Observations on the Bionomics of the Freshwater Nematode Chromadorina bioculata

The biology and morphology of Chromadorina bioculata is presented. Tile nematode was abundant on the alga Cladophora of one lily pond, but absent from similar habitats in nearby ponds. The setae, caudal glands, high Iocomotory rates and positive photo response have been interpreted in relation to maintenance on, amongst and between algal filaments, suspended over large volumes of water.When placed in tap or distilled water, C. bioculata became inactive and died. The influence of pH buffers, tonicity, temperature and starvation on activity were investigated. C. bioculata survived longer in artificial sea water diluted 10 or 100 times with distilled water, or in NaCl isotonic with sea water diluted 100 or 1000 times, than in tap or distilled water. No evidence of wide osmotic toleration or osmoregulation was observed. Activity was influenced by temperature, with peak activities occurring at the seasonal normal temperature. These findings are discussed in terms of general hematology and habitat selection.     

Nitrate Inhibition of Legume Nodule Growth and Activity : II. Short Term Studies with High Nitrate Supply

Soybean plants (Glycine max [L.] Merr) were grown in sand culture with 2 millimolar nitrate for 37 days and then supplied with 15 millimolar nitrate for 7 days. Control plants received 2 millimolar nitrate and 13 millimolar chloride and, after the 7-day treatment period, all plants were supplied with nil nitrate. The temporary treatment with high nitrate inhibited nitrogenase (acetylene reduction) activity by 80% whether or not Rhizobium japonicum bacteroids had nitrate reductase (NR) activity. The pattern of nitrite accumulation in nodules formed by NR⁺ rhizobia was inversely related to the decrease and recovery of nitrogenase activity. However, nitrite concentration in nodules formed by NR⁻ rhizobia appeared to be too low to explain the inhibition of nitrogenase. Carbohydrate composition was similar in control nodules and nodules receiving 15 millimolar nitrate suggesting that the inhibition of nitrogenase by nitrate was not related to the availability of carbohydrate.

Nodules on plants treated with 15 millimolar nitrate contained higher concentrations of amino N and, especially, ureide N than control nodules and, after withdrawal of nitrate, reduced N content of treated and control nodules returned to similar levels. The accumulation of N₂ fixation products in nodules in response to high nitrate treatment was observed with three R. japonicum strains, two NR⁺ and one NR⁻. The high nitrate treatment did not affect the allantoate/allantoin ratio or the proportion of amino N or ureide N in bacteroids (4%) and cytosol (96%).

     

Effects of nitrogen dioxide and nitrate nutrition on growth and nitrate assimilation in bean leaves

The influence of nutrient nitrate level (0-20 millimolar) on the effects of NO₂ (0-0.5 parts per million) on growth, K, photosynthetic pigment, N contents, and the activities of enzymes of N assimilation was studied in bean (Phaseolus vulgaris L. cv Kinghorn Wax) leaves. Exposing 7-day old bean seedlings for 5 days continuously to 0.02 to 0.5 parts per million NO₂ increased plant height, fresh weight, chlorophyll, carotenoid, organic N and nitrate contents, and nitrate reductase and glutamate synthase activities in the leaves of seedlings supplied with no external N. At 20 millimolar nitrate, most of the parameters examined were inhibited except for organic N and nitrate contents and glutamate synthase activity which increased in most cases. Generally, with an increase in NO₂ concentration, the stimulatory effect declined and/or the inhibitory effect increased. A 3-hour exposure of 12-day-old bean seedlings to 0.1 to 2.0 parts per million NO₂ increased nitrate content and nitrate reductase activity at each nutrient nitrate level except for a slight inhibition of enzyme activity during exposure to 2.0 parts per million NO₂ at 20 millimolar nitrate. The experiments demonstrated that the effect of NO₂ is strongly influenced by nutrient N level and that NO₂ is assimilated into organic nitrogenous compounds to serve as a source of N, only to a limited extent.     

