Lipolytic activity of marine bacteria. Influence of NaCl and MgCl2

A method for the determination of volatile fatty acids (VFA) in coastal marine sediments is presented. Acidified porewater was vacuum distilled to extract the VFA and the distillate was analysed by gas chromatography (Porapak QS column and flame ionization detection). The limit of detection was 2 M in the samples, but was increased tenfold by lyophilization. In the upper 10 cm of the sediments 2–70 nmol acetate cm^-3 sediment was found. Uniformly labelled ¹⁴C-acetate (0.02 nmol, 10^-3 ci) was injected at 1- to 2-cm intervals through silicone-stoppered holes in the tubing of undisturbed sediment cores. Turnover rate constants were determined from semilogrithmic plots of the ¹⁴C-acetate radioactivity versus the incubation time. The ¹⁴C-acetate was shown to be distributed in at least three sediment pools: a porewater pool, an adsorbed pool which was displaced by excess acetate, and an adsorbed pool which was not displaced by excess acetate. The rate constants ranged from 1.5–13 h^-1 in the investigated sediments. The turnover rates of acetate were calculated from the turnover rate constants and the acetate concentrations in the porewater. The rate of acetate turnover calculated from the NH ₄ ^* turnover and the N:C ratio of the sediment organic matter was only 16% of the measured rate of acetate turnover. The apparent overstimation of the acetate turnover was most likely due to an overestimation of the degradable acetate pool. A gel filtration of ¹⁴C-acetate-containing porewater showed that the fractions which contained the tracer had only 25% of the total acetate. This implied that a large fraction of the acetate in the porewater was unavailable to the microbes. This was also indicated by the fact that the measured acetate pool in porewater incubated with ¹⁴C-acetate did not decrease, when the added ¹⁴C-acetate was oxidized.     

Zooxanthellae providing assimilatory power for the incorporation of exogenous acetate in Heteroxenia fuscescens (Cnidaria: Alcyonaria)

The soft coral Heteroxenia fuscescens (Ehrb.) and its isolated zooxanthellae (endosymbiotic dinoflagellates) were investigated with particular regard to uptake and utilization of exogenously supplied ¹⁴C-acetate in the light and in the dark. The incorporation of ¹⁴C from ¹⁴C-acetate into the host tissue and into the zooxanthellae was consistently much higher in the light than in the dark. The incorporated ¹⁴C-acetate was rapidly metabolized by the host and algae and was recovered from different assimilate fractions. The major proportion of radiocarbon from metabolized ¹⁴C-acetate was located in host tissue. The CHCl₃-soluble fraction composed of diverse lipids showed the strongest ¹⁴C-labelling. Zooxanthellae isolated prior to incubation accounted for about 80% of the acetate incorporation recorded for zooxanthellae in situ (in vivo). It is concluded from a comparison of acetate incorporation and conversion under light and dark conditions that most of the lipid reserve of the host tissue originates from fatty acids, which are synthesized within the algal symbionts and are then translocated to the heterotrophic partner via extrusion. The acetate units needed for lipid synthesis are obtained by absorption of free acetate from dissolved organic matter (DOM) in the seawater as well as by photosynthetic assimilation of inorganic carbon. Thus, in H. fuscescens, lipogenesis is operated as a light-driven process to which the zooxanthellae considerably contribute assimilatory power by performing fatty acid synthesis and translocation of lipid compounds to their intracellular environment (host cell). A metabolic scheme is proposed to account for the different pathways of carbon conversion observed in H. fuscescens. The incubations took place in August 1980 and the analytical part from October 1980 to January 1984.     

