海洋氮循环中细菌的厌氧氨氧化

细菌厌氧氨氧化过程是在一类特殊细菌的厌氧氨氧化体内完成的以氨作为电子供体硝酸盐作为电子受体的一种新型脱氮反应.厌氧氨氧化菌的发现,改变人们对传统氮的生物地球化学循环的认识:反硝化细菌并不是大气中氮气产生的唯一生物类群.而且越来越多的证据表明,细菌厌氧氨氧化与全球的氮物质循环密切相关,估计海洋细菌的厌氧氨氧化过程占到全球海洋氮气产生的一半左右.由于氮与碳的循环密切相关,因此可以推测,细菌的厌氧氨氧化会影响大气中的二氧化碳浓度,从而对全球气候变化产生重要影响.另外,由于细菌厌氧氨氧化菌实现了氨氮的短程转化,缩短了氮素的转化过程,因此为开发更节约能源、更符合可持续发展要求的废水脱氮新技术提供了生物学基础.     

厌氧氨氧化细菌及其群落内细菌互作关系研究进展

厌氧氨氧化细菌具有的厌氧氨氧化反应是在厌氧条件下将氨氮和亚硝氮或一氧化氮转化为硝氮、生成氮气的过程,因其能够高效低能地处理低碳氮比废水而广受关注。目前,厌氧氨氧化细菌仍未实现纯培养,借助宏组学手段研究厌氧氨氧化细菌及其群落内细菌之间的互作关系是近年来的研究趋势。本文介绍了厌氧氨氧化细菌的种类和特性,综述了厌氧氨氧化细菌的代谢多样性及其群落内细菌间的物质协同利用和信息交流方式,这对厌氧氨氧化群落的稳定具有重要影响,最后对值得进一步深入研究的问题做了总结和展望,以期为后续深入研究细菌间的互作关系提供参考,进而为构建稳定高效的厌氧氨氧化脱氮体系提供思路。     

海洋厌氧氨氧化细菌分子生态学研究进展

厌氧氨氧化细菌是能在厌氧的条件下将氨氧化为氮气的一类细菌,这类细菌执行着以前未被人们所认知的一个独特的过程--氧氨氧化过程,据估计厌氧氨氧化过程对于海洋氮气的形成有30%～50%的贡献率;海洋厌氧氨氧化细菌能与氨氧化细菌及氨氧化古菌存在潜在的耦合作用,对于海洋氮循环复杂机制的阐述有着非常重要的意义;同时海洋厌氧氨氧化细菌独特的细胞和基因组结构,也成为了解海洋细菌进化重要的模式微生物之一.本文综述了近年来国内外厌氧氨氧化细菌分子生态学方面的进展,并结合作者的工作对未来的研究进行展望.     

基于数据库分析不同类型生境中厌氧氨氧化细菌的多样性分布特征

【目的】厌氧氨氧化过程是一种能在厌氧条件下氧化NH4+同时还原NO2–或者NO3–生成N2的过程,是氮素循环过程的重要途径之一。厌氧氨氧化过程由厌氧氨氧化细菌催化完成,目前通过分子生物学的手段已证实了厌氧氨氧化细菌存在于多种类型的生境中,本文对厌氧氨氧化细菌在不同类型生境中的多样性分布规律进行了系统分析。【方法】基于NCBI数据库中厌氧氨氧化细菌的16SrRNA基因序列,利用Mothur分析平台系统分析了厌氧氨氧化细菌在不同生境中的多样性分布规律和特征。【结果】分析表明,海洋环境中Ca. Scalindua属的厌氧氨氧化细菌占绝对主导;淡水和农业土壤中Ca. Brocadia属的厌氧氨氧化细菌占优势;工程系统中普遍存在Ca. Brocadia和Ca. Kuenenia属的厌氧氨氧化细菌;而湿地和河口环境中厌氧氨氧化细菌多样性最高,Ca. Scalindua、Ca. Brocadia和Ca. Kuenenia属的厌氧氨氧化细菌均有较高的相对丰度,显示出了陆地与海洋交汇的显著特征。【结论】本研究系统展示了不同的生境中厌氧氨氧化细菌的多样性群落结构生境分布特征,表明环境特征差异直接影响了厌氧氨氧化细菌的种群分布和系统演化。     