Studies in the bivalve, Tellina tenuis Da Costa. IV. Further experiments in enriched sea water

Tellina tennis Da Costa was kept for four months in four large outdoor tanks containing sand and sea water. There was a 10 % daily exchange of sea water, pumped directly from the sea. Three tanks received daily addition of nutrients in the form of sodium nitrate and sodium dihydrogen phosphate, giving enrichment of approximately 3, 10, and 30 times natural sea-water levels of nitrate in the different tanks. Phosphate, nitrate, chlorophyll, and organic carbon in the water were measured regularly, the nitrate by Autoanalyser. Water temperature and solar radiation were recorded. Zooplankton samples were taken daily and Tellina were sampled monthly for length, weight, and biochemical analysis of tissues.Phosphate was always present in excess. The lowest level of nitrogen enrichment resulted in almost complete utilisation of nitrate, with a significant increase of organic carbon and chlorophyll above control levels. Zooplankton occurred in the greatest numbers in this tank, and Tellina showed the best survival, growth, and condition. In the tanks with the higher levels of enrichment, excess nutrients led to growth of macrophytic algae on the surface and sides of tank. This had an adverse effect on the phytoplankton production: zooplankton numbers were lower, as was growth of Tellina.     

Food sources for three species of Nihonotrypaea (Decapoda: Thalassinidea: Callianassidae) from western Kyushu, Japan, as determined by carbon and nitrogen stable isotope analysis

Three species of the callianassid genus Nihonotrypaea occur intertidally in the Ariake Sound estuarine system, southern Japan; they consist of two sandflat species (N. japonica; N. harmandi) and one boulder-beach species (N. petalura). Nihonotrypaea harmandi and N. petalura are distributed along the coastline in the relatively oligotrophic sea area extending from the outermost part of the sound to the open sea, while N. japonica occurs in the more eutrophic area situated at the middle part of the sound. The trophic conditions of the two areas affect the abundance of phytoplankton in the water column relative to that of benthic microalgae in the sediment. The carbon and nitrogen stable isotope compositions of N. japonica and its potential food sources have been analysed in an earlier study, specifying phytoplankton as the exclusive food source. Potential food sources for N. harmandi and N. petalura were analysed to make interspecific comparisons of the assimilated diets in relation to the shrimp habitat characteristics. Food sources of the shrimps were assessed based on the diet-tissue isotopic fractionation of N. harmandi and N. japonica (δ¹³C = 2.0‰, δ¹⁵N = 4.0‰), which had been determined by an earlier laboratory feeding experiment. Of several potential food sources for N. harmandi and N. petalura, riverine organic matter, sewage effluents, live/detrital terrestrial plants, and seagrass were not food sources. For N. petalura, live seaweed, in particular Sargassum spp., growing on boulders and cobbles during the seaweed high-growth season, and seaweed-derived detritus buried in the sediment and live Enteromorpha compressa during the seaweed low-growth season were the most likely food sources. For N. harmandi, phytoplankton (or fresh phytoplankton-derived detritus) and benthic microalgae constituted the most likely food sources. The δ¹³C value of the estimated diet for N. harmandi was higher than that for N. japonica by 0.6‰, while the δ¹⁵N value for N. harmandi was lower by 2.6‰. The food sources for the three species of Nihonotrypaea were species-specific, depending on each habitat characteristics.     

