A Method for Cell Culture and Maintenance of Ammonia-Oxidizing Archaea in Agar Stab

Ammonia oxidizing archaea (AOA) are predominantly found and closely linked with geochemical cycling of nitrogen in non-extreme habitats. However, these strains have mainly been investigated using liquid cultures of enriched cells. Here, we provide an agar stab as a simple and reliable means of cultivating and maintaining AOA.     

新疆艾丁湖中度嗜盐苯酚降解菌多样性研究

高盐含酚废水属于极难处理的废水之一,筛选具有生物学降解能力的嗜盐菌有助于解决这一难题。从新疆艾丁湖盐湖中分离筛选能够降解苯酚的中度嗜盐菌,了解盐湖中度嗜盐苯酚降解菌的多样性组成和降解能力。研究结果表明,10%(质量分数)的盐浓度条件下,分离得到166株嗜盐菌,通过以苯酚为唯一碳源的培养基进行降解活性筛选后得到45株阳性菌,根据细菌16S rRNA基因序列系统进化分析,这45株菌分别归类到3个门,5个科,9个属。其中拟诺卡氏菌属(Nocardiopsis)是优势菌,占总量的68.8%,其余菌分布于Bacillus、Gracilibacillus、Pontibacillus、Halobacillus、Marinococcus和Halomonas属。在含100 mg/L苯酚的液体培养基,经过10 d培养后,这45株菌降解效率为1%~17%。本研究为工业应用提供了嗜盐微生物种质资源,极具进一步发掘和研究价值。     

长期不同施肥制度对水稻土氨氧化微生物数量和群落结构的影响

由氨氧化微生物驱动的氨氧化过程是硝化作用的限速步骤,在土壤氮素循环过程中扮演着重要角色.以湖南省宁乡县长达30 a定位试验水稻土壤为研究对象,采用荧光定量PCR和Illumina MiSeq高通量测序分析方法,以amoA基因为靶标,研究了4种施肥制度[不施肥(CK)、化肥(CF)、70%化肥+30%有机肥(CFM₁)和40%化肥+60%有机肥(CFM₂)]水稻土壤氨氧化微生物的数量和群落结构变化.结果表明: 不同施肥处理氨氧化古菌(AOA)和氨氧化细菌(AOB) amoA基因拷贝数分别为3.09×10⁷～8.37×10⁷和1.04×10⁷～7.03×10⁷ copies·g^-1干土.施肥显著提高了AOA和AOB数量,但处理CFM₂中AOB数量与CK差异不显著.有机肥配施比例对AOB群落α多样性指数的影响强于AOA,处理CFM₁中AOA群落的多样性指数(Shannon)和AOB群落的丰富度指数(ACE和Chao1)均显著高于CK.奇古菌门和泉古菌门是AOA群落的优势门类群,占AOA amoA基因总序列的83.4%;亚硝化螺菌属、environmental_samples_norank、Bacteria_unclassified和Nitrosomonadales_unclassified是AOB群落的优势属类群,占AOB amoA基因总序列的97.8%.维恩分析结果显示,有机肥配施比例对AOB群落操作分类单元(OTU)数量的影响强于AOA,但对各处理共有AOA和AOB amoA基因序列条数的影响均较小.冗余分析结果显示,不同施肥处理AOB群落结构差异强于AOA,且所有土壤理化性质均与AOA和AOB群落结构存在显著相关关系.综上可知:有机肥配施比例显著改变了AOA和AOB数量、多样性和群落结构,配施30%有机肥时,AOA群落的Shannon指数最高,AOB群落数量、ACE和Chao1指数均最高.研究结果可为进一步探讨农业系统中氨氧化微生物对不同施肥制度的响应机制及其在氮素转化中的作用提供科学依据.     

Isolation and Identification of Halophilic and Halotolerant Bacteria From Badab-e Surt Travertine Spring,Kiasar, Iran,and Investigation of Calcite Biomineralization Induction

Badab-e Surt spring is a travertine spring that has low to moderate levels of salt, so it is a good model for isolating moderately halophilic bacteria and investigating the relationship between microbe and environment. For isolating bacterial strains, water and sediment samples were collected from different springheads of the Badab-e Surt spring. Among the 171 bacterial isolates, 110 strains were halophiles. According to comparative partial 16S rRNA sequence analysis, the selected halophilic gram-positive and gram-negative strains were identified as members of the genera: Roseovarius, Labrenzia, Erythrobacter, Erythromicrobium, Massilia, Marinobacter, Halomonas, Shewanella, Pseudomonas, Flavobacterium, Bacillus, Brevibacterium, Staphylococcus, Microbacterium, Kocuria, and Streptomyces. To investigate mineralization, potential strains were screened by the culturing method, and then analyzed with a polarizing and scanning microscope. Five strains, Bss-11a, Bss-3, Bsw-1c1, Bsw-28d, and Bsw-39b, had potential for the mineralization of calcite that very closely resembled species Bacillus cohenii DSM 6307^T, Labrenzia aggregate IAM 12614^T, Bacillus safensis FO-036b^T, Marinobacter flavimaris SW-145^T, and Marinobater adhaerens HP15^T, respectively.     

