True marine and halophilic anoxygenic phototrophic bacteria

Anoxygenic phototrophic bacteria are widely distributed in marine sediments and shallow waters of the coastal zone, where they often form intensely colored mass developments. The phototrophic bacteria have adapted to the whole spectrum of salt concentrations, from freshwater to saturated brines, and it is apparent that individual species have adapted well to particular habitats and mineral salts compositions, both qualitatively and quantitatively. This adaptation is reflected not only in the demand for defined ranges of salt concentrations, but also in the phylogenetic relationships of these bacteria, as established by 16S rDNA sequences. Major phylogenetic branches of purple sulfur bacteria are represented by: (1) marine and extremely halophilic Ectothiorhodospiraceae, (2) truly marine and halophilic Chromatiaceae and (3) freshwater Chromatiaceae, some of which are tolerant to low salt concentrations and are successful competitors in brackish and marine habitats. Quite similarly, salt-dependent green sulfur bacteria form distinct phylogenetic lines. In addition, also among the phototrophic alpha-Proteobacteria (purple nonsulfur bacteria), distinct phylogenetic lines of salt-dependent species are recognized. Available data give rise to the assumption that salt concentrations of natural habitats are an important selective factor that determines the development of a selected range of phototrophic bacteria in an exclusive way. As a consequence, the salt responses of these bacteria are reflected in their phylogenetic relationships.     

Na+-translocating NADH-quinone reductase of marine and halophilic bacteria

The respiratory chain of marine and moderately halophilic bacteria requires Na⁺ for maximum activity, and the site of Na⁺-dependent activation is located in the NADH-quinone reductase segment. The Na⁺-dependent NADH-quinone reductase purified from marine bacteriumVibrio alginolyticus is composed of three subunits, , , and , with apparentM _r of 52, 46, and 32kDa, respectively. The FAD-containing -subunit reacts with NADH and reduces ubiquinone-1 (Q-1) by a one-electron transfer pathway to produce ubisemiquinones. In the presence of the FMN-containing -subunit and the -subunit, Q-1 is converted to ubiquinol-1 without the accumulation of free radicals. The reaction catalyzed by the -subunit is strictly dependent on Na⁺ and is strongly inhibited by 2-n-heptyl-4-hydroxyquinoline N-oxide (HQNO), which is tightly coupled to the electrogenic extrusion of Na⁺. A similar type of Na⁺-translocating NADH-quinone reductase is widely distributed among marine and moderately halophilic bacteria. The respiratory chain ofV. alginolyticus contains another NADH-quinone reductase which is Na⁺ independent and has no energy-transducing capacity. These two types of NADH-quinone reductase are quite different with respect to their mode of quinone reduction and their sensitivity toward NADH preincubation.     

Denitrification by extremely halophilic bacteria

Abstract Extremely halophilic bacteria were isolated from widely separated sites by anaerobic enrichment in the presence of nitrate. The anaerobic growth of several of these isolates was accompanied by the production of nitrite, nitrous oxide, and dinitrogen. These results are a direct confirmation of the existence of extremely halophilic denitrifying bacteria, and suggest that such bacteria may be common inhabitants of hypersaline environments.     

Community analysis and metabolic pathway of halophilic bacteria for phenol degradation in saline environment

A moderately halophilic bacterial enrichment was able to degrade 120 mg/L of phenol in the presence of 1–2 M of NaCl within 3 d or 2.5–3 M of NaCl within 6 d. The optimal degradation was achieved at 1.5 M of NaCl and 350 mg/L of phenol. PCR-DGGE profile of the enrichment showed that the Acidobacterium sp. and Chloroflexus sp. dominated the community. The phenol-biodegradation pathways consisted of an initial oxidative attack by phenol hydroxylase, and subsequent ring fission by catechol 1,2-dioxygenase and catechol 2,3-dioxygenase. Nuclear magnetic resonance (NMR) spectroscopy profiles showed that ectoine and hydroxyectoine were the main compatible solutes to adjust the bacterial osmotic pressure. This study provides further information on the understanding of phenol-degradation over a wide range of salinity and remediation of phenol as a pollutant in the environment.     