厌氧氨氧化在污水处理中的研究进展

厌氧氨氧化(ANAMMOX)是指厌氧氨氧化细菌在厌氧条件下以亚硝酸盐为电子受体将氨氮氧化为氮气的过程。由于在节能降耗和环境友好上的独特优点,基于厌氧氨氧化原理的脱氮技术被公认是目前最具应用前景的生物脱氮技术,因此自发现以来一直是国内外研究的热点。综述近年有关厌氧氨氧化细菌、厌氧氨氧化机理、反应的影响因素及其在污水处理应用方面的研究进展,并展望厌氧氨氧化在污水处理领域的发展方向。     

厌氧氨氧化菌驱动脱氮途径的研究进展

厌氧氨氧化菌(anaerobic ammonia-oxidizing bacteria, AnAOB)的代谢多样性,使得该菌群能够在海洋、湿地和陆地等不同的自然生态系统中广泛分布,甚至在一些极热和极寒环境中也检测到了该菌群的存在。本文回顾并总结了厌氧氨氧化菌在不同生态系统中的发现、分布及脱氮贡献等方面的研究,分析了厌氧氨氧化菌分布的主要环境影响因素。该综述将帮助我们更好地理解全球氮循环中厌氧氨氧化菌的实际角色和功能,并基于厌氧氨氧化(anaerobicammoniaoxidation,anammox)过程,探究能与其进行协作的新型生物脱氮工艺,以期为这些工艺的研发和推广提供生态学基础和新的思考,从而实现脱氮工艺的技术变革。     

厌氧氨氧化菌的中心代谢研究进展

摘要: 厌氧氨氧化是以NH +4为电子供体,以NO－2为电子受体产生N2的生物反应。厌氧氨氧化菌是厌氧氨氧化过程的执行者,在废水生物脱氮和地球氮素循环中扮演着重要角色。研究厌氧氨氧化菌的代谢特性,将有助于理解厌氧氨氧化过程,开发厌氧氨氧化工艺。厌氧氨氧化菌是化能自养型细菌,以CO2或HCO－3为碳源,并通过偶联NH+4氧化和NO －2还原的生物反应获得能量。在NH+4/NO－2的生物氧化还原反应过程中,检出了中间产物N2H4,但未检出其他中间产物(如NH2OH、NO)。此外,由基因组信息推断,厌氧氨氧化菌     

湖泊氮素氧化及脱氮过程研究进展

自然界中氮的生物地球化学循环主要由微生物驱动,由固氮作用、硝化作用、反硝化作用和氨化作用来完成。过去数十年间,随着异养硝化、厌氧氨氧化和古菌氨氧化作用的发现,人们对环境中氮素循环认识逐步深入,提出了多种脱氮途径新假说。对湖泊生态系统中氮素的输入、输出及其在水体、沉积物和水土界面的迁移转化过程进行了概括,对湖泊生态系统中反硝化和厌氧氨氧化脱氮机理及脱氮效率的最新研究进展进行了探讨,并对以后的氮素循环研究进行了展望。     

高通量测序分析多种典型生境中厌氧氨氧化细菌的多样性分布特征

【背景】厌氧氨氧化过程是氮素循环过程的重要途径之一,在氮素循环中发挥重要作用。先前的研究已经证实了厌氧氨氧化细菌存在于多种生境中,但对其多样性分布还没有系统的研究。【目的】对厌氧氨氧化细菌在不同类型生境中的多样性分布规律进行深入分析,充分展示其在不同生境中的群落结构特点,并揭示多样性分布与环境因素之间的关系。【方法】在建立厌氧氨氧化细菌16S rRNA基因序列数据库的基础上,运用高通量测序技术分析其在不同生境中的多样性分布特征。【结果】厌氧氨氧化细菌在红树林、海湾和河口生境中的多样性水平较高,而污泥和红壤的多样性水平明显较低。系统发育分析表明,这些生境中的厌氧氨氧化细菌主要由Candidatus Brocadia、Ca.Scalindua和未明确分类地位的菌属组成;从河流到红树林生态系统,随着盐度的增加,厌氧氨氧化细菌的优势种属由Ca. Brocadia转变到Ca. Scalindua,相关性分析也表明了盐度是导致不同生境中厌氧氨氧化细菌群落结构差异的主要因素。【结论】不同生境中存在不同的厌氧氨氧化细菌种群结构,环境条件的差异影响了厌氧氨氧化细菌的种群分布和系统演化。     

