Global pattern of carbon stable isotopes of suspended particulate organic matter in lakes

Carbon stable isotopes (??¹³C) of particulate organic matter (POM) are useful indicators for tracking the sources of organic matter, CO₂ concentrations, primary productivity and the trophic base in lakes. Here we provide a synthesis of literature data from 228 lakes around the world to assess the distribution pattern of ??¹³C_POM along latitudinal, morphometric and biogeochemical gradients, and the feasibility of utilizing ??¹³C_POM as an indicator for lake metabolism. Results from this analysis revealed a large variation in ??¹³C_POM among lakes with a range from ?46.2 to ?13.0?? and a median of ?29.7??. The ??¹³C_POM generally decreased from low to high latitude along with the decreases in total phosphorus (TP), pH, lake size and the increases in partial pressure of CO₂. The combination of these factors may play a significant role in shaping the pattern of ??¹³C_POM distribution. A multiple regression model using matching data (n?=?92 lakes) indicated that latitude, lake size and TP concentration were the important factors determining ??¹³C_POM, although only 25% of the variance in ??¹³C_POM was explained by the model. Compared to the average ??¹³C value (?27??) of terrestrial plants, 165 lakes (72%) in this analysis were isotopically depleted in ??¹³C_POM, with a mean of ?31.5??, which is indicative of an allochthonous contribution of terrestrial organic matter. This finding is consistent with the view that the majority of lakes in the world receive a terrestrial subsidy of carbon and are sources of CO₂ to the atmosphere.     

Bottom dynamics in lakes

A proper understanding of the bottom dynamic conditions (erosion, transportation, accumulation) in lakes is essential in most sedimentological contexts. Fine cohesive materials generally dominate the open water areas, whereas coarser deposits (sand, gravel) dominate shallow regions where erosion and transportation of fine materials prevail. At present, there is no physical model available which describes the linkage between the energy content of the water-mass and the capacity for sediment entrainment in open water areas. Water-mass energy depends on, e.g. wind direction, duration, velocity, fetch, and the presence of a thermocline. Entrainment depends on, e.g. density, compaction, water and organic content of the sediments and the number and type of bottom fauna. Four different methods are used to determine bottom dynamics, two aresite typical and two arelake typical.Site andlake typical methods each include one method based on collected field data and one based on theoretical data. One method, the cone apparatus, is presented for the first time. It consists of two cones, one of which has a narrow angle and the other a wide angle, which are zero adjusted at the sediment surface before being released to penetrate the sediments. The differential cone penetration, refered to as the penetration ratio, is used to indicate the degree of surficial sediment compaction. This simple, inexpensive instrument provides quantitative data on physical sediment characteristics which may be related to bottom dynamic conditions.     

The dynamics of freshwater phytoplankton stability in the Naroch Lakes (Belarus)

The phytoplankton community of the Belarus Lakes Naroch, Myastro and Batorino, which have a Trophic State Index of 42.3, 60.7 and 66.8, respectively, underwent drastic changes to their structure during the period between 1968 and 2012. Thanks to an extensive monitoring program, these changes were well-documented and were qualitatively interpreted as signs of the community destabilization. The main objective of this study was the quantification of the ecological stability of the phytoplankton community in the Naroch Lakes. The approach to the quantification of ecological stability was based on defining the stability index as an inverse of the Euclidean Distance between the current and the reference states of the algal community (EuD-approach). The stability of the phytoplankton community was characterized by two indices: a “combined” index (SI[Comb]), and a “total community” index (SI[TotB]). SI[Comb] was calculated based on the individual taxonomic group biomasses and thus characterizes the stability of a community structure. SI[TotB] was calculated based on the values of the total algal biomass. Analyses of the results of this study extended the plausibility of the EuD-approach for the quantification of lake phytoplankton stability and allowed us to identify the dynamics of the stability of the Naroch Lakes phytoplankton. For the Naroch Lakes, we observed relatively larger SI[TotB] values in comparison with the SI[Comb] values. The results enabled us to examine the relationship between the lake trophic status and the stability of the phytoplankton community.     

A conceptual mathematical model of the aquatic communities of lakes Naroch and Myastro (Belarus)

A conceptual mathematical model of the dynamics of fish and zooplankton (rotifer) populations of connected lakes Naroch and Myastro (Belarus) is built and examined with parameters based on field data. It is shown that community coupling and trophic interactions give rise to both regular and irregular oscillations in population numbers.     

Geochemistry of suspended and settling solids in two freshwater lakes

This study describes the 1987–1992 time variationof the bulk chemical composition, levels of heavymetals, arsenic, nitrogen and phosporous insuspended and settling solids in Lake Volkerak andLake Zoom (The Netherlands). Suspended and setlingsolids were collected with continuous flowcentrifuges and sediment traps, respectively. Therelations between solids characteristics and metalconcentrations in the particles were investigatedusing correlation and factor-analysis. Heavy metals,except manganese, were associated with clay contentof the particles and with organic carbon which wasmainly determined by phytoplankton growth. Manganesewas correlated with Org-C only. Clay and organicmatter with associated heavy metals showed negativetrends on all locations, and a seasonality due toalgal biomass dilution. It is concluded that thetrophic state significantly affects trace metalcycling. Sediment traps collect different types ofparticles than continuous flow centrifuges. Thetraps collect particles with higher clay content,lower Org-C concentrations and higher Org-C/Nelemental ratios than the centrifuges. This revised version was published online in July 2006 with corrections to the Cover Date.     

