芦岭煤田微生物群落结构和生物成因气的产甲烷类型研究

【目的】揭示芦岭煤田微生物群落组成,并分析其潜在的产甲烷类型及产甲烷途径。【方法】采集芦岭煤田的煤层气样品和产出水样品,分别分析样品的地球化学性质特征;利用Illumina HiSeq高通量测序技术分析产出水中的微生物群落结构;采用添加不同底物的厌氧培养实验进一步证实芦岭煤田生物成因气的产甲烷类型。【结果】该地区煤层气为生物成因和热成因的混合成因气;古菌16S rRNA基因分析表明在产出水中含有乙酸营养型、氢营养型和甲基营养型的产甲烷菌。丰度较高的细菌具有降解煤中芳香族和纤维素衍生化合物的潜力。厌氧富集培养结果表明,添加乙酸盐、甲酸盐、H2+CO2为底物的矿井水样均有明显的甲烷产生。【结论】芦岭煤田具有丰富的生物多样性,该地区同时存在三种产甲烷类型。本研究为利用微生物技术提高煤层气的采收率,实现煤层气的可持续开采提供科学依据。     

丁酸氧化菌群对抗生素及活性炭协同作用响应

本研究构建了以丁酸为唯一碳源的厌氧消化反应器,利用16S rRNA基因测序技术分析氯四环素(Chlortetracycline,CTC)单独抑制及CTC与颗粒活性炭(Granular active carbon,GAC)协同作用下,互营丁酸氧化微生物群落结构的动态变化,探究环境胁迫下微生物之间的相互作用及其对CTC及CTC和GAC协同作用的响应。结果表明,原始反应器群落中,已知的互营丁酸氧化菌Syntrophomonas(11.6%)和乙酸营养型产甲烷古菌Methanosaeta(48.5%)分别在细菌和古菌群落中占主导优势。添加40mg/L和50 mg/L CTC条件下,甲烷产量分别降低40.4%和49.3%。Syntrophomonas对CTC表现出耐受性,但与其呈正相关联系的细菌(如unclassified Firmicutes和unclassified Comamonadaceae)以及乙酸氧化菌Tepidanaerobacter活性被CTC明显抑制,从而影响丁酸降解率,同时造成代谢产物积累,导致产甲烷量降低。单独添加GAC以及在40 mg/L和50 mg/L CTC抑制下添加GAC,甲烷产量分别降低2.9%、48.5%和64.7%。共现网络分析结果显示,添加GAC明显增强了Geobacter以及与其呈正相关联系的细菌(Azonexus等)的活性。而产甲烷古菌Methanosaeta和Methanoculleus与Azonexus等大部分细菌呈负相关,因此,添加GAC可能间接影响了产甲烷古菌的活性。     

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。     

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。     

寺河矿煤地质产甲烷微生物菌群的保藏和产甲烷性能

【背景】煤地质产甲烷微生物菌群可以代谢煤基质产生甲烷,对于实现煤层气资源的再利用具有重要意义。【目的】检测产甲烷菌群在保藏过程中群落结构的动态变化以及在产气实验中甲烷气的生成情况,以验证保藏方法的可行性,同时为煤层气的微生物增产奠定基础。【方法】分别于不同温度条件下比较3种菌种保藏方法,即甘油/L-半胱氨酸法、富营养法和煤基-基础盐法。通过产气实验检测不同保藏条件下产甲烷菌群的活力。同时,采用454高通量测序技术测定16S r RNA基因序列,分析25°C条件下煤基-基础盐菌种保藏过程中微生物群落结构的变化。【结果】比较了9组菌种保藏方法,发现菌种最佳保藏条件为25°C的煤基-基础盐保藏。在该条件下保藏的产甲烷菌群活性最高,甲烷生成量最大。以无烟煤为碳源进行产气实验时甲烷生成量为12%-25%,而以褐煤为碳源时甲烷生成量可达24%-73%。在25°C的煤基-基础盐菌种保藏条件下,保藏初期细菌的主要优势菌为假单胞菌属(Pseudomonas),而古菌的主要优势菌为甲烷八叠球菌属(Methanosarcina)。随着保藏时间的增加,细菌的群落结构变化显著,发酵细菌及产氢产乙酸细菌成为优势细菌,古菌的群落结构则相对稳定。【结论】菌种保藏的最佳条件为25°C的煤基-基础盐,保藏的产甲烷菌群能长期维持在较高的活性状态,具有较好的产甲烷能力。     