厌氧氨氧化菌脱氮机理及其在污水处理中的应用

厌氧氨氧化细菌(anammox)可以将亚硝酸盐和氨氮转化为氮气从而缩短氨氮转化的过程,它已经成为新型生物污水脱氮技术研究的热点之一。当前,有关厌氧氨氧化菌特有的生理结构特点、种群分类及其功能酶等方面的研究取得了一定突破,为实现其工业应用奠定了良好的理论基础;同时分子生物学技术在厌氧氨氧化细菌种群分布、群落多样性及其共生关系等方面的应用也大大促进了污水生物脱氮技术的革新和进步。总结了厌氧氨氧化菌主要的生理生化特点、细胞结构特点、脱氮机理、污水处理体系中的应用以及分子生物学方法对污水处理体系中厌氧氨氧化菌种群分析的研究现状,并指出未来anammox细菌在生物特性及在污水脱氮处理实际应用的研究中的热点问题。生物特性方面的主要研究热点有：（1）anammox细菌除厌氧氨氧化作用外,其它新陈代谢途径有待探索;（2）anammox细菌在不同环境中分布的倾向性问题;（3）新型anammox细菌的确定。污水处理的实际应用方面的主要研究热点有：（1）anammox污泥的快速高效富集问题;（2）设计高特异性引物;（3）anammox细菌和其他微生物的共生关系。     

厌氧氨氧化菌火山口结构

厌氧氨氧化(anaerobic ammonium oxidation, anammox)是微生物学、地质学和环境学领域的重要反应,厌氧氨氧化菌(anaerobic ammonium-oxidizing bacteria, AnAOB)是厌氧氨氧化的驱动器,探明AnAOB的生物学性状对厌氧氨氧化的应用具有重要意义。火山口结构是AnAOB的标志性微观结构,也是AnAOB的重要识别特征。由于迄今没有获得AnAOB纯培养物,相关研究进展缓慢。本文对AnAOB及其所归属的浮霉状菌的火山口结构研究进展作了综述,探讨了火山口结构的形态特征、生理功能和生态意义,得出以下结论:(1) AnAOB的火山口结构均匀分布在细胞表面,其直径约5 nm;(2) AnAOB的火山口结构推测向外可连通细胞外膜和内膜,向内可与厌氧氨氧化体膜相连,对于物质转运及转化具有重要意义;(3)火山口结构具有遗传稳定性,其形成可能与鞭毛脱落相关;(4) AnAOB的火山口结构可能通过促进细胞物质交流、信息通讯等在维持其生态位稳定方面起作用。     

2014厌氧氨氧化专刊序言

厌氧氨氧化是环境微生物领域的重要发现,在废水生物脱氮和地球氮素循环中具有重大作用。为了反映近年来国内外厌氧氨氧化研究的一些重要进展,组织出版了"厌氧氨氧化专刊"。本期专刊包括综述和研究论文两部分,内容涉及厌氧氨氧化的菌群富集、菌群分析、菌种保藏、碳源影响、工艺应用、优化对策等。     

厌氧氨氧化体的组成、结构与功能

厌氧氨氧化(Anammox)是微生物和环境领域的研究热点之一。厌氧氨氧化菌(AnAOB)是Anammox的功能载体。不同于大部分原核微生物,AnAOB具有独特的细胞器——厌氧氨氧化体,它是进行Anammox代谢的场所。研究厌氧氨氧化体有助于探明厌氧氨氧化菌的代谢特性。本文综述了厌氧氨氧化体的组成、结构与功能,以期为从事Anammox研究的同行提供参考。     

Diversity of ammonium-oxidizing bacteria in a granular sludge anaerobic ammonium-oxidizing (anammox) reactor