Ecological responses and remediation ability of water fern (Azolla japonica) to water pollution

The ability of the water fern Azolla japonica to remediate phosphorus (P), nitrogen (N), and iron (Fe) contamination, and its physiological responses to three common sources of water pollution (landfill leachate, swine lagoon sewage, and fish farm sewage) and standard solution were investigated. The biomass, water content, and chlorophyll content of Azolla japonica in each solution were measured, and the concentrations and accumulation rates of polluting elements in the solutions were determined. A. japonica showed over eight-fold increase in biomass within only 20 d in every solution except in swine lagoon sewage, extremely high in N concentration. Consistent chlorophyll and water contents of the plant in most solutions showed that A. japonica can adapt to highly concentrated solutions. N, P, and Fe concentrations of the solutions decreased significantly within the 20 d. In most treatments, A. japonica showed high N accumulation and also showed total uptake of P and Fe from the solutions. In reference to this result, using this species as a phytoremediator plant would have additional benefits of helping maintaining endangered populations of A. japonica. Therefore, the plant??s fast growth, good element remediation efficiency, and conservation needs makes A. japonica a suitable plant species for pollution remediation.     

Effect of nitrate on the organic Acid and amino Acid composition of legume nodules

Nitrate supplied to legume plants inhibits the activity of nitrogenase in Rhizobium bacteroids in root nodules. The accumulation of amino N which is known to occur in Glycine max (L.) Merr. nodules as nitrogenase activity declines was studied in more detail by analysis of changes in free amino acid composition in response to high nitrate supply. A 6-fold increase in asparagine concentration in Bradyrhizobium japonicum bacteroids was found about the time of maximum nitrogenase inhibition. However, the accumulation of amino acids in soybean nodules lagged behind the inhibition of nitrogenase. Furthermore, in studies of a second legume, Phaseolus vulgaris (L.) inoculated with two different strains of Rhizobium phaseoli, a high nitrate treatment inhibited nitrogenase but had no significant effect on amino acid composition of nodules. The possibility that nitrate may interfere with the supply of carbon substrates to bacteroids was examined by the analysis of organic acids in legume nodules supplied with nitrate. Nitrate had a small (10-20%) negative effect on the concentration of tricarboxylic acid cycle acids in P. vulgaris nodules. However, in G. max nodules, high nitrate treatment resulted in significant increases in the concentration of malate, succinate, fumarate, and citrate. Thus, carbon deprivation of bacteroids also seems unlikely as a cause of the inhibition of nitrogenase by nitrate. There was a transient increase in ammonium concentration in P. vulgaris nodules in response to high nitrate treatment. This effect was rapid relative to other effects of nitrate on nodule composition and was roughly coincident with the rapid decline in acetylene reduction activity.     

The effect of nitrate in stream water on the relationship between gentrification and nitrification in a stream-sediment microcosm

SUMMARY 1. Microcosm experiments were carried out to simulate, in the laboratory, the conditions occurring at the water-sediment interface of a stream draining agricultural land. Constant boundary conditions were attained by passing synthetic 'stream water', saturated with dissolved oxygen and containing 1 mmol NO₃?N dm^?3 (or 1 mmol Cl? dm^?3, control), once only over the sediment surface. 2. Measurements were made of inorganic-N (nitrate, nitrite, ammonium), redox potential, potential denitrification and nitrification activities, and readily mineralizable carbon sediment profiles at three incubation times up to 24 days. The peaks in denitrification and nitrification activity moved down the profile with time in the nitrate-treated sediment, but stayed relatively stationary in the control treatment. Although the zone of nitrification was restricted to the top 2–3 mm of sediment in the control treatment, high fluxes of both dissolved oxygen and NH₄?N maintained a high nitrifier activity within this zone for the duration of the experiment. 3. Increases in denitrifier activity immediately below the nitrifier activity peak indicated that a coupled nitrification-denitrification sequence was operating in both the control and nitrate-treated sediment. The greater depth of nitrification when nitrate was present in the ‘stream water’ was attributed to a feedback mechanism in which enhanced denitrification in the sediment reduced the local demand for oxygen and permitted dissolved oxygen to diffuse further into the sediment. The progressively greater depth to which oxygen penetrated caused the contiguous peaks of potential nitrifier and denitrifier enzyme activity to migrate farther from the interface. However, diffusion rates of the reactants limited the depth to which these coupled reactions could extend. 4. The possible effect of this feedback mechanism on the nitrate status of natural sediment-stream water systems is briefly discussed.     

