异化铁还原梭菌Clostridium bifermentans EZ-1产氢与电化学特性

【目的】从黄河三角洲滨海湿地土壤中获得同时具备产氢、产电以及异化铁还原能力的多功能菌株。【方法】通过厌氧分离技术从黄河三角洲土壤中分离得到纯菌株,16S r RNA基因测序后与数据库已有序列进行比对。利用革兰氏染色及扫描电镜观察菌株形态,并用气相色谱(gas chromatography,GC)和液相色谱(high performance liquid chromatography,HPLC)检测其生理代谢底物和产物。通过添加不同形态铁氧化物检测该菌株Fe(Ⅲ)的还原能力。构建微生物燃料电池(Microbial fuel cells,MFCs)检测该菌株的电化学活性。【结果】16S r RNA基因序列比对发现其与双酶梭菌Clostridium bifermentans的相似性达97.99%。革兰氏染色结果显示为阳性菌。能够利用葡萄糖为底物发酵产生氢气、二氧化碳、乙酸和丁酸。Fe(Ⅲ)还原能力检测发现,其不仅可以还原柠檬酸铁(FeC_6H_5O_7)中可溶性的Fe(Ⅲ),还可以还原无定形铁水铁矿(FeOOH)和晶型纳米磁铁矿(Fe_3O_4)中的Fe(Ⅲ)。此外,经MFCs检测发现,该菌具有电化学活性,最大电流输出密度可达6.5 m A/m~2,且在0.15 V位置存在氧化峰。【结论】本研究从土壤中成功分离得到了一株同时具有产氢、产电以及异化铁还原能力的多功能梭菌菌株,保藏并命名为Clostridium bifermentans EZ-1。     

一株土壤产电菌Clostridium sporogenes的分离及其产电性能

【目的】从土壤中分离获得产电菌纯菌株SE6,鉴定其种类并分析其产电性能。【方法】通过厌氧培养分离得到纯菌株,根据其形态、生理生化性质及16S r RNA基因测序分析确定其种属。以该菌株作为产电菌接种源,液体LB培养基和铁氰化钾溶液分别作为阳极液和阴极液,构建双室微生物燃料电池(Microbial fuel cells,MFCs),研究其产电能力;根据交流阻抗图谱,分析MFCs的内阻。应用循环伏安测试确定该菌株的胞外电子传递方式。并利用扫描电镜对阳极表面产电菌形态进行观察。【结果】菌株SE6的16S r RNA基因序列与Clostridium sporogenes有100%同源性,结合其形态特征和生理生化特性,确定其属于梭菌属(Clostridium)。SE6接种到MFCs中可以获得44.42 m W/m~2的最大功率密度。MFCs的阳极内阻、阴极内阻和欧姆内阻分别为(1488±193)Ω/cm~2、(0.92±0.01)Ω/cm~2和(20.69±1.76)Ω/cm~2。其循环伏安图谱显示体系中存在电化学活性物质且峰值电流随扫速升高线性增大。扫描电镜观察到阳极表面聚集附着着长度约1μm的杆菌。【结论】本研究成功从土壤中分离出具有一定产电能力的菌株C.sporogenes SE6,可直接将电子传递至阳极,其产电过程阻抗较大。     

Mcc在脱色希瓦氏菌S12电极呼吸中的作用

【目的】研究脱色希瓦氏菌S12周质空间c型细胞色素Mcc的功能,进一步探索和补充微生物胞外电子传递过程的机制。【方法】借助自杀质粒敲除mcc基因,通过细胞浓度测定和激光共聚焦显微镜比较分析突变株和野生株之间的浮游细胞和生物膜的生长情况,并比较分析二者在微生物燃料电池电极还原、铁还原和胞外偶氮染料还原过程中的功能。【结果】Mcc缺失对铁还原和偶氮还原没有影响,但却造成电极呼吸活性下降34.1%;与野生株相比,mcc突变株的好氧生长和厌氧浮游细胞生长无明显影响,但却显著抑制了电极表面生物膜的形成。【结论】Mcc是希瓦氏菌S12电极呼吸过程中周质空间电子传递的重要组分之一,缺失会显著抑制其电极呼吸效率以及生物膜的形成。     

