Biological fractionation of stable carbon isotopes at the aerobic/anaerobic water interface of meromictic water bodies

Mass-spectrometric investigation of carbon isotope composition (δ¹³C) was carried out for suspended organic matter and dissolved mineral compounds for the water column of some meromictic water bodies differing in salinity and trophic state. As a rule, a more pronounced carbon isotope fractionation (resulting from the metabolism of phytoplankton and anoxygenic phototrophic bacteria) was revealed in the zones of enhanced oxygenic and anoxygenic photosynthesis. Carbon isotope fractionation at the border between oxidized and reduced waters depends both on the activity of microbial communities and on the dominant species of phototrophic microorganisms. Analysis of the distribution profiles of the isotopic composition of suspended organic matter and dissolved mineral carbon revealed active mineralization of the organic matter newly formed via anoxygenic photosynthesis in the monimolimnion by microbial communities, resulting in the release of isotopically light carbon dioxide. Mineral carbon in the anaerobic zones of highly productive meromictic water bodies is therefore enriched with the light ¹²C isotope.     

Characteristics of Culicoides (Diptera, Ceratopogonidae) breeding places near Salisbury, Rhodesia

Abstract. 1. A survey of Culicoides breeding places was made around Salisbury. Out of forty species caught in light traps, only nineteen were reared from breeding places.
2. The seven most abundant species with their characteristic sites were C.pycnostictw in mud around water bodies, especially dams; C.nivosus very prevalent around puddles rich in organic matter: C. distinctipennis along drainage canals intermediate in organic matter; C.gulbenkiani in cow dung especially on damp soil; Caccraensis gp. only in rot holes and tree forks; Cschultzei gp. along streams and drainage canals in mud rather poor in organic matter; C.tropi-calis in drainage canals very low in organic matter; C.imicola possibly breeds widely dispersed mainly in a rich mixture of organic matter and damp soil, with cow pats and edges of water bodies being marginal.
3. The prevalent species are believed to breed all year round. Preponderance of females in the breeding places was found in C.pycnostictus, C.nivosus and C.accraensis gp. while the reverse was true in C.distinctipennis and C.gulbenkiani. The preponderance of males as indication of proximity to breeding sites is thus probably questionable.     

Nitrogen and phosphor compounds in bottom sediments: mechanisms of accumulation,transformation and release

This paper is an overview of Russian literature dealing with the accumulation, the transformations and the release of phosphate and nitrogen compounds in a great number of Russian lakes and reservoirs. A considerable data bank has been analysed. Special attention is given to the relations of N- and P-accumulation with the input and transformation of organic carbon, as well as to the release mechanisms, often in relation to eutrophication of the lakes and reservoirs. It is shown that the major input of organic matter into the sediments comes from autochthonous material, and is usually > 70 %. The relative importance of phytoplankton and macrophytes as sources of organic matter is discussed; it appears that trophic state, depth and other factors may have a large influence on this ratio. In shallow eutrophic lakes macrophytes may be the source of organic matter, which source can amount to 1.5–2.5 times that of phytoplankton. It is also shown that the C/N ratio is not a good indicator of the source of the organic matter, because their C/N ratios often are not very different. The decomposition rate of organic matter was analysed; it depends on trophic state and other factors. Sediment N accumulation is mostly (> 90%) in organic form, and depends on nitrogen and organic matter inputs coming from phytoplankton or macrophytes. A correlation coefficient of 0.9–0.95 was found in 176 lakes. In 113 lakes the N accumulation was 0.11 x C accumulation, with C/N ratios between 7.4 and 12.9. Ammonification was rather constant in different groups of lakes; values were often about 20–25 mg m⁻² d⁻¹. The presence of the different forms of nitrogen in interstitial water and in adsorbed forms is discussed. The N in interstitial water is usually in the form of NH₃. Sediment P-accumulation is usually in inorganic form and is related to primary production. Three different groups of sediments could be distinguished with C/P ratios of 31–100, of 101–350 and > 350. In hard water lakes P sedimentation was found to be 0.3–0.5 times that in soft water lakes with comparable primary production. The relative occurrence of apatite, non-apatite and residual P in sediments was calculated. In the interstitial water the P concentration appeared to be controlled by the input and decomposition of organic matter. The concentration of phosphate dissolved in the interstitial water of the top 2 cm layer is often 10–100 times lower than that of the dissolved N. The concentrations of interstitial phosphate are from a few μgl⁻¹ up to 15 mgl⁻¹, but the higher concentrations occur only rarely. Different types of vertical profiles of P compounds in the sediments were shown to be related with the presence of an oxidised zone, the presence of clay etc. Autochthonous apatite and non-apatite phosphates are more mobile than the allochthonous ones and are in equilibrium with interstitial phosphate. Accumulation of autochthonous apatite in sediments is controlled by decomposition of organic matter and accumulation of carbonates.     

