微生物高盐渗透适应策略及其耐盐强化研究进展

高盐废水因具有硬度高、可生化性差、水质成分复杂等特点,是较难处理的工业废水之一。现有物化处理技术存在运行成本高、处理效率低、二次污染重等诸多瓶颈。耐盐/嗜盐微生物可在高盐环境下进行正常生理代谢,因此,开发经济、高效、可靠的高盐废水生物处理技术有望成为高盐废水处理的主流方向之一。本文系统综述了耐盐/嗜盐微生物盐溶、胞内小分子相容溶质积累、蛋白质稳定和细胞表面稳定等高渗透压适应策略。由于嗜盐微生物存在生长条件苛刻、功能微生物种类稀缺等问题,因此,耐盐微生物在高盐废水处理的未来应用空间更大。最新研究发现强化调控技术(电、光、磁)可提升微生物的高渗透压适应能力,其中电调控技术或是未来高盐废水生物处理的重点研究方向。     

嗜盐耐盐微生物抗盐胁迫相关离子转运蛋白研究进展

离子转运蛋白在维持细胞内pH稳态、离子动态平衡等方面发挥着重要作用。钠离子转运体和钾离子转运体在嗜盐耐盐微生物中广泛存在,其"保钾排钠"机制是微生物抗盐胁迫的两大策略之一。近年来,嗜盐耐盐微生物中许多新型钠、钾离子转运体被陆续发现,如RDD蛋白、UPF0118蛋白、DUF蛋白和KimA蛋白等;Fe³⁺、Mg²⁺等其他金属离子的转运蛋白也被证实可通过影响微生物胞内相容性溶质的合成起到渗透调节的作用。本文综述了嗜盐耐盐微生物中抗盐胁迫相关的各类离子转运蛋白,分析其分子结构和工作机理,并对这些蛋白在农业方面的应用进行了展望。继续发现新的离子转运蛋白,探究抗盐胁迫相关离子转运蛋白的结构和机理,解析各转运系统的协同作用及分子调控机制,将进一步加深对嗜盐耐盐微生物抗盐胁迫调控的认识,并为盐碱地农作物的改良等提供新的思路。     

宏基因组学应用于耐盐酶类及耐盐基因研究的进展

耐盐酶在高盐浓度下仍具备催化活性和稳定性,在高盐食品和海产品加工、洗涤及其它高盐环境生物技术领域被广泛应用;耐盐基因在高盐条件下可以使微生物维持正常功能,获取并研究不同环境中的耐盐基因对揭示微生物的耐盐机制,以及实现其在高盐环境中的定向应用具有的重要意义。宏基因组学避开纯培养技术探知微生物的多样性及其功能,为我们提供了一种发现新基因、开发新的微生物活性物质和研究微生物群落结构及其功能的新技术。文中结合本课题组的研究工作,综述了利用宏基因组学获取耐盐酶类及耐盐基因的策略,同时着重介绍利用宏基因组学从海洋、土壤、胃肠道等环境中获取耐盐酶类及耐盐基因的研究。     

嗜盐微生物在环境修复中的研究进展

人类活动产生的污染物,使一些天然盐环境遭受不同程度的污染,或者使环境受到污染物与高盐的双重污染。在高盐条件下,非嗜盐微生物的代谢会受到抑制,其生物修复效率明显降低,甚至丧失修复能力。嗜盐微生物则能够在高盐环境中栖息繁殖,凸显其修复被污染高盐环境的生物学效率和广阔的应用前景。就嗜盐微生物降解石油烃、芳香烃衍生物和有机磷等污染物的研究进展进行了综述和讨论。     

中度嗜盐菌的研究进展

地球上存在着多种多样的盐域环境,这类环境中有自然形成的,如死海,美国的大盐湖等水环境,还有盐土环境;人工形成的如盐场、盐池等;另外,还有很多盐腌制的食品。自然界的高盐环境由于形成过程和所处地质情况的不同其离子组成和盐浓度有很大差异。生活在这些高盐环境中的动、植物物种较为有限,而以处于不同类群的微生物,如绿藻、嗜盐古菌及嗜盐和耐盐的细菌等为主要生命形式。根据微生物对盐浓度的反应可分为不同的种(如表1[1])。     