产甲烷条件下岩溶湿地沉积物中古菌群落的变化规律

【背景】桂林会仙湿地位于喀斯特峰丛洼地和峰丛平原的过渡区,主要由岩溶地下河补给,水质呈现富钙偏碱特征,是一处典型的岩溶湿地环境,湿地沉积物以厌氧环境为主,独特的环境特征使之成为研究新型厌氧微生物的理想场所。氢型产甲烷菌和乙酸型产甲烷菌是环境中有机质厌氧降解的重要参与者,但目前会仙湿地产甲烷菌生理生态功能的研究十分有限。【目的】揭示乙酸盐营养型产甲烷条件和氢气营养型产甲烷条件下岩溶湿地环境古菌群落结构的变化规律和产甲烷菌的主要类群,探讨岩溶环境古菌的功能和相互关系。【方法】以会仙岩溶湿地沉积物为研究材料,分别以乙酸盐和氢气为唯一能源物进行富集培养,结合未添加任何能源底物的对照处理,动态监测产甲烷通量,分别构建了3个共包含146条古菌16S rRNA基因全长序列的文库,以及3个共包含138条甲基辅酶M还原酶基因mcr A基因序列的文库,通过构建系统发育树比较分析不同产甲烷底物培养条件下典型岩溶湿地古菌群落的变化规律。【结果】从乙酸型和氢型产甲烷条件培养物顶空气中都检测到了几乎等浓度的甲烷产生,甲烷八叠球菌是mcr A文库中主要的古菌类群,其中包含了Methanosarcina属古菌、Zoige Cluster I (ZC-I)和ANME-2d Cluster (AD)类群古菌,以及两个相对独立且不包含任何参考序列的分支KT-I和KT-II,可能代表产甲烷菌的新类群;经过两种产甲烷条件的富集培养后,ZC-I、AD和KT-II类群古菌的序列数占比有较为显著的增加(45%–155%);深古菌(Bathyarchaeota)是所有古菌16Sr RNA基因文库的优势类群,序列占比为88%–100%,其中MCG-11亚群最为丰富,占所有深古菌的84%,并且在乙酸盐产甲烷条件下增加了17%。【结论】会仙湿地沉积物中蕴涵着丰富的新型古菌序列,沉积物中主要的氢型产甲烷菌和乙酸型产甲烷菌都来自甲烷八叠球菌目,深古菌在岩溶环境和乙酸型产甲烷条件下可能都发挥着重要的作用。     

基于16S rRNA和RubisCO基因对嗜酸硫杆菌的系统发育及多样性北大核心CSCD

【目的】明确不同地理来源的Acidithiobacillus spp.种群是否表现出显著的地域性和异域物种形成;为了解微生物谱系地理、多样性维持机制和微生物分子地理学提供基础数据。【方法】采用16S r RNA基因、核酮糖-1,5-二磷酸羧化酶/加氧酶(Rubis CO)功能基因序列同源性分析构建相应的系统发育树,分析Acidithiobacillus spp.种群的遗传多样性。【结果】从3个不同的地域分离到35株菌聚为5大类群,其中菌株YNTR4-15可能是铁氧化细菌(Leptspirillum ferrooxidans),菌株HBDY3-3被鉴定为另一铁氧化细菌(Leptospirillum ferrodiazotrophum);有4株可能是Acidithiobacillus ferrivorans;6株是Acidithiobacillus ferridurans,其余菌株均被鉴定为Acidithiobacilus ferrooxidan。对26株代表性菌株的Rubis CO I型cbb L基因和II型cbb M基因的分析,发现19株菌具有双拷贝cbb L基因,分别为cbb L1和cbb L2基因;7株菌只检测到了cbb L1。cbb L1和cbb L2基因都有3个序列型;而cbb M基因是单拷贝。Rubis CO基因的密码子偏爱性不强。【结论】分离自3个地域的菌株16S r RNA/Rubis CO基因存在序列差异,Acidithiobacillus spp.种群存在显著的遗传多样性。嗜酸硫杆菌分离菌株基于16S r RNA基因的系统发育树和Rubis CO基因的发育树不一致。     

