The role of algae in the removal of Escherichia coli in a tropical eutrophic lake

Eutrophication and its accompanying algal development in lakes is a nuisance and may be problematic for aquatic life, but limited algal development may have some beneficial consequences. Dissolved oxygen concentration and pH increases attributed to algae in algal-based treatment ponds may occur in eutrophic lakes and can result in the inactivation of faecal coliforms in eutrophic lakes. We investigated the die-off of Escherichia coli placed in dialysis tubes in a eutrophic lake at different depths and locations. The importance of E. coli attachment to algae and suspended matter was also assessed. Algal presence in the lake resulted in significant decay of E. coli. At chlorophyll a concentration ≤0.08 mg L⁻¹ in Weija Lake, decay rate of E. coli is directly proportional to the chlorophyll a concentration of the lake. Under laboratory conditions, as chlorophyll a concentration increases in light however, an optimum chlorophyll a concentration (0.24 mg/L) is reached after which the rate of decay of E. coli decreases. These results show that limited algal presence representing optimum chlorophyll a concentration in restored ecosystems may have public health benefits for rural communities in developing countries that depend on raw water for domestic activities.     

Multiple addition bioassay of Tjeukemeer water

Multiple addition bioassay of water from the eutrophic lake Tjeukemeer revealed that in 1979 from the end of May until the end of November, when the lake was dominated by Oscillatoria agardhii, N and not P was the principal factor limiting algal growth. During periods with very low concentrations of Tot-Fe_diss in the lake, chelated Fe also limited algal growth in the bioassays. The results of this study further suggested that the concentrations of trace metals have reached levels toxic to phytoplankton. Trace metals inhibited growth particularly when the lake received relatively humus-poor IJsselmeer water with a lower metal binding capacity.     

Decomposition of Blue-Green Algal (Cyanobacterial) Blooms in Lake Mendota, Wisconsin

Decomposition of natural populations of Lake Mendota phytoplankton dominated by blue-green algae (cyanobacteria) was monitored by using oxygen uptake and disappearance of chlorophyll, algal volume (fluorescence microscopy), particulate protein, particulate organic carbon, and photosynthetic ability (¹⁴CO₂ up-take). In some experiments, decomposition of ¹⁴C-labeled axenic cultures of Anabaena sp. was also measured. In addition to decomposition, mineralization of inorganic nitrogen and phosphorus were followed in some experiments. Decomposition could be described as a first-order process, and the rate of decomposition was similar to that found by others using pure cultures of eucaryotic algae. Nitrogen and phosphorus never limited the decomposition process, even when the lake water was severely limited in soluble forms of these nutrients. This suggests that the bacteria responsible for decomposition can obtain all of their key nutrients for growth from the blue-green algal cells. Filtration of lake water through plankton netting that removed up to 90% of the algal biomass usually did not cause a similar decrease in oxygen demand, suggesting that most of the particulate organic matter used for respiration of the decomposing bacteria was in a small-particle fraction. Short-term oxygen demand correlated well with the particulate chlorophyll concentration of the sample, and a relationship was derived that could be used to predict community respiration of the lake from chlorophyll concentration. Kinetic analysis showed that not all analyzed components disappeared at the same rate during the decomposition process. The relative rates of decrease of the measured parameters were as follows: photosynthetic ability > algal volume > particulate chlorophyll > particulate protein. Decomposition of ¹⁴C-labeled Anabaena occurred at similar rates with aerobic epilimnetic water and with anaerobic sediment, but was considerably slower with anaerobic hypolimnetic water. Of the various genera present in the lake, Aphanizomenon and Anabaena were more sensitive to decomposition than was Microcystis. In addition to providing a general picture of the decomposition process, the present work relates to other work on sedimentation to provide a detailed picture of the fate of blue-green algal biomass in a eutrophic lake ecosystem.     

Experimental study of the effect of nutrients on phytoplankton of the shallow highly eutrophic Lake Nero

Experimental studies of the effect of phosphorus, nitrogen, and silicon on the phytoplankton of the shallow highly eutrophic Lake Nero have been carried out. It is shown that the enrichment of lake water with nitrogen leads to an increased concentration of chlorophyll a and the growth of the biomass of dominant algae species. Phosphorus limits the abundance of a certain species of algae; the limiting role of silicon in the development of spring phytoplankton has not been experimentaly confirmed.     

