The anammoxosome: an intracytoplasmic compartment in anammox bacteria

Anammox bacteria belong to the phylum Planctomycetes and perform anaerobic ammonium oxidation (anammox); they oxidize ammonium with nitrite as the electron acceptor to yield dinitrogen gas. The anammox reaction takes place inside the anammoxosome: an intracytoplasmic compartment bounded by a single ladderane lipid-containing membrane. The anammox bacteria, first found in a wastewater treatment plant in The Netherlands, have the potential to remove ammonium from wastewater without the addition of organic carbon. Very recently anammox bacteria were also discovered in the Black Sea where they are responsible for 30-50% of the nitrogen consumption. This review will introduce different forms of intracytoplasmic membrane systems found in prokaryotes and discuss the compartmentalization in anammox bacteria and its possible functional relation to catabolism and energy transduction.     

Isolation and characterization of a prokaryotic cell organelle from the anammox bacterium Kuenenia stuttgartiensis

Anaerobic ammonium oxidizing (anammox) bacteria oxidize ammonium with nitrite to nitrogen gas in the absence of oxygen. These microorganisms form a significant sink for fixed nitrogen in the oceans and the anammox process is applied as a cost‐effective and environment‐friendly nitrogen removal system from wastewater. Anammox bacteria have a compartmentalized cell plan that consists of three separate compartments. Here we report the fractionation of the anammox bacterium Kuenenia stuttgartiensis in order to isolate and analyze the innermost cell compartment called the anammoxosome. The subcellular fractions were microscopically characterized and all membranes in the anammox cell were shown to contain ladderane lipids which are unique for anammox bacteria. Proteome analyses and activity assays with the isolated anammoxosomes showed that these organelles harbor the energy metabolism in anammox cells. Together the experimental data provide the first thorough characterization of a respiratory cell organelle from a bacterium and demonstrate the essential role of the anammoxosome in the production of a major portion of the nitrogen gas in our atmosphere.     

Biochemistry and molecular biology of anammox bacteria

Anaerobic ammonium-oxidizing (anammox) bacteria are one of the latest additions to the biogeochemical nitrogen cycle. These bacteria derive their energy for growth from the conversion of ammonium and nitrite into dinitrogen gas in the complete absence of oxygen. These slowly growing microorganisms belong to the order Brocadiales and are affiliated to the Planctomycetes. Anammox bacteria are characterized by a compartmentalized cell architecture featuring a central cell compartment, the “anammoxosome”. Thus far unique “ladderane” lipid molecules have been identified as part of their membrane systems surrounding the different cellular compartments. Nitrogen formation seems to involve the intermediary formation of hydrazine, a very reactive and toxic compound. The genome of the anammox bacterium Kuenenia stuttgartiensis was assembled from a complex microbial community grown in a sequencing batch reactor (74% enriched in this bacterium) using a metagenomics approach. The assembled genome allowed the in silico reconstruction of the anammox metabolism and identification of genes most likely involved in the process. The present anammox pathway is the only one consistent with the available experimental data, thermodynamically and biochemically feasible, and consistent with Ockham’s razor: it invokes minimum biochemical novelty and requires the fewest number of biochemical reactions. The worldwide presence of anammox bacteria has now been established in many oxygen-limited marine and freshwater systems, including oceans, seas, estuaries, marshes, rivers and large lakes. In the marine environment over 50% of the N₂ gas released may be produced by anammox bacteria. Application of the anammox process offers an attractive alternative to current wastewater treatment systems for the removal of ammonia-nitrogen. Currently, at least five full scale reactor systems are operational.     

Ecological characteristics of anaerobic ammonia oxidizing bacteria

Anaerobic ammonium oxidation (anammox) is the microbial conversion of ammonium and nitrite to dinitrogen gas. The functional microbes of anammox reaction are anammox bacteria, which were discovered in a wastewater treatment system for nitrogen removal. Anammox bacteria are prevalent in anoxic ecosystems and play an important role in both biological nitrogen cycle and nitrogen pollution control. In this paper, we reviewed the investigation on ecological characteristics of anammox bacteria, and tried to figure out their complicated intraspecies and interspecies relationships. As for intraspecies relationship, we focused on the quorum sensing system, a cell density-dependent phenomenon. As for interspecies relationship, we focused on the synergism and competition of anammox bacteria with other microorganisms for substrate and space. Finally, we discussed the great influence of environmental factors (e.g., dissolved oxygen, organic matters) on the constitution, structure and function of anammox bacteria community.     

