Dominance of ‘Gallionella capsiferriformans’ and heavy metal association with Gallionella‐like stalks in metal‐rich pH 6 mine water discharge

Heavy metal‐contaminated, pH 6 mine water discharge created new streams and iron‐rich terraces at a creek bank in a former uranium‐mining area near Ronneburg, Germany. The transition from microoxic groundwater with ~5 mm Fe(II) to oxic surface water may provide a suitable habitat for microaerobic iron‐oxidizing bacteria (FeOB). In this study, we investigated the potential contribution of these FeOB to iron oxidation and metal retention in this high‐metal environment. We (i) identified and quantified FeOB in water and sediment at the outflow, terraces, and creek, (ii) studied the composition of biogenic iron oxides (Gallionella‐like twisted stalks) with scanning and transmission electron microscopy (SEM, TEM) as well as confocal laser scanning microscopy (CLSM), and (iii) examined the metal distribution in sediments. Using quantitative PCR, a very high abundance of FeOB was demonstrated at all sites over a 6‐month study period. Gallionella spp. clearly dominated the communities, accounting for up to 88% of Bacteria, with a minor contribution of other FeOB such as Sideroxydans spp. and ‘Ferrovum myxofaciens’. Classical 16S rRNA gene cloning showed that 96% of the Gallionella‐related sequences had ≥97% identity to the putatively metal‐tolerant ‘Gallionella capsiferriformans ES‐2’, in addition to known stalk formers such as Gallionella ferruginea and Gallionellaceae strain R‐1. Twisted stalks from glass slides incubated in water and sediment were composed of the Fe(III) oxyhydroxide ferrihydrite, as well as polysaccharides. SEM and scanning TEM‐energy‐dispersive X‐ray spectroscopy revealed that stalk material contained Cu and Sn, demonstrating the association of heavy metals with biogenic iron oxides and the potential for metal retention by these stalks. Sequential extraction of sediments suggested that Cu (52–61% of total sediment Cu) and other heavy metals were primarily bound to the iron oxide fractions. These results show the importance of ‘G. capsiferriformans’ and biogenic iron oxides in slightly acidic but highly metal‐contaminated freshwater environments.     

Regulation of Fe3+-oxide Formation Among Fe2+-oxidizing Bacteria

Helical stalks (resembling Gallionella ferruginea, Mariprofundus ferrooxydans) and filamentous sheaths (resembling Leptothrix ochracea) of Fe²⁺-oxidizing bacteria (FeOB) are mineralized by hydrous ferric oxides (HFO). To perform both inter-species and inter-site size comparisons of HFO particles on stalks and sheaths we measured HFO particles in samples of natural bacteriogenic iron oxides (BIOS) from 3 contrasting field sites: the Loihi Seamount (southern Hawaii); Äspö Hard Rock Laboratory (eastern Sweden); and Chalk River Laboratories (northern Canada) representing seafloor saline, underground brackish, and surface freshwater aqueous conditions. Ambient temperatures were in the psychrophilic range and pHs measured for Loihi, CRL, and Äspö were 5.6, 6.9 and 7.4, respectively. Dissolved Fe was lowest for CRL (0.2 mg · L^?1) followed by Äspö (1.5 mg · L^?1), then Loihi (4.5–14.9 mg · L^?1). L. ochraceasheaths appear to have surface properties that restrict HFO particle growth in comparison to G.ferruginea-M.ferrooxydans stalks in the same environment, which we attribute to interfacial surface energy (γ). An inverse relationship between particle size and stalk/sheath length due to restrictions in reactive surface area was also observed, which may provide insight into FeOB survival strategies to alleviate oxidative stress arising from Fe³⁺ production.     

The ultrastructure of chemolithoautotrophic Gallionella ferruginea and Thiobacillus ferrooxidans as revealed by chemical fixation and freeze-etching

