Motility of Marichromatium gracile in Response to Light, Oxygen, and Sulfide

The motility of the purple sulfur bacterium Marichromatium gracile was investigated under different light regimes in a gradient capillary setup with opposing oxygen and sulfide gradients. The gradients were quantified with microsensors, while the behavior of swimming cells was studied by video microscopy in combination with a computerized cell tracking system. M. gracile exhibited photokinesis, photophobic responses, and phobic responses toward oxygen and sulfide. The observed migration patterns could be explained solely by the various phobic responses. In the dark, M. gracile formed an ~500-μm-thick band at the oxic-anoxic interface, with a sharp border toward the oxic zone always positioned at ~10 μM O₂. Flux calculations yielded a molar conversion ratio S_tot/O₂ of 2.03:1 (S_tot = [H₂S] + [HS⁻] + [S²⁻]) for the sulfide oxidation within the band, indicating that in darkness the bacteria oxidized sulfide incompletely to sulfur stored in intracellular sulfur globules. In the light, M. gracile spread into the anoxic zone while still avoiding regions with >10 μM O₂. The cells also preferred low sulfide concentrations if the oxygen was replaced by nitrogen. A light-dark transition experiment demonstrated a dynamic interaction between the chemical gradients and the cell's metabolism. In darkness and anoxia, M. gracile lost its motility after ca. 1 h. In contrast, at oxygen concentrations of >100 μM with no sulfide present the cells remained viable and motile for ca. 3 days both in light and darkness. Oxygen was respired also in the light, but respiration rates were lower than in the dark. Observed aggregation patterns are interpreted as effective protection strategies against high oxygen concentrations and might represent first stages of biofilm formation.     

A Benthic Gradient Chamber for culturing phototrophic sulfur bacteria on reconstituted sediments

Abstract: The growth of phototrophic sulfur bacteria in benthic systems is restricted to well-defined layers within the sedimentary oxygen, sulfide, pH and light gradients. In order to culture these microorganisms under more ecologically relevant conditions, we have developed a Benthic Gradient Chamber (BGC) in which phototrophic sulfur bacteria can be grown within experimentally imposed solute and light gradients. The new autoclavable device is composed of a reconstituted sand core sandwiched in between a lower anoxic sulfide-containing compartment and an upper oxic compartment. The core can be illuminated from above by a collimated light beam. An axenic biofilm of Thiocapsa roseopersicina strain EP 2204 developed from a tiny inoculum within the sand core, using a 5-week incubation period and a 16:8 h light/dark illumination regime. The metabolic activities in this biofilm were inferred from the analyses of oxygen, sulfide and pH profiles, and their shifts during light-dark cycles.     

Oxygen Responses and Mat Formation by Beggiatoa spp

The behavioral response of single Beggiatoa sp. filaments moving on a gas-permeable membrane was studied by the combined use of microscopy and oxygen microelectrodes during controlled oscillations of oxygen tension. The bacteria reacted to increasing oxygen by reversing the direction of movement. The same step-up phobic response to oxygen was observed when a filament tip or loop glided into a stable microgradient of increasing oxygen. The response was sensitive to a change in oxygen tension of <5% of air saturation min⁻¹. The response time was 20 to 50 s. Frequently, only part of the filament responded, which led to the formation of sharp bends, loops, and coils. This partial response facilitated the positioning of the long filaments within the narrow O₂-H₂S interface. The structure of whole Beggiatoa mats on sediment surfaces varied from loose to dense in relation to shallow or steep oxygen gradients in the 0.3- to 2-mm-thick, unstirred boundary layer. In an illuminated sediment Beggiatoa spp. lived together with photosynthetic organisms and migrated vertically in accordance with light/dark variations. The combined effect of phobic responses to light and oxygen can explain this migration.     