The effect of humic substances on the toxicity of copper and zinc for Daphnia magna]

The results of laboratory experiments of humic matter influence on toxic resistance of Daphnia magna to zinc and copper using water samples from a few Karelia water bodies are presented. The increasing of humic matter content in water samples has been shown to promote the binding of a part of metals in organic complexes that leads to decrease of their toxicity for hydrobionts.     

The Effects of pH and Levels of Organic Matter on the Death Rates of Salmonellas in Chicken Scald-tank Water

The immersion scalding of chicken carcases at 52°C for 2.5 min was found to result in the accumulation of bacteria and organic matter in the water. Disassociation of ammonium urate present in chicken faeces caused the pH value of the water to fall rapidly from 8.4 to 6.0. This pH was maintained for most of the time the tank was in operation. The change in pH value greatly increased the heat resistance of some common salmonella serotypes with a strain of Salmonella typhimurium being the most resistant, having a D52°C value of 34.5 min. The pH value of the water was found to be close to the optimum for the heat resistance of salmonellas. In scald water at pH 5.9–6.0 the death rate of Salm. typhimurium was shown to be independent of organic matter levels indicating that pH was the major influence on heat resistance.     

Trace metal speciation in a wastewater wetland and its bioaccumulation in tilapia Oreochromis niloticus

Trace metal species in the water column of a canal system forming a wetland filled with wastewater were analyzed to determine their correlation with metal accumulation in the gills of locally fished Oreochromis niloticus. The metal concentrations in the suspended particles and water dissolved were analyzed. The metal species were calculated using Windermere Humic Aqueous Model version VII showing that the high organic matter and major cation contents were important parameters. Also, the free ion metal concentration was expected to correlate with the organic matter aromaticity; however, organic compounds other than humic susbtances seem to be complexing the metals in the system. Additionally, no clear correlation could be found between metal accumulation in gills and any of the dissolved metal species. Nonetheless, certain trends could be seen between the calculated metal species and metal accumulation in the tilapia from the suspended particles.     

Analysis of accumulation of heavy metals from river bottom sediments of the urban environment in the bodies of oligochaetes

The content of heavy metals in the bodies of oligochaetes in two small rivers that flow along the central part of a large industrial city has been studied. It has been established that the concentration of mobile (bioavailable) forms of metals in oligochaetes is higher than that in bottom sediments. The similarity of the pattern of accumulation of pollutants in the bodies of oligochaetes and the correlation of heavy metals with the organic matter of river sediments has been revealed in both urban watercourses.     

Evaluating the ecological performance of wetland restoration in the Yellow River Delta,China

Long-term monitoring is essential to evaluate the effects of wetland restoration projects. A monitoring program before and after restoration has been carried out in the study area located in the Yellow River Delta since 2001. Water quality, soil salinity, soil organic matter, plant community, and bird species were chosen as indicators in this program. During the past seven years, the restored wetland showed increasing efficiency in reducing water pollution levels. Soil quality was constantly improved through salinity reduction and soil organic matter accumulation. The vegetation community quickly re-established after the restoration was initiated in 2002. The restored vegetation communities provide favorable habitat conditions for birds and thirty-seven bird species were observed in October 2007. Based on Canonical Correspondence Analysis (CCA), plant species and vegetation community are mainly influenced by soil salinity and water depth. These indicate that conducting freshwater to the project area is an efficient measure for vegetation restoration. While monitoring results show that the restoration project had positive effects on the wetland ecosystem over the past seven years, two issues remain for future study: (1) the contribution of harvesting vegetation to stabilizing nutrient removal rate and the accumulation of soil organic matter in the soil; and (2) the effects of excessive propagation of Phragmites australis on spatial heterogeneity and plant diversity.     