人肠道梭菌和甲烷马赛球菌协同代谢甜菜碱和胆碱产甲烷研究

【目的】根据人肠道富含胆碱和甜菜碱,同时肠道微生物组中具有裂解胆碱和还原甜菜碱产三甲胺的细菌,以及利用三甲胺产甲烷的古菌,本研究探讨肠道细菌与古菌协同代谢甜菜碱和胆碱产甲烷的可能性。【方法】调查不同年龄段人群粪便中的16S rRNA基因多样性,分析肠道中古菌的菌群组成;利用定量PCR(quantitativePCR,qPCR)定量甲烷马赛球菌(Methanomassiliicoccus)特异的甲醇甲基转移酶基因mtaB和甲烷八叠球菌(Methanosarcina)及细菌的16SrRNA基因拷贝数,分析肠道中甲基营养型产甲烷古菌及总细菌的含量;宏基因组组装基因组(metagenome-assembled genomes, MAGs)分析携带甜菜碱还原酶基因grdH和胆碱裂解酶基因cutC的细菌组成。从粪便中分离代谢甜菜碱及胆碱产生三甲胺的细菌,并与分离自人肠道的甲烷马赛球菌构建共培养物,测定其协同转化甜菜碱和胆碱产甲烷的能力。【结果】年轻人粪便中含有甲烷杆菌科(Methanobacteriaceae,82.16%)的甲烷短杆菌属(Methanobrevibacter,49.18%)和甲烷...     

扎龙盐碱湿地芦苇根际土的优势产甲烷途径分析

【背景】芦苇湿地是甲烷主要的排放源之一,产甲烷古菌是唯一产生大量甲烷的生物,而盐碱湿地芦苇根际土优势甲烷途径鲜有研究。【目的】调查扎龙低温盐碱湿地芦苇根际土中的优势产甲烷途径。【方法】通过16S rRNA基因扩增子测序,分析扎龙湿地芦苇生长季根际土壤深度0–20 cm的产甲烷古菌和细菌组成。用已知的产甲烷底物三甲胺、甲醇、乙酸和H₂/CO₂,以及高盐环境植物和细菌的相似相容物质——甜菜碱(被细菌还原成三甲胺)在pH 8.0培养获得芦苇根际土的产甲烷富集物。测定各种富集物的产甲烷速率鉴定芦苇根际土的优势产甲烷途径;测定甜菜碱富集物中的16S rRNA基因多样性,并用RT-qPCR定量优势细菌和古菌的物种组成,从而推测协同代谢甜菜碱产甲烷的细菌和古菌类群。【结果】扎龙盐碱湿地芦苇根际土含有氢营养型的甲烷杆菌属(Methanobacterium,36.42%)、偏好低氢的Rice Cluster Ⅱ (11.55%)、乙酸营养型的甲烷鬃菌属(Methanosaeta,11.29%)、甲基营养型的甲烷八叠球菌属(Methanosarcina,6.53...     