Growth and mechanism of filamentous-sulfur formation by Candidatus Arcobacter sulfidicus in opposing oxygen-sulfide gradients

Studies were conducted in opposing gradients of oxygen and sulfide in microslide capillaries to (i) characterize the chemical microenvironment preferred by Candidatus Arcobacter sulfidicus, a highly motile, sulfur-oxidizing bacterium that produces sulfur in filamentous form, and (ii) to develop a model describing the mechanism of filamentous-sulfur formation. The highly motile microorganisms are microaerophilic, with swarms effectively aggregating within oxic-anoxic interfaces by exhibiting a chemotactic response. The position of the band was found to be largely independent of the sulfide concentration as it always formed at the oxic-anoxic interface. Flux calculations based on steady state gradients of oxygen and sulfide indicate that sulfide is incompletely oxidized to sulfur, in line with the formation of filamentous sulfur by these organisms. It is proposed that Candidatus Arcobacter sulfidicus effectively competes with other sulfur-oxidizing bacteria in the environment by being able to tolerate higher concentrations of hydrogen sulfide (1-2 mM) and by possessing the ability to grow at very low oxygen concentrations (1-10 muM). The formation of mat-like structures from filamentous sulfur appears to be a population mediated effort allowing these organisms to effectively colonize environments characterized by high sulfide, low oxygen and dynamic fluid movement.     

Diel Vertical Movements of the Cyanobacterium Oscillatoria terebriformis in a Sulfide-Rich Hot Spring Microbial Mat

Oscillatoria terebriformis, a thermophilic cyanobacterium, carried out a diel vertical movement pattern in Hunter's Hot Springs, Oreg. Throughout most daylight hours, populations of O. terebriformis covered the surface of microbial mats in the hot spring outflows below an upper temperature limit of 54°C. Upon darkness trichomes moved downward by gliding motility into the substrate to a depth of 0.5 to 1.0 mm, where the population remained until dawn. At dawn the population rapidly returned to the top of the mats. Field studies with microelectrodes showed that the dense population of O. terebriformis moved each night across an oxygen-sulfide interface, entering a microenvironment which was anaerobic and reducing, a dramatic contrast to the daytime environment at the mat surface where oxygenic photosynthesis resulted in supersaturated O₂. Laboratory experiments on motility with the use of sulfide gradients produced in agar revealed a negative response to sulfide at concentrations similar to those found in the natural mats. The motility response may help explain the presence of O. terebriformis below the mat surface at night. The movement back to the surface at dawn appears to be due to a combination of phototaxis, photokinesis, and the onset of oxygenic photosynthesis which consumes sulfide.     

Colorless Sulfur Bacteria, Beggiatoa spp. and Thiovulum spp., in O(2) and H(2)S Microgradients

The interactions between colorless sulfur bacteria and the chemical microgradients at the oxygen-sulfide interface were studied in Beggiatoa mats from marine sediments and in Thiovulum veils developing above the sediments. The gradients of O(2), H(2)S, and pH were measured by microelectrodes at depth increments of 50 mum. An unstirred boundary layer in the water surrounding the mats and veils prevented microturbulent or convective mixing of O(2) and H(2)S. The two substrates reached the bacteria only by molecular diffusion through the boundary layer. The bacteria lived as microaerophiles or anaerobes even under stirred, oxic water. Oxygen and sulfide zones overlapped by 50 mum in the bacterial layers. Both compounds had concentrations in the range of 0 to 10 mumol liter and residence times of 0.1 to 0.6 s in the overlapping zone. The sulfide oxidation was purely biological. Diffusion calculations showed that formation of mats on solid substrates or of veils in the water represented optimal strategies for the bacteria to achieve a stable microenvironment, a high substrate supply, and an efficient competition with chemical sulfide oxidation. The continuous gliding movement of Beggiatoa cells in mats or the flickering motion of Thiovulum cells in veils were important for the availability of both O(2) and H(2)S for the individual bacteria.     