THE ACCUMULATION OF ELECTROLYTES : XII. ACCUMULATION OF HALIDE AND NITRATE BY VALONIA IN HYPERTONIC SOLUTIONS

When cells of Valonia macrophysa were placed in hypertonic sea water, the concentration of halide and of nitrate increased, and the sum of halide + nitrate became 0.05 M greater inside than outside, which is about the same difference as is found in cells in normal sea water. In ordinary sea water the ratio of halide to nitrate is 80,000 to 1. When this was changed by substituting nitrate for halide so that the concentration of halide was 1.75 times that of nitrate the rate of entrance of halide was 1.68 times that of nitrate in 276 hours and the ratio of halide to nitrate in the sap decreased from 38 to 18.5. No halide came out in exchange for entering nitrate. The retention of chloride may well be due to the fact that even when the halide concentration of the sea water is reduced as low as 0.4 M, there is still an inwardly directed activity gradient of sodium chloride.     

5-bromodeoxyuridine induction of hematopoietic neoplasia and retrovirus activation in the soft-shell clam, Mya arenaria

Hematopoietic neoplasia and virus replication were induced in shoft-shell clams, Mya arenaria, by 5-bromodeoxyuridine (5-BrdUrd). Eighty clams were found to be nonneoplastic by the in vivo bleeding method. These clams were randomly distributed into four aquaria and maintained in seawater at 1°C. 5-BrdUrd was added to aquaria in the following concentrations: 0, 20, 100, and 200 μg/ml. After 4 days of treatment, the aquaria were drained, rinsed, and fresh sea water without 5-BrdUrd was added. Sea water was changed on a weekly basis thereafter. The clams were diagnosed for neoplasia by the in vivo method at days 4, 9, 16, and 23 of the experiment. Results showed that on day 23, neoplasia was not found in the aquarium without 5-BrdUrd, but in the aquaria containing 20, 100, and 200 μg/ml of 5-BrdUrd the incidences of neoplasia were 37, 79, and 35%, respectively. 5-BrdUrd-induced neoplastic tissue was homogenized and subjected to differential ultracentrifugation. Retrovirus-like particles resembling ones previously shown to induce neoplasia were isolated from neoplastic clams which were induced by 5-BrdUrd. When these particles were inoculated into healthy clams, the clams developed neoplasia. Neoplastic hemocytes, cultured in sea water containing 50 μg/ml of 5-BrdUrd, formed pseudopodia after 4 days. Pseudopod formation is a trait of normal hemocytes. This indicates that differentiation of neoplastic hemocytes may be induced by the drug.     

Nitrogen form, availability, and mycorrhizal colonization affect biomass and nitrogen isotope patterns in Pinus sylvestris