By using sodium thioglycolate to dissolve the high amount of excreted stalk material in axenic cultures of the chemolithoautotrophic iron bacterium Gallionella ferruginea, the ultrastructure of Gallionella cells from pure cell suspensions could be studied without any loss of viability or disturbance by dense ferric stalk fibers, and compared with Thiobacillus ferrooxidans, also grown chemolithoautotrophically with ferrous iron as energy source. Both organisms were chemically fixed or freeze-etched. Particular structural differences between these iron-bacteria could be ascertained. G. ferruginea possesses intracytoplasmic membranes and soluble d-ribulose-1,5-bisphosphate-carboxylase, whereas T. ferrooxidans contains carboxysomes but no intracytoplasmic membranes; Gallionella forms poly--hydroxybutyrate and glycogen as storage material; T. ferrooxidans produces only glycogen. Both organisms also differ from each other with respect to the freeze fracture behaviour of the cell envelope layers. Whereas the cells of T. ferrooxidans exhibit a characteristic double cleavage, exposing the plasmic fracture face and exoplasmic fracture face of the outer membrane and cytoplasmic membrane, the exceptionally thin multilayered cell envelope of G. ferruginea revealed a particularly intimate association between the layers, resulting in a visualisation of the supramolecular organisation of only the inner fracture face of the cytoplasmic membrane. The results are discussed predominantly in relation to the extremely distinct environments of both organisms.     

In situ ecological development of a bacteriogenic iron oxide-producing microbial community from a subsurface granitic rock environment

The initial development and diversity of an in situ subsurface microbial community producing bacteriogenic iron oxides (BIOS) were investigated at the initiation of biofilm growth (2‐month period) and after a 1‐year period of undisturbed growth. Water chemistry data, samples of iron encrusted biofilm material and groundwater were collected from BRIC (BIOS reactor, in situ, continuous flow) apparatuses installed 297 m below sea level at the Äspö Hard Rock Laboratory (HRL) in south eastern Sweden. Comparisons between the BIOS BRIC system and an anaerobic control (AC) BRIC revealed that water mixing at the inflow leads to profuse development of BIOS related to a slightly elevated level of O₂ (up to 0.3 mg L^?1 at the transition zone between BIOS development and non‐development) and elevated Eh (>120 mV) in the first 70 mm of water depth. Decreases in dissolved and particulate iron were connected to the visible appearance of BIOS biofilms. The basic phylogenetic diversity of this site was evaluated using amplified ribosomal DNA restriction enzyme analysis (ARDRA), denaturing gradient gel electrophoresis (DGGE) and partial sequencing of 16S rDNA. From 67 clones that were positive for 16S rDNA inserts, a total of 42 different ARDRA profiles were recognized, representing four bacterial phyla and 14 different metabolic lifestyles. DGGE profiles indicated that there are differences in the representative bacteria when considering either BIOS biofilms or groundwater. DGGE also indicated that the DNA extraction protocols and any polymerase chain reaction biases were consistent. Bacterial metabolic groups associated with indirect metal adsorption and reduction along with bacteria utilizing many alternative electron acceptors were strongly represented within the clones. This study indicates that the microbial diversity of BIOS is greater than previously thought.     

A Comparison of the Rates of Fe(III) Reduction in Synthetic and Bacteriogenic Iron Oxides by Shewanella putrefaciens CN32

The susceptibility of various bacteriogenic iron oxides (BIOS) to bacterial Fe(III) reduction was examined. Reduction resulted in complete dissolution of the iron mineral from the surfaces of the Fe-oxidizing consortium. Reduction rates were compared to that of synthetic ferrihydrite (HFO). The reduction rate of HFO (0.162 day^{? 1}) was significantly lower than that of Äspö (Gallionella dominated) BIOS (0.269 day^{? 1}). Two Canadian (Leptothrix dominated) BIOS samples showed statistically equivalent rates of reduction (0.541 day^?1 and 0.467 day^{? 1}), which were higher than both Äspö BIOS and HFO. BIOS produced by different iron-oxidizing genera have different susceptibilities to microbial reduction.     

Benefits associated with the stalk of Gallionella ferruginea,evaluated by comparison of a stalk-forming and a non-stalk-forming strain and biofilm studies in situ