Dissolved organic matter in Cumbrian lakes and streams

SUMMARY. 1. A survey of dissolved organic carbon concentration [DOC] and optical absorbance at 340 nm (A340) was carried out for thirteen lakes and twenty-three streams in Cumbria over the period May 1986 to April 1987.
2. Values of [DOC] were in the range 0-6.2 mg 1-1-1, no water having a mean [DOC] greater than 3.6mgI-1. Streamwaters showed no gross seasonal dependence in [DOC], but there was a peak in [DOC] associated with the first major rain event of autumn 1986. Summer values of [DOC] in lakes were greater than winter values, probably because of the production of DOC by phytoplankton.
3. In streams, [DOC] was weakly positively correlated (r2 <0.3) with discharge (as estimated from rainfall); A340 was more strongly correlated (0.4 < r2 < 0.6). Linear regression of mean A340 against mean [DOC] for streams gave a slope consistent with the absorptivities of aquatic humic substances, and a positive intercept on the abscissa that suggests the presence of, on average 0.6 mg 1-1 of DOC that does not absorb at 340 nm. Lake samples taken in winter gave a similar A.340/[DOC] relationship to that for streams, but in summer A340/[DOC] ratios were lower, suggesting that phytoplankton-derived [DOC] absorbs weakly or not at all at 340nm.     

Inherent optical properties of suspended particulates in four temperate lakes: application of in situ spectroscopy

Instrumentation measuring hyperspectral particle attenuation and absorption was used to assess particle concentration and size, chlorophyll, and spectral characteristics as a function of depth in four temperate lakes of different trophy. Partitioning the absorption coefficient permitted us to analyze properties of phytoplankton absorption as a function of ambient illumination and hydrographic conditions. Stratification was found to be a controlling factor in the size distribution and concentration of particles. Bloom cycles (chlorophyll > 10 mg m^?3) were observed to evolve over several weeks but on occasion did change rapidly. Total chlorophyll concentration revealed the majority of the lakes did not follow the typical seasonal succession of biomass associated with temperate waters. Particle and chlorophyll concentration maxima did not always coincide, cautioning the use of chlorophyll a as a surrogate for algal biomass. Phytoplankton near the base of the euphotic zone, including a deep chlorophyll maximum in an oligotrophic system, were found to exhibit significant chromatic adaptation. Unique absorption peaks identified the ubiquitous presence of cyanobacteria in all four lakes. Finally, particle resuspension and possible nepheloid layers were observed in the two smallest lakes.     

Case studies of variations in suspended matter transport in small catchments

Changes of water and suspended sediment composition during three single flood events were investigated in two small catchments in the Mosel region. In addition to suspended sediment characteristics (turbidity, loss on ignition, density, chlorophyll content), several different nutrients and heavy metals were determined in the dissolved and particulate phase. The flood events investigated were characterized by a single peaked hydrograph. In contrast suspended sediment concentrations and the other parameters showed more complex behaviour. The transport of suspended sediment was not only controlled by discharge magnitude. In the course of a flood event different suspended sediment sources are activated. Using the chemograph and the timing of samples collected during the hydrograph these suspended sediment sources can be identified. In addition to the remobilization of sediment and channel erosion, inputs of suspended solids from a sewage plant, road discharge, topsoil and interflow could be identified.     

Influence of airborne suspended matter on mitotic cell division

The effect of organic extracts of airborne suspended matter collected in the highly polluted industrial region of Silesia (Poland) on mitotic cell division was evaluated in the Chinese hamster V79 cell line. Crude benzene extracts as well as sequential elution solvent chromatography (SESC) fractions were investigated for their ability to affect the mitotic index, the proportion of anaphases-telophases to metaphases (AT/M ratio), the cloning efficiency and to produce aneuploid cells. The incidence of cell division disturbances in V79 cells exposed to extracts increased in a concentration-dependent manner. Mitotic arrest, manifested as a highly increased mitotic index and a concomitant decrease in the AT/M ratio, was found for the crude extract at a dose corresponding to 0.75 m3 of air. Comparable effects were noticed for SESC fraction 4, probably containing monophenol compounds. A strong dose-dependent reduction of cloning efficiency of V79 cells demonstrated cytotoxic activity of both the crude extract and fraction 4.     

Quality of suspended fine particulate matter in the Little Tennessee River

Hydrobiologia - Fine particulate organic matter is a major food resource in southeastern river food webs, but natural variability in the quality of this resource has not been assessed. We measured...     