Publisher's note

During the late spring and early summer 1976, laboratory cultured cells of five marine algae were enclosed in dialysis sacks and grown in situ, in Ligurian coastal waters.Skeletonema costatum (Greville) Cleve did not grow at all. Hemiselmis virescens Droop stayed alive, but did not grow significantly. Platymonas suecica (Butcher) Manton &; Parke grew on cell reserves. Only Phaeodactylum tricornutum Bohlin and Thalassiosira pseudonana Hasle &; Heimdal took up nutrients from sea water when all reserves were exhausted. When division ended, all cells were capable of growing when sub-cultured, but physiologically were only slightly active. During immersion in oligotrophic waters, cell contents adapted quickly from nutrient-rich to nutrient-limited growth conditions. During adjustment to equilibrium with natural conditions, the three species became impoverished mainly in phosphorus (67–88% of initial values), ATP (54–92%), and chlorophyll a (59–89%); losses of nitrogen were lower (24–53%).To obtain algal material similar to that in the wild, the data suggest that the cells have to be kept in situ only until they divide five times, which usually requires no more than a week. Counting the cell density each day is probably the most convenient method of control, and each culture should be counted, because the difference of growth between aliquot dialysis cultures can be important (up to 28%).Data obtained for “wild-like” cells of Platymonas suecica, Phaeodactylum tricornutum, Thalassiosira pseudonana, and a wild contaminant population of Cylindrotheca closterium Rabenhorst with biochemical analysis used to run the Droop's model and with enrichment bioassays demonstrate that, during the period studied, phosphorus was the limiting factor for the algal growth. Bioassays also demonstrate that there were some specific variations; some algae were permanently limited by phosphorus, while for a few others nitrogen and phosphorus could be equally limiting.     

Phytoplankton of an eutrophic tropical reservoir: comparison of biomass estimated from counts with chlorophyll-a biomass from HPLC measurements

The seasonal variation of phytoplankton in an eutrophic tropical reservoir was evaluated through photosynthetic pigments analyzed by HPLC. The contributions of algal classes to total chlorophyll a (TChl-a) were estimated by two procedures. The first one used fixed marker pigment/chlorophyll a ratio available from culture studies of the major species of each class. In the second procedure, a matrix factorization program (CHEMTAX) was used to analyze the pigment data. The pigment data were compared with carbon biomass estimated from microscope analysis. A significant correlation between total chlorophyll a (measured by HPLC) and total biomass was obtained, indicating only a slight variation in the content of algal chlorophyll a when compared to its fluctuations in carbon biomass. The interpretation of pigment data with CHEMTAX resulted in a good agreement with biomass. Although displaying some differences, the general pattern of the phytoplankton community dynamics and the major shifts in composition, biomass and the cyanobacterial bloom were evidenced. In contrast, Chl-a biomass estimates from fixed Xan/Chl-a ratios presented poor agreement with microscope data and did not register the principal changes in phytoplankton. Our results also highlighted the needs of better understanding of the relationships between marker pigments, chlorophyll-a and algal biomass.     

Limiting nutrients for periphyton growth in sub-alpine, forest, agricultural and urban streams

1. Nutrient-diffusing artificial substrata were used in summer and autumn to assess limiting nutrients for periphytic algal growth in streams draining sub-alpine, forested, agricultural and urban catchments in eastern Victoria, Australia. 2. Chlorophyll a density was primarily limited by nitrogen in most cases; often phosphorus was secondarily limiting. One sub-alpine, one forest and one agricultural stream were primarily phosphorus limited in at least one season. Added trace elements and vitamins did not increase chlorophyll density. 3. The dominant filamentous algal genera did not differ greatly between various nutrient enrichments. However, the relative abundance of Stigeodanium spp. was sometimes increased on substrata containing the limiting nutrient. 4. The results suggest that nutrient limitation is a widespread phenomenon in Victorian streams, and that limiting nutrients can be inferred from stream-water nitrogen to phosphorus ratios in many instances.     