Photosynthetic oxygen evolution and CO2 photoassimilation by cyanobacteria that form water-bloom spots in a sulfur spring with a high sulfide content

Cyanobacteria belonging mainly to the genera Anabaena and Oscillatoria were isolated from water-bloom spots of a sulfur spring in Staraya Matsesta. Their suspensions evolved O2 at a rate of 6--8 nM/min per 1 mg of dry cell weight at an intensity of solar radiation being 60--75 mV/cm2 per 1 sec. The cells were also capable of CO2 photoassimilation in the presence of solfide at a rate of 10(-4) mg C per mg per hour. DCMU at a concentration of 10(-5) M completely inhibited O2 evolution and inhibited CO2 fixation by 80%. Oxygen assimilation in dark by the suspensions did not depend on the addition of cyanide and was caused apparently by nonenzymatic reduction of O2 with sulfide dissolved in the spring water. Oxygen assimilation by the suspensions in light in the presence of DCMU was by 20--30% greater than in dark. Therefore, the cells of cyanobacteria are characterized by photorespiration at the level of photosystem I. Presumably, sulfide at a concentration of 9 mM cannot significantly inhibit the photosynthetic processes in cyanobacteria producing water-bloom spots in the sulfur spring.     

Potential sulfur metabolisms and associated bacteria within anoxic surface sediment from saline meromictic Lake Kaiike (Japan)

The effects of light and of added electron donors and sulfur compounds on sulfur metabolisms in the microbial mat dilutions from the saline meromictic Lake Kaiike were investigated. Sulfide concentrations in the mat dilution without any electron donor gradually increased by approximately 0.6-1 mM in the dark. Additions of lactate, acetate, H(2)/CO(2), propionate and iso-butylate stimulated sulfide production, whereas benzoate did not, indicating the limitation of sulfate reduction by available electron donor concentrations. More sulfide was produced, without a decrease of sulfate, in an elemental sulfur-amended dilution than in a non-amended control. In contrast, the addition of a high concentration of sulfide slowed down sulfide production. After enrichment under various conditions, microbial communities in the dilutions were characterized by a denaturing gradient gel electrophoresis of PCR-amplified 16S rRNA gene and sequencing. As a result, microorganisms affiliated with mesophilic sulfate-reducing bacteria group within the Deltaproteobacteria and the Epsilonproteobacteria were mainly enriched by the addition of electrons used in this study, suggesting that these microorganisms might play an important role in sulfur metabolisms within the surficial sediment of Lake Kaiike.     

Uptake rates of oxygen and sulfide measured with individual Thiomargarita namibiensis cells by using microelectrodes

Gradients of oxygen and sulfide measured towards individual cells of the large nitrate-storing sulfur bacterium Thiomargarita namibiensis showed that in addition to nitrate oxygen is used for oxidation of sulfide. Stable gradients around the cells were found only if acetate was added to the medium at low concentrations.     

Monitoring of oxygenic and anoxygenic photosynthesis in a unicyanobacterial biofilm, grown in benthic gradient chamber

In order to assess the role of cyanobacteria in the formation and dynamics of microenvironments in microbial mats, we studied an experimental biofilm of a benthic, halotolerant strain, belonging to the Halothece cluster of cyanobacteria. The 12-week-old biofilm developed in a sand core incubated in a benthic gradient chamber under opposing oxygen and sulfide vertical concentration gradients. At the biofilm surface, and as a response to high light irradiances, specific accumulation of myxoxanthophyll was detected in the cells, consistent with the typical vertical distribution of sun versus shade species in nature. The oxygen turn-over in terms of gross photosynthesis and net productivity rates was comparable to oxygen dynamics in natural microbial mats. Sulfide blocked O(2) production at low irradiances in deep biofilm layers but the dynamics of H(2)S and pH demonstrated that sulfide removal by anoxygenic photosynthesis was taking place. At higher irradiances, as soon as H(2)S was depleted, the cells switched to oxygenic photosynthesis as has been postulated for natural communities. The similarities between this experimental biofilm and natural benthic microbial mats demonstrate the central role of cyanobacteria in shaping microenvironmental gradients and processes in other complex microbial communities.     