Nitrogen (N) isotope patterns are useful for understanding carbon and nitrogen dynamics in mycorrhizal systems but questions remain about how different N forms, fungal symbionts, and N availabilities influence δ¹⁵N signatures. Here, we studied how biomass allocation and δ¹⁵N patterns in Pinus sylvestris L. cultures were affected by nitrogen supply rate (3% per day or 4% per day relative to the nitrogen already present), nitrogen form (ammonium versus nitrate), and mycorrhizal colonization by fungi with a greater (Laccaria laccata) or lesser (Suillus bovinus) ability to assimilate nitrate. Mycorrhizal (fungal) biomass was greater with ammonium than with nitrate nutrition for Suillus cultures but similar for Laccaria cultures. Total biomass was less with nitrate nutrition than with ammonium nutrition for nonmycorrhizal cultures and was less in mycorrhizal cultures than in nonmycorrhizal cultures. The sequestration of available N by mycorrhizal fungi limited plant N supply. This limitation and the higher energetic cost of nitrate reduction than ammonium assimilation appeared to control plant biomass accumulation. Colonization decreased foliar δ¹⁵N by 0.5 to 2.2‰ (nitrate) or 1.7 to 3.5‰ (ammonium) and increased root tip δ¹⁵N by 0 to 1‰ (nitrate) or 0.6 to 2.3‰ (ammonium). Root tip δ¹⁵N and fungal biomass on root tips were positively correlated in ammonium treatments (r ²?=?0.52) but not in nitrate treatments (r ²?=?0.00). Fungal biomass on root tips was enriched in ¹⁵N an estimated 6–8‰ relative to plant biomass in ammonium treatments. At high nitrate availability, Suillus colonization did not reduce plant δ¹⁵N. We conclude that: (1) transfer of ¹⁵N-depleted N from mycorrhizal fungi to plants produces low plant δ¹⁵N signatures and high root tip and fungal δ¹⁵N signatures; (2) limited nitrate reduction in fungi restricted transfer of ¹⁵N-depleted N to plants when nitrate is supplied and may account for many field observations of high plant δ¹⁵N under such conditions; (3) plants could transfer assimilated nitrogen to fungi at high nitrate supply but such transfer was without ¹⁵N fractionation. These factors probably control plant δ¹⁵N patterns across N availability gradients and were here incorporated into analytical equations for interpreting nitrogen isotope patterns in mycorrhizal fungi and plants.     

The action of <Emphasis Type="Italic">Laminaria japonica</Emphasis> extractives on 1,3-β-D-glucanase,a digestive enzyme of the <Emphasis Type="Italic">Strongylocentrotus intermedius</Emphasis> sea urchin

Nutritional attractiveness of the brown alga Laminaria japonica for the sea urchin Strongylocentrotus intermedius was studied. The composition of L. japonica was analyzed after one and two years of its life under natural conditions, in its seedlings, and in the alga partially degraded by natural factors. Substances extracted with various solvents were tested for the presence of inhibitors and activators of 1,3-β-D-glucanase, a digestive enzyme of the sea urchin. Ethanolic extract of freshly harvested L. japonica was found to suppress the enzyme activity. Substances present in ethanolic extracts of the alga after one or two years of its life cycle and in the alga, partly degraded by natural factors, activated the sea urchin enzyme. This fact is in agreement with earlier natural observations concerning the nutritional attractiveness of such L. japonica samples for Strongylocentrotus intermedius.     

THE CONCENTRATION EFFECT WITH VALONIA: POTENTIAL DIFFERENCES WITH DILUTED POTASSIUM-RICH SEA WATERS

The concentration effect with sea waters containing more than the normal amount of potassium has been studied in Valonia macrophysa. This was done by comparing the initial changes in P.D. across the protoplasm when natural sea water bathing the cell was replaced by various isotonic dilutions of KCl-rich sea waters. With small dilutions of KCl-rich sea waters, the P.D.-time curves are of the same form as with the undiluted solution, exhibiting the fluctuations characteristic of KCl-rich solutions. This indicates that with these solutions K⁺ enters Valonia protoplasm and plays an important part in the P.D. The value of the initial rise in P.D. decreases with increasing dilution. With high dilutions of KCl-rich sea waters, the P.D.-time curves are of quite different shape, resembling the curves with diluted natural sea water; the P.D. is practically independent of small changes in the concentration of potassium, and increases with increasing dilution. That is, with these higher dilutions, the sign of the concentration effect is reversed, becoming the same as with diluted natural sea water. The greater the concentration of KCl in the undiluted sea water, the higher is the critical dilution at which K⁺ ceases to influence the P.D. For a wide range of sea waters containing both KCl and NaCl, it is shown that the concentration effect above the critical dilution is determined solely by the activity of NaCl in the external solution. It is concluded that with dilute natural sea water and with high dilutions of KCl-rich sea waters we have to do with a diffusion potential, involving only the Na⁺ and Cl^- ions, which are diffusing out from the vacuole. A quantitative relation between the composition of the sea water and the critical dilution has been deduced from the classical theory of the diffusion of electrolytes. It is shown that with dilutions less than this critical value the diffusion of K⁺ in the outer non-aqueous layer of the protoplasm is directed inward; hence K⁺ enters the protoplasm from these solutions. With dilutions greater than the critical value, the diffusion of K⁺ in this layer is directed outward; hence K⁺ does not enter the protoplasm. Since the P.D. shows no evidence of this outward diffusion of K⁺, it is concluded that the amount of K⁺ ordinarily present in the protoplasm is too small to produce any lasting electrical effect, and that the outward diffusion of K⁺ from the vacuole is prevented by the mechanism responsible for the accumulation of KCl in the cell sap.     