Polyhydroxybutyrate production in halophilic marine bacteria Vibrio proteolyticus isolated from the Korean peninsula

Polyhydroxybutyrates (PHB) are biodegradable polymers that are produced by various microbes, including Ralstonia, Pseudomonas, and Bacillus species. In this study, a Vibrio proteolyticus strain, which produces a high level of polyhydroxyalkanoate (PHA), was isolated from the Korean marine environment. To determine optimal growth and production conditions, environments with different salinity, carbon sources, and nitrogen sources were evaluated. We found that the use of a medium containing 2% (w/v) fructose, 0.3% (w/v) yeast extract, and 5% (w/v) sodium chloride (NaCl) in M9 minimal medium resulted in high PHA content (54.7%) and biomass (4.94 g/L) over 48 h. Addition of propionate resulted in the production of poly(3-hydroxybutyrate-co-3-hydroxyvalerate) (P(HB-co-HV)) copolymer as propionate acts as a precursor for the HV unit. In these conditions, the bacteria produced poly(3-hydroxybutyrate-co-3-hydroxyvalerate) containing a 15.8% 3HV fraction with 0.3% propionate added as the substrate. To examine the possibility of using unsterilized media with high NaCl content for PHB production, V. proteolyticus was cultured in sterilized and unsterilized conditions. Our results indicated a higher growth, leading to a dominant population in unsterilized conditions and higher PHB production. This study showed the conditions for halophilic PHA producers to be later implemented at a larger scale.

     

海洋环境异养硝化-好氧反硝化菌的研究进展

异养硝化-好氧反硝化（heterotrophic nitrifying-aerobic denitrification,HN-AD）菌的发现打破了传统的脱氮理论,可以在有氧条件下同时进行硝化和反硝化,成为近年来的研究热点。HN-AD细菌在海洋氮循环中发挥着重要作用。本文对海洋环境中HN-AD菌的多样性和部分已知氮代谢途径及相关酶系进行了介绍,分析了盐度、碳氮比、溶解氧、pH等环境因素对HN-AD菌脱氮效果的影响,对其工艺和技术应用、前景和发展方向进行了综述和展望。     

Biocalcification using B. pasteurii for strengthening brick masonry civil engineering structures

Microbiologically induced calcite precipitation in bricks by bacterium Bacillus pasteurii (NCIM 2477) using a media especially optimized for urease production (OptU) was demonstrated in this study. Effect of biocalcification activity on compressive strength and water absorption capacity of bricks was investigated. Various other parameters such as pH, growth profile, urease activity, urea breakdown and calcite precipitated were monitored during the 28 days curing period. Efficiency of B. pasteurii to form microbial aided calcite precipitate in OptU media resulted into 83.9 % increase in strength of the bricks as compared to only 24.9 % with standard media, nutrient broth (NB). In addition to significant increase in the compressive strength, bricks treated with B. pasteurii grown in OptU media resulted in 48.9 % reduction in water absorption capacity as compared to control bricks immersed in tap water. Thus it was successfully demonstrated that microbial calcification in optimized media by Bacillus pasteurii has good potential for commercial application to improve the life span of structures constructed with bricks, particularly structures of heritage importance.     