Factors that regulate and induce stalk formation by the iron-oxidizing and stalk-forming bacterium Gallionella ferruginea were studied in laboratory cultures and in situ. A stalk-forming strain, Sta⁺, and a non-stalk-forming strain, Sta^-, were used for comparative studies of the benefits associated with the stalk. Two different growth media were used: a ferrous sulfide medium (FS-medium), with slow oxidation of iron giving high concentrations of toxic oxygen radicals and a ferrous carbonate medium (FC-medium), with fast iron oxidation giving low concentration of the toxic oxygen radicals. It was found that Sta⁺ cells grown in the FS-medium survived 3 weeks longer than Sta^- cells grown in the FS-medium. When each strain was grown in the FC-medium, the Sta^- cells had an advantage and survived 8 weeks longer than the Sta⁺ cells. No difference in survival was found for Sta⁺ cells grown in FS-medium compared to growth in FC-medium. In laboratory cultures, the average stalk length per cell values were 7–2.5 times higher (92 h and 150–300 h growth, respectively) in a medium with 620 m iron than in a medium with 290 m iron. Gallionella ferruginea Sta⁺ outcompeted Sta^- cells when inoculated as mixed populations in FC-medium. It has previously been suggested that stalk formation in vitro is induced by oxygen. To confirm this observation, biofilm development in natural waters was studied in two wells, one with trace amounts of oxygen (LH) and one without (TH). A dense biofilm developed on surfaces exposed to flowing well LH water, but no biofilm developed in well TH. Stalks were formed in water samples from both wells when allowed to make contact with air. This work demonstrates for the first time that the stalk has a protecting function against the toxic oxygen radicals formed during the chemical iron oxidation. It also shows that it is the oxidation rate of the ferrous iron and not its concentration that is harmful to the cells. The stalk gives G. ferruginea a unique possibility to colonize and survive in habitats with high contents of iron, inaccessible for bacteria without a defense system against the oxidation of iron. Correspondence to: L. Hallbeck     

Preliminary characterization and biological reduction of putative biogenic iron oxides (BIOS) from the Tonga-Kermadec Arc, southwest Pacific Ocean

Sediment samples were obtained from areas of diffuse hydrothermal venting along the seabed in the Tonga sector of the Tonga‐Kermadec Arc, southwest Pacific Ocean. Sediments from Volcano 1 and Volcano 19 were analyzed by X‐ray diffraction (XRD) and found to be composed primarily of the iron oxyhydroxide mineral, two‐line ferrihydrite. XRD also suggested the possible presence of minor amounts of more ordered iron (hydr)oxides (including six‐line ferrihydrite, goethite/lepidocrocite and magnetite) in the biogenic iron oxides (BIOS) from Volcano 1; however, Mössbauer spectroscopy failed to detect any mineral phases more crystalline than two‐line ferrihydrite. The minerals were precipitated on the surfaces of abundant filamentous microbial structures. Morphologically, some of these structures were similar in appearance to the known iron‐oxidizing genus Mariprofundus spp., suggesting that the sediments are composed of biogenic iron oxides. At Volcano 19, an areally extensive, active vent field, the microbial cells appeared to be responsible for the formation of cohesive chimney‐like structures of iron oxyhydroxide, 2–3 m in height, whereas at Volcano 1, an older vent field, no chimney‐like structures were apparent. Iron reduction of the sediment material (i.e. BIOS) by Shewanella putrefaciens CN32 was measured, in vitro, as the ratio of [total Fe(II)]:[total Fe]. From this parameter, reduction rates were calculated for Volcano 1 BIOS (0.0521 day^?1), Volcano 19 BIOS (0.0473 day^?1), and hydrous ferric oxide, a synthetic two‐line ferrihydrite (0.0224 day^?1). Sediments from both BIOS sites were more easily reduced than synthetic ferrihydrite, which suggests that the decrease in effective surface area of the minerals within the sediments (due to the presence of the organic component) does not inhibit subsequent microbial reduction. These results indicate that natural, marine BIOS are easily reduced in the presence of dissimilatory iron‐reducing bacteria, and that the use of common synthetic iron minerals to model their reduction may lead to a significant underestimation of their biological reactivity.     

Microalgae for phosphorus removal and biomass production: a six species screen for dual‐purpose organisms

