Benithic-pelagic coupling of nutrient metabolism along an estuarine eutrophication gradient

The shallow, brackish (11–18% salinity) Roskilde Fjord represents a eutrophication gradient with annual averages of chlorophyll, ranging from 3 to 25 mg chl a m^–3. Nutrient loadings in 1985 were 11.3–62.4 g N m^–2 yr^–1 and 0.4–7.3 g P m^–2 yr^–1. A simple one-layer advection-diffusion model was used to calculate mass balances for 7 boxes in the fjord. Net loss rates varied from –32.2 to 17.9 g P m^–2 yr^–1 and from –3.3 to 66.8 g N m^–2, corresponding to 74% of the external P-loading and 88% of the external N-loading to the entire estuary.Gross sedimentation rates measured by sediment traps were between 7 and 52 g p m^–2 yr^–1 and 50 and 426 g N M^–2 yr^–1, respectively. Exchangeable sediment phosphorus varied in annual average between 2.0 and 4.8 g P m^–2 and exchangeable sediment nitrogen varied from 1.9 to 33.1 g N m–1. Amplitudes in the exchangeable pools followed sedimentation peaks with delays corresponding to settling rates of 0.3 m d^–1. Short term nutrient exchange experiments performed in the laboratory with simultaneous measurements of sediment oxygen uptake showed a release pattern following the oxygen uptake, the changes in the exchangeable pools and the sedimentation peaks.The close benthic-pelagic coupling also exists for the denitrification with maxima during spring of 5 to 20 mmol N m^–2 d–1. Denitrification during the nitrogen-limited summer period suggests dependence on nitrification. Comparisons with denitrification from other shallow estuaries indicate a maximum for denitrification in estuaries of about 250 µmol N m^–2 h^–2 achieved at loading rates of about 25–125 g N m^–2 yr^–1.     

Phosphorus in soil,water and sediment: an overview

The geochemistry, availability and abundance of different forms of phosphorus in soil, water and sediments are reviewed. The present knowledge of phosphorus pathways in ecosystems and their regulation is discussed.In a drainage basin, anthropogenic phosphorus is brought into the system mainly as fertilizers and detergents. Sewer systems and outwash processes transfer the phosphorus from the terrestrial environment to the aquatic part of the ecosystem where an accumulation occurs in the sediments of the watercourse.A great part of the phosphates in soil is sorbed to soil particles or incorporated into soil organic matter. The release and export of phosphorus from uncultivated soil is a function of the geology and soil composition, but also of the air temperature, precipitation and the hydrological condition, pH etc.The solubility of phosphates is controlled by either sorption-desorption or precipitation-dissolution reactions depending on the environment in the soil or sediments. In soil and sediments with large amounts of iron and aluminium hydrous oxides, sorption-desorption reactions are largely responsible for determining the level of orthophosphate in the solution at equilibrium.Algal availability of phosphorus associated with soil-derived materials present in aquatic systems deserves more research. In addition, processes responsible for transport of phosphorus from cropland to aquatic systems and chemical and microbial transformations of phosphorus in lakes and streams deserve more attention.     

Recruitment,mortality and growth of mangrove (<Emphasis Type="Italic">Rhizophora</Emphasis> sp.) seedlings in Ulugan Bay,Palawan, Philippines

Propagule dispersal, establishment and recruitment to the sapling stage are critical steps in the life cycle of mangroves. Specific (i.e., per capita) rates of recruitment and mortality, and the growth rates of Rhizophora seedlings in three mangrove stands in Ulugan Bay (Palawan, Philippines) were estimated between March 1999 and February 2001. Recruitment and mortality were variable in space and time, with mortality exceeding rates of recruitment at all sites. The specific rates of seedling recruitment and mortality were higher in Buenavista (0.66 year^–1 and –1.67 year^–1) than in Umalagan (0.05 year^–1 and –0.33 year^–1) and Oyster Bay (0.13 year^–1 and –0.24 year^–1). The annual rate of production of internodes by the main stem was similar at the three sites (5.4–5.5 internodes year^–1), but the annual rate of elongation of the main stem was higher in Buenavista (10.6 cm year^–1) than in Oyster Bay (7.6 cm year^–1) and Umalagan (5.6 cm year^–1).     