Slipping through the Cracks: The Taxonomic Impediment Conceals the Origin and Dispersal of Haminoea japonica,an Invasive Species with Impacts to Human Health

Haminoea japonica is a species of opisthobranch sea slug native to Japan and Korea. Non-native populations have spread unnoticed for decades due to difficulties in the taxonomy of Haminoea species. Haminoea japonica is associated with a schistosome parasite in San Francisco Bay, thus further spread could have consequence to human health and economies. Anecdotal evidence suggests that H. japonica has displaced native species of Haminoea in North America and Europe, becoming locally dominant in estuaries and coastal lagoons. In this paper we study the population genetics of native and non-native populations of H. japonica based on mt-DNA data including newly discovered populations in Italy and France. The conclusions of this study further corroborate a Northeastern Japan origin for the non-native populations and suggest possible independent introductions into North America and Europe. Additionally, the data obtained revealed possible secondary introductions within Japan. Although non-native populations have experienced severe genetic bottlenecks they have colonized different regions with a broad range of water temperatures and other environmental conditions. The environmental tolerance of this species, along with its ability to become dominant in invaded areas and its association with a schistosome parasite, suggest H. japonica could be a dangerous invasive species.     

The small-scale pattern of seepage water nitrate concentration in an N saturated spruce forest is regulated by net N mineralization in the organic layer

Soil net nitrogen (N) mineralization and nitrification as well as gross nitrification rates were studied in a forest soil within a 30?×?18m homogeneous plot located in an N saturated mature spruce stand at the Höglwald Forest (Bavaria, Germany) in order to explain the small-scale variation in nitrate (NO₃ ^?) concentration in seepage water. Seepage water was sampled below the main rooting zone in 40cm depth with suction cups over two periods at 20 measuring spots respectively. The sampling spots were uniformly distributed over the plot for both sampling periods, and represented the whole concentration range of seepage water NO₃ ^?concentrations measured within a close mesh of 121 suction cups. At each measuring spot soil net N mineralization, gross and net nitrification, heterotrophic soil respiration, extractable soil ammonium (NH₄ ⁺) and NO₃ ^?, and additional physical and chemical soil parameters were measured in the organic layer and correlated with the NO₃ ^? concentrations in seepage water. Furthermore, the effects of environmental parameters on N conversion processes were evaluated using multiple linear regression analysis. We found that the small-scaled variations in seepage water NO₃ ^? concentration were related to similar small-scaled variations in key processes of microbial N turnover rates in the organic layer. Within this study net N mineralization in the organic layer could explain 51–59% of the corresponding small-scale variation of nitrate concentrations in seepage water below the main rooting zone using a multiple linear regression model with stepwise procedure. In addition, we found that small-scale patterns of N turnover in the organic layer were strongly influenced by water content in the organic layer and the dry mass of organic matter.     