黑暗限气条件下铜绿微囊藻细胞死亡的形态结构和生理生化变化

【目的】研究铜绿微囊藻细胞死亡过程中形态和生理生化变化,探讨蓝藻细胞死亡机制。【方法】通过黑暗限气处理模拟水华爆发后期水体环境,在处理后不同时间取样,对藻液的OD值,溶氧含量和pH值进行监测,使用透射电镜对细胞形态结构变化进行观察,通过胱天蛋白酶(Cysteine-dependent aspartate specificprotease,Caspase)活性检测、活性氧含量测定、末端脱氧核糖核酸转移酶介导的dUTP缺口末端标记(Terminal deoxynucleotidyl transferase-mediated dUTP nick end-labeling,TUNEL)染色和琼脂糖凝胶电泳对处理后藻细胞的死亡生理进行研究。【结果】黑暗限气处理后,藻培养液pH值和溶解氧含量下降,处理12 h后藻液开始变黄,48 h后藻细胞全部死亡。电镜观察结果表明,藻细胞在黑暗限气处理所导致的死亡过程中出现空泡和类囊体、核糖体等内部结构解体但细胞壁仍保持完整等现象。活性氧含量和caspase活性检测表明,在藻细胞死亡过程中活性氧含量和caspase活性上升。TUNEL染色和琼脂糖凝胶电泳分析发现,藻细胞在死亡过程中DNA发生断裂和降解。【结论】铜绿微囊藻细胞在黑暗和限气处理中表现出和真核生物细胞程序性死亡相类似的死亡特征,这说明细胞死亡机制是保守的,原核细胞和真核细胞一样具有程序性死亡机制。     

Rapid hydrogen sulfide consumption by Tetrahymena pyriformis and its implications for the origin of mitochondria

Although sulfide is typically regarded as toxic to eukaryotic cells, it is avidly consumed by Tetrahymena pyriformis. That was observed only when the sulfide concentration was kept below 1 microM. Previously concentrations that were too high had been tested. A new device (Sulfidostat) was used to measure sulfide consumption in steady-state concentrations as low as 10(-12)M. The technique was validated non-biologically by slowly injecting AgNO(3) into buffer and using Ag(2)S precipitation to mimic sulfide consumption, confirming that rates of sulfide consumption could be measured independently of sulfide concentrations. With T. pyriformis, sulfide consumption was 0.25 micromol (gprotein)(-1)s(-1) in 0.5 microM sulfide. Sulfide consumption required O(2) and was inhibited by HCN or by too much sulfide. When cells were separated into fractions, sulfide consumption occurred in the particulate (mitochondrial) fraction. Unexpectedly, the soluble cytosolic fraction slowly produced sulfide even when aerated. The observations are consistent with the conjecture that mitochondria evolved from sulfidotrophic symbionts in a sulfidogenic host cell.     

Competition for sulfide among colorless and purple sulfur bacteria in cyanobacterial mats

Abstract The vertical zonation of light, O₂, H₂S, pH, and sulfur bacteria was studied in two benthic cyanobacterial mats from hypersaline ponds at Guerrero Negro, baja California, Mexico. The physical-chemical gradients were analyzed in the upper few mm at ≥ 100 μm spatial resolution by microelectrodes and by a fiber optic microprobe. In mats, where oxygen produced by photosynthesis diffused far below the depth of the photic zone, colorless sulfur bacteria ( Beggiatoa sp.) were the dominant sulfide oxidizing organisms. In a mat, where the O₂–H₂S interface was close to the photic zone, but yet received no significant visible light, purple sulfur bacteria ( Chromatium sp.) were the dominant sulfide oxidizers. Analysis of the spectral light distribution heare showed that the penetration of only 1% of the incident near-IR light (800–900 nm) into the sulfide zone was sufficient for the development of Chromatium in a narrow band of 300 μm thickness. The balance betweem O₂ and light penetration down into the sulfide zone thus deterined in mcro-scale which type of sulfur bacteria becamed dominant.     