不同成熟度煤样产甲烷潜力

摘要:【目的】评估不同类型煤炭生物降解转化为甲烷的潜力,研究原位煤层的微生物群落结构特征。【方法】分别在原位模拟、补加烃降解产甲烷菌系和补加碳源下厌氧培养煤样,利用气相色谱监测甲烷产生趋势,及高通量测序技术研究原位煤层的细菌和古菌群落。【结果】10个样品中有3个高成熟度煤样可以被厌氧降解转化为甲烷。通过生物强化和添加外源底物可以促进HF煤样的产甲烷潜力。其中SL 煤样中的古菌类群主要是氢营养型产甲烷菌Methanoculleus和乙酸营养型产甲烷菌Methanosaeta为主,细菌类群主要 属于Firmicutes(54.4%)、Proteobacteria(30.9%)、未培养微生物(10.8%)、Caldiserica(1.5%)及Thermotogae(1.3%)。【结论】不同成熟度煤样降解产气潜力不同,在部分原位煤层中可能存在参与烃降解与甲烷产生的功能菌。     

以pH为扰动因子探究电化学厌氧消化产甲烷代谢通量与微生物的关系

【背景】电化学厌氧消化(electrochemical anaerobic digestion,EAD)系统的代谢途径由具备不同功能的微生物所主导,其代谢通量与功能微生物丰度、活性及群落结构相关。【目的】探究EAD产甲烷代谢通量与微生物的关系。【方法】采用代谢通量分析(metabolic flux analysis,MFA)方法,以pH为扰动因子得到微生物群落与产甲烷通量的响应关系。【结果】pH 7.5扰动时产甲烷通量最大为0.398 4±0.029 3,较对照组(pH 6.9)的0.297 4±0.012 7和扰动组(pH 6.3)的0.136 5±0.012 0分别提高了25%和65%。另外,平均有33.8%±3.1%的氢气(通量)用于还原二氧化碳产甲烷和乙酸,平均有21.0%±2.6%的乙酸(通量)转化为甲烷。此外,产甲烷通量与Mariniphaga、Methanosaeta和Desulfomicrobium的丰度呈正相关,与Sedimentibacter的丰度呈负相关且影响显著。【结论】在EAD产甲烷体系中产甲烷菌和产酸菌共存时,pH值略大于7.0的环境有利于甲烷的生成,改变E...     

不同生境微生物转化H2/CO2产乙酸及其在合成气发酵中应用

【目的】合成气发酵对大力开发可再生资源和促进国家可持续发展具有重要意义,研究旨在探究不同生境微生物转化H2/CO2产乙酸及其合成气发酵的潜力。【方法】采集剩余污泥、牛粪、产甲烷污泥和河道底物样品在中温(37 °C)条件下生物转化H2/CO2气体,将来源于牛粪样品的H2/CO2转化富集物用于合成气发酵,通过454高通量技术和定量PCR技术分析复杂微生物群落的组成,GC气相色谱法检测气体转化产生的挥发性脂肪酸(VFAs)浓度。【结果】牛粪和剩余污泥微生物利用H2/CO2气体生成乙酸、乙醇和丁酸等,最高乙酸浓度分别为63 mmol/L和40 mmol/L,明显高于河道底物和产甲烷污泥样品的最高乙酸浓度3 mmol/L和16 mmol/L。牛粪和剩余污泥微生物中含有种类多样化的同型产乙酸菌,剩余污泥中同型产乙酸菌主要为Clostridium spp.、Sporomusa malonica和Acetoanaerobium noterae,牛粪中则为Clostridium spp.、Treponema azotonutricium和Oxobacter pfennigii。【结论】同型产乙酸菌的丰富度和数量两个因素都对复杂微生物群落转化H2/CO2产乙酸效率至关重要;转化H2/CO2得到的富集物可用于合成气发酵产乙酸和乙醇,这为基于混合培养技术的合成气发酵提供了依据。     