不同抑制剂对乙酸降解产甲烷及产甲烷菌群结构的影响

摘要:【目的】研究不同温度条件下的石油烃降解产甲烷菌系中是否存在乙酸互营氧化产甲烷代谢途径。【方法】以3个不同温度条件的正十六烷烃降解产甲烷菌系Y15(15℃)、M82(35℃)和SK(55℃)作为接种物,通过乙酸喂养实验、并添加乙酸营养型产甲烷古菌的选择性抑制剂NH4Cl和CH3F,结合末端限制性片段长度多态性(terminal restriction fragment length polymorphism,T-RFLP)和克隆文库技术,分析乙酸产甲烷潜力及产甲烷古菌群落的演替趋势,推测产甲烷代谢途径的变化趋势。【结果】无论是否添加NH4Cl和CH3 F,这3个菌系都可以利用乙酸生长并产生甲烷,但是添加NH4Cl和CH3 F后产甲烷延滞期增加,最大比甲烷增长速率降低;只添加乙酸后,3个不同温度的菌系的古菌群落主要由乙酸营养型产甲烷古菌甲烷鬃毛菌属(Methanosaeta)组成,其丰度分别为92.8±1.4%、97.3±2.4%和82.8±9.0%;当添加选择性抑制剂NH4Cl,3 个菌系中的Methanosaeta的丰度分别变为98.5±0.7%、87.4±4.8%和6.1±8.6%,中温菌系M82中氢营养型产甲烷古菌甲烷袋装菌属(Methanoculleus)的相对丰度增加到12. 6±4.0%,高温菌系SK中另一类氢营养型产甲烷古菌甲烷热杆菌属(Methanothermobacter)增至84.3±1.5%;当添加选择性抑制剂CH3 F,Methanosaeta丰度分别降至77.1 ± 14.5%,86.4±6.1%和35.8±7.8%,低温菌系Y15中的甲烷八叠球菌属(Methanosarcina)增高(15.7±21%),这类产甲烷古菌具有多种产甲烷代谢途径,M82中Methanoculleus丰度上升到13.6±13.1%,SK中Methanothermobacter丰度增大到48.5±11.2%。【结论】在低温条件下,菌系Y15可能主要通过乙酸裂解完成产甲烷代谢,在中高温条件下,菌系M82和SK中可能存在乙酸互营氧化产甲烷代谢途径,并且甲烷的产生分别通过不同种群的氢营养型产甲烷古菌来完成。     

人肠道梭菌和甲烷马赛球菌协同代谢甜菜碱和胆碱产甲烷研究

【目的】根据人肠道富含胆碱和甜菜碱,同时肠道微生物组中具有裂解胆碱和还原甜菜碱产三甲胺的细菌,以及利用三甲胺产甲烷的古菌,本研究探讨肠道细菌与古菌协同代谢甜菜碱和胆碱产甲烷的可能性。【方法】调查不同年龄段人群粪便中的16S rRNA基因多样性,分析肠道中古菌的菌群组成;利用定量PCR(quantitative PCR,qPCR)定量甲烷马赛球菌(Methanomassiliicoccus)特异的甲醇甲基转移酶基因mtaB和甲烷八叠球菌(Methanosarcina)及细菌的16S rRNA基因拷贝数,分析肠道中甲基营养型产甲烷古菌及总细菌的含量;宏基因组组装基因组(metagenome-assembled genomes,MAGs)分析携带甜菜碱还原酶基因grdH和胆碱裂解酶基因cutC的细菌组成。从粪便中分离代谢甜菜碱及胆碱产生三甲胺的细菌,并与分离自人肠道的甲烷马赛球菌构建共培养物,测定其协同转化甜菜碱和胆碱产甲烷的能力。【结果】年轻人粪便中含有甲烷杆菌科(Methanobacteriaceae,82.16%)的甲烷短杆菌属(Methanobrevibacter,49.18%)和甲烷杆菌属(Methanobacterium,33.34%)、甲基营养型的甲烷八叠球菌科(Methanosarcinaceae,5.67%)的甲烷八叠球菌属(Methanosarcina,5.70%),以及甲烷马赛球菌科(Methanomassiliicoccaceae,3.13%)的甲烷马赛球菌属(Methanomassiliicoccus,3.14%)。而中老年人粪便中的甲烷古菌多样性较低,也未检测到甲烷马赛球菌。qPCR定量分析显示年轻人比中老年人肠道的总古菌含量高3.11倍,其中甲烷马赛球菌高6.53倍、甲烷八叠球菌高5.52倍,总细菌含量高2.90倍。宏基因组分析组装了229个细菌基因组,其中42个携带基因grdH和cutC,这些细菌属于毛螺菌科(Lachnospiraceae)、肠杆菌科(Enterobacteriaceae)和梭菌科(Clostridiaceae)等。从粪便中分离到恶名梭菌(Clostridium malenominatum)B8,菌株B8与卢米尼甲烷马赛球菌(Methanomassiliicoccus luminyensis)B10共培养物可降解47.03%的甜菜碱和25.83%胆碱,并产生甲烷,在培养液中检测到三甲胺先积累后被降解。【结论】人肠道细菌恶名梭菌B8和卢米尼甲烷马赛球菌B10可协同代谢甜菜碱和胆碱产甲烷,推测它们在人肠道中可将部分食物中的甜菜碱和胆碱代谢产生甲烷。     

