomass spectra suggest a potential limitation in their use for environmental monitoring.

Decontextualizing Big Data for a Better Perception of Macroecology

ABSTRACTFish species are charismatic subjects widely used for ecological assessment and modelling. We investigated the influence of electrofishing in an attempt to illuminate the extent to which datasets might be merged together. Three American Midwestern regions in Ohio were chosen as study area and the changes in the size-biomass spectra of more than 2000 fish assemblages were analysed. These communities behaved differently according to the sampling method in conjunction to the morphology of the investigated streams and rivers, as shown by decreasing predatory species and lowering of allometric slopes. There are here several lines of evidence indicating that the chosen sampling method, as determined by different habitats, acts as a pitfall and strongly influences the allometry of fish spectra. In the ongoing data-rich era, our results highlight that macroecological investigations, often performed by machine-learning systems without considering the different procedures adopted to collect original data, can easily produce artefactual allometric scalings.

Surfing the biomass size spectrum: some remarks on history, theory, and application

Charles Elton introduced the “pyramid of numbers” in the late 1920s, but this remarkable insight into body-size dependent patterns in natural communities lay fallow until the theory of the biomass size spectrum was introduced by aquatic ecologists in the mid-1960s. They noticed that the summed biomass concentration of individual aquatic organisms was roughly constant across equal logarithmic intervals of body size from bacteria to the largest predators. These observations formed the basis for a theory of aquatic ecosystems, based on the body size of individual organisms, that revealed new insights into constraints on the structure of biological communities. In this review, we discuss the history of the biomass spectrum and the development of underlying theories. We indicate how to construct biomass spectra from sample data, explain the mathematical relations among them, show empirical examples of their various forms, and give details on how to statistically fit the most robust linear and nonlinear models to biomass spectra. We finish by giving examples of biomass spectrum applications to production and fisheries ecology and offering recommendations to help standardize use of the biomass spectrum in aquatic ecology.

Benthic biomass size spectra in shelf and deep-sea sediments

The biomass distributions of marine benthic metazoans (meio- to macro-fauna, 1 μg–32 mg wet weight) across three contrasting sites were investigated to test the hypothesis that allometry can consistently explain observed trends in biomass spectra. Biomass (and abundance) size spectra were determined from observations made at the Faroe–Shetland Channel (FSC) in the Northeast Atlantic (water depth 1600 m), the Fladen Ground (FG) in the North Sea (150 m), and the hypoxic Oman Margin (OM) in the Arabian Sea (500 m). Observed biomass increased with body size as a power law at FG (scaling exponent, b = 0.16) and FSC (b = 0.32), but less convincingly at OM (b = 0.12 but not significantly different from 0). A simple model was constructed to represent the same 16 metazoan size classes used for the observed spectra, all reliant on a common detrital food pool, and allowing the three key processes of ingestion, respiration and mortality to scale with body size. A micro-genetic algorithm was used to fit the model to observations at the sites. The model accurately reproduces the observed scaling without needing to include the effects of local influences such as hypoxia. Our results suggest that the size-scaling of mortality and ingestion are dominant factors determining the distribution of biomass across the meio- to macrofaunal size range in contrasting marine sediment communities. Both the observations and the model results are broadly in agreement with the "metabolic theory of ecology" in predicting a quarter power scaling of biomass across geometric body size classes.