Microalgae biofuel production can be feasible when a second function is added, such as wastewater treatment. Microalgae differ in uptake of phosphorus (P) and growth, making top performer identification fundamental. The objective of this screen was to identify dual‐purpose candidates capable of high rates of P removal and growth. Three freshwater – Chlorella sp., Monoraphidium minutum sp., and Scenedesmus sp. – and three marine – Nannochloropsis sp., N. limnetica sp., and Tetraselmis suecica sp. – species were batch cultured in 250 mL flasks over 16 days to quantitate total phosphorus (TP) removal and growth as a function of P loads (control, and 5, 10, and 15 mg L^?1 enrichment of control). Experimental design used 100 μmol m^?2 s^?1 of light, a light/dark cycle of 14/10 h, and no CO₂ enrichment. Phosphorus uptake was dependent on species, duration of exposure, and treatment, with significant interaction effects. Growth was dependant on species and treatment. Not all species showed increased P removal with increasing P addition, and no species demonstrated higher growth. Nannochloropsis sp and N. limnetica sp. performed poorly across all treatments. Two dual‐purpose candidates were identified. At the 10 mg L^?1 treatment Monoraphidium minutum sp. removed 67.1% (6.66 mg L^?1 ± 0.60 SE) of TP at day 8, 79.3% (7.86 mg L^?1 ± 0.28 SE) at day 16, and biomass accumulation of 0.63 g L^?1 ± 0.06 SE at day 16. At the same treatment Tetraselmis suecica sp. removed 79.4% (6.98 mg L^?1 ± 0.24 SE) TP at day 8, 83.0% (7.30 mg L^?1 ± 0.60 SE) at day 16, and biomass of 0.55 g L^?1 ± 0.02 SE at day 16. These species merit further study using high‐density wastewater cultures and lipid profiling to assess suitability for a nutrient removal and biomass/biofuel production scheme.     

Dependence of In Situ Bacterial Fe(II)-Oxidation and Fe(III)-Precipitation on Sequential Reactive Transport

A study was conducted to determine in situ rates of Fe(II) oxidation and Fe(III) precipitation along a 5.0 m reach of a ferruginous groundwater discharge zone under two distinct conditions; (i) the natural state featuring abundant flocculent mats of bacteriogenic iron oxides (BIOS) produced by Fe(II)-oxidizing bacteria, and (ii) after a manual washout of the streambed to remove the microbial mat. Examination of mat samples by differential interference contrast light microscopy revealed tangled meshworks of filamentous Leptothrix sheaths and helical Gallionella stalks intermixed with fine-grained hydrous ferric oxide (HFO) precipitates. The greatest accumulation of BIOS mat was 1.0 m downstream of the groundwater spring. Redox potential (Eh) increased sharply from 200 mV to over 300 mV over the last 2.0 m of the reach. Similarly, dissolved oxygen increased from < 10% saturation to almost 100% saturation over the last 2.0 m of the reach, whereas pH increased from 6.4 to 7.3. Pseudo-first-order rate constants determined on the basis of analytical solutions to sequential partial differential advection-dispersion-reaction equations for the linear Fe(II)→Fe(III)→HFO reaction network yielded in situ Fe(II) oxidation rate constants (k_ox) of 1.70 ± 0.20 min^?1 in natural conditions and 0.48 ± 0.14 min^?1 after washout. Corresponding Fe(III)-precipitation rates (k_p) before and after washout were 3.45 ± 0.10 min^?1 and 0.90 ± 0.01 min^?1, respectively. These values for k_ox and k_p are higher than estimates obtained from closed batch microcosm and laboratory experiments, underscoring the crucial dependence of in situ Fe(II) oxidation and Fe(III) precipitation rates on advective and dispersive mass transport. The results also highlight the influence that BIOS microbial mats exert on the reaction kinetics of the multiple heterogeneous reactions contributing not only to Fe(II)/Fe(III) redox transformations in groundwater discharge zones, but also the precipitation of HFO.     

Effect of linear alkylbenzene sulfonate on Cu2+ removal by Spirulina platensis strain (FACHB‐834)