Predicting concentration of total phosphorus and chlorophyll a in a lake with short hydraulic residence time

The relationship between total phosphorus and chlorophyll a concentration was determined for Skinner Lake, Indiana over an annual cycle in 1978–79. Total nitrogen:total phosphorus ratios in the epilimnion ranged from 19 to 220 suggesting a phosphorus-dependent algal yield in the epilimnion. Approximately 90% of annual TP loading reached the lake via streamflow, and 93% of this entered during snowmelt and spring-overturn periods. At that time incoming water flushed the lake 2.4 times. Atmospheric loading accounted for 1.4% of annual TP load. Internal hypolimnetic TP loading occurred during summer stratification. Mean [chl a] for the ice-free period was 15.15 mg m^–3, within the range expected for eutrophic lakes.The 1978–79 data were used in conjuction with the Vollenweider & Kerekes (1980) model to produce a model specific for the Skinner Lake system. The model predicted mean epilimnetic total phosphorus and chlorophyll a concentrations from mean total phosphorus concentration in inlet streams and from lake water residence time during the period of spring overturn and summer stratification. The Skinner-specific model was tested in 1982 and it closely predicted observed mean epilimnetic [TP] and [chl a] during the ice-free period. This study shows that variability in lake models which average data over an annual period can be reduced by considering lake-specific seasonal variation in hydrology and external TP loading.     

Pigment-Based Chemotaxonomy - A Quick Alternative to Determine Algal Assemblages in Large Shallow Eutrophic Lake?

Pigment-based chemotaxonomy and CHEMTAX software have proven to be a valuable phytoplankton monitoring tool in marine environments, but are yet underdeveloped to determine algal assemblages in freshwater ecosystems. The main objectives of this study were (1) to compare the results of direct microscopy and CHEMTAX in describing phytoplankton community composition dynamics in a large, shallow and eutrophic lake; (2) to analyze the efficiency of the pigment-based method to detect changes in phytoplankton seasonal dynamics and during rapid bloom periods; (3) to assess the suitability of specific marker pigments and available marker pigment:chlorophyll a ratios to follow seasonal changes in eutrophic freshwater environment. A 5-year (2009-2013) parallel phytoplankton assessment by direct microscopy and by CHEMTAX was conducted using published marker pigment:chlorophyll a ratios. Despite displaying some differences from microscopy results, the pigment-based method successfully described the overall pattern of phytoplankton community dynamics during seasonal cycle in a eutrophic lake. Good agreement between the methods was achieved for most phytoplankton groups - cyanobacteria, chlorophytes, diatoms and cryptophytes. The agreement was poor in case of chrysophytes and dinoflagellates. Our study shows clearly that published marker pigment:chlorophyll a ratios can be used to describe algal class abundances, but they need to be calibrated for specific freshwater environment. Broader use of this method would enable to expand monitoring networks and increase measurement frequencies of freshwater ecosystems to meet the goals of the Water Framework Directive.     

Composition of inorganic and organic nutrient sources influences phytoplankton community structure in the New River Estuary, North Carolina

The New River Estuary, NC, is a nutrient-sensitive, eutrophic water body that is prone to harmful algal blooms. High annual loading from the watershed of varying nutrient forms, including inorganic phosphorus and inorganic and organic nitrogen, may be linked to the persistence of algal blooms in the estuary. In order to evaluate phytoplankton response to nutrient inputs, a series of in situ nutrient addition experiments were carried out during June 2010 to July 2011 on water from an estuarine site known to support algal blooms. Estuarine water was enriched with nutrients consisting of individual and combined sources of dissolved inorganic nitrogen, orthophosphate, urea, and a natural dissolved organic nitrogen (DON) addition derived from upstream New River water. The combined inorganic N and P addition most frequently stimulated phytoplankton biomass production as total chlorophyll a. The responses of diagnostic (of major algal groups) photopigments were also evaluated. Significant increases in peridinin (dinoflagellates), chlorophyll b (chlorophytes), and myxoxanthophyll (cyanobacteria) were most frequently promoted by additions containing riverine DON. Significant increases in zeaxanthin (cyanobacteria) were more frequently promoted by inorganic nitrogen additions, while increases in fucoxanthin (diatoms) and alloxanthin (cryptophytes) were not promoted consistently by any one nutrient treatment. Evaluating the impact of varying nutrient forms on phytoplankton community dynamics is necessary in order to develop strategies to avoid long-term changes in community structure and larger-scale changes in ecosystem condition.     