不同生境微生物转化H_2/CO_2产乙酸及其在合成气发酵中应用（英文）

【目的】合成气发酵对大力开发可再生资源和促进国家可持续发展具有重要意义,研究旨在探究不同生境微生物转化H_2/CO_2产乙酸及其合成气发酵的潜力。【方法】采集剩余污泥、牛粪、产甲烷污泥和河道底物样品在中温(37°C)条件下生物转化H_2/CO_2气体,将来源于牛粪样品的H_2/CO_2转化富集物用于合成气发酵,通过454高通量技术和定量PCR技术分析复杂微生物群落的组成,GC气相色谱法检测气体转化产生的挥发性脂肪酸(VFAs)浓度。【结果】牛粪和剩余污泥微生物利用H_2/CO_2气体生成乙酸、乙醇和丁酸等,最高乙酸浓度分别为63 mmol/L和40 mmol/L,明显高于河道底物和产甲烷污泥样品的最高乙酸浓度3 mmol/L和16 mmol/L。牛粪和剩余污泥微生物中含有种类多样化的同型产乙酸菌,剩余污泥中同型产乙酸菌主要为Clostridium spp.、Sporomusa malonica和Acetoanaerobium noterae,牛粪中则为Clostridium spp.、Treponema azotonutricium和Oxobacter pfennigii。【结论】同型产乙酸菌的丰富度和数量两个因素都对复杂微生物群落转化H_2/CO_2产乙酸效率至关重要;转化H_2/CO_2得到的富集物可用于合成气发酵产乙酸和乙醇,这为基于混合培养技术的合成气发酵提供了依据。     

Enrichment of acetate-, propionate-, and butyrate-degrading co-cultures from the biofilm of an anaerobic fluidized bed reactor

Summary Scanning electron microphotographs from the biofilm of a pilot scale anaerobic fluid-ized-bed reactor fed with acetate, propionate, and butyrate as carbon sources showed a predominance of filamentous organisms resembling Methanothrix sp. which could be isolated as an al-most pure culture as well as a Methanosarcina strain. Three syntrophic cultures, enriched in the medium of Boone and Xun, contained four or five microscopically distinguishable microorganisms, among them Methanospirillum sp., Methanothrix sp., Methanosarcina sp., and rods of acetogenic bacteria degrading propionate or butyrate effectively.     

Anaerobic degradation of volatile fatty acids at different sulphate concentrations

The effect of sulfate on the anaerobic breakdown of mixtures of acetate, propionate and butyrate at three different sulfate to fatty acid ratios was studied in upflow anaerobic sludge blanket reactors. Sludge characteristics were followed with time by means of sludge activity tests and by enumeration of the different physiological bacterial groups. At each sulfate concentration acetate was completely converted into methane and CO₂, and acetotrophic sulfate-reducing bacteria were not detected. Hydrogenotrophic methanogenic bacteria and hydrogenotrophic sulfate-reducing bacteria were present in high numbers in the sludge of all reactors. However, a complete conversion of H₂ by sulfate reducers was found in the reactor operated with excess sulfate. At higher sulfate concentrations, oxidation of propionate by sulfate-reducing bacteria became more important. Only under sulfate-limiting conditions did syntrophic propionate oxidizers out-compete propionate-degrading sulfate reducers. Remarkably, syntrophic butyrate oxidizers were well able to compete with sulfate reducers for the available butyrate, even with an excess of sulfate. Correspondence to: A. Visser     