The removal efficiency of Cu²⁺ by Spirulina platensis (strain FACHB‐834), in viable and heat‐inactivated forms, was investigated in the presence and absence of linear alkylbenzene sulfonate (LAS). When the initial Cu²⁺ concentration was in the range of 0.5–1.5 mg · L^?1, a slight increase in growth rate of FACHB‐834 was observed. In contrast, when Cu²⁺ or LAS concentrations were at or higher than 2.0 or 6.0 mg · L^?1, respectively, the growth of FACHB‐834 was inhibited and displayed yellowing and fragmentation of filaments. The presence of LAS improved Cu²⁺ removal by ~20%, and accelerated attainment of Cu²⁺ retention equilibrium. For the 2‐ mg · L^?1 Cu²⁺ treatments, retention equilibrium occurred within 2 d and showed maximum Cu²⁺ removal of 1.83 mg · L^?1. In the presence of LAS, the ratio of extracellular bound Cu²⁺ to intracellular Cu²⁺ taken up by the cells was lower (1.05–2.26) than corresponding ratios (2.46–7.85) in the absence of LAS. The percentages of extracellular bound Cu²⁺ to total Cu²⁺ removal (both bound and taken up by cells) in the presence of LAS ranged from 51.2% to 69.3%, which was lower than their corresponding percentages (71.1%–88.7%) in the absence of LAS. LAS promoted biologically active transport of the extracellular bound form of Cu²⁺ into the cell. In contrast, the addition of LAS did not increase the maximum removal efficiency of Cu²⁺ (61.4% ± 5.6%) by heat‐inactivated cells compared to that of living cells (59.6% ± 6.0%). These results provide a theoretical foundation for designing bioremediation strategies using FACHB‐834 for use in surface waters contaminated by both heavy metals and LAS.     

Growth of Iron-Oxidizing Bacteria Gallionella ferruginea and Leptothrix cholodnii in Oligotrophic Environments: Ca,Mg, and C as Limiting Factors and G. ferruginea Necromass as C-Source

Abstract

Iron-oxidizing bacteria (FeOB) can successively populate low-nutrient aquatic environments and adapt to a broad concentration range of alkaline earth metals, with optimum conditions widely differing from one species to another. For the most abundant known FeOB genera Gallionella and Leptothrix, there is a lack of reports on substrate affinity for calcium and magnesium and necromass assimilability. Single nutrient and combined affinity for Ca and Mg of a wild Gallionella ferruginea isolate and a Leptothrix cholodnii strain as well as growth of heterotrophic L. cholodnii on necromass of autotrophic G. ferruginea were determined by cell density measurements. G. ferruginea responds with Monod-shaped preferences and thus favors waters rich in Ca and Mg. Maximum growth occurred at Ca concentrations five times above those of commonly used modified mineral Wolfe’s medium. L. cholodnii showed a Monod-shaped preference in the low concentration range and an inhibitory response to increasing hardness: concentrations >2?mM Ca or >0.6?mM Mg allow only 50 or 75%, respectively, of maximum specific cell densities. Considering the concentration range with a Monod-shaped response (for L. cholodnii only lower concentration range), both FeOB show a type I independent colimitation for Ca and Mg with lower requirements of Mg than Ca. On a C-limited medium containing G. ferruginea necromass as the only C-source, L. cholodnii cell counts were higher by two orders of magnitude compared to pyruvate medium. Thus, the necromass may serve as a primary C-source for heterotrophic FeOB and other heterotrophic bacteria with technical and economical relevance.     

Ion flux and cortisol responses of cardinal tetra,Paracheirodon axelrodi (Schultz, 1956), to additives (tetracycline,tetracycline + salt or Amquel®) used during transportation: contributions to Amazonian ornamental fish trade

The cardinal tetra, Paracheirodon axelrodi (Schultz), is the most important ornamental fish exported from Brazil and Colombia. During the transport of this species, Amazon fishermen usually add unmeasured amounts of tetracycline and/or table salt to the water in an effort to mitigate stress and mortality. The aim of the present study was to analyze the effect of salt, the antibiotic tetracycline and the ammonia chelating agent Amquel^® in the transport of this species. Cardinal tetras were submitted to a 24‐h boat transport in water containing either tetracycline hydrochloride (2.5 mg L^?1), Amquel^® (26.41 mg L^?1), tetracycline + table salt (2.5 mg L^?1 + 66.67 mg L^?1), or additive‐free water (control treatment). Whole‐body cortisol measurements showed that fish transported with any water additive had lower cortisol levels compared to control. However, based on ionoregulatory and water quality parameters, the addition of tetracycline, Amquel^® or the combination tetracycline + salt to the water of transport of cardinal tetras is not recommended when compared to control. Although Amquel^® helped stabilize the pH and diminish total ammonia levels in the transport water, this compound dramatically increased net Na⁺ and Cl^? uptake, and therefore compromised cardinal tetra ionoregulation.     