Content of Plant Pigments in the Bottom Sediments of the Water Bodies of Vietnam

Data on the content of plant pigments in the bottom sediments (BSs) of the water bodies of Central and South Vietnam are given for the first time. The average concentration of chlorophyll a and phaeopigments (Chl + Ph) in total reaches up to 3.9 μg/g dry matter in rivers, 5.6 in ponds, 13.8 in sand quarries, 56.8 in reservoirs, and 245 in lakes. Most frequently, the concentrations of Chl + Ph in the coastal zones of watercourses and water bodies fall in the oligotrophic category, and those in the central areas are in the hypertrophic category. Relationships between concentrations of Chl + Ph and water depth, content of oxygen near the bottom, moisture content, volumetric mass, and concentrations of organic matter (OM) in the BSs are found. The content of sedimentary pigments in tropical waters of Vietnam is similar to that in freshwater ecosystems of temperate latitudes, despite the substantial differences of climatic zones in temperature and light regimes.     

Primary production of plankton and decomposition of organic matter in saline lakes of the crimea peninsula

The lakes under study can be classified as eutrophic-hypertrophic waterbodies according to the level of primary production. High concentrations of suspended matter (up to 7326 g/m³) and total phosphorus (up to 5625 mg/m³) were registered in the lakes. The values of the primary production of plankton and the destruction of organic matter do not depend on the absolute concentration of salts in water. Unlike the destruction of organic matter, the primary production of plankton is higher in winter than in summer. Thus, the accumulation of organic matter in saline lakes occurs mainly in winter. The negative relationship between the primary production of plankton and the biomass of the filter feeder Artemia sp. has been determined.     

Recent patterns of sediment accumulation in a small closed eutrophic lake revealed by the sediment records

A short-core palaeolimnological investigation was undertaken with the aim ofacquiring knowledge of sediment deposition. Analyses of the lithological composition of sediments from the whole-lake basin were performed on the small eutrophic L. Linajärv (northern Estonia) and the concentrations of mineral and organic matter were measured on 647 sub-samples from 14 sediment cores. The accumulation rate of the sediment sequences was established and C/N ratios of organic matter in some cores were recorded. Results indicate that the water depth, basin slopes and distance to the shore have the most important impact on the physical sediment properties. It was shown that variations in the mineral matter concentrations were influenced by the changes in deposition conditions in the areas with steep slopes. The study indicated that more objective information about the sedimentation mechanisms is obtained using analysis of the concentration ratio of mineral and organic matter since it reduces the implied role of diagenetic compaction.     

The glacial oceans

The accumulation of carbonate and carbonaceous matter increased during the glacial age due to intensified sink water formation in the northernmost Atlantic Ocean and the intensified upwellings in the Indo-Pacific Oceans. As a consequence of that there was a decrease of the ΣCO₂ concentration in the ocean as well as of the CO₂ content in the atmosphere.As a whole the accumulation area of calcareous matter was enlarged by ca. 20% during glacial times. The decreased accumulation area in the North Atlantic was well compensated by a large increase in the Indo-Pacific oceans.The northernmost part of the Atlantic Ocean was quasi-stagnant during the most intense deglacial times, thus causing a reduced exchange between surface water and deep water which, in its turn, led to a decrease of the accumulation of carbon (as CaCO₃ and organic matter). The concentration of ΣCO₂ rose in the seawater and the pCO₂ increased as well.     

The effect of aquatic plant abundance on shell crushing resistance in a freshwater snail