嗜盐微生物的工业应用研究及进展

嗜盐微生物是一类生长于高盐环境的微生物,在新型生物化工产业及生物修复领域具有突出的应用潜力。本文简要介绍了嗜盐微生物的种类、生理特性,着重阐述了嗜盐微生物产生的活性物质在工业生产上的应用价值和开发前景,总结了近年来国内外在嗜盐微生物工业应用上的研究进展,对嗜盐微生物的应用研究做了概括。     

微生物嗜盐酶盐适应性的分子结构基础研究

由高盐环境中生长的微生物里分离出的嗜盐酶在高盐度下仍然具有催化活性,工业上具有良好的应用前景。一些嗜盐酶已被克隆纯化出来,它们的分子结构特点也已经被广泛研究。该文从嗜盐酶的蛋白质序列和结构特征等方面综述了嗜盐酶嗜盐的分子结构基础研究进展,分析了存在的问题并对未来工作提出了展望。研究嗜盐酶盐适应性的分子基础,可以为新的功能蛋白的发展和鉴定提供依据。     

嗜盐微生物

高盐环境通常是指那些盐浓度高于海水的环境．在这些环境中能够生存的微生物可划分为三类：一“类是能耐受一定浓度的盐溶液,但在无盐存在条件下生长最好的菌称为耐盐菌．第二类是一定浓度的盐为菌体生长所必需,且在一定浓度的盐溶液中生长最好,称为嗜盐菌．在盐浓度从零至饱和的盐溶液中均能生长,在一定浓度的盐溶液中生长最好的特殊类群称为多能盐生苗。依据嗜盐浓度的不同,嗜盐菌又可分为轻度嗜盐菌（最适盐浓度0．2—0．smol／L）、中度嗜盐菌（最适盐浓度0．5—2．omol／L）和极端嗜盐菌（最适盐浓度＞3mol／U,其中部分极端嗜…     

微生物嗜盐酶的研究进展

嗜盐酶一般来自于嗜盐菌,它的主要特点是严格依赖体系中一定的盐离子浓度,可以在高盐环境中维持其结构稳定,并且能够抵抗高温、p H和有机溶剂存在下的变性,因此在高盐、水/有机和非水介质环境的催化中具有重要的应用价值。本综述从盐对嗜盐酶活性和稳定性的影响、金属离子和有机溶剂对嗜盐酶的影响几个方面介绍了嗜盐酶的特点。在总结蛋白质数据库(PDB)中已有嗜盐酶的结构和特点的基础上,对嗜盐酶的嗜盐机制进行了分析,认为嗜盐酶不同于非嗜盐酶的特点在于盐桥和氢键明显增多,含有一些特殊的盐离子结合位点并且常以低聚体的形式存在,表面酸性氨基酸含量明显增多。最后对嗜盐酶的分子改造和应用进行了简要的介绍。     

嗜盐古菌分类学研究进展

嗜盐古菌是一类需要高盐维持生长的古菌。到目前为止,已发现的嗜盐古菌都属于古菌域的广古菌门,主要包括:嗜盐甲烷古菌类群、嗜盐古菌纲的全部成员以及尚不能培养的纳米嗜盐古菌类群。嗜盐古菌是盐环境的土著类群,驱动着盐环境生态系统的生物地球化学循环。作为极端微生物,嗜盐古菌在理论研究和应用领域具有重要的研究价值。本文从嗜盐古菌分类学地位的变迁、分类学方法、分类学研究现状及我国的嗜盐古菌分类学研究等方面综述了嗜盐古菌分类学的最新研究进展。     

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.     

Formation and breakdown of glycine betaine and trimethylamine in hypersaline environments

Glycine betaine is accumulated as a compatible solute in many photosynthetic and non-photosynthetic bacteria — the last being unable to synthesize the compound - and thus large pools of betaine can be expected to be present in hypersaline environments. A variety of aerobic and anaerobic microorganisms degrade betaine to among other products trimethylamine and methylamine, in a number of different pathways. Curiously, very few of these betaine breakdown processes have yet been identified in hypersaline environments. Trimethylamine can also be formed by bacterial reduction of trimethylamine N-oxide (also by extremely halophilic archaeobacteria). Degradation of trimethylamine in hypersaline environments by halophilic methanogenic bacteria is relatively well documented, and leads to the formation of methane, carbon dioxide and ammonia.     