Light‐Nutrient Influences on Biomass,Photosynthetic Potential and Composition of Suspended Algal Assemblages in the Middle Cape Fear River,USA

Dilution bioassays were conducted to evaluate the impact of nutrients on biomass (chlorophyll a), photosynthetic potential, and class composition of suspended algal assemblages in the middle Cape Fear River (USA). Ambient concentrations of dissolved inorganic nitrogen (DIN) and soluble reactive phosphorus (SRP) varied from 37.2 to 83.8 and from 1.0 to 7.1 μmol L^–1. Experiments conducted at photosynthetic photon flux densities (PPFDs) similar to the mixed water column (< 1 to 5.3 E m^–2d^–1) showed no change in chlorophyll a, photosynthetic potential, or algal class composition at 15, 30, and 45% dilutions of DIN, SRP, or both. However, chlorophyll a and photosynthetic potential increased significantly in nutrient dilution bioassays conducted at PPFDs four‐fold above ambient, while the abundance of diatoms and Chrysophytes increased under elevated PPFD and ambient or elevated nutrients. Overall, the data indicate that irradiance is more important than nutrients in determining the size and class composition of suspended algal assemblages. (© 2008 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)     

Grazing by Talorchestia longicornis on an algal mat in a new England salt marsh

Grazing experiments using ¹⁴C and an analysis of fecal pellets and gut contents established that the gammaridean amphipod, Talorchestia longicornis Say, ingests blue-green algae on algal mats in a Massachusetts salt marsh. This grazing had a measurable effect on the lower algal mat, where the density of T. longicornis was high. Exclusion of amphipods resulted in increases in chlorophyll a content, carbon incorporation, and nitrogen fixation. This effect was not seen on the upper mat where T. longicornis was less abundant. The assimilation efficiency of T. longicornis feeding on a diet consisting mainly of blue-green algae was surprisingly high (67 %) considering that blue-green algae are usually considered as a poor quality food for herbivores. The population of T. longicornis seems to be annual, with growth of the overwintered juveniles in spring and early summer.     

Uncoupling of chlorophyll and nutrients in lakes – possible reasons,expected consequences

Total phosphorus and total nitrogen explained a low percentage of summer chlorophyll variability in epilimnia of the Great Masurian Lakes. Division of the whole data set into two subgroups of lakes improved approximation of the chlorophyll nutrient relationship but revealed also functional differences between the lakes distinguished in that way. Chlorophyll in eutrophic lakes correlated well with nitrogen and phosphorus, that in mesotrophic lakes (those with summer chlorophyll <=22 mg m^–3 as calculated in the model) was related to none of the nutrients. Higher summer chlorophyll content in epilimnetic waters was accompanied by higher chl:PP and chl:PN ratios. Algal adaptation to poor light conditions in eutrophic lakes is postulated as a possible reason for that difference.Chlorophyll – nutrient relationships varied with the trophic status of lakes. Epilimnetic chlorophyll strictly followed phosphorus changes in eutrophic lakes but did not do so in mesotrophic ones. Detailed comparison of selected meso- and eutrophic lakes showed marked differences in the seasonal changes of chlorophyll and nutrient concentrations and in sedimentation rates, especially in spring. Nutrient limitation rather than zooplankton grazing is suggested as a possible mechanism of controlling algal abundance and the sequence of spring events in a eutrophic lake. It is hypothesised that phosphorus turnover in eutrophic lakes is dominated by seasonal vertical fluxes, while in mesotrophic lakes it is more conservative with consumption and regeneration restricted mostly to metalimnion. Possible consequences of such conclusion are discussed in the paper.     