Typical methanogenic inhibitors can considerably alter bacterial populations and affect the interaction between fatty acid degraders and homoacetogens

The effects of two typical methanogenic inhibitors [2-bromoethanesulfonate (BES) and chloroform (CHCl₃)] on the bacterial populations were investigated using molecular ecological techniques. Terminal restriction fragment length polymorphism analyses (T-RFLP) in combination with clone library showed that both the toxicants not only inhibited methanogenic activity but also considerably altered the bacterial community structure. Species of low % G + C Gram-positive bacteria (Clostridiales), high % G + C Actinomycetes, and uncultured Chloroflexi showed relatively greater tolerance of CHCl₃, whereas the BES T-RFLP patterns were characterized by prevalence of Geobacter hydrogenophilus and homoacetogenic Moorella sp. In addition, due to indirect thermodynamic inhibition caused by high hydrogen partial pressures, the growth of obligately syntrophic acetogenic Syntrophomonas and Syntrophobacter was also affected by selective inhibition of methanogenesis. Interestingly, by comparing the fermentative intermediates detected in BES- and CHCl₃-treated experiments, it was furthermore found that when methanogenesis is specifically inhibited, the syntrophic interaction between hydrogen-producing fatty acid degraders and hydrogen-utilizating homoacetogens seemed to be strengthened.     

Fatty Acid-Oxidizing Consortia along a Nutrient Gradient in the Florida Everglades

The Florida Everglades is one of the largest freshwater marshes in North America and has been subject to eutrophication for decades. A gradient in P concentrations extends for several kilometers into the interior of the northern regions of the marsh, and the structure and function of soil microbial communities vary along the gradient. In this study, stable isotope probing was employed to investigate the fate of carbon from the fermentation products propionate and butyrate in soils from three sites along the nutrient gradient. For propionate microcosms, 16S rRNA gene clone libraries from eutrophic and transition sites were dominated by sequences related to previously described propionate oxidizers, such as Pelotomaculum spp. and Syntrophobacter spp. Significant representation was also observed for sequences related to Smithella propionica, which dismutates propionate to butyrate. Sequences of dominant phylotypes from oligotrophic samples did not cluster with known syntrophs but with sulfate-reducing prokaryotes (SRP) and Pelobacter spp. In butyrate microcosms, sequences clustering with Syntrophospora spp. and Syntrophomonas spp. dominated eutrophic microcosms, and sequences related to Pelospora dominated the transition microcosm. Sequences related to Pelospora spp. and SRP dominated clone libraries from oligotrophic microcosms. Sequences from diverse bacterial phyla and primary fermenters were also present in most libraries. Archaeal sequences from eutrophic microcosms included sequences characteristic of Methanomicrobiaceae, Methanospirillaceae, and Methanosaetaceae. Oligotrophic microcosms were dominated by acetotrophs, including sequences related to Methanosarcina, suggesting accumulation of acetate.     