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     

Enrichment and characterization of marine anammox bacteria associated with global nitrogen gas production

Microbiological investigation of anaerobic ammonium oxidizing (anammox) bacteria has until now been restricted to wastewater species. The present study describes the enrichment and characterization of two marine Scalindua species, the anammox genus that dominates almost all natural habitats investigated so far. The species were enriched from a marine sediment in the Gullmar Fjord (Sweden) using a medium based on Red Sea salt. Anammox cells comprised about 90% of the enrichment culture after 10 months. The enriched Scalindua bacteria displayed all typical features known for anammox bacteria, including turnover of hydrazine, the presence of ladderane lipids, and a compartmentalized cellular ultrastructure. The Scalindua species also showed a nitrate-dependent use of formate, acetate and propionate, and performed a formate-dependent reduction of nitrate, Fe(III) and Mn(IV). This versatile metabolism may be the basis for the global distribution and substantial contribution of the marine Scalindua anammox bacteria to the nitrogen loss from oxygen-limited marine ecosystems.     

厌氧氨氧化颗粒污泥聚集机制研究进展

厌氧氨氧化(anaerobic ammonium oxidation,anammox)工艺被认为是当前污水生物脱氮领域最经济的处理工艺,有利于实现污水处理厂的能源自给。厌氧氨氧化菌是该工艺的核心功能微生物。以厌氧氨氧化菌为主导微生物形成的厌氧氨氧化颗粒污泥具有沉速大、污泥持留能力强及对不利环境抵抗能力强等突出优势,是实现厌氧氨氧化工艺最有前景的污泥形态。本论文围绕厌氧氨氧化颗粒,介绍了厌氧氨氧化菌的特性、种类及代谢途径,综述了厌氧氨氧化颗粒污泥的形成假说及与厌氧氨氧化颗粒污泥聚集密切相关的胞外聚合物(extracellular polymeric substance,EPS)和群体感应研究现状,并对今后厌氧氨氧化颗粒的研究进行了展望,以期为后续厌氧氨氧化颗粒的研究及厌氧氨氧化颗粒工艺的优化提供参考。     

厌氧铵氧化过程中关键酶及相关分子标记在生态学研究中的应用进展

厌氧铵氧化是由微生物介导的氮素循环过程中的重要途径之一。近20年来,通过对厌氧铵氧化细菌生态学、基因组学和生理代谢特性的探索,人们对其微生物学机制已经有了较多的认识:厌氧铵氧化细菌通过亚硝酸盐还原酶将亚硝酸根离子还原为一氧化氮,进而与铵离子结合在联氨合成酶的作用下生成联氨,最后通过联氨氧化酶的催化产生终产物氮气。同时,对参与这些过程的关键酶及其功能基因的认识有助于选择新的分子标记,从而为研究厌氧铵氧化细菌的多样性和分子生态学特征提供新的工具,以弥补16S rRNA基因特异性相对较低且难以与生态功能关联等方面的不足。对目前已知的参与厌氧铵氧化过程的3种关键酶的研究历程和现状进行了评述,并总结了利用3种功能基因进行厌氧铵氧化细菌生态学研究的最新进展。     

Anaerobic Ammonium-Oxidizing Bacteria: Unique Microorganisms with Exceptional Properties

Summary: Anaerobic ammonium-oxidizing (anammox) bacteria defy many microbiological concepts and share numerous properties with both eukaryotes and archaea. Among their most intriguing characteristics are their compartmentalized cell plan and archaeon-like cell wall. Here we review our current knowledge about anammox cell biology. The anammox cell is divided into three separate compartments by bilayer membranes. The anammox cell consists of (from outside to inside) the cell wall, paryphoplasm, riboplasm, and anammoxosome. Not much is known about the composition or function of both the anammox cell wall and the paryphoplasm compartment. The cell wall is proposed to be proteinaceous and to lack both peptidoglycan and an outer membrane typical of Gram-negative bacteria. The function of the paryphoplasm is unknown, but it contains the cell division ring. The riboplasm resembles the standard cytoplasmic compartment of other bacteria; it contains ribosomes and the nucleoid. The anammoxosome occupies most of the cell volume and is a so-called “prokaryotic organelle” analogous to the eukaryotic mitochondrion. This is the site where the anammox reaction takes place, coupled over the curved anammoxosome membrane, possibly giving rise to a proton motive force and subsequent ATP synthesis. With these unique properties, anammox bacteria are food for thought concerning the early evolution of the domains Bacteria, Archaea, and Eukarya.     