Most of the shell material in snails is composed of calcium carbonate but the organic shell matrix determines the properties of calcium carbonate crystals. It has been shown that the deposition of calcium carbonate is affected by the ingestion of organic compounds. We hypothesize that organic compounds not synthesized by the snails are important for shell strength and must be obtained from the diet. We tested this idea indirectly by evaluating whether the abundance of the organic matter that snails eat is related to the strength of their shells. We measured shell crushing resistance in the snail Mexipyrgus churinceanus and the abundance of the most common aquatic macrophyte, the water lily Nymphaea ampla, in ten bodies of water in the valley of Cuatro Ciénegas, Mexico. We used stable isotopes to test the assumption that these snails feed on water lily organic matter. We also measured other factors that can affect crushing resistance, such as the density of crushing predators, snail density, water pH, and the concentration of calcium and phosphorus in the water. The isotope analysis suggested that snails assimilate water lily organic matter that is metabolized by sediment bacteria. The variable that best explained the variation in crushing resistance found among sites was the local abundance of water lilies. We propose that the local amount of water lily organic matter provides organic compounds important in shell biomineralization, thus determining crushing resistance. Hence, we propose that a third trophic level could be important in the coevolution of snail defensive traits and predatory structures.     

Comparison of different methods of water quality evaluation by means of oligochaetes

Using as examples water bodies in different geographical zones (Lake Ladoga, the River Sukhona, shallow-water ponds of the North Caucasus) the known methods of water quality evaluation by means of oligochaetes are considered. There is no unique universal method of pollution bioindication in. this way. In water bodies of all types the mass development of oligochaetes and the reduction of their species diversity are indications of. (1) large quantities of organic matter; (2) favourable oxygen regime; (3) absence or insignificant quantity of heavy metal solids, petroleum substances and agricultural chemicals; (4) intensive self-purification of the water body.     

How do salinity and water stress affect transport of water,assimilates and ions to tomato fruits?

The study was conducted in order to determine whether water stress affects the accumulation of dry matter in tomato fruits similarly to salinity, and whether the increase in fruit dry matter content is solely a result of the decrease in water content. Although the rate of water transport to tomato fruits decreased throughout the entire season in saline water irrigated plants, accumulation rates of dry matter increased significantly. Phloem water transport contributed 80–85% of the total water transport in the control and water-stressed plants, and over 90% under salinity. The concentration of organic compounds in the phloem sap was increased by 40% by salinity. The rate of ions transported via the xylem was also significantly increased by salinity, but their contribution to fruit osmotic adjustment was less. The rate of fruit transpiration was also markedly reduced by salinity. Water stress also decreased the rate of water transport to the tomato fruit and increased the rate of dry matter accumulation, but much less than salinity. The similar changes, 10–15%, indicate that the rise in dry matter accumulation was a result of the decrease in water transport. Other parameters such as fruit transpiration rates, phloem and xylem sap concentration, relative transport via phloem and xylem, solutes contributing to osmotic adjustment of fruits and leaves, were only slightly affected by water stress. The smaller response of these parameters to water stress as compared to salinity could not be attributed to milder stress intensity, as leaf water potential was found to be more negative. Measuring fruit growth of girdled trusses, in which phloem flow was inactive, and comparing it with ungirdled trusses validated the mechanistic model. The relative transport of girdled as compared to ungirdled fruits resembled the calculated values of xylem transport.     

Vertical distribution of organic matter in eight vegetation types near Eagle Summit, Alaska

The amount and distribution of organic matter was measured in different categories in six montane tundra vegetation types in a snow accumulation area and in tussock and intertussock areas in Eriophorum vaginatum tussock tundra in central Alaska. In root properties, the tussock and intertussock areas were more similar to the fellfield zone than to the vegetation zones below the snow accumulation area. Root density apparently increased as soil nutrients decreased, but this increase may be caused by higher soil moisture and higher root relative water content. The tussock tundra has accumulated more dead soil organic matter than any of the montane zones.     

Influence of quantity and lability of sediment organic matter on the biomass of two isoetids,Littorella uniflora and Echinodorus repens