青藏高原三个盐碱湖的产甲烷菌群和产甲烷代谢途径分析

【目的】分析青藏高原不同类型盐碱湖中的优势产甲烷菌群和优势产甲烷代谢途径。【方法】以不同盐度和植被类型的公珠错、昆仲错和无植被的兹格塘错的沉积物为研究对象,通过高通量测序和q PCR定量古菌16S r RNA多样性分析优势古菌类群;模拟原位盐浓度及p H,比较不同产甲烷底物(甲醇、三甲胺、乙酸和H_2/CO_2)富集沉积物的产甲烷速率,分析其优势产甲烷菌代谢类型。通过添加产甲烷抑制剂(2-溴乙烷磺酸盐),检测沉积物中产甲烷底物积累,确定不同盐碱湖中主要的产甲烷途径。【结果】昆仲错的优势菌群包括甲基/乙酸型的甲烷八叠球菌科(Methanosarcinaceae,11%),乙酸型的甲烷鬃菌科(Methanosaetaceae,7.9%)和氢型甲烷菌甲烷杆菌目(Methanomicrobiales,7.4%);公珠错和兹格塘错的优势菌群为甲烷鬃菌科(Methanosaetaceae)分别占15%和15.3%,及甲烷杆菌属(Methanobacterium)和甲基型的甲烷叶菌属(Methanolobus)。公珠错和昆仲错分别以乙酸和甲醇产甲烷速率最高,而兹格塘错从不同底物产甲烷速率无差异。抑制甲烷产生后,公珠错主要积累乙酸,昆仲错主要积累甲醇;兹格塘错不仅甲烷排放低,也无产甲烷物质显著积累。【结论】昆仲错沉积物中的甲烷主要来自甲醇,公珠错中的甲烷主要来自乙酸,而兹格塘错产甲烷和底物积累不活跃。因而推测高原盐碱湖主要的产甲烷途径和菌群可能与周围植被类型的相关性更高,而与盐度的直接相关性较低。     

Phylogenetic and functional diversity of propionate-oxidizing bacteria in an anaerobic digester sludge

The phylogenetic and functional diversity of syntrophic propionate-oxidizing bacteria (POB) present in an anaerobic digester was investigated by microautoradiography combined with fluorescent in situ hybridization (MAR–FISH) that can directly link 16S rRNA phylogeny with in situ metabolic function. The syntrophic POB community in the anaerobic digester sludge consisted of at least four phylogenetic groups: Syntrophobacter, uncultured short rod Smithella (Smithella sp. SR), uncultured long rod Smithella (Smithella sp. LR), and an unidentified group. The activities of these POB groups were dependent on the propionate concentrations. The uncultured Smithella sp. SR accounted for 52–62% of the total active POB under all the propionate concentrations tested (0.5–15 mM). In contrast, uncultured Smithella sp. LR was active only at lower propionate concentrations and became a dominant active POB at 0.5 mM of propionate. Syntrophobacter accounted for 16–31% of the total active POB above 2.5 mM propionate, whereas the active Syntrophobacter population became low (ca. 6%) at 0.5 mM of propionate. The anaerobic digester was operated in a fill and draw mode, resulting in periodical changes in propionate concentration ranging from 0 to 10 mM. These phylogenetically and functionally diverse, to some extent functionally redundant, active POB communities were dynamically responding to the periodical changes in propionate concentration.     

Anaerobic Degradation of Normal- and Branched-Chain Fatty Acids with Four or More Carbons to Methane by a Syntrophic Methanogenic Triculture

Syntrophic degradation of normal- and branched-chain fatty acids with 4 to 9 carbons was investigated with a mesophilic syntrophic isobutyrate-butyrate-degrading triculture consisting of the non-spore-forming, syntrophic, fatty acid-degrading, gram-positive rod-shaped strain IB, Methanobacterium formicicum T1N, and Methanosarcina mazei T18. This triculture converted butyrate and isobutyrate to methane and converted valerate and 2-methylbutyrate to propionate and methane. This triculture also degraded caproate, 4-methylvalerate, heptanoate, 2-methylhexanoate, caprylate, and pelargoate. During the syntrophic conversion of isobutyrate and butyrate, a reversible isomerization between butyrate and isobutyrate occurred; isobutyrate and butyrate were isomerized to the other isomeric form to reach nearly equal concentrations and then their concentrations decreased at the same rates. Butyrate was an intermediate of syntrophic isobutyrate degradation. When butyrate was degraded in the presence of propionate, 2-methylbutyrate was synthesized from propionate and isobutyrate formed from butyrate. During the syntrophic degradation of valerate, isobutyrate, butyrate, and 2-methylbutyrate were formed and then degraded. During syntrophic degradation of 2-methylbutyrate, isobutyrate and butyrate were formed and then degraded.     