Turnover of tracer (14C, 3H labelled) alanine in inshore marine sediments

The turnover rate constants (k) of alanine in coastal marine sediments were measured using ³H-and ¹⁴C-alanine in tracer amounts (less than in situ concentrations of alanine in the porewater). After incubation ¹⁴C-label was recovered in free dissolved alanine, adsorbed alanine, volatile fatty acids and carbon dioxide pools. Alanine left the free dissolved pool by two processes: 1) adsorption (k=0.06 min^-1) and 2) biological uptake (k=0.16 min^-1). Adsorption of alanine was deduced from the persistence of ¹⁴C-alanine, which was slowly metabolized after an initial rapid rate of degradation. Adsorption was confirmed in biologically inactivated sediments. The adsorbed ¹⁴C-alanine was only partially exchanged by the addition of excess non-labelled alanine, indicating the existence of at least 2 different adsorbed pools. The rates of adsorption and desorption were equal, but the k-values were different, indicating that the adsorbed pool was 2500 fold greater than the free pool. From the biological turnover rate constant (0.16 min^-1), the mineralization percentage (80%) and the concentration of alanine (800 nmol l^-1 of porewater) a mineralization rate in the sediment of 75 nmol cm^-3 d^-1 was determined. This was in excess of the measured total NH ₄ ⁺ production. It is concluded that much of the dissolved alanine (800 nm) was biologically unavailable and a more realistic free dissolved pool would be 10 nM.     

A reevaluation of the role of glycerol in carbon translocation in zooxanthellae-coelenterate symbiosis

Glycerol has been traditionally viewed as the main form of carbon translocated from zooxanthellae to the coelenterate host. Most of this glycerol was postulated to be used by the coelenterate host for lipid synthesis. Recent work suggests that large amounts of photosynthetically fixed carbon is synthesized into lipid in the algae, and then translocated as lipid droplets to the host. These two hypotheses of carbon translocation are not mutually exclusive, but to reconcile them the role of glycerol must be reevaluated. In this study the short term metabolic fate of uniformly labelled ¹⁴C-glycerol, ¹⁴C-bicarbonate, and ¹⁴C-acetate was examined in zooxanthellae and coelenterate host tissue isolated from Condylactis gigantea tentacles. When host and algal triglycerides, synthesized during 90-min light and dark incubations in ¹⁴C-bicarbonate and ¹⁴C-acetate, were deacylated, more than 80% of the activity was found in the fatty acid moiety. In contrast, triglycerides isolated from zooxanthellae and coelenterate host tissue incubated in ¹⁴C-glycerol in the dark for 90 min were found to have more than 95% of their radioactivity in the glycerol moiety. During the 90-min ¹⁴C-glycerol incubations in the light, the percentage of radioactivity in the fatty acid moiety of zooxanthellae triglycerides increased to 37%. The percentage of radioactivity in the host tissue triglycerides fatty acid moiety stayed below 5% during the 90-min ¹⁴C-glycerol incubations in the light. These results show that neither the zooxanthellae nor the host can rapidly convert glycerol to fatty acid. Radioactivity from ¹⁴C-glycerol, which does eventually appear in host lipid, may have been respired to ¹⁴CO₂, then photosynthetically fixed by the zooxanthellae and synthesized into lipid fatty acid.     

The size and function of the internal inorganic carbon pool of the foraminifer Amphistegina lobifera

The existence of an internal inorganic carbon pool in the perforate foraminifer Amphistegina lobifera, as suggested recently (ter Kuile and Erez 1987), has been established by direct measurements using a new ¹⁴C tracer method. The imperforate species Amphisorus hemprichii does not contain such a pool. The size of the pool in A. lobifera is proportional to its calcification rate and approximately equals the amount of carbon incorporated into the skeleton during 24 h. Time course experiments show that inorganic carbon (Ci) is photoassimilated at constant rates by the algal symbionts, that the pool is filled to maximum capacity in ca. 24 h, and that Ci incorporation into the skeleton starts only after the pool is filled up. During the chase phase of pulsechase experiments, all ¹⁴C initially residing in the pool is transferred to the skeleton, indicating that the pool serves for calcification and not for photosynthesis. Uptake of Ci into the pool occurs only in the light, indicating that energy may be required for this process. Furthermore, calculations of the Ci concentration inside the pool suggest that it is higher by 2 to 3 orders of magnitude compared to seawater concentration, suggesting that its accumulation is an energy dependent process.     