Function of coenzyme F420-dependent NADP reductase in methanogenic archaea containing an NADP-dependent alcohol dehydrogenase

Methanogenic archaea growing on ethanol or isopropanol as the electron donor for CO₂ reduction to CH₄ contain either an NADP-dependent or a coenzyme F₄₂₀-dependent alcohol dehydrogenase. We report here that in both groups of methanogens, the N ⁵, N ¹⁰-methylenetetrahydromethanopterin dehydrogenase and the N ⁵, N ¹⁰-methylenetetrahydromethanopterin reductase, two enzymes involved in CO₂ reduction to CH₄, are specific for F₄₂₀. This raised the question how F₄₂₀H₂ is regenerated in the methanogens with an NADP-dependent alcohol dehydrogenase. We found that these organisms contain catabolic activities of an enzyme catalyzing the reduction of F₄₂₀ with NADPH. The F₄₂₀-dependent NADP reductase from Methanogenium organophilum was purified and characterized. The N-terminal amino acid sequence showed 42% sequence identity to a putative gene product in Methanococcus jannaschii, the total genome of which has recently been sequenced. Received: 12 May 1997 / Accepted: 1 July 1997     

Tetramethylammonium:coenzyme M methyltransferase system from Methanococcoides sp.

A methanogen (strain NaT1) that belongs to the family of Methanosarcinaceae and that can grow on tetramethylammonium as the sole energy source has recently been isolated. We report here that cell extracts of the archaeon catalyze the formation of methyl-coenzyme M from coenzyme M and tetramethylammonium. The activity was dependent on the presence of Ti(III) citrate and ATP, and was rapidly lost under oxic conditions. Anoxic chromatography on DEAE-Sepharose revealed that two fractions, fractions 3 and 4, were required for activity. A 50-kDa protein that together with fraction 3 catalyzed methyl-coenzyme M formation from tetramethylammonium and coenzyme M was purified from fraction 4. From fraction 3, a 22-kDa corrinoid protein and a 40-kDa protein exhibiting methylcobalamin:coenzyme M methyltransferase (MT2) activity were purified. The N-terminal amino acid sequences of these purified proteins were determined. The 40-kDa protein showed sequence similarity to MT2 isoenzymes from Methanosarcina barkeri. Cell extract of strain NaT1 grown on trimethylamine rather than on tetramethylammonium did not exhibit tetramethylammonium:coenzyme M methyltransferase activity. The strain was identified as belonging to the genus of Methanococcoides, its closest relative being Methanococcoides methylutens. Received: 7 April 1998 / Accepted: 26 June 1998     

Two malate dehydrogenases in Methanobacterium thermoautotrophicum

Methanobacterium thermoautotrophicum (strain Marburg) was found to contain two malate dehydrogenases, which were partially purified and characterized. One was specific for NAD⁺ and catalyzed the dehydrogenation of malate at approximately one-third of the rate of oxalacetate reduction, and the other could equally well use NAD⁺ and NADP⁺ as coenzyme and catalyzed essentially only the reduction of oxalacetate. Via the N-terminal amino acid sequences, the encoding genes were identified in the genome of M. thermoautotrophicum (strain ΔH). Comparison of the deduced amino acid sequences revealed that the two malate dehydrogenases are phylogenetically only distantly related. The NAD⁺-specific malate dehydrogenase showed high sequence similarity to l-malate dehydrogenase from Methanothermus fervidus, and the NAD(P)⁺-using malate dehyrogenase showed high sequence similarity to l-lactate dehydrogenase from Thermotoga maritima and l-malate dehydrogenase from Bacillus subtilis. A function of the two malate dehydrogenases in NADPH:NAD⁺ transhydrogenation is discussed. Received: 29 December 1997 / Accepted: 4 March 1998     

Structure and Function of the A1A0-ATPases from Methanogenic Archaea

Recent molecular studies revealed nine to ten gene products involved infunction/assembly of the methanoarchaeal ATPase and unravel a closerelationship of the A₁A₀-ATPase and theV₁V₀-ATPase with respect to subunit composition and thestructure of individual subunits. Most interestingly, there is anastonishing variability in the size of the proteolipids in methanoar chaealA₁A₀-ATPases with six, four, or two transmembranehelices and a variable number of conserved protonizable groups per monomer.Despite the structural similarities the A₁A₀-ATPasediffers fundamentally from the V₁V₀-ATPase by itsability to synthesize ATP, a feature shared withF₁F₀-ATPases. The discovery of duplicated andtriplicated versions of the proteolipid in A₁A₀-ATPsynthases questions older views of the structural requirements for ATPsynthases versus ATP hydrolases and sheds new light on the evolutionof these secondary energy converters.     

小兴安岭酸性泥炭土硝化作用的类型及其驱动因子

以小兴安岭酸性森林泥炭土为研究对象,通过加入10 mL·L^-1乙炔及不同浓度的外源硫酸铵(0、1.2、6.0 mmol N·kg^-1)进行硝化培养试验,探究酸性泥炭土中硝化作用类型及主要驱动因子.结果表明:无论有无外加氮源,酸性泥炭土均存在较强的矿化作用(0.9～1.4 mg N·kg^-1·d^-1),经过2周的培养均发生了硝化作用(0.4～0.6 mg N·kg^-1·d^-1),且不同浓度硫酸铵处理之间无显著差异;而乙炔处理虽有较强的矿化作用(0.8 mg N·kg^-1·d^-1),但未发生明显的硝化作用(0 mg N·kg^-1·d^-1),说明该酸性泥炭土以自养硝化为主,外源无机氮源浓度对硝化作用无显著影响,硝化底物NH₃的主要来源不是外源硫酸铵,更可能来源于土壤中有机氮的矿化.培养0～14 d,无论有无外加氮源,酸性泥炭土氨氧化细菌(AOB)和古菌(AOA)丰度均显著增加,但不同浓度硫酸铵处理间无显著差异,表明外源无机氮浓度对氨氧化微生物的生长无显著促进作用.与不加乙炔的对照相比,乙炔处理AOB和AOA丰度随时间均无显著变化,推测AOA与AOB在该酸性泥炭土的硝化过程中都可能起一定的作用.