Anaerobic sulfide oxidation with nitrate by a freshwater Beggiatoa enrichment culture

A lithotrophic freshwater Beggiatoa strain was enriched in O2-H2S gradient tubes to investigate its ability to oxidize sulfide with NO3- as an alternative electron acceptor. The gradient tubes contained different NO3- concentrations, and the chemotactic response of the Beggiatoa mats was observed. The effects of the Beggiatoa sp. on vertical gradients of O2, H2S, pH, and NO3- were determined with microsensors. The more NO3- that was added to the agar, the deeper the Beggiatoa filaments glided into anoxic agar layers, suggesting that the Beggiatoa sp. used NO3- to oxidize sulfide at depths below the depth that O2 penetrated. In the presence of NO3- Beggiatoa formed thick mats (>8 mm), compared to the thin mats (ca. 0.4 mm) that were formed when no NO3- was added. These thick mats spatially separated O2 and sulfide but not NO3- and sulfide, and therefore NO3- must have served as the electron acceptor for sulfide oxidation. This interpretation is consistent with a fourfold-lower O2 flux and a twofold-higher sulfide flux into the NO3- -exposed mats compared to the fluxes for controls without NO3-. Additionally, a pronounced pH maximum was observed within the Beggiatoa mat; such a pH maximum is known to occur when sulfide is oxidized to S0 with NO3- as the electron acceptor.     

Uptake Rates of Oxygen and Sulfide Measured with Individual Thiomargarita namibiensis Cells by Using Microelectrodes

Gradients of oxygen and sulfide measured towards individual cells of the large nitrate-storing sulfur bacterium Thiomargarita namibiensis showed that in addition to nitrate oxygen is used for oxidation of sulfide. Stable gradients around the cells were found only if acetate was added to the medium at low concentrations.     

Anaerobic sulfur oxidation in the absence of nitrate dominates microbial chemoautotrophy beneath the pelagic chemocline of the eastern Gotland Basin, Baltic Sea

Oxic–anoxic interfaces harbor significant numbers and activity of chemolithoautotrophic microorganisms, known to oxidize reduced sulfur or nitrogen species. However, measurements of in situ distribution of bulk carbon dioxide (CO₂) assimilation rates and active autotrophic microorganisms have challenged the common concept that aerobic and denitrifying sulfur oxidizers are the predominant autotrophs in pelagic oxic–anoxic interfaces. Here, we provide a comparative investigation of nutrient, sulfur, and manganese chemistry, microbial biomass distribution, as well as CO₂ fixation at the pelagic redoxcline of the eastern Gotland Basin, Baltic Sea. Opposing gradients of oxygen, nitrate, and sulfide approached the detection limits at the chemocline at 204 m water depth. No overlap of oxygen or nitrate with sulfide was observed, whereas particulate manganese was detected down to 220 m. More than 70% of the bulk dark CO₂ assimilation, totaling 9.3 mmol C m⁻² day⁻¹, was found in the absence of oxygen, nitrite, and nitrate and could not be stimulated by their addition. Maximum fixation rates of up to 1.1 μmol C L⁻¹ day⁻¹ were surprisingly susceptible to altered redox potential or sulfide concentration. These results suggest that novel redox-sensitive pathways of microbial sulfide oxidation could account for a significant fraction of chemolithoautotrophic growth beneath pelagic chemoclines. A mechanism of coupled activity of sulfur-oxidizing and sulfur-reducing microorganisms is proposed.     

Hydrogen sulfide can inhibit and enhance oxygenic photosynthesis in a cyanobacterium from sulfidic springs

We used microsensors to investigate the combinatory effect of hydrogen sulfide (H₂S) and light on oxygenic photosynthesis in biofilms formed by a cyanobacterium from sulfidic springs. We found that photosynthesis was both positively and negatively affected by H₂S: (i) H₂S accelerated the recovery of photosynthesis after prolonged exposure to darkness and anoxia. We suggest that this is possibly due to regulatory effects of H₂S on photosystem I components and/or on the Calvin cycle. (ii) H₂S concentrations of up to 210 μM temporarily enhanced the photosynthetic rates at low irradiance. Modelling showed that this enhancement is plausibly based on changes in the light‐harvesting efficiency. (iii) Above a certain light‐dependent concentration threshold H₂S also acted as an inhibitor. Intriguingly, this inhibition was not instant but occurred only after a specific time interval that decreased with increasing light intensity. That photosynthesis is most sensitive to inhibition at high light intensities suggests that H₂S inactivates an intermediate of the oxygen evolving complex that accumulates with increasing light intensity. We discuss the implications of these three effects of H₂S in the context of cyanobacterial photosynthesis under conditions with diurnally fluctuating light and H₂S concentrations, such as those occurring in microbial mats and biofilms.     