不同培养条件对海洋沉积环境细菌的选择性分离

海洋环境中存在着大量未被培养和利用的微生物资源。本研究对一份南海沉积物样品采用不同培养温度、盐度、pH、样品稀释倍数和营养浓度条件进行可培养细菌的多样性研究。经过16S rRNA基因序列分析,获得825株菌分属于5个门,8个纲,17个目,26个科,57个属。分离到最多的属级类群为芽胞杆菌属（Bacillus）。通过不同培养条件的分离实验发现,厚壁菌类群在4 °C~60 °C、0%~15%盐度、pH 5~8及不同的样品稀释倍数和营养浓度实验条件中均为优势培养类群,具有广泛的环境适应性,但2~200的样品稀释倍数可以大大减少分离培养基中厚壁菌的数量。放线菌类群在4 °C低温和0%NaCl添加条件下的可培养多样性较高,同时pH 6和寡营养培养基有助于分离获得稀有放线菌类群。另外,本研究发现新物种资源的获取几率分别在寡营养培养基、5%~10%较高盐度和60°C高温培养有所增加。分离获得的5个主要细菌门类分别为厚壁菌门（Firmicutes,86%）、放线菌门（Actinobacteria,13%）、变形菌门（Proteobacteria,1%）、拟杆菌门（Bacteroidetes）和异常球菌-栖热菌门（Deinococcus-Thermus）。本研究共分离得到29株潜在新种,分别属于芽胞杆菌纲（Bacilli）、放线菌纲（Actinobacteria）、酸微菌纲（Acidimicrobiia）、嗜热油菌纲（Thermoleophilia）、红色杆菌纲（Rubrobacteria）和异常球菌纲（Deinococci）。海洋环境微生物新类群、海洋放线菌稀有类群等微生物新资源的选择性分离培养提供了有效的方法和方案,为后期的深入开展打下良好的基础。     

Proteinase production by halophilic isolates from marine sediments

Twenty-one strains of spore-forming bacteria were isolated from marine sediments of the Tyrrhenian seaboard (Livorno, Italy) and identified asBacillus licheniformis by their morphological, physiological and biochemical characteristics. All strains were able to grow at 15% NaCl and on media prepared with 100% seawater. In these conditions 75% of the strains were able to produce a bacitracin-like antibiotic and 100% of the strains showed proteolytic activity. Particularly, all strains showed proteinase production with an activity optimum at pH 8.5 and 60°C. Three strains produced high levels of proteolytic activity only when cultured in the presence of seawater.     

Diversity of extremely halophilic bacteria

In this review, the history of the classification of the family Halobacteriaceae, the extremely halophilic aerobic Archaea, is reviewed with some emphasis on the recently described new genera Halobaculum, Halorubrum, Natrialba, Natronomonas, and "Haloterrigena." Speculation is made about the evolutionary relationship between members of the Halobacteriaceae and the extremely halophilic, anaerobic methanogens of the genera Methanohalobium and Methanohalophilus. Efforts to find missing links between the two groups are also reviewed. Received: January 22, 1998 / Accepted: February 16, 1998     

Isolation of an obligately chemolithoautotrophic,halophilic and aerobic hydrogen-oxidizing bacterium from marine environment

An obligately chemolithoautotrophic and aerobic hydrogen-oxidizing bacterium was isolated from seawater of the Shonan Coast, Kanagawa Pref., Japan. The isolate was a Gram-negative, comma-shaped rod cell measuring 0.2 to 0.5 by 1 to 2 m. The cells occurred singly and were motile by a polar flagellum. The deoxyribonucleic acid base composition of the isolate was 44.1 mol% guanine plus cytosine. The optimal temperature for autotrophic growth on H₂–O₂–CO₂ was around 37°C, and no growth was observed at 5° C or 45° C. The optimal pH for growth was around 6.5. NaCl was required for growth with an optimum of 0.5 M. Elemental sulfur, thiosulfate or tetrathionate was utilized, as well as molecular hydrogen, as the sole energy source. No heterotrophic growth was observed on organic media tested. To our knowledge, this is the first report of the isolation of a marine, aerobic hydrogen-oxidizing bacterium, and of an obligately chemolithoautotrophic, mesophilic and aerobic hydrogen-oxidizing bacterium.     