The antagonistic relationship between chlorophyll a concentrations and the growth areas of Trapa during summer in a shallow eutrophic lake

The relationship between concentrations of chlorophyll a in an open water area and growing areas of the macrophytes Trapa spp. and Nelumbo nucifera was investigated to clarify the role of macrophytes in phytoplankton growth in summer in a eutrophic shallow sand lake, Lake Honsagata, Japan. The chlorophyll a concentrations formed peaks in June 2007 and July 2008 in summer with cyanobacterial blooms composed of mainly Microcystis, Anabaena, Phormidium, and Oscillatoria, which decreased toward August and were maintained at different annual levels. The decline of blooms in August was caused by the rapid growth of macrophytes. The composition of phytoplankton and the level of bloom development in summertime differed characteristically from year to year. Also the total vegetation area of N. nucifera and Trapa spp. showed annually marked changes. A significant negative correlation between the concentrations of chlorophyll a and the growth areas of Trapa spp. in August was detected, indicating that the floating-leaved plants, Trapa spp., produced irregular, clear and turbid water states in this shallow eutrophicated lake. These antagonistic relations are explained based on a likely scenario of allelopathic effects on the development of cyanobacteria by Trapa spp. vegetation and the nutrient absorption competition among them. Our study demonstrated the potential of Trapa spp. to control cyanobacterial blooms producing harmful toxins.     

A Limnological Reconnaissance of the Lough Erne System,Ireland

The Lough Erne System (Northwest Ireland) consists of two linked eutrophic lakes. Phosphorus input budgets suggested mean catchment exports of 30–62 kg total P km⁻² a⁻¹, resulting in a heavy P loading to the small upper lake. The export of soluble P is related to the human population density in the catchment. Although complex in outline, the upper lake has similar phytoplankton populations throughout, but the populations in the simpler shaped lower lake differ quantitatively and qualitatively from place to place. This is probably due to differences in mixed depth. A chlorophyll a map of the surface water of the lower lake, obtained by fluorometry, showed the relationship between algal biomass and depth of water.     

Predicting the spring algal biomass in Lough Neagh using time series analysis

1. Lough Neagh is a large eutrophic lake covering 387 km² with a mean depth of 8.9 m. It is an important natural resource, being the largest single source of potable water for Belfast, Northern Ireland. 2. This report examines the causes of the year-to-year variation in the April–June (spring) algal biomass, measured as chlorophyll a, for the period 1974–92. 3. The spring chlorophyll a declined following the introduction of a phosphorus (P) reduction programme at major sewage treatment works in 1981. However, since 1990 the chlorophyll a concentrations in the spring have increased. 4. Time series methodology was employed to develop a model which explained 76% of the annual variation in spring chlorophyll a concentrations. 5. The independent variables used in the multiple regression model were the previous year’s spring chlorophyll a concentration, soluble reactive P inputs for April–June and the particulate P concentration in the Lough during the previous summer.     

Phosphorus concentrations into a subtropical lake strongly influence nitrogen accumulation,nitrogen export,and Chl a concentrations

We measured water quality monthly for 22 years in water entering, within, and exiting a 65 km² shallow polymictic and eutrophic freshwater lake in the northern Gulf of Mexico. Fertilizer use in the watershed is the dominate source of phosphorous (P) going into the lake and controls the lake’s P concentrations, but nitrogen (N) fertilizer use was not related to total nitrogen concentration in the lake. Half of the particulate P entering the lake is trapped within it and there is a net accumulation of N that appears to be from the stimulation of nitrogen fixation. The lake’s concentration of Chlorophyll a (µg Chl a l^?1) and increase in N in the lake was directly related to the concentration of P in water entering the lake. Variations in the Chl a concentration within a freshwater lake downstream are also directly related to the annual use of P fertilizer, but not to N fertilizer use. Reducing agriculture-sourced P runoff will lower (but not eliminate) both the frequency of algal blooms within Lac des Allemands and the amount of N delivered to the estuary.

     

Periphyton nutrient limitation and other potential growth-controlling factors in Lake Okeechobee,U.S.A.