Stable oxygen isotope records of corals and a sclerosponge in the Western Pacific warm pool

High-resolution measurements of the stable oxygen isotopic signature (δ¹⁸O) of two new 10-year Porites lobata coral cores and one previously studied multi-decadal sclerosponge Acanthocheatetes wellsi from the Republic of Palau (7°16′N, 134°31′E) located in the Western Pacific warm pool were analyzed and monthly interpolated time-series records developed. Despite significant differences in collection depth and growth rates, both coral and sclerosponge faithfully recorded the interannual changes of sea surface salinity (SSS) driven by the strong influence of the El Niño Southern Oscillation (ENSO). The strong relationship of coral skeletal δ¹⁸O with SSS, but not sea surface temperature or precipitation, confirms previous findings that changes in Palau regional surface water are driven by the advection of water masses into the area over interannual timescales associated with ENSO. Opportunities exist for the expansion of short coral proxy records with longer sclerosponge records to verify the stability of ENSO-induced SSS variability over longer timescales.     

Seasonal production of primmorphs from the marine sponge Petrosia ficiformis (Poiret, 1789) and new culturing approaches

The need to produce bioactive compounds from marine sponges leads several groups of research to the culture of primmorphs from different species, which are generally maintained in aquaria for long time before processing. Here we present a study where the importance of several parameters on primmorphs production from the symbiotic sponge Petrosia ficiformis has been evaluated: (i) the sterility of sea water, (ii) the maintenance in aquarium before processing, (iii) the seasonal cycle. Sterility of sea water does not improve primmorphs production in this species. The maintenance of sponges in aquaria before processing negatively affects cell cultures. Regarding seasonality, it is evident that both the number and the size of primmorphs can deeply change depending on the period of the year the sponge is collected. April and July are the months that lead to the highest number of primmorphs, May and June are the months that lead to their biggest sizes. Possible relationships of these results with the life cycle of P. ficiformis are discussed.     

The functional group approach to bioturbation: II. The effects of the Macoma balthica community on fluxes of nutrients and dissolved organic carbon across the sediment-water interface

We have examined the effects of individual members of the two dominant functional groups of the Macoma balthica community on fluxes of nutrients and dissolved organic carbon between sediment and overlying water. The biodiffusers M. balthica and Mya arenaria and the gallery-diffuser Nereis virens were added to microcosms containing sieved tidal flat sediment, using identical biovolume for each treatment to facilitate comparison. Both functional groups enhanced fluxes over a control without macrofauna. The gallery-diffuser had the greatest effect. The two biodiffusers had opposite effects on the flux of nitrate. M. balthica, which lives near the sediment surface, caused nitrate release whereas M. arenaria caused nitrate uptake. Both organisms increased the release of ammonia, but M. arenaria had the greater effect. We attribute this intra-functional difference not so much to different functionality as to interactions between organisms and the depth distribution of pore water constituents. Because the burrow of M. balthica is located within the nitrification zone of the sediment, the depth averaged concentration of nitrate in its burrow is higher than in the overlying water, and burrow flushing leads to net release of nitrate. In contrast, the burrow of M. arenaria includes both nitrification and denitrification zones, which lower the depth averaged concentration of nitrate below the concentration in the overlying water. The functional group approach needs to take the processes that control sediment chemistry into account in order to predict fluxes sucessfully.     

Effects of light intensity and nutrients on gametophytes and gametogenesis of Lessonia nigrescens Bory (Phaeophyta)

Meiospores of Lessonia nigrescens Bory collected in Central Chile, were cultivated under different light and nutrient conditions to test for their influence on the development of gametophytes and gametogenesis. The microscopic stages of the life cycle are described. Under 45 μE·m^?2 ·s^?1 (12 h daily) and sea water enriched with nitrate and phosphate, development of few-celled gametophytes, gametogenesis and sporophyte differentiation occur within 35 days. At 10 μE ·m^?2 · s^?1, most gametophytes are multicellular and remain vegetative up to 65 days. Only enriched sea water or enriched sea water with double concentrations of phosphate lead to fertile few-celled gametophytes under 45 μE · m^?2 · s^?1. The addition of double concentrations of nitrate allows for the development of few-celled gametophytes but inhibits gametogenesis. The average gametophyte size progressively decreases when increasing amounts of nitrate and phosphate are added to the media.