1. Despite real improvement in the water quality of many previously eutrophic lakes, the recovery of submerged vegetation has been poor. This lack of recovery is possibly caused by the accumulation of organic matter on the top layer of the sediment, which is produced under eutrophic conditions. Hence, our objective was to study the combined effects of quantity and lability of sediment organic matter on the biomass of Echinodorus repens and Littorella uniflora and on the force required to uproot plants of L. uniflora. 2. Lake sediments, rich in organic matter, were collected from four lakes, two with healthy populations of isoetids and two from which isoetids had disappeared. The four lake sediments were mixed with sand to prepare a range of experimental sediments that differed in quantity and lability of sediment organic matter. Two isoetid species, E. repens and L. uniflora, were grown in these sediments for 8 weeks. Sediment quality parameters, including elemental composition, nutrient availability and mineralisation rates, were determined on the raw sources of sediment from the lakes. Porewater and surface water were analysed for the chemical composition in all mixtures. At the end of the experiment, plants were harvested and their biomass, tissue nutrient concentration and (for L. uniflora) uprooting force were measured. 3. For both species, all plants survived and showed no signs of stress on all types of sediment. The biomass of E. repens increased as the fraction of organic matter was increased (from 6 to 39% of organic content, depending upon sediment type). However, in some of the sediment types, a higher fraction of organic matter led to a decline in biomass. The biomass of L. uniflora was less responsive to organic content and was decreased significantly only when the least labile sediment source was used to create the gradient of organic matter. The increase in shoot biomass for both species was closely related to higher CO₂ concentrations in the porewater of the sediment. The force required to uproot L. uniflora plants over a range of sediment organic matter fitted a Gaussian model; it reached a maximum at around 15% organic matter and declined significantly above that. 4. Increasing organic matter content of the sediment increased the biomass of isoetid plants, as the positive effects of higher CO₂ production outweighed the negative effects of low oxygen concentration in more (labile) organic sediments. However, sediment organic matter can adversely affect isoetid survival by promoting the uprooting of plants.     

Water quality management in the River Gudenaa,a Danish lake-stream-estuary system

Waste water purification has been established to some extent throughout the 3,260 km² catchment area of the River Gudenaa water system during the last 20 years. Biological treatment and phosphorus removal are now undertaken in almost all towns, and organic matter and phosphorus loading from fishponds and farms has been reduced. The pollution abatement strategy employed has been to coordinate and differentiate waste water treatment so as to maximise the environmental benefit/cost ratio. The time lag between implementing an abatement measure and observing an improvement in water quality varies considerably depending on the nature and cultural history of the water bodies involved and the processes occurring during the passage of water between them.Nutrient transformation and retention within water bodies of the Gudenaa system is of great importance for nutrient loading of the downstream lakes and of the estuary (Randers Fjord), and even for the Danish Belt sea. When loading is reduced retention changes, but to a different extent in different water bodies.     

Simulation of accumulated matter from human feces in the sawdust matrix of the composting toilet

A bio-kinetic model for aerobic biodegradation of human feces was applied to the practical operation of the composting toilet. The first aim of this study was to describe nitrogen transformation in the toilet as well as organic carbon. Second aim was to obtain the kinetic parameters for better prediction of accumulated matter for a long time of the practical operation. Six simple fractions of fecal carbon (slowly hydrolyzable matter, easily hydrolyzable matter, readily biodegradable matter, biologically inert type of matter etc.) were prepared in the model. Nitrogen factors were incorporated to each factor of fecal carbon. Modification of only one kinetic parameter for hydrolysis of slowly hydrolyzable carbon was required to obtain the best fitting curve of accumulation in the toilet. Model prediction for one-year operation of the toilet showed that temporal accumulation of biodegradable organic matter was significant in the first stage whereas main accumulation would be biologically inert type of organic matter at the end of the operation.     

Degradation of Macromolecular Organic Compounds in a Tropical Lagoon (Ciénaga Grande,Colombia) and its Ecological Significance

Primary production and decomposition of organic substances were investigated in a tropical lagoon during the rainy season. Production and mineralization were measured using the oxygen method. Total bacteria numbers and biomasses were estimated with epifluorescence microscopy, and the enzymatic degradation capacity of model substrates was determined photometrically. These parameters were measured in the water and sediment of the lagoon itself and also in its effluents and incoming waters. The aim of the study was to determine the sites of highest microbial activity in the lagoon and to compare its activity with other coastal water bodies. Since the shallow water lagoon contains a large amount of particulate matter, it was of special interest to study the degradation of this material and its influence on the microbial population. It was found that up to 14 % of the bacteria colonized the particles and that 62 % of the respiration originated in the particle fraction >8 μm. Highest exoenzymatic activities were measured in the sediment and water of the mangrove belt. It is concluded that decomposition and conditioning of particulate organic matter play dominant roles in the recycling of organic carbon in the lagoon.