一株单环刺螠肠道电活性希瓦氏菌Shewanella marisflavi的生理学特性

【目的】探究以单环刺螠为代表的海洋环节动物肠道中电活性微生物的存在情况,并表征其生理学及电化学特性。【方法】采用平板划线法、16S rRNA基因测序技术分离纯化菌株并进行菌株鉴定。利用扫描电镜表征菌株形态。高效液相色谱(high performance liquid chromatography,HPLC)检测其无氧呼吸底物氧化及产物生成情况。通过菲啰嗪和甲醛肟显色法检测菌株的异化Fe(Ⅲ)和Mn(Ⅳ)还原能力。借助单室微生物燃料电池(single-chamber microbial fuel cells,SCMFCs)及循环伏安法检测菌株的电化学活性。【结果】从单环刺螠肠道中成功分离得到了一株兼性厌氧菌,16S rRNA基因序列比对结果显示该菌株与Shewanellamarisflavi的相似性达99.93%。扫描电镜结果显示其为杆状,长约2μm,宽度约为0.5μm。HPLC检测结果表明,该菌能以乳酸钠为电子供体,富马酸为电子受体进行无氧呼吸并伴随代谢产物乙酸钠和琥珀酸产生。菲啰嗪和甲醛肟显色法结果证实,该菌具有异化铁、锰还原能力。单室MFCs检测结果发现该菌的最大电流输出密度为146 mA/m2,循环伏安法检测结果显示该菌在0.14 V和–0.51 V位置处分别存在氧化峰和还原峰。【结论】本研究结果证实以单环刺螠为代表的海洋环节动物肠道中存在以Shewanella marisflavi UU-3-2为代表的电活性微生物。表明电化学活性微生物在海洋环节动物肠道中广泛存在。     

Coenzyme M binds to a [4Fe-4S] cluster in the active site of heterodisulfide reductase as deduced from EPR studies with the [33S]coenzyme M-treated enzyme

Heterodisulfide reductase (Hdr) from methanogenic Archaea catalyzes the reversible reduction of the heterodisulfide (CoM-S-S-CoB) of the methanogenic thiol coenzymes, coenzyme M (CoM-SH) and coenzyme B (CoB-SH). Upon reaction of the oxidized enzyme with CoM-SH a unique paramagnetic species is formed, which has been shown to be due to a novel type of [4Fe-4S](3+) cluster. In this work, it was addressed whether CoM-SH is directly attached to this [4Fe-4S] cluster using CoM-(33)SH as substrate and purified Hdr from Methanothermobacter marburgensis and Methanosarcina barkeri. With both enzymes treatment with CoM-(33)SH in the presence of duroquinone as an oxidant resulted in a significant broadening of the electron paramagnetic resonance spectrum as compared to CoM-SH as substrate. The signal broadening resulted from an unresolved anisotropic hyperfine coupling between the (33)S nucleus and the paramagnetic center. The results provide compelling evidence for a direct binding of CoM-SH to the [4Fe-4S] cluster in the active site of the enzyme.     