Microbial activities and chemical gradients in the chemocline of a meromictic lake in relation to the precision of the sampling procedure

Abstract The dark CO₂ fixation rate, and sulfide and oxygen concentrations, were measured in the chemocline of the eutrophic, meromictic lake Saelenvannet in Western Norway. Sulfide and oxygen coexisted at a depth of 4–5 m in a narrow layer, only 2.5–10 cm wide. Coexistence of oxygen and sulfide coincided with an increase in the rate of dark CO₂ fixation. Maximal potential for light-dependent CO₂ fixation was found 2.5 cm below the sulfide and oxygen coexistence region. Our results demonstrate that a number of conventional sampling techniques are unsuitable for the study of such interfaces, and that very precise sampling techniques are needed to measure the chemical gradients and biological processes taking place in the chemocline of shallow meromictic lakes.     

Survival of sulfate-reducing bacteria after oxygen stress, and growth in sulfate-free oxygen-sulfide gradients

Abstract The survival after oxygen stress was studied with eight species of sulfate-reducing bacteria. In the absence of sulfide all species tolerated 6 min of aeration without loss of viability. Even after 3 h of aeration the viability of four species ( Desulfovibrio vulgaris, D. desulfuricans, D. salexigens and Desulfobacter postgatei ) was not impaired. Four other species were sensitive to 3 h of aeration: the surviving fractions of Desulfotomaculum ruminis, D. nigrificans and Desulfococcus multivorans were about 1%, that of Desulfotomaculum orientis about 0.01%. Formation of spores resulted in oxygen resistance of D. orientis . Reducing agents did not protect the vegetative cells of this strain against oxygen toxicity. In contrast, sulfhydryl group-containing agents increased the oxygen sensitivity considerably.
Growth of sulfate- and sulfur-reducing bacteria in oxygen-sulfide gradients in agar tubes was studied. In the gradients these strictly anaerobic bacteria revealed oxygen-dependent growth in sulfate- and sulfur-free medium. Three sulfate-reducing bacteria that could not use thiosulfate or sulfur as electron acceptor failed to grow in oxygen-sulfide gradients. Obviously, not directly molecular oxygen, but oxidation products of sulfide, such as thiosulfate or sulfur, were used as electron acceptors and were continuously regenerated in a cycling process from sulfide by autoxidation. The conceivable ecological significance of a short sulfur cycle driven by autoxidation of sulfide is discussed.     

Coexistence of organisms competing for the same substrate: An example among the purple sulfur bacteria

The purpose of this study was to find a possible explanation for the coexistence of large and small purple sulfur bacteria in natural habitats. Experiments were carried out withChromatium vinosum SMG 185 andChromatium weissei SMG 171, grown in both batch and continuous cultures. The data may be summarized as follows: (a) In continuous light, with sulfide as growth rate-limiting substrate, the specific growth rate ofChr. vinosum exceeds that ofChr. weissei regardless of the sulfide concentration employed. Consequently,Chr. weissei is unable to compete successfully and is washed out in continuous cultures. (b) With intermittant light-dark illumination, the organisms showed balanced coexistence when grown in continuous cultures. The “steady-state” abundance ofChr. vinosum was found to be positively related to the length of the light period, and that ofChr. weissei to the length of the dark period. (c) Sulfide added during darkness is rapidly oxidized on subsequent illumination, resulting in the intracellular storage of reserve substances, which are later utilized for growth. The rate of sulfide oxidation/mg cell N/hr was found to be over twice as high inChr. weissei as inChr. vinosum. The observed coexistence may be explained as follows. In the light, with both strains growing, most of the sulfide will be oxidized byChr. vinosum [see (a)]. In the dark, sulfide accumulates. On illumination, the greater part of the accumulated sulfide will be oxidized byChr. weissei [see (c)]. A changed light-dark regimen should then have the effect as observed [see (b)]. These observations suggest that intermittant illumination may, at least in part explain the observed coexistence of both types of purple sulfur bacteria in nature.