Nitrate metabolism in sediments from seagrass (Zostera capricorni) beds of Moreton Bay,Australia

The fate of nitrate in sediments from seagrass (Zostera capricorni Aschers.) beds of Moreton Bay on the subtropical eastern coast of Queensland, Australia, was investigated. Added nitrate was metabolised at rates of 0.4 to 3.4 g N cm^-3 d^-1 when sediments were incubated under anaerobic conditions with a large excess of nitrate. The potential rate of nitrate utilization was as rapid in sediments from subtidal bare areas as from adjacent seagrass beds. Ammonium was produced rapidly from¹⁵N-nitrate by microbial action in all the subtidal sediments examined. After 12 h of incubation, 13 to 28% of the¹⁵N initially added as labelled nitrate was detected as labelled ammonium in the sediments. Denitrification, although not measured directly, appeared to be a relatively minor fate of nitrate. Benthic microbes took up large amounts of¹⁵N but only after a delay of 6 h; this pattern could have been due to induction and synthesis of the enzymes necessary for nitrate uptake, and the assimilation of labelled ammonium. Under field conditions, assimilation by seagrasses and denitrification by bacteria were probably not significant sinks for nitrate in comparison with uptake by benthic microbes and dissimilatory reduction to ammonium.     

In vivo binding of a biologically active oligopeptide in vegetative buds of the scyphozoan Cassiopea andromeda: demonstration of receptor-mediated induction of metamorphosis

Vegetative buds of Cassiopea andromeda (Cnidaria, Scyphozoa) metamorphose into polyps in the presence of short synthetic peptides containing proline as the preterminal amino acid at the carboxyl terminus. In an in vivo assay, the binding of the biologically active hexapeptide ¹⁴C-dansyl-GPGGPA in buds was shown to be specific and saturable. Scatchard plot analysis of the specific binding data revealed a dissociation constant (K _D) of about 7 M. The total number of receptors was calculated to be approximately 1×10¹⁰ bud^-1 under saturation conditions. In correlation with the results of prior investigations, our finding of receptor-mediated induction of metamorphosis strongly supports the hypothesis that binding of biologically active peptides to receptors leads to initiation of phosphatidylinositol breakdown and activation of protein kinase C.     

Tertiary-butyl acetate metabolism,toxicity, and human health considerations

Tertiary-butyl acetate (TBAC) (CAS No. 540-88-5) is an organic solvent with a potential for occupational and environmental exposure as a result of its use in industrial coatings, adhesives, inks, and degreasers. The objective of these studies was to extend the toxicological database upon which health hazard and risk assessments of TBAC can be made. The metabolism of TBAC was studied in rats exposed by inhalation for 6?h to concentrations of 100 or 1000?ppm. There was an evidence of partial saturation of TBAC absorption and metabolism at some concentration below 1000?ppm. Approximately 5% of the low dose and 26% of the high dose was expired without change within 12?h, while the retained material was rapidly metabolised and excreted, mostly in the urine, within 24?h. Very little radioactivity remained in the tissues after day 7. The metabolism of TBAC appears to follow two major routes: hydroxylation of the tertiary-butyl moiety to form 2-hydroxymethylisopropyl acetate and ester hydrolysis to form tertiary-butyl alcohol (TBA). A minor route involves oxidation of the acetate moiety. Based on the proportion of metabolites that can clearly be assigned to one or the other major pathway, hydroxylation of the tertiary-butyl moiety prevails at 100?ppm, while hydrolysis of the ester bond predominates at 1000?ppm.

Based on nose-only inhalation exposure of rats to TBAC for 6?h, the LC50 for males and females combined is approximately 4200?ppm. Clinical signs included exaggerated breathing, staggering, tremors, and lethargy approximately 1?h after the exposure, but all surviving rats appeared normal from 24?h until the end of the 14?day observation period. An LC₅₀ was not identified for mice. After exposure of whole body for 6?h to 3000?ppm, the highest concentration tested, all mice were prostrate for most of the exposure time, but there were no deaths.