海洋沉积物中铁还原细菌组成及异化铁还原与产氢性质分析

【背景】一些铁还原细菌具有异化铁还原与产氢的能力,该类细菌在环境污染修复的同时能够解决能源问题。【目的】从海洋沉积物中富集获得异化铁还原菌群,明确混合菌群组成、异化铁还原及产氢性质。获得海洋沉积物中异化铁还原混合菌群组成,分析菌群异化铁还原和产氢性质。【方法】利用高通量测序技术分析异化铁还原菌群的优势菌组成,在此基础上,分析异化铁还原混合菌群在不同电子供体培养条件下异化铁还原能力和产氢性质。【结果】高通量数据表明,在不溶性氢氧化铁为电子受体和葡萄糖为电子供体厌氧培养条件下,混合菌群的优势菌属主要是梭菌(Clostridium),属于发酵型异化铁还原细菌。混合菌群能够利用电子供体蔗糖、葡萄糖以及丙酮酸钠进行异化铁还原及发酵产氢。葡萄糖为电子供体时,菌群累积产生Fe(Ⅱ)浓度和产氢量最高,分别是59.34±6.73 mg/L和629.70±11.42 mL/L。【结论】异化铁还原混合菌群同时具有异化铁还原和产氢能力,拓宽了发酵型异化铁还原细菌的种质资源,探索异化铁还原细菌在生物能源方面的应用。     

Immunocytochemical localization of the coenzyme F420-reducing hydrogenase in Methanosarcina barkeri Fusaro.

The cytological localization of the 8-hydroxy-5-deazaflavin (coenzyme F420)-reducing hydrogenase of Methanosarcina barkeri Fusaro was determined by immunoelectron microscopy, using a specific polyclonal rabbit antiserum raised against the homogeneous deazaflavin-dependent enzyme. In Western blot (immunoblot) experiments this antiserum reacted specifically with the native coenzyme F420-reducing hydrogenase, but did not cross-react with the coenzyme F420-nonreducing hydrogenase activity also detectable in crude extracts prepared from methanol-grown Methanosarcina cells. Immunogold labelling of ultrathin sections of anaerobically fixed methanol-grown cells from the exponential growth phase revealed that the coenzyme F420-reducing hydrogenase was predominantly located in the vicinity of the cytoplasmic membrane. From this result we concluded that the deazaflavin-dependent hydrogenase is associated with the cytoplasmic membrane in intact cells of M. barkeri during growth on methanol as the sole methanogenic substrate, and a possible role of this enzyme in the generation of the electrochemical proton gradient is discussed.     

Acetogens and acetoclastic methanosarcinales govern methane formation in abandoned coal mines

In abandoned coal mines, methanogenic archaea are responsible for the production of substantial amounts of methane. The present study aimed to directly unravel the active methanogens mediating methane release as well as active bacteria potentially involved in the trophic network. Therefore, the stable-isotope-labeled precursors of methane, [(13)C]acetate and H(2)-(13)CO(2), were fed to liquid cultures from hard coal and mine timber from a coal mine in Germany. Guided by methane production rates, samples for DNA stable-isotope probing (SIP) with subsequent quantitative PCR and denaturing gradient gel electrophoretic (DGGE) analyses were taken over 6 months. Surprisingly, the formation of [(13)C]methane was linked to acetoclastic methanogenesis in both the [(13)C]acetate- and the H(2)-(13)CO(2)-amended cultures of coal and timber. H(2)-(13)CO(2) was used mainly by acetogens related to Pelobacter acetylenicus and Clostridium species. Active methanogens, closely affiliated with Methanosarcina barkeri, utilized the readily available acetate rather than the thermodynamically more favorable hydrogen. Thus, the methanogenic microbial community appears to be highly adapted to the low-H(2) conditions found in coal mines.     