Benthic biomass size spectra in shelf and deep-sea sediments

The biomass distributions of marine benthic organisms (meio- to macro-fauna, 1 μg–32 mg wet weight) across three contrasting sites were investigated to test the hypothesis that allometry can consistently explain observed trends in biomass spectra. Biomass (and abundance) size spectra were determined from observations made at the Faroe–Shetland Channel in the north-east Atlantic (water depth 1600 m), the Fladen Ground in the North Sea (150 m), and the hypoxic Oman Margin (500 m) in the Arabian Sea. Observed biomass increased with body size as a power law at FG (scaling exponent, b = 0.16) and FSC (b = 0.32), but less convincingly at OM (b = 0.12 but not significantly different from 0). A simple model was constructed to represent the same 16 metazoan size classes used for the observed spectra, all reliant on a common detrital food pool, and allowing the three key processes of ingestion, respiration and mortality to scale with body size. A micro-genetic algorithm was used to fit the model to observations at the sites. The model accurately reproduces the observed scaling without recourse to including the effects of local influences such as hypoxia. Our results suggest that the size-scaling of mortality and ingestion are dominant factors determining the distribution of biomass across the meio- to macrofaunal size range in contrasting marine sediment communities. Both the observations and the model results are broadly in agreement with the "Metabolic Theory of Ecology" in predicting a quarter power scaling of biomass across geometric body size classes.

Controls on benthic biomass size spectra in shelf and deep-sea sediments – a modelling study

Factors controlling biomass distributions in marine benthic organisms (meio- to macro-fauna, 1 μg–32 mg wet weight) were investigated through observations and allometric modelling. Biomass (and abundance) size spectra were measured at three locations: the Faroe-Shetland Channel in the north-east Atlantic (FSC, water depth 1600 m, September 2000); the Fladen Ground in the North Sea (FG, 150 m, September 2000); and the hypoxic Oman Margin (OM, 500 m, September 2002) in the Arabian Sea. Biomass increased with body size through a power law at FG (allometric exponent, b = 0.16) and at FSC (b = 0.32), but less convincingly at OM (b was not significantly different from −1/4 or 0). Our results question the assumption that metazoan biomass spectra are bimodal in marine sediments. The model incorporated 16 metazoan size classes, as derived from the observed spectra, all reliant on a common detrital food pool. All physiological (ingestion, mortality, assimilation and respiration) parameters scaled to body size following optimisation to the data at each site, the resulting values being consistent within expectations from the literature. For all sites, body size related changes in mortality played the greatest role in determining the trend of the biomass size spectra. The body size trend in the respiration rate was most sensitive to allometry in both mortality and ingestion, and the trend in body size spectra of the production: biomass ratio was explained by the allometry in ingestion. Our results suggest that size-scaling mortality and ingestion are important factors determining the distribution of biomass across the meiofauna to macrofauna size range in marine sedimentary communities, in agreement with the general observation that biomass tends to accumulates in larger rather than smaller size classes in these environments.

Describing assemblages of sediment-living organisms

One of the most fruitful aspects of ecological research is the search for common patterns in the bewildering variability of nature. Given current concerns about global warming, climate change, and habitat degradation, the determination and protection of biodiversity has become paramount. There are essentially three ways of describing an assemblage of organisms, and each of these gives more information on the patterns and interrelationships. First, we have the classical taxonomic method of identifying all species in the assemblage, to the highest taxonomic separation possible (usually to species) and then counting the abundance and weighing the biomass of each taxon. Secondly, we can determine the size and/or biomass spectra of all organisms in the assemblage irrespective of their identities, on the basis that organisms of different sizes or body weights play a different role in the ecosystem. Thirdly, we can determine the role that each organism can play in the system, again irrespective of its name, and define these as ecological groups or guilds—hence separating those feeding in different ways or those building tubes from their free-living associates (e.g. see Elliott et al. 2007 for a discussion of the guild concept). There are many methods of analysing assemblage data; for example Elliott (1994) identified over 25 groups of techniques for macrobenthic analysis (these are mentioned throughout this book and summarized in Chapter 11). Using these methods, when considering assemblages of marine organisms living in sediment, we can ask if there are any ‘rules’ that can be applied to patterns of abundance, size, and biomass distributions and how data on species distributions can be organized. Here, we first treat abundance, then size and biomass spectra, and finally how species assemblages can be assessed. Another way of describing assemblages is to examine the number of species and how abundance is distributed among species, although these are aspects of species diversity which will be addressed in the next chapter. In any sample of a biological community, whether marine, terrestrial, or freshwater, the immediately observable pattern is that most species are rare, represented by one or a few individuals, and only a few species are very common, represented by many individuals.