Periphyton nutrient limitation was assessed in Lake Okeechobee, a large, shallow, eutrophic lake in the southeastern U.S.A. Nutrient assays were performed to determine if the same nutrients that limit phytoplankton also limit periphyton growth in the lake. Nutrient diffusing clay substrates containing agar spiked with nitrogen, phosphorus, or both, along with nutrient-free controls, were incubated at four sites in the lake. Three sites were located in a pelagic–littoral interface (ecotone) and one site was located in the interior littoral region. Incubations lasted for 20–26 days, and were repeated on a quarterly basis between 1996 and 1997, to incorporate seasonal variability into the experimental design. The physical and chemical conditions at each site also were measured. Periphyton biomass (chlorophyll a and ash-free dry mass) was highest at the littoral and northern ecotone sites. At the littoral site, nitrogen limited biomass in four of five incubations, although the largest biomass differences between the treatments and controls (3 g cm^–2 as chl) were probably not ecologically significant. Periphyton biomass at the western and southern ecotone sites was low compared to the other two sites. Increases in water column depth and associated declines in light penetration strongly correlated with periphyton growth and suggested that they may have limited growth most often at all three ecotone sites. Nitrogen also was found to limit periphyton growth approximately 20% of the time at the ecotone sites and phosphorus was found to limit growth once at the west site.     

Determining trophic state in Lake Whatcom,Washington (USA), a soft water lake exhibiting seasonal nitrogen limitation

We evaluated an eleven year data set to assess trophic state and nutrient limitation in Lake Whatcom, an oligotrophic, soft water, chain lake located in the Puget Sound lowlands of Washington (U.S.A.). Although total phosphorus (TP) and soluble reactive phosphate (SRP) concentrations were relatively low throughout the lake, there were significant differences between the northern basin (Site 1) and the other sampling sites (Sites 2–4). Nonparametric correlation coefficients (Kendall's ) were highest between chlorophyll (CHL), Secchi depth (SD), total nitrogen (TN), and dissolved inorganic nitrogen (DIN). Late summer algal biomass correlated best with DIN and TP. Trophic State Indices based on TP, TN, CHL and SD revealed that although algal growth was most likely phosphorus limited throughout the year, the northern basin of the lake may have developed nitrogen co-limitation during late summer and fall. During this period, N/P ratios were often less than 20, and in 1998 the epilimnetic DIN concentrations dropped below 20 g l^–1 while DIN/TP ratios fell below 4. Reviews of the literature suggest that while co-limitation by phosphorus and nitrogen is fairly common in unproductive lakes, the patterns seen in Lake Whatcom were more similar to those reported for eutrophic lakes experiencing secondary nitrogen limitation resulting from excess phosphorus loading.     

Algal growth on organic compounds as nitrogen sources

Two experimental series were run to evaluate the potential of algal development on dissolved organic nitrogen (DON) compounds as the sole source of nitrogen (N) nutrition. Monocultures of several common Lake Kinneret algae (Pediastrum duplex, Synechococcus sp., Microcystis aeruginosa, Aphanizomenon ovalisporum and Cyclotella sp.) were incubated for 3 weeks in the laboratory with different inorganic (NH4⁺, NO3^-) or organic (hypoxanthine, urea, guanine, ornithine, glucosamine, lysine) nitrogen sources. Even though the cultures were not axenic, marked differences were observed in algal growth response. Pediastrum, Cyclotella and Aphanizomenon grew well on most N sources, and cyanobacterial growth and yield were consistently greatest when the urea was the only N source. We also followed algal growth and eventual species dominance in batch samples of GF/F-filtered lake water, supplemented with orthophosphate and different inorganic or organic N compounds and inoculated with concentrated lake phytoplankton. Although no clear impact on phytoplankton growth (as chlorophyll concentration) was observed, in seven out of 11 experiments we could discern changes in the algal species that became dominant in flasks with different organic and inorganic N sources. Our results are consistent with the proposition that components of the DON pool are not only an important potential, direct or indirect N source for phytoplankton, but also that different algal species can exploit these sources with varying capabilities so that different N substrates may selectively stimulate the development of dominant algal species.