互营氧化产甲烷微生物种间电子传递研究进展

甲烷是重要的温室气体,也是典型的可再生性生物质能源。目前约70%的大气甲烷排放来源于产甲烷微生物过程。在产甲烷环境中,产甲烷菌与互营细菌形成互营关系,从而克服有机质厌氧分解反应的热力学能垒,实现短链脂肪酸和醇类物质的互营氧化产甲烷过程。该过程中,种间电子传递是关键步骤。本文首先概述了甲烷的研究意义及微生物互营降解有机质产甲烷的过程,然后分别综述了种间H2转移、种间甲酸转移和种间直接电子传递这3种种间电子传递机制的起源、发展、研究现状和未来所需要解决的研究问题。     

Inhibition of Methanogenesis by Methyl Fluoride: Studies of Pure and Defined Mixed Cultures of Anaerobic Bacteria and Archaea

Methyl fluoride (fluoromethane [CH(inf3)F]) has been used as a selective inhibitor of CH(inf4) oxidation by aerobic methanotrophic bacteria in studies of CH(inf4) emission from natural systems. In such studies, CH(inf3)F also diffuses into the anaerobic zones where CH(inf4) is produced. The effects of CH(inf3)F on pure and defined mixed cultures of anaerobic microorganisms were investigated. About 1 kPa of CH(inf3)F, similar to the amounts used in inhibition experiments, inhibited growth of and CH(inf4) production by pure cultures of aceticlastic methanogens (Methanosaeta spp. and Methanosarcina spp.) and by a methanogenic mixed culture of anaerobic microorganisms in which acetate was produced as an intermediate. With greater quantities of CH(inf3)F, hydrogenotrophic methanogens were also inhibited. At a partial pressure of CH(inf3)F of 1 kPa, homoacetogenic, sulfate-reducing, and fermentative bacteria and a methanogenic mixed culture of anaerobic microorganisms based on hydrogen syntrophy were not inhibited. The inhibition by CH(inf3)F of the growth and CH(inf4) production of Methanosarcina mazei growing on acetate was reversible. CH(inf3)F inhibited only acetate utilization by Methanosarcina barkeri, which is able to use acetate and hydrogen simultaneously, when both acetate and hydrogen were present. These findings suggest that the use of CH(inf3)F as a selective inhibitor of aerobic CH(inf4) oxidation in undefined systems must be interpreted with great care. However, by a careful choice of concentrations, CH(inf3)F may be useful for the rapid determination of the role of acetate as a CH(inf4) precursor.     

Sulfate-Dependent Interspecies H(2) Transfer between Methanosarcina barkeri and Desulfovibrio vulgaris during Coculture Metabolism of Acetate or Methanol

We compared the metabolism of methanol and acetate when Methanosarcina barkeri was grown in the presence and absence of Desulfovibrio vulgaris. The sulfate reducer was not able to utilize methanol or acetate as the electron donor for energy metabolism in pure culture, but was able to grow in coculture. Pure cultures of M. barkeri produced up to 10 mumol of H(2) per liter in the culture headspace during growth on acetate or methanol. In coculture with D. vulgaris, the gaseous H(2) concentration was 相似文献   

Magnetite production and transformation in the methanogenic consortia from coastal riverine sediments

Minerals that contain ferric iron, such as amorphous Fe(III) oxides (A), can inhibit methanogenesis by competitively accepting electrons. In contrast, ferric iron reduced products, such as magnetite (M), can function as electrical conductors to stimulate methanogenesis, however, the processes and effects of magnetite production and transformation in the methanogenic consortia are not yet known. Here we compare the effects on methanogenesis of amorphous Fe (III) oxides (A) and magnetite (M) with ethanol as the electron donor. RNA-based terminal restriction fragment length polymorphism with a clone library was used to analyse both bacterial and archaeal communities. Iron (III)-reducing bacteria including Geobacteraceae and methanogens such as Methanosarcina were enriched in iron oxide-supplemented enrichment cultures for two generations with ethanol as the electron donor. The enrichment cultures with A and non-Fe (N) dominated by the active bacteria belong to Veillonellaceae, and archaea belong to Methanoregulaceae and Methanobacteriaceae, Methanosarcinaceae (Methanosarcina mazei), respectively. While the enrichment cultures with M, dominated by the archaea belong to Methanosarcinaceae (Methanosarcina barkeri). The results also showed that methanogenesis was accelerated in the transferred cultures with ethanol as the electron donor during magnetite production from A reduction. Powder X-ray diffraction analysis indicated that magnetite was generated from microbial reduction of A and M was transformed into siderite and vivianite with ethanol as the electron donor. Our data showed the processes and effects of magnetite production and transformation in the methanogenic consortia, suggesting that significantly different effects of iron minerals on microbial methanogenesis in the iron-rich coastal riverine environment were present.     