Groups of five male and five female Sprague-Dawley rats were exposed nose-only to 0, 100, 400, or 1600?ppm TBAC 6?h?day^?1 5 days?wk^?1 for 2?weeks. There were no effects on body weight, feed or water consumption, or necropsy findings. Male rats exposed to 1600?ppm had increased liver weights and hypertrophy of centrilobular hepatocytes. An increased proportion of cortical tubule cells with hyaline droplet accumulation was observed in all treated groups of males. Groups of five male and five female CD-1 mice were exposed whole body to 0, 190, 375, 750, or 1500?ppm TBAC 6?h?day^?1 for 14 consecutive days. There were no effects on body weight, feed consumption, or necropsy findings. Liver weights were increased in female mice at 750 and 1500?ppm. Minimal hypertrophy of centrilobular hepatocytes was found in female mice at 375, 750, and 1500?ppm and in male mice at 1500?ppm TBAC.

TBAC did not induce gene mutations in bacterial tests with strains of S. typhimurium and E. coli. Further, there was no evidence of clastogenic activity from tests either for the induction of chromosomal aberrations in human lymphocytes in vitro in the presence or absence of S9 mix or for the induction of micronuclei in bone marrow cells of rats exposed by inhalation for 6?h to 1600?ppm TBAC.

These results are relevant to human health risk assessment and are discussed in the context of previous studies. The weight of the scientific evidence supports the conclusion that TBAC has lower acute toxicity than previously suggested, that it is rapidly excreted when inhaled, and that neither TBAC nor its TBA metabolite are genotoxic or potential human carcinogens.     

Toxicity studies on the components of an oil-spill emulsifier using Lichina pygmaea and Xanthoria parietina

Previous work on lichens suggested that the toxic component of the oil-spill emulsifier BP 1002 might be the surfactant rather than the solvent, to which toxicity is usually attributed. The effect of the emulsifier on both Lichina pygmaea and Xanthoria parietina (measured by reduced total photosynthetic ¹⁴C-fixation and enhanced loss of labelled material from the lichen) was shown to be mainly due to Surfactant B (coconut fatty diethanolamide) altering the permeability of the algal cell membranes. Surfactant A (nonylphenol ethylene oxide condensate) was less inhibitory but, by comparison with the response of free-living algae to the emulsifier, induced both leakiness and lysis of the blue-green algal cells in L. pygmaea. Pure solvent slightly reduced total ¹⁴C-fixation without altering the pattern of ¹⁴C-fixation. Observations on pigment removal showed the solvent to be capable of removing only the extra-cellular pigment parietin; Surfactant B induced loss of lipid- and water-soluble intracellular pigments.     

Rates of ammonium turnover and the role of amino-acid deamination in seagrass (Zostera capricorni) beds of Moreton Bay,Australia

Samples of sediments from Australian seagrass (Zostera capricorni Aschers.) beds were taken in June to August 1983 (for¹⁵N experiments) and November 1982 to January 1983 (¹⁴N experiments). The ammonium pool turned-over every 0.4 to 0.8 d, as determined with a¹⁵N isotope-dilution technique. The ammonium pool in subtidal bare areas turned-over two to three times more slowly than in adjacent seagrass beds. Gross rates ofin situ ammonium regeneration equalled those of utilization, and ranged from 0.04 to 0.35 mol cm^-3 d^-1, or from 50 to 490 mg N m^-2 d^-1 over the upper 10 cm of the sediment. The potential rate of glycine utilization, measured with a large excess of glycine added to anaerobic incubations, ranged from 0.21 to 0.39mol cm^-3 d^-1, butin situ rates were probably much lower. Between 35 and 65% of added¹⁵N-glycine was deaminated over 12 h, and the remainder was most likely assimilated by microbes. Evidence for the seagrasses taking up glycine was equivocal, owing to the rapid deamination of the amino acid and the likelihood that they assimilated the labelled ammonium produced from the glycine.     