The ammonium-oxidizing microbial community was investigated in a granular sludge anaerobic ammonium-oxidizing (anammox) reactor that was operated for about 1 year with high anaerobic ammonium oxidation activity (up to 0.8 kg NH(4)(+)-N m(-3) day(-1)). A Planctomycetales-specific 16S rRNA gene library was constructed to analyse the diversity of the anaerobic ammonium-oxidizing bacteria (AnAOB). Most of the specifically amplified sequences (15/16) were similar to each other (> 99%) but were distantly related to all of the previously recognized sequences (< 94%), with the exception of an unclassified anammox-related clone, KSU-1 (98%). An ammonia monooxygenase (amoA) gene library was also analysed to investigate the diversity of 'aerobic' ammonium-oxidizing bacteria (AAOB) from the beta-Proteobacteria. Most of the amoA gene fragments (53/55) clustered in the Nitrosomonas europaea-Nitrosococcus mobilis group which has been reported to prevail under oxygen-limiting conditions. The quantitative results from real-time polymerase chain reaction (PCR) amplification showed that the dominant AnAOB comprised approximately 50% of the total bacterial 16S rRNA genes in the reactor, whereas the AAOB of beta-Proteobacteria represented only about 3%. A large fragment (4008 bp) of the rRNA gene cluster of the dominant AnAOB (AS-1) in this reactor sludge was sequenced and compared with sequences of other Planctomycetales including four anammox-related candidate genera. The partial sequence of hydrazine-oxidizing enzyme (hzo) of dominant AnAOB was also identified using new designed primers. Based on this analysis, we propose to tentatively name this new AnAOB Candidatus'Jettenia asiatica'.     

保藏温度对厌氧氨氧化颗粒污泥特性的影响

为考察保藏温度对厌氧氨氧化污泥颗粒特性的影响,同时优化保藏厌氧氨氧化颗粒污泥温度参数,本试验首先通过HRT调控进水基质负荷培养厌氧氨氧化颗粒污泥,并采用KHCO3和Na HCO3交替提供无机碳源。然后分别在–40℃、4℃、(27±4)℃室温和35℃条件下避光保藏。结果表明,Na HCO3可代替KHCO3作为厌氧氨氧化菌生长的无机碳源。相比于其他保藏温度,4℃保藏能够较好地维持生物量和生物活性,同时能较好地维持颗粒污泥的沉降性能、颗粒污泥和细胞结构完整性。在保藏过程中,一阶衰减指数模型可拟合厌氧氨氧化颗粒污泥生物量及活性的衰减过程,衰减指数与胞溶程度正相关,而且生物量的衰减比活性的衰减更快。同时,颗粒污泥胞外聚合物中蛋白质与多糖的比值(PN/PS)和血红素不能有效指示保藏过程中颗粒污泥沉降性能和活性的变化,而生物活性与胞溶程度呈负相关。     

Sequentially aerated membrane biofilm reactors for autotrophic nitrogen removal: microbial community composition and dynamics

Membrane‐aerated biofilm reactors performing autotrophic nitrogen removal can be successfully applied to treat concentrated nitrogen streams. However, their process performance is seriously hampered by the growth of nitrite oxidizing bacteria (NOB). In this work we document how sequential aeration can bring the rapid and long‐term suppression of NOB and the onset of the activity of anaerobic ammonium oxidizing bacteria (AnAOB). Real‐time quantitative polymerase chain reaction analyses confirmed that such shift in performance was mirrored by a change in population densities, with a very drastic reduction of the NOB Nitrospira and Nitrobacter and a 10‐fold increase in AnAOB numbers. The study of biofilm sections with relevant 16S rRNA fluorescent probes revealed strongly stratified biofilm structures fostering aerobic ammonium oxidizing bacteria (AOB) in biofilm areas close to the membrane surface (rich in oxygen) and AnAOB in regions neighbouring the liquid phase. Both communities were separated by a transition region potentially populated by denitrifying heterotrophic bacteria. AOB and AnAOB bacterial groups were more abundant and diverse than NOB, and dominated by the r‐strategists Nitrosomonas europaea and Ca. Brocadia anammoxidans, respectively. Taken together, the present work presents tools to better engineer, monitor and control the microbial communities that support robust, sustainable and efficient nitrogen removal.     