Incorporation of [methyl-3H]thymidine by obligate and facultative anaerobic bacteria when grown under defined culture conditions

Abstract Incorporation of [ methyl -³H]thymidine into bacterial DNA was determined for a range of axenic anaerobic bacterial cultures: fermentative heterotrophs, sulphate-reducing bacteria, purple sulphur bacteria, acetogens and methanogens. Anaerobically growing Bacillus sp. and the obligate aerobe Thiobacillus ferrooxidans were also investigated. Actively growing cultures of sulphate-reducing bacteria belonging to the genera Desulfovibrio, Desulfotomaculum, Desulfobacter, Desulfobotulus and Desulfobulbus , purple sulphur bacteria ( Chromatium vinosum OP2 and Thiocapsa roseopersicina OP1), methanogens ( Methanococcus GS16 and Methanosarcina barkeri ) and an acetogen ( Acetobacterium woodii ) did not incorporate [ methyl -³H]thymidine into DNA. The only obligate anaerobes in which thymidine incorporation into DNA could be unequivocally demonstrated were members of the genus Clostridium . Anaerobically growing Bacillus sp. also incorporated thymidine. These data demonstrate that pure culture representatives of major groups of anaerobic bacteria involved in the terminal oxidation of organic carbon and anoxygenic phototrophs within sediments are unable to incorporate [ methyl -³H]thymidine into DNA, although some obligate and facultative anaerobes can. Variability in thymidine incorporation amongst pure culture isolates indicates that unless existing techniques can be calibrated to take this into consideration then productivity estimates in both aerobic and anaerobic environments may be greatly underestimated using the [ methyl -³H]thymidine technique.     

异化铁还原细菌Clostridium sp.LQ25分离及其产氢与铁还原特性

[背景] 一些异化铁还原细菌兼具铁还原和发酵产氢能力,可作为发酵型异化铁还原细菌还原机制研究的对象。[目的] 筛选出一株发酵型异化铁还原细菌。在异化铁还原细菌培养体系中,设置不同电子供体并分析电子供体。[方法] 通过三层平板法从海洋沉积物中筛选纯菌株,基于16S rRNA基因序列进行菌株鉴定。通过测定细菌培养液Fe （II）浓度及发酵产氢量分析菌株异化铁还原和产氢性质。[结果] 菌株LQ25与Clostridium butyricum的16S rRNA基因序列相似性达到100%,结合电镜形态观察,菌株命名为Clostridium sp.LQ25。在氢氧化铁为电子受体培养条件下,菌株生长较对照组（未添加氢氧化铁）显著提高。菌株LQ25能够利用丙酮酸钠、葡萄糖和乳酸钠进行生长。丙酮酸钠为电子供体时,菌株LQ25细胞生长和异化铁还原效率最高,菌体蛋白质含量是（78.88±3.40） mg/L,累积产生Fe （II）浓度为（8.27±0.23） mg/L。以葡萄糖为电子供体时,菌株LQ25发酵产氢量最高,达（475.2±14.4） mL/L,相比对照组（未添加氢氧化铁）产氢量提高87.7%。[结论] 筛选到一株具有异化铁还原和发酵产氢能力的菌株Clostridium sp.LQ25,为探究发酵型异化铁还原细菌胞外电子传递机制提供了新的实验材料。