Modelling the recovery of hypertrophic L. Glumsø (Denmark)

Diversion of sewage from L. Glumsø reduced phosphorus loading from 6.0 g P.m^–2.yr^–1 to 1.6 g P.m^–2.yr^–1. Chlorophyll levels during summer were reduced from 6–800 mg Chl.m^–3 to about 200 mg Chl.m^–3 mainly by extended periods with phosphorus limitation. Internal phosphorus loading was significant in the first 2 years after nutrient reduction. Predictions of the recovery were made by both simple, empirical models and with complex, dynamic model versions. The actual responses of L. Glumsø were compared with both previously published predictions and predictions made with improved model versions. Objective functions of 0.18 and global correlation coefficients of 0.89 could be achieved.     

Influence of Deleterious Concentrations of Copper on the Growth of Chlorella pyrenoidosa

The effect of deleterious concentrations of ionic Cu on the growth of Chlorella pyrenoidosa has been studied. An earlier paper showed a distinct effect of the same concentrations on the photosynthesis of the alga. Several substances, e.g. Fe and citric acid counteract the effect of Cu. In media ordinarily used for growing unicellular algae the influence of Cu is relatively slight due to the extraordinarily large concentrations. of Fe. At a concentration of 6 μg/I Fe – near to that in nature –even one μg/I Cu significantly decreases the growth during the first 24 hours. Cu is adsorbed to the negative charges on micelles of Fe(OH)₃ created in the alkaline medium. Citric acid is readily assimilated by Chlorella and thus counteracts the influence of Cu for only relatively short period. Cell concentration is of decisive importance for the deleterious influence of Cu on growth. The effect of a certain Cu concentration stops at a certain concentration of of the algae regardless of whether the experiment is started at this cell concentration or this concentration is attained during the experiment. This is due to the binding of Cu by the organic matter of cell walls and slime envelopes. H⁺ ions compete with Cu both when combining with the organic matter in the cell walls and when occupying the active sites of the cell membranes. The latter explains the fact that the influence of Cu is only slight at pH 5 compared with that at pH 8. At a Cu-concentration where no growth of algae can take place, the algae are by no means killed. After being transferred to an ordinary medium the algae start to grow again. The influence of Cu depends on the division stage of the algae. If the initial steps of cell division have taken place, the cell continues to divide.     

Modelling the influence of bioturbation on the vertical distribution of sedimentary phosphorus in L. Esrom

A multilayer sediment-water exchange model was used to evaluate the importance of bioturbation in the profundal sediments of L. Esrom. The temporal variation of the vertical distribution of sedimentary phosphorus fractions was modelled with an objective function of 1.50. Deviations between measured and simulated values occurred in the spring, where the measured pool of sedimentary phosphorus sharply declined in the surface sediments. The application of a model for the activity ofChironomus anthracinus based on biomass, oxygen consumption and temperature improved the model in the spring period. The downwards transport of easy-degradable surface sediments reduced the average release of sedimentary phosphorus from 12 mg P · m⁻² · day⁻¹ to 11 mg P · M⁻² · day⁻¹. The introduction of a similar model for the other important burrowing species in L. Esrom,Potamothrix hammoniensis, lowered the objective function to 1.37 and increased the average release to 12.5 mg P · m⁻² · day⁻¹. The minor role of bioturbation in sediment processes is discussed.     

The Effect of Deleterious Concentrations of Copper on the Photosynthesis of Chlorella pyrenoidosa

If a single salt solution of CuSO₄ is used, Cu penetrates immediately iuto the plasma of Chlorella cells, reducing the rates of photosynthesis at both high and low illumination. If CuSO₄ is added to ordinary Österlind culture-medium (pH 8) it takes some hours before any influence of deleterious concentrations of Cu is observed and initially only at light saturation. The algae must have been illuminated during the whole period. Maximum influence of CuSO₄ is found duriug the first 24 hours of treatment. A significant deleterious influence of Cu concentrations as low as about 1 μg/l is found. The influence of Cu increases with decreasing concentrations of the alga. If a culture medium at pH 5 is used instead of the ordinary one at pH 8, copper concentrations ahout 10 times as high must he used be order to obtain the same deleterious effect. An increase of the cotncentration of K reduces the influence of Cu to some extent. These facts show that the effect of deleterious concentrations of Cu in halanced solutions is not due to a marked penelration of this ion into the plasma but to a binding to the cytoplasmic membrane whereby the celts i.a. become more or less unable to divide. The cells become saturated with assimilation products which have a depressant effect on the rate of photosynthesis. Other cations compete with Cu for the “active sites” on the membranes.