Precipitation of minerals by 22 species of moderately halophilic bacteria in artificial marine salts media: Influence of salt concentration

Precipitation of minerals was shown by 22 species of moderately halophilic bacteria in both solid and liquid artificial marine salts media at different concentration and different Mg2+-to-Ca2+ ratio. Precipitation of minerals was observed for all the bacteria used. When salt concentration increased, the quantity and the size of bioliths decreased, the time required for precipitation being increased. The precipitated minerals were calcite, magnesian calcite, aragonite, dolomite, monohydrocalcite, hydromagnesite and struvite in variable proportions, depending on the bacterial species, the salinity and the physical state of the medium; the Mg content of the magnesian calcite also varied according to the same parameters. The precipitated minerals do not correspond exactly to those which could be precipitated inorganically according to the saturation indices. Scanning electron microscopy showed that the formation of the bioliths is initiated by grouping of calcified cells and that the dominant final morphologies were spherulitic with fibrous radiated interiors. It was demonstrated that moderately halophilic bacteria play an active role in the precipitation of carbonates and we hypothesize about this process of biomineralization.     

Biodegradation of organic pollutants by halophilic bacteria and archaea

Hypersaline environments are important for both surface extension and ecological significance. As all other ecosystems, they are impacted by pollution. However, little information is available on the biodegradation of organic pollutants by halophilic microorganisms in such environments. In addition, it is estimated that 5% of industrial effluents are saline and hypersaline. Conventional nonextremophilic microorganisms are unable to efficiently perform the removal of organic pollutants at high salt concentrations. Halophilic microorganisms are metabolically different and are adapted to extreme salinity; these microorganisms are good candidates for the bioremediation of hypersaline environments and treatment of saline effluents. This literature survey indicates that both the moderately halophilic bacteria and the extremely halophilic archaea have a broader catabolic versatility and capability than previously thought. A diversity of contaminating compounds is susceptible to be degraded by halotolerant and halophile bacteria. Nevertheless, significant research efforts are still necessary in order to estimate the true potential of these microorganisms to be applied in environmental processes and in the remediation of contaminated hypersaline ecosystems. This effort should be also focused on basic research to understand the overall degradation mechanism, to identify the enzymes involved in the degradation process and the metabolism regulation.     

Biomineralization of carbonate and phosphate by moderately halophilic bacteria

We investigated the precipitation of carbonate and phosphate minerals by 19 species of moderately halophilic bacteria using media with variable Mg(2+)/Ca(2+) ratios. The precipitated minerals were calcite, magnesium (Mg) calcite, and struvite (MgNH(4)PO(4) x 6H(2)O) in variable proportions depending on the Mg(2+)/Ca(2+) ratio of the medium. The Mg content of the Mg-calcite decreased with increasing Ca(2+) concentration in the medium. According to the saturation indices, other minerals could also have precipitated. We observed important differences between the morphology of carbonate and phosphate, which may help us to recognize these minerals in natural systems. We studied the growth and pH curves of four bacteria in media specific for carbonate and struvite precipitation. We consider the biomineralization processes that produce carbonate and phosphate minerals, and propose a hypothesis for the lack of struvite in natural environments and ancient rocks.     

Isolation and characterization of surfactant degrading bacteria in a marine environment

Abstract Sea water and sediment samples taken near the coasts of Hyeres bay (France) were used for anionic surfactant titrations with surface and bottom waters and the finest part of sediments. The capacity for surfactant degradation by the 'in situ' microflora was evaluated. By using a selective plating technique 26 strains able to utilize anionic surfactant were isolated from the selected bacterial communities. Their ability to degrade anionic surfactant was verified according to the biodegradation standard method. Isolated strains were characterized by morphological and physiological properties using API 20 NE micro-method. All tested strains were Gram negative, strictly aerobic, rod or helical shaped. Their weak utilization of phenolic substrates suggests that they degrade preferentially the alkyl chain of the surfactant molecule. Biodegradation was more efficient with bacterial communities rather than with any isolated strains. Such observations indicate that complete mineralization involves several other so far non-isolated strains which complete the degradation initiated by the isolated strains.