Porphyromonas gingivalis: an invasive and evasive opportunistic oral pathogen

Archaea that live at high salt concentrations are a phylogenetically diverse group of microorganisms. They include the heterotrophic haloarchaea (class Halobacteria) and some methanogenic Archaea, and they inhabit both oxic and anoxic environments. In spite of their common hypersaline environment, halophilic archaea are surprisingly diverse in their nutritional demands, range of carbon sources degraded (including hydrocarbons and aromatic compounds) and metabolic pathways. The recent discovery of a new group of extremely halophilic Euryarchaeota, the yet uncultured Nanohaloarchaea, shows that the archaeal diversity and metabolic variability in hypersaline environments is higher than hitherto estimated.     

Phylogeny and ecophysiological features of prokaryotes isolated from temporary saline tidal pools

Although hypersaline environments have been extensively examined, only a limited number of microbial community studies have been performed in saline tide pools. We have studied a temporary salt-saturated tide pool and isolated prokaryotes from the water. Chlorinity measurements revealed that the tide pool brine could be characterized as one of the most hypersaline ecosystems on earth. Enumeration of microorganisms at different salinities showed that the tide pool was dominated by moderate halophiles. Based on 16S rRNA gene sequence analysis, the prokaryotic strains isolated were related to the bacterial genera Rhodovibrio, Halovibrio, Aquisalimonas, Bacillus and Staphylococcus and to the haloarchaeal species Haloferax alexandrinus. Four bacterial isolates were distantly related to their closest validly described species Aquisalimonas asiatica (96.5 % similarity), representing a novel phylogenetic linkage. Ecophysiological analysis also revealed distinct phenotypic profiles for the prokaryotic strains analyzed. The herbicide 2,4-dichlorophenoxyacetate could be effectively utilized by selected strains as the sole carbon source, but phenolic compounds could not be utilized by any of the halophilic isolates examined. None of the halophilic strains were able to grow without the presence of sea salt or seawater. Based on these results, we conclude that moderate halophilic bacteria rather than extremely halophilic archaea dominate in such a hypersaline environment.     

安徽定远盐矿可培养嗜盐微生物多样性

【背景】嗜盐微生物多生活于高盐环境,具有独特的生理代谢特征,是一类重要的极端环境微生物资源。【目的】为更好地认识我国陆相盐矿的嗜盐微生物多样性组成,更好地开发利用嗜盐微生物资源积累丰富的微生物菌种。【方法】对安徽定远盐矿盐芯样品进行嗜盐微生物的纯培养分离,并对所分离菌株进行基于16SrRNA基因的测序和序列相似性分析,并对所分离菌株进行物种多样性分析。在此基础上,对代表菌株进行菌落形态和耐盐度及酶活测定。【结果】通过纯培养共分离获得了嗜盐微生物264株,其中嗜盐古菌150株,占56.8%;嗜盐细菌114株,占43.2%。嗜盐古菌物种分别来自于Halorubrum、 Halopenitus、 Haloterrigena、 Natrinema、 Natronoarchaeum和Natronomonas等6个属;嗜盐细菌物种分别来自于Pseudomonas、Aliifodinibius、Halobacillus、Halomonas和Halospina等5个属。通过代表菌株的酶活平板检测,发现产胞外蛋白酶菌株1株,酯酶1株,淀粉酶2株;能液化明胶菌株2株。在物种多样性组成方面,发现嗜盐古菌的物种多样性指数高于嗜盐细菌。【结论】本研究对我国安徽定远陆相盐矿的可培养嗜盐微生物多样性进行探究,积累了丰富的嗜盐微生物菌株资源。     