Seasonal and vertical variation in the C : P ratio of suspended and settling seston of lakes

In the absence of field data it is often assumed that the C : P ratio of the seston in lakes corresponds to the ideal ratio of 106 : 1, reported by Redfield et al. (1963) for marine phytoplankton. However, we found out that in nearly all lakes studied C : P ratios deviate systematically from this value especially during periods, when phosphorus is growth limiting. Thus, during summer the sestonic C : P ratio generally exceeds 106 in the epilimnion, but decreases with depth in the hypolimnion. Possible mechanisms which may lead to these seasonal and spatial changes in the C : P ratio are discussed.     

Hydrologic control of dissolved organic matter in low-order Precambrian Shield lakes

Concentrations of dissolved organic carbon (DOC) and color were measuredas a function of time in enclosures and lakes at the Experimental Lakes Area,to calculate their net loss rates. Loss rates in enclosures werefirst order for both DOC and color, with half-times for loss of 166and 122 d, respectively. Thus, the colored, light-attenuating componentof the DOC pool is lost from water more rapidly than is bulk DOC. Loss ratesin lakes, calculated from a steady state model, were similar to values forcolor in enclosures, but for DOC in lakes were four times slower than inenclosures. In lakes, loss rate for DOC increased rapidly with decreasingwater residence time (_w) but was independent of_w when it was greater than 3 years. In lakes, theloss rate for color was independent of water residence time. Thedifference in losses of DOC and color between lakes and enclosurescould be from release of low-color DOC from sediments.     

Detritus and nutrient dynamics in the shore zone of lakes: a review

The importance of detritus varies greatly among shore zones of lakes, but in a large majority of these regions detrital pathways prevail. Aside from a great spatial and seasonal variability, macrophytes and bottom sediments appear to be dominant stores of nutrients in these habitats. Macrophytes hold a central position in nutrient cycling in the shore-littoral lake zones. They are the main source of autochthonous detritus as they prevail in the total biomass of littoral organisms, and they are only rarely available as direct food of consumers. Various processes and interactions determine the role of macrophytes in nutrients dynamics. These are: the intensity of nutrient uptake and translocation, release of nutrients by healthy plants and from decomposing plants, exchange of elements between macrophytes and their periphyton, as well as interception of seston by macrophyte stands. Particular plant species differ in their time of dying and susceptibility to decomposition. The changes in decomposing material (size structure of particles and nutrient content) mean that detritus in various stages of decomposition differs in its role in trophic dynamics of shore-littoral lake zones. Several types of shore regions as regards detritus sources and retention level are discussed.     

Extracellular enzyme activity associated with suspended matter in the River Rhine

SUMMARY. 1. Spatial and temporal variations in exoenzymatic proteolysis and alkaline phosphatase activity in the River Rhine were measured fluorometrically using L-leucyi (ß-naphthylamide and methylumbelliferyl phosphate (MUFP), respectively, as test substances.
2. Extracellular proteolytic activity measured in the lower 150-km reach of the river during 1988 followed the changes in the concentration of particulate nitrogen associated with the occurrence of phytoplankton blooms. Alkaline phosphatase activity was not related to the concentration of particulate phosphate and correlated weakly with particulate nitrogen and phytoplankton concentrations.
3. Seasonal observations (1989) in the lower River Rhine and transport studies in a 660-km-long reach of the river (1990) indicated that the variations in the exoenzyme activities were unrelated (or not closely related) to fluctuating bacterial numbers. Exoproteolytic activity correlated well with thymidine incorporation and algal density, confirming indications in the literature that the exoenzyme activity is related to the overall metabolic rate of the bacterial populations.
4. The exoproteolytic activities in the Rhine are similar to the highest observed in eutrophic freshwaters, indicating a rapid turnover of proteins in the river. Bacterial phosphatase activities, measured with MUFP, were similar to those in the few marine and inland waters studied so far. However, phosphate-limited algal blooms, such as reported for the plume of the Rhine in the North Sea, are likely to contribute substantially to hydrolysis of natural organic phosphates.     

Mutagenicity and genotoxicity of suspended particulate matter in the Seine river estuary

Highly mutagenic compounds such as some PAHs have been identified in surface waters and sediments of the Seine river estuary. Suspended particulate matter (SPM) represents a dynamic medium that may contribute to the exposure of aquatic organisms to toxic compounds in the water column of the estuary. In order to investigate major sources of mutagenic contaminants along the estuary, water samples were taken at 25 m downstream of the outlet of an industrial wastewater-treatment plant (WWTP). SPM samples were analyzed for their genotoxicity with two short-term tests, the Salmonella typhimurium mutagenicity assay (TA98+S9 mix) and the comet assay in the human HepG2 cell line. Sampling sites receiving effluents from a chemical dye industry and WWTP showed the highest mutagenic potencies, followed by petrochemical industries, petroleum refinery and pulp and paper mills. These data indicate that frame-shift mutagens are present in the Seine river estuary. Furthermore, the comet assay revealed the presence of compounds that were genotoxic for human hepatocytes (HepG2 cells). We also observed a high level of mutagenic potency in the sediment of the lower estuary (3 × 10? revertants/g). The source of mutagenic and genotoxic compounds seems to be associated with various types of effluents discharged in the Seine river estuary. Both test systems resulted in the same assessment of the genotoxicity of particulate matter, except for three of the 14 samples, underlying the complementarity of bioassays.