Effects of metalaxyl enantiomers stress on root activity and leaf antioxidant enzyme activities in tobacco seedlings

The objective of this experiment was to study the effects of metalaxyl enantiomers on the activity of roots and antioxidative enzymes in tobacco seedlings. Water culture experiment was conducted to analyze the effects of different concentrations of metalaxyl enantiomers (30 and 10 mg L^?1) on root activity and leaf superoxide dismutase (SOD), peroxidase (POD), and catalase (CAT) activities and malondialdehyde (MDA) content of tobacco seedlings. The results showed that metalaxyl significantly inhibited root activity and significantly improved leaf SOD, POD, and CAT activities and MDA content. A better physiological response in tobacco seedlings was observed at 30 mg L^?1 than at 10 mg L^?1 metalaxyl. The stereoselectivity for different enantiomers had no obvious effect on root activity and the leaf POD activity, but it affected significantly the SOD and CAT activities and MDA content. The SOD activity was promoted more by R‐enantiomer than by S‐enantiomer at 30 mg L^?1 metalaxyl, and the same effect was observed on CAT activity from the beginning to the end of the stress period. The MDA content under the stress by R‐enantiomer was higher than that under the stress by S‐enantiomer at 10 mg L^?1 metalaxyl.     

Differentiation between Gallionella and Metallogenium

Summary The DNA base composition and the sensitivity to iron of an ironoxidizing Metallogenium was determined. A comparison of the organism with Gallionella ferruginea suggests that the iron-oxidizing Metallogenium may be a common contaminant of G. ferruginea cultures.     

Surface chemistry and reactivity of bacteriogenic iron oxides from Axial Volcano, Juan de Fuca Ridge, north-east Pacific Ocean

Iron oxides were collected from the caldera of Axial Volcano, a site of hydrothermal vent activity along the Juan de Fuca Ridge. Mineralogical inspection using X‐ray diffraction (XRD) revealed the majority of samples to be 2‐line ferrihydrite, with one of the samples corresponding to poorly ordered goethite. Examination using environmental scanning electron microscopy (ESEM) found the constituents of the iron oxides to consist predominantly of bacterial‐like structures that resembled the iron oxidizing bacteria Leptothrix ochracea, Gallionella ferruginea and a novel PV‐1 strain. X‐ray photoelectron spectroscopy (XPS) detected the presence of Fe, O, C, N, Ca, Si and P on all the samples with the exception of poorly ordered goethite, where Ca and P were absent, in addition to a weak N peak. Binding energy shifts of the Fe 2p and O 1s peaks were indicative of ferrihydrite and hydroxyl functional groups, while the presence and speciation of the C 1s peak was attributed to the presence of bacteria. Use of acid‐base titration data modelling in conjunction with a linear programming regression method (LPM) indicated that the iron oxides are composed of heterogeneous surface functional groups. Differences in iron oxide reactivity values correlated with differences in the bacterial and mineral fabric of the samples. The diverse surface chemistry and high reactivity of these iron oxides may be important in the global cycling of various elements throughout the oceans due to their presence along widespread mid‐ocean ridges.     

Different fermentation strategies by Schizochytrium mangrovei strain pq6 to produce feedstock for exploitation of squalene and omega‐3 fatty acids

Schizochytrium mangrovei strain PQ 6 was investigated for coproduction of docosahexaenoic acid (C22: 6ω‐3, DHA ) and squalene using a 30‐L bioreactor with a working volume of 15 L under various batch and fed‐batch fermentation process regimes. The fed‐batch process was a more efficient cultivation strategy for achieving higher biomass production rich in DHA and squalene. The final biomass, total lipid, unsaponifiable lipid content, and DHA productivity were 105.25 g · L^?1, 43.40% of dry cell weight, 8.58% total lipid, and 61.66 mg · g^?1 · L^?1, respectively, after a 96 h fed‐batch fermentation. The squalene content was highest at 48 h after feeding glucose (98.07 mg · g^?1 of lipid). Differences in lipid accumulation during fermentation were correlated with changes in ultrastructure using transmission electron microscopy and Nile Red staining of cells. The results may be of relevance to industrial‐scale coproduction of DHA and squalene in heterotrophic marine microalgae such as Schizochytrium .     