Uptake of inorganic carbon and internal carbon cycling in symbiont-bearing benthonic foraminifera

Incorporation rates of inorganic carbon and its distribution between the organic matter and the skeleton have been measured using ¹⁴C tracer techniques on two species of symbiont-bearing benthonic foraminifera in the Gulf of Elat: Amphistegina lobifera (a perforate species) and Amphisorus hemprichii (an imperforate species). Under constant experimental conditions, incorporation rates of the radiotracer become linear with time after several hours in A. hemprichii and after one day in A. lobifera. A. lobifera showed a lag time of 24 h for skeletal incorporation, whereas in A. hemprichii uptake into the skeleton started within 2 h. Pulse-chase incubations in radioactive seawater, followed by unlabelled incubations, demonstrate transfer of photosynthetically acquired ¹⁴C into the skeleton of A. lobifera. No such transfer was found in A. hemprichii. The total ¹⁴C uptake by A. lobifera increased during the first 24 h of cold chase incubation. This increase suggests the existence of an internal inorganic carbon pool that was lost (probably evaporated) during the analysis of pulse incubations. However, during the following chase incubations, the ¹⁴C in this pool was incorporated mainly into the skeleton and retained during analysis, causing the increase in the total uptake. No such increase was found in A. hemprichii. Additional ¹⁴C uptake experiments on other species of the genera Operculina, Heterostegina and Borelis suggest that the differences in pathways for incorporation of carbon between A. lobifera and A. hemprichii can be generalized to the perforate and imperforate foraminiferal groups. In perforate species, respired carbon originally taken up through photosynthesis is partly recycled into the skeleton. In imperforate species such a transfer has not been demonstrated. Perforate species seem to have a large internal inorganic carbon pool which serves mainly for calcification and possibly also for photosynthesis, while imperforate species may take up carbon for calcification directly from seawater or have a very small inorganic carbon pool.     

Absence of sterol synthesis in larvae of the mud crab Rhithropanopeus harrisii and of the spider crab Libinia emarginata

A dietary requirement for sterols in crustacean larvae was established by the use of isotopic tracer techniques. Larvae of the mud crab Rhithropanopeus harrisii and larvae of the spider crab Libinia emarginata were exposed to acetate-¹⁴C or mevalonate-¹⁴C. Radioanalysis of the fatty acids of each species indicated sufficient incorporation of acetate for lipid synthesis. No radioactivity was detected in the sterols of animals exposed to either acetate-¹⁴C or mevalonate-¹⁴C. It was concluded that R. harrisii and L. emarginata larvae are unable to synthesize sterols from acetate or mevalonate and, therefore, require them in their diet.     

An evaluation of two diffusion culture techniques for estimating phytoplankton growth rates In situ

In comparative tests, acrylic diffusion chambers (voltume=42 ml) with polycarbonate filter membranes (1 m pore diameter) consistently supported higher cell yields and faster growth rates of summer phytoplankton populations and species from Narragansett Bay than did dialysis bags (volume=50 ml, 0.24–0.48 nm pore diameter) or bottle cultures (with or without added nutrients). Stirring of diffusion chambers or dialysis bags had less effect on growth responses than did the choice of the containment membrane. Exchange measurements showed the polycarbonate filters (0.49 ml cm^-2 h^-1) to be five times more permeable than dialysis membranes (0.09 ml cm^-2 h^-1) per unit area. The mean of measured half-life times for water in diffusion chambers was less than one hour while comparable half-life times for dialysis bags were approximately 3 h. Diatoms from the <10 m size fraction had higher growth rates than assemblages of microflagellates and non-motile ultraplankton. Stirring of diffusion chambers did not adversly effect the growth of microflagellates or non-motile ultraplankton. Growth responses in diffusion chambers moored in situ were generally similar to those measured in diffusion chambers incubated in outdoor tanks connected to a running seawater system.     