Combined structural and chemical analysis of the anammoxosome: a membrane-bounded intracytoplasmic compartment in anammox bacteria

Anammox bacteria have unique intracellular membranes that divide their cytoplasm into three separate compartments. The largest and innermost cytoplasmic compartment, the anammoxosome, is hypothesized to be the locus of all catabolic reactions in the anammox metabolism. Electron tomography showed that the anammoxosome and its membrane were highly folded. This finding was confirmed by a transmission electron microscopy study using different sample preparation methods. Further, in this study electron-dense particles were observed and electron tomography showed that they were confined to the anammoxosome compartment. Energy dispersive X-ray analysis revealed that these particles contained iron. The functional significance of a highly folded anammoxosome membrane and intracellular iron storage particles are discussed in relation to their possible function in energy generation.     

高含氮稻田深层土壤的氨氧化古菌和厌氧氨氧化菌共存及对氮循环影响

随着海洋生态系统中的厌氧氨氧化反应和氨氧化古菌的发现,自然生态系统的氮循环过程被重新认识,但是目前尚无在陆地深层的相关报道。结合同位素示踪与分子生物学技术探索了稻田深层土壤中anammox与AOA的存在及特性。结果表明,在沼渣处理废水浇灌的高含氮稻田深层土壤中,anammox与AOA共存。通过构建克隆文库发现,此土壤中厌氧氨氧化菌的生物多样性相对较低,35个克隆序列只分为4个独立操作单元(OTU),代表序列与Genebank数据库中已探明的厌氧氨氧化菌Candidatus 'Kuenenia stuttgartiensis’的同源性超过95%;对氨氧化古菌的分析发现,20个克隆子共得到5个OTU,其与基因库中土壤/沉积物进化分支关系最近,序列的同源性部分超过98%。同位素示踪的初步结果表明,anammox产生的氮气占此土壤总氮气生成量的24.1%-29.8%。AOA与anammox的共存为anammox反应的广泛存在与发生提供了新思路。     

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.     

Cell division ring, a new cell division protein and vertical inheritance of a bacterial organelle in anammox planctomycetes

Anammox bacteria are members of the phylum Planctomycetes that oxidize ammonium anaerobically and produce a significant part of the atmosphere's dinitrogen gas. They contain a unique bacterial organelle, the anammoxosome, which is the locus of anammox catabolism. While studying anammox cell and anammoxosome division with transmission electron microscopy including electron tomography, we observed a cell division ring in the outermost compartment of dividing anammox cells. In most Bacteria, GTP hydrolysis drives the tubulin-analogue FtsZ to assemble into a ring-like structure at the cell division site where it functions as a scaffold for the molecular machinery that performs cell division. However, the genome of the anammox bacterium ' Candidatus Kuenenia stuttgartiensis' does not encode ftsZ . Genomic analysis of open reading frames with potential GTPase activity indicated a possible novel cell division ring gene: kustd1438, which was unrelated to ftsZ . Immunogold localization specifically localized kustd1438 to the cell division ring. Genomic analyses of other members of the phyla Planctomycetes and Chlamydiae revealed no putative functional homologues of kustd1438, suggesting that it is specific to anammox bacteria. Electron tomography also revealed that the bacterial organelle was elongated along with the rest of the cell and divided equally among daughter cells during the cell division process.     