A novel gaseous dimethylamine sensor utilizing cataluminescence on zirconia nanoparticles

A novel cataluminescence (CTL) sensor using ZrO₂ nanoparticles as the sensing material was developed for the determination of trace dimethylamine in air samples based on the catalytic chemiluminescence (CL) of dimethylamine on the surface of ZrO₂ nanoparticles. The CTL characteristics and the different factors on the signal intensity for the sensor, including nanomaterials, working temperature, wavelength and airflow rate, were investigated in detail. The CL intensity on ZrO₂ nanoparticles was the strongest among the seven examined catalysts. This novel CL sensor showed high sensitivity and selectivity to gaseous dimethylamine at optimal temperature of 330°C. Quantitative analysis was performed at a wavelength of 620 nm. The linear range of CTL intensity vs concentration of gaseous dimethylamine was 4.71 × 10^?3 to 7.07 × 10^?2 mg L^?1 (r = 0.9928) with a detection limit (3σ) of 6.47 × 10^?4 mg L^?1. No or only very low levels of interference were observed while the foreign substances such as benzene, hydrochloric acid, methylbenzene, chloroform, n‐hexane and water vapor were passing through the sensor. The response time of the sensor was less than 50 s, and the sensor had a long lifetime of more than 60 h. The sensor was successfully applied to the determination of dimethylamine in artificial air samples, and could potentially be applied to analysis of nerve agents such as Tabun (GA). Copyright © 2009 John Wiley & Sons, Ltd.     

Nitrogen fixation activity of a filamentous,nonheterocystous cyanobacterium in the presence and absence of exogenous,organic substrates

Gallionella ferruginea is able to utilize Fe(II) and the reduced sulfur compounds sulfide and thiosulfate as electron donor and energy source. Tetrathionate and elemental sulfur, on the other hand, are not metabolized. In sulfide-O₂ microgradient cultures G. ferruginea grows at the interface between the oxidizing and the reducing zones. Optimal growth depends on low oxygen and sulfide concentrations. Establishing within the gradient protects the bacterium from too high sulfide concentrations. G. ferruginea excretes extracellular polymeric substances (EPS). While in FeS-gradient cultures 2×10⁶ cells/ml were obtained the bacterial mass could be increased to 1–3×10⁸ cells/ml in shaken batch cultures using thiosulfate as substrate. A further increase of bacterial mass by adding an organic carbon source was not possible confirming that G. ferruginea is an obligate autotrophic organism. When growing on sulfide or thiosulfate the otherwise characteristic twisted stalk consisting of ferric hydroxide is lacking. It is thus shown to be a metabolic end product of Fe(II) oxidation rather than metabolically active cellular material.     

Contrasting effects of low‐level phosphorus and nitrogen enrichment on growth of the mat‐forming alga Didymosphenia geminata in an oligotrophic river

相似文献   

Reference values for selected hematological and serum biochemical parameters of Senegalese sole (Solea senegalensis Kaup, 1858) juveniles under intensive aquaculture conditions

This work aims to establish normal reference intervals for selected hemato‐biochemical parameters, based on their potential clinical relevance, and which may contribute to evaluating the health, nutritional and welfare status of Senegalese sole (Solea senegalensis Kaup, 1858) juveniles. Thirty‐one healthy Senegalese sole juveniles grown under intensive aquaculture conditions were used in the study. Based on the robust method with Box–Cox transformation data the established reference intervals for hematological parameters were: hematocrit 12–26%, hemoglobin 2.8–6 g dl^?1, erythrocytes 90–97.0% total, leucocytes 4–10% total; erythrocyte indices and differential leucocytes counts were also evaluated. Reference intervals for biochemical parameters were (g dl^?1) glucose 19–86 mg dl^?1, total protein 2.6–6.3, albumin 1–2.34, globulins 1.8–4.1, lipids 0.7–1.3, triglycerides 0.3–1.8, total cholesterol 0.1–0.9 g dl^?1, HDL‐cholesterol 4–65 mg dl^?1, LDL‐cholesterol 7–532 mg dl^?1, sodium 124–202 mmol L^?1), potassium 1.1–4.6 mmol L^?1, calcium 7.6–13.2 mg L^?1, magnesium 1.8–4.8 mg L^?1, inorganic phosphorus 3.4–9.5 mg L^?1, alkaline phosphatase 93–598 U L^?1, aspartate aminotransferase 118–605 U L^?1, lactate dehydrogenase 8.7–782 U L^?1, and creatine phosphokinase 31.5–552 U L^?1. This data is expected to provide a valuable tool to monitor the stress, health and nutritional conditions of Senegalese sole juveniles under aquaculture production.