Sediment ammonium availability and eelgrass (Zostera marina) growth

The interaction of sediment ammonium (NH ₄ ⁺ ) availability and eelgrass (Zostera marina L.) growth, biomass and photosynthesis was investigated using controlled environment and in-situ manipulations of pore water ammonium concentrations. Sediment diffusers were used to create pore water diffusion gradients to fertilize and deplete ammonium levels in sediments with intact eelgrass rhizospheres. Between October, 1982 and September, 1983 controlled environment experiments using plants from shallow (1.3 m) and deep (5.5 m) stations in a Great Harbor, Woods Hole, Massachusetts, USA eelgrass meadow along with in-situ experiments at these stations provided a range of sediment ammonium concentrations between 0.1 and 10 mM (adsorbed+interstitial NH ₄ ⁺ ). The results of the in-situ experiments indicate that nitrogen limitation of eelgrass growth does not occur in the Great Harbor eelgrass meadow. A comparison of NH ₄ ⁺ regeneration rates and eelgrass nitrogen requirements indicates an excess of nitrogen supply over demand and provides an explanation for the lack of response to the manipulations. Results of controlled environment experiments combined with in-situ results suggest that sediment ammonium pool concentrations above approximately 100 mol NH ₄ ⁺ per liter of sediment (interstitial only) saturate the growth response of Zostera marina.     

Ultrastructural and radiotracer studies of pore function in foraminifera

Clusters of mitochondria have been observed close to the inner end of the pores in Nonionella stella, Globobulimina pacifica, Buliminella tenuata, Bolivina argentea, Loxostomum pseudobeyrichi, Cassidulinoides cornuta and Bolivina cf. subexcavata, pointing to a pore function of oxygen-uptake. The relationship between mitochondria and pores is most distinct in Buliminella tenuata, Bolivina argentea and L. pseudobeyrichi collected from a deep-water, low-oxygen environment. Amphistegina lobifera Larsen, 1976 readily took up ¹⁴CO₂ through its pores, indicating a pore function related to the photosynthetic activities of its symbionts. ¹⁴C-labelled glucose did not pass through the pores in traceable amounts during a 2 h exposure time.     

Uptake,metabolism and discharge of polycyclic aromatic hydrocarbons by marine fish

The uptake, metabolism and discharge of two polycyclic aromatic hydrocarbons, ¹⁴C-naphthalene and ³H-3,4-benzopyrene, were studied in 3 species of marine fish (mudsucker or sand goby, Gillichthys mirabilis; sculpin, Oligocottus maculosus; sand dab, Citharichthys stigmaeus). The path of hydrocarbons through the fish included entrance through the gills, metabolism by the liver, transfer of hydrocarbons and their metabolites to the bile, and, finally, excretion. The gall bladder was a major storage site of labeled hydrocarbons and their metabolites. The major product of ²H-3,4-benzypyrene metabolism was tentatively identified as 7,8-dihydro-7,8-dihydroxybenzopyrene. The ¹⁴C-naphthalene was metabolized to 1,2-dihydro-1,2-dihydroxynaphthalene after 24 h exposure. The urine appeared to the major avenne for discharge of labeled hydrocarbon from the body. Our laboratory results indicated that certain polycyelic aromatic hydrocarbons were rapidly taken up from seawater by the above fish, but detoxification mechanisms existed for efficient removal of these compounds from their body tissues.     

Absorption of volatile fatty acids from ambient water by the lugwormArenicola marina

Absorption of volatile fatty acids (propionate, acetate, butyrate, and formiate) from the ambient water by the lugwormarenicola marina was demonstrated using¹⁴C-labelled compounds and by gas-liquid chromatography. Uptake was investigated in the presence of antibiotics. The rate of uptake was highest with propionate (v_max 0,58 mol g^-1 w wt · h, K_t 0.75 mol l^-1). Butyrate, acetate, and formiate were absorbed at lower rates in that order. Absorption of propionate, butyrate, and acetate showed saturation kinetics. In the presence of butyrate and acetate, propionate absorption was inhibited (maximum inhibition 78%). These results indicate that a carrier is involved in the absorption of propionate. Following absorption, the volatile fatty acids were rapidly metabolized. The largest proportion of label was incorporated into amino acids, with the pattern of distribution of radioactivity being specific for each volatile fatty acid.     