Stable-Isotope Probing of Microorganisms Thriving at Thermodynamic Limits: Syntrophic Propionate Oxidation in Flooded Soil

Propionate is an important intermediate of the degradation of organic matter in many anoxic environments. In methanogenic environments, due to thermodynamic constraints, the oxidation of propionate requires syntrophic cooperation of propionate-fermenting proton-reducing bacteria and H₂-consuming methanogens. We have identified here microorganisms that were active in syntrophic propionate oxidation in anoxic paddy soil by rRNA-based stable-isotope probing (SIP). After 7 weeks of incubation with [¹³C]propionate (<10 mM) and the oxidation of ~30 μmol of ¹³C-labeled substrate per g dry weight of soil, we found that archaeal nucleic acids were ¹³C labeled to a larger extent than those of the bacterial partners. Nevertheless, both terminal restriction fragment length polymorphism and cloning analyses revealed Syntrophobacter spp., Smithella spp., and the novel Pelotomaculum spp. to predominate in “heavy” ¹³C-labeled bacterial rRNA, clearly showing that these were active in situ in syntrophic propionate oxidation. Among the Archaea, mostly Methanobacterium and Methanosarcina spp. and also members of the yet-uncultured “rice cluster I” lineage had incorporated substantial amounts of ¹³C label, suggesting that these methanogens were directly involved in syntrophic associations and/or thriving on the [¹³C]acetate released by the syntrophs. With this first application of SIP in an anoxic soil environment, we were able to clearly demonstrate that even guilds of microorganisms growing under thermodynamic constraints, as well as phylogenetically diverse syntrophic associations, can be identified by using SIP. This approach holds great promise for determining the structure and function relationships of further syntrophic or other nutritional associations in natural environments and for defining metabolic functions of yet-uncultivated microorganisms.     

Effects of the antimicrobial tylosin on the microbial community structure of an anaerobic sequencing batch reactor

The effects of the antimicrobial tylosin on a methanogenic microbial community were studied in a glucose‐fed laboratory‐scale anaerobic sequencing batch reactor (ASBR) exposed to stepwise increases of tylosin (0, 1.67, and 167 mg/L). The microbial community structure was determined using quantitative fluorescence in situ hybridization (FISH) and phylogenetic analyses of bacterial 16S ribosomal RNA (rRNA) gene clone libraries of biomass samples. During the periods without tylosin addition and with an influent tylosin concentration of 1.67 mg/L, 16S rRNA gene sequences related to Syntrophobacter were detected and the relative abundance of Methanosaeta species was high. During the highest tylosin dose of 167 mg/L, 16S rRNA gene sequences related to Syntrophobacter species were not detected and the relative abundance of Methanosaeta decreased considerably. Throughout the experimental period, Propionibacteriaceae and high GC Gram‐positive bacteria were present, based on 16S rRNA gene sequences and FISH analyses, respectively. The accumulation of propionate and subsequent reactor failure after long‐term exposure to tylosin are attributed to the direct inhibition of propionate‐oxidizing syntrophic bacteria closely related to Syntrophobacter and the indirect inhibition of Methanosaeta by high propionate concentrations and low pH. Biotechnol. Bioeng. 2011;108: 296–305. © 2010 Wiley Periodicals, Inc.     

The effect of sulfate and nitrate on methane formation in a freshwater sediment

A freshwater sediment from a ditch of a peat grassland near Zegveld (Province of Utrecht, The Netherlands) was investigated for its potential methanogenic and syntrophic activity and the influence of sulfate and nitrate on these potential activities. Methanogenesis started after a 10 days lagphase. After 35–40 days aceticlastic methanogens were sufficiently enriched to cause a net decrease of acetate. In the presence of sulfate methane formation was only slightly affected. The addition of nitrate led to an outcompetion of aceticlastic methanogens by nitrate reducers. When inorganic electron acceptors were absent, substrates like propionate and butyrate were converted by syntrophic methanogenic consortia. Addition of inorganic electron acceptors resulted in an outcompetition of the syntrophic propionate and butyrate degrading consortia by the sulfate and nitrate reducers.