The ecology and taxonomy of aerobic chemoorganotrophic halophilic eubacteria

Abstract There exists a wide diversity of halophilic eubacteria with chemoorganotrophic-aerobic metabolism. Most of them have a more moderate salt response than halophilic archaebacteria, falling into the category of moderately halophilic bacteria. Although mostly isolated from salted food, their natural habitats are hypersaline waters of intermediate levels of salt concentration, and hypersaline soils. In hypersaline waters, the taxonomic groups found are the ones that also predominate in ocean waters, such as representatives of the genera Vibrio, Pseudomonas and Flavobacterium . However, in hypersaline soils, the taxonomic groups present are those typical of normal soils, such as Pseudomonas, Bacillus and Gram-positive cocci. The halophilic bacteria from soils are also more resistant to exposure to low salt concentrations than the organisms isolated from waters. Therefore, it seems that the general characteristics of the hypersaline environments drastically affect the types of halophilic bacteria present, and that the halophilic character has arisen in many phylogenetic groups of eubacteria.     

Evolution of bacterial flora from a subterranean saline well by graduated salinity changes in enrichment media

The bacterial flora of samples taken from a subterranean saline well was enriched (1) by periodic salinity increase and (2) by periodic salinity decrease, both at 25° and 35°C. During the enrichment process, bacterial flora, including halotolerant, marine, moderately and extremely halophilic bacteria, were enumerated. Results were similar at both temperatures. Marine bacteria and moderately halophilic microorganisms were the most favoured groups, predominating between 3 and 30% (w/v) salt content; extremely halophilic bacteria also appeared when salinity reached 30% (w/v) and halotolerant bacteria were poorly represented. The taxonomic distribution of 125 selected strains, chosen at random from counting media, was essentially similar to those from other hypersaline environments.     

The bioenergetic basis for the decrease in metabolic diversity at increasing salt concentrations: implications for the functioning of salt lake ecosystems

Examination of the microbial diversity in hypersaline lakes of increasing salt concentrations shows that certain types of dissimilatory metabolism do not occur at the highest salinities. Examples are methanogenesis from hydrogen and carbon dioxide or from acetate, dissimilatory sulfate reduction with oxidation of acetate, and autotrophic nitrification. The observations can be explained on the basis of the energetic cost of haloadaptation used by the different metabolic groups and the free-energy change associated with the dissimilatory reactions. All halophilic microorganisms spend large amounts of energy to maintain steep gradients of Na⁺ and K⁺concentrations across their cytoplasmic membrane. Most Bacteria and also the methanogenic Archaea produce high intracellular concentrations of organic osmotic solutes at a high energetic cost. The halophilic aerobic Archaea (order Halobacteriales) and the halophilic fermentative Bacteria (order Halanaerobiales) use KCl as the main intracellular solute. This strategy, while requiring far-reaching adaptations of the intracellular machinery, is energetically more favorable than production of organic compatible solutes. By combining information on the amount of energy available to each physiological group and the strategy used to cope with salt stress, a coherent model emerges that provides explanations for the upper salinity limit at which the different microbial conversions occur in hypersaline lakes.     

Phenol degradation by halophilic bacteria isolated from hypersaline environments

Phenol is a toxic aromatic compound used or produced in many industries and as a result a common component of industrial wastewaters. Phenol containing waste streams are frequently hypersaline and therefore require halophilic microorganisms for efficient biotreatment without dilution. In this study three halophilic bacteria isolated from different saline environments and identified as Halomonas organivorans, Arhodomonas aquaeolei and Modicisalibacter tunisiensis were shown to be able to grow on phenol in hypersaline media containing 100 g/L of total salts at a concentration of 3 mM (280 mg/L), well above the concentration found in most waste streams. Genes encoding the aromatic dioxygenase enzymes catechol 1,2 dioxygenase and protocatechuate 3,4-dioxygenase were present in all strains as determined by PCR amplification using primers specific for highly conserved regions of the genes. The gene for protocatechuate 3,4-dioxygenase was cloned from the isolated H. organivorans and the translated protein was evaluated by comparative protein sequence analysis with protocatechuate 3,4-dioxygenase proteins from other microorganisms. Although the analysis revealed a wide range of sequence divergence among the protocatechuate 3,4-dioxygenase family, all of the conserved domain amino acid structures identified for this enzyme family are identical or conservatively substituted in the H. organivorans enzyme.