Regulation of the Si and C uptake and of the soluble free-silicon pool in a synchronised culture of<Emphasis Type="Italic"> Cylindrotheca fusiformis</Emphasis> (Bacillariophyceae): effects on the Si/C ratio

Silicon and carbon uptake rates were studied over a 24 h light/dark cycle in a synchronised culture of the marine diatom Cylindrotheca fusiformis (Reimann et Lewin) using ³²Si and ¹⁴C. The silicic acid uptake rate per cell (^cSi) varied between 1.2 and 20.0 fmol Si cell^–1 h^–1 and was closely correlated to the G2+M phase of the cell cycle. A linear and significant relationship was determined between the percentage of cells present in G2+M and ^cSi. Evolution of the soluble free-silicon pool was studied simultaneously. The concentration of the total soluble free pool of silicon (Q^PSi) varied from 1% to 7% of the total silicon content. A significant difference of 1.5 fmol Si cell^–1 between Q^PSi and the labelled free pool (Q^npSi) was measured, indicating the presence of an unlabelled fraction of the pool. The concentration of Q^npSi was around 1.0 fmol Si cell^–1 prior to cell division and did not change as a function of ^cSi, which indicated a feedback mechanism coupling uptake into the free pool and incorporation into the frustule. In parallel, ¹⁴C uptake variation (^cC) was measured during the division of the population. The value of ^cC varied between 0.44 and 0.78 pmol C cell^–1 h^–1 and appeared to be maximal when cells were in the G1 phase. This variation of ^cC marginally affected the total carbon content of the cells (Q^TC) in comparison with the light/dark cycle. The variations in the Si/C ratio, from 0.021 to 0.046, demonstrated the different control mechanisms of Si and C metabolisms during the course of the cell- and photocycle.Communicated by S.A. Poulet, Roscoff     

Development of sol–gel formulations for slow release of pheromones

A new type of dispenser for slow-release of sex pheromones and other semiochemicals was developed based on sol–gel polymers that can be useful for monitoring, mass trapping, and mating disruption in integrated pest management (IPM). Sol–gel matrices exhibit glass characteristics and allow control of the degree of cross-linking during the polymerization process in order to provide an optimal release rate for a particular pheromone. The advantages of sol–gel (silica) matrixes include keeping the added molecules chemically stable and enabling the sol–gel material to be applied in any desired thickness and pheromone quantity, and thereby readily modify release rates. In addition, sol–gels are primarily silica and water that are common in the environment and therefore safe for field dispensing. We developed a method for the entrapment of pheromones in sol–gel matrices that allowed release at an almost constant rate over many days in the field. For example, 2.5 mg (E)-5-decenyl acetate pheromone of peach twig borer, Anarsia lineatella, entrapped in various sol–gel formulations released 14–45 μg/day for up to 28 days. The codling moth (Cydia pomonella) pheromone in sol–gels was used in field tests to capture more codling moth males than unbaited control traps. We describe how the method may be modified to entrap other types of pheromones by making sol–gels with different pore sizes.     

Suitability of various chemically prepared activated carbons for the removal of copper(II) ions

Studies on the suitability of various chemically prepared activated carbons (CPACs) like straw carbon (SC), sawdust carbon (SDC), dates nut carbon (DNC) and commercial activated carbon (CAC) for the removal of copper(II) ions by adsorption from simulated wastewater have been carried out under batch mode at 30?±?1°C and the results are compared. The percentage removal of Cu(II) ions increased with a decrease in initial concentration, particle size and added electrolytes (ionic strength) and increased with an increase in contact time, dose of adsorbent and initial pH of the solution. The adsorption data were fitted with the Langmuir isotherm. The applicability of the first order kinetic equation viz. Lagergren equation was tested by correlation analysis. The adsorption process is concluded to be a spontaneous, first order reaction, occurring with increased randomness at the solid–liquid interface. Studies on the desorption of Cu²⁺-loaded activated carbons (ACs) were carried out with nitric acid (0.2–1?N). The possibility of reuse of the regenerated ACs in cycle (in cue-one after another) was tested. SC was found to be a suitable adsorbent alternative to CAC among CPACs for the removal of metal ions, in general, and Cu²⁺ ions, in particular.