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。     

Bacterial community structure of a lab‐scale anammox membrane bioreactor

Autotrophic nitrogen removal technologies have proliferated through the last decade. Among these, a promising one is the membrane bioreactor (MBR) Anammox, which can achieve very high solids retention time and therefore sets a proper environment for the cultivation of anammox bacteria. In this sense, the MBR Anammox is an efficient technology for the treatment of effluents with low organic carbon and high ammonium concentrations once it has been treated under partial nitrification systems. A lab‐scale MBR Anammox bioreactor has been built at the Technological University of Delft, The Netherlands and has been proven for efficient nitrogen removal and efficient cultivation of anammox bacteria. In this study, next‐generation sequencing techniques have been used for the investigation of the bacterial communities of this MBR Anammox for the first time ever. A strong domination of Candidatus Brocadia bacterium and also the presence of a myriad of other microorganisms that have adapted to this environment were detected, suggesting that the MBR Anammox bioreactor might have a more complex microbial ecosystem that it has been thought. Among these, nitrate‐reducing heterotrophs and primary producers, among others, were identified. Definition of the ecological roles of the OTUs identified through metagenomic analysis was discussed. © 2014 American Institute of Chemical Engineers Biotechnol. Prog., 31:186–193, 2015     

Anaerobic ammonium oxidation (anammox) in different natural ecosystems

Anammox (anaerobic ammonium oxidation), which is a reaction that oxidizes ammonium to dinitrogen gas using nitrite as the electron acceptor under anoxic conditions, was an important discovery in the nitrogen cycle. The reaction is mediated by a specialized group of planctomycete-like bacteria that were first discovered in man-made ecosystems. Subsequently, many studies have reported on the ubiquitous distribution of anammox bacteria in various natural habitats, including anoxic marine sediments and water columns, freshwater sediments and water columns, terrestrial ecosystems and some special ecosystems, such as petroleum reservoirs. Previous studies have estimated that the anammox process is responsible for 50% of the marine nitrogen loss. Recently, the anammox process was reported to account for 9-40% and 4-37% of the nitrogen loss in inland lakes and agricultural soils respectively. These findings indicate the great potential for the anammox process to occur in freshwater and terrestrial ecosystems. The distribution of different anammox bacteria and their contribution to nitrogen loss have been described in different natural habitats, demonstrating that the anammox process is strongly influenced by the local environmental conditions. The present mini-review summarizes the current knowledge of the ecological distribution of anammox bacteria, their contribution to nitrogen loss in various natural ecosystems and the effects of major influential factors on the anammox process.     

The ultrastructure of the compartmentalized anaerobic ammonium-oxidizing bacteria is linked to their energy metabolism

The most striking example of a complex prokaryotic intracytoplasmic organization can be found in the members of the phylum Planctomycetes. Among them are the anammox (anaerobic ammonium-oxidizing) bacteria, which possess a unique cell compartment with an unprecedented function in bacteria: the anammoxosome is a prokaryotic cell organelle evolved for energy metabolism. It is an independent entity, which is enclosed by a contiguous membrane. Several lines of evidence indicate its importance in the anammox reaction and the unusual subcellular organization may well be essential for the lifestyle of anammox bacteria. The present review summarizes our knowledge about the ultrastructure of anammox cells and the connection between the anammoxosome and the energy metabolism of the cell. In the future, much more research will be necessary to validate the current models and to answer questions on the functional cell biology of anammox bacteria.     

Anammox bacteria disguised as denitrifiers: nitrate reduction to dinitrogen gas via nitrite and ammonium

Anaerobic ammonium-oxidizing (anammox) bacteria oxidize ammonium with nitrite and produce N(2). They reside in many natural ecosystems and contribute significantly to the cycling of marine nitrogen. Anammox bacteria generally live under ammonium limitation, and it was assumed that in nature anammox bacteria depend on other biochemical processes for ammonium. In this study we investigated the possibility of dissimilatory nitrate reduction to ammonium by anammox bacteria. Physically purified Kuenenia stuttgartiensis cells reduced (15)NO(3) (-) to (15)NH(4) (+) via (15)NO(2) (-) as the intermediate. This was followed by the anaerobic oxidation of the produced ammonium and nitrite. The overall end-product of this metabolism of anammox bacteria was (15)N(15)N dinitrogen gas. The nitrate reduction to nitrite proceeds at a rate of 0.3 +/- 0.02 fmol cell(-1) day(-1) (10% of the 'normal' anammox rate). A calcium-dependent cytochrome c protein with a high (305 mumol min(-1) mg protein(-1)) rate of nitrite reduction to ammonium was partially purified. We present evidence that dissimilatory nitrate reduction to ammonium occurs in Benguela upwelling system at the same site where anammox bacteria were previously detected. This indicates that anammox bacteria could be mediating dissimilatory nitrate reduction to ammonium in natural ecosystems.