Reactivation of aerobic and anaerobic ammonium oxidizers in OLAND biomass after long-term storage

The biomass of an oxygen-limited autotrophic nitrification/denitrification (OLAND) biofilm reactor was preserved in various ways to find a storage method for both aerobic and anaerobic ammonium-oxidizing bacteria (AerAOB and AnAOB). Storage occurred at −20°C with and without glycerol as cryoprotectant and at 4 and 20°C with and without nitrate as redox buffer. After 2 and 5 months, reactivation of AerAOB and AnAOB was achieved with the biomass stored at 4°C with and without nitrate and at 20°C with nitrate. Moreover, the presence of the AerAOB and AnAOB was confirmed with fluorescent in situ hybridization (FISH). Preservation in a nitrate environment resulted in a lag phase for the AnAOB reactivation. The supplied nitrate was denitrified during storage, and a real-time polymerase chain reaction with nitrifying and denitrifying genes allowed to estimate that at least 1.0 to 6.0% of the OLAND biofilm consisted of denitrifiers. It was concluded that reactivation after long-term storage is possible and that preservation at 4°C without nitrate addition is the recommended storage technique. The possibility to store OLAND biomass will facilitate research on AnAOB and can overcome larger-scale start-up and inhibition problems of novel nitrogen processes involving AnAOB.     

Vertical migration of aggregated aerobic and anaerobic ammonium oxidizers enhances oxygen uptake in a stagnant water layer

Ammonium can be removed as dinitrogen gas by cooperating aerobic and anaerobic ammonium-oxidizing bacteria (AerAOB and AnAOB). The goal of this study was to verify putative mutual benefits for aggregated AerAOB and AnAOB in a stagnant freshwater environment. In an ammonium fed water column, the biological oxygen consumption rate was, on average, 76 kg O₂ ha⁻¹ day⁻¹. As the oxygen transfer rate of an abiotic control column was only 17 kg O₂ ha⁻¹ day⁻¹, biomass activity enhanced the oxygen transfer. Increasing the AnAOB gas production increased the oxygen consumption rate with more than 50% as a result of enhanced vertical movement of the biomass. The coupled decrease in dissolved oxygen concentration increased the diffusional oxygen transfer from the atmosphere in the water. Physically preventing the biomass from rising to the upper water layer instantaneously decreased oxygen and ammonium consumption and even led to the occurrence of some sulfate reduction. Floating of the biomass was further confirmed to be beneficial, as this allowed for the development of a higher AerAOB and AnAOB activity, compared to settled biomass. Overall, the results support mutual benefits for aggregated AerAOB and AnAOB, derived from the biomass uplifting effect of AnAOB gas production.     

Characterization of an autotrophic nitrogen-removing biofilm from a highly loaded lab-scale rotating biological contactor

In this study, a lab-scale rotating biological contactor (RBC) treating a synthetic NH(4)(+) wastewater devoid of organic carbon and showing high N losses was examined for several important physiological and microbial characteristics. The RBC biofilm removed 89% +/- 5% of the influent N at the highest surface load of approximately 8.3 g of N m(-2) day(-1), with N(2) as the main end product. In batch tests, the RBC biomass showed good aerobic and anoxic ammonium oxidation (147.8 +/- 7.6 and 76.5 +/- 6.4 mg of NH(4)(+)-N g of volatile suspended solids [VSS](-1) day(-1), respectively) and almost no nitrite oxidation (< 1 mg of N g of VSS(-1) day(-1)). The diversity of aerobic ammonia-oxidizing bacteria (AAOB) and planctomycetes in the biofilm was characterized by cloning and sequencing of PCR-amplified partial 16S rRNA genes. Phylogenetic analysis of the clones revealed that the AAOB community was fairly homogeneous and was dominated by Nitrosomonas-like species. Close relatives of the known anaerobic ammonia-oxidizing bacterium (AnAOB) Kuenenia stuttgartiensis dominated the planctomycete community and were most probably responsible for anoxic ammonium oxidation in the RBC. Use of a less specific planctomycete primer set, not amplifying the AnAOB, showed a high diversity among other planctomycetes, with representatives of all known groups present in the biofilm. The spatial organization of the biofilm was characterized using fluorescence in situ hybridization (FISH) with confocal scanning laser microscopy (CSLM). The latter showed that AAOB occurred side by side with putative AnAOB (cells hybridizing with probe PLA46 and AMX820/KST1275) throughout the biofilm, while other planctomycetes hybridizing with probe PLA886 (not detecting the known AnAOB) were present as very conspicuous spherical structures. This study reveals that long-term operation of a lab-scale RBC on a synthetic NH(4)(+) wastewater devoid of organic carbon yields a stable biofilm in which two bacterial groups, thought to be jointly responsible for the high autotrophic N removal, occur side by side throughout the biofilm.