青海湖3种类型高寒湿地甲烷氧化菌群落特征

【背景】甲烷氧化菌在维持湿地生态系统碳平衡方面发挥着重要作用,青海湖高寒湿地具有十分重要的生态地位,但目前有关该地区甲烷氧化菌的研究相对较少。【目的】探究不同类型高寒湿地土壤甲烷氧化菌的群落特征与驱动因素。【方法】以青海湖流域内的小泊湖沼泽湿地、鸟岛湖滨湿地、瓦颜山河源湿地为研究对象,通过高通量测序技术对土壤甲烷氧化菌进行检测。【结果】3种不同类型高寒湿地土壤甲烷氧化菌的优势菌门均为变形菌门(Proteobacteria)。鸟岛湖滨湿地与瓦颜山河源湿地的甲烷氧化菌α多样性存在显著差异(P<0.05),而小泊湖沼泽湿地与二者的甲烷氧化菌α多样性的差异不显著(P>0.05)。LEfSe分析表明,不同类型高寒湿地共存在40个差异菌群,尤以瓦颜山河源湿地差异菌群数量最多,从门到属水平均存在显著差异。冗余分析(redundancy analysis,RDA)表明,甲烷氧化菌菌群变化的主要驱动因子为土壤温度、土壤水分、电导率。【结论】整体而言,青海湖3种类型高寒湿地土壤理化性质及甲烷氧化菌群落多样性均存在差异,且部分菌群的相对丰度具有显著性差异(P<0.05)。     

油藏注入水靶向脱硫潜力的高温脱硫菌群富集驯化

【背景】海上油田见聚后产出水硫化物超标,影响到注聚水的配聚黏度,采用生物脱硫时,由于常规除硫菌难以适应除油后产出液的高温,使得脱硫效果不佳。【目的】分析海上采出液水处理过程的菌群结构,明确生物处理各节点的菌群构成变化;开展耐高温脱硫菌驯化筛选,获得耐高温的高效脱硫菌。【方法】采集来自胜利油田海三站的水样,以16S rRNA基因高通量测序技术分析样本菌群结构,并分别在不同温度(55、60和65℃)下的无机富集培养基中进行多轮转接驯化,结合常压室温等离子体(atmospheric and room temperature plasma, ARTP)诱变技术筛选获得耐高温的脱硫菌群,采用宏基因组测序技术分析富集菌群的组成,并测定其脱硫能力。【结果】处理前的采出液水样含有较多的嗜热菌和硫酸盐还原菌,如Thermodesulfovibrio、Pseudothermotoga、Thermolithobacter、Fervidobacterium、Thermovenabulales和Pseudomonas;以厌氧气浮除油工艺处理的出水中,嗜氢菌属(Hydrogenophilus)成为最主要的优势菌,...     

汉阳陵陶俑表面微生物群落结构与种群多样性分析

【背景】汉阳陵是我国截至目前发现的规模最大、陪葬级别最高的汉代陶俑群,出土了大量形神毕肖的裸体俑群,考古学家认为这种裸体陶俑原本“着衣、装木臂”,称为“着衣式陶俑”,为皇室独有,异常珍贵。然而这些推测尚无科学依据,而且陶俑表面附着微生物可能会腐蚀俑体。【目的】通过比较研究汉陶俑表面微生物的组成差异,为汉裸体陶俑着有衣物且装有断臂的推测提供一定的科学佐证,同时为汉陶俑微生物腐蚀的防控提供靶标。【方法】应用微生物高通量测序与纯培养相结合的方法,对着衣式陶俑不同部位微生物进行测定。【结果】高通量测序结果显示女俑头部微生物多样性较高;男俑上半身微生物多样性最高,腿部居中,头部较低。汉陶俑表面微生物组成按俑的类别及不同部位聚集在一起,其优势菌为放线菌门的克洛斯氏菌属、糖多孢菌属、假诺卡氏菌属及链霉菌科,其他各部位优势类群相对丰度存在差异,断臂处与碳循环相关功能微生物的相对丰度最高。纯培养结果显示女俑头部的可培养细菌数量高于男俑头部可培养的细菌数量;男俑上身与腿部可培养的微生物数量高于男俑头部,表明上半身与腿部可能有衣物覆盖,导致其营养差异。【结论】汉陶俑头部与身体表面部位微生物多样性与组成存在明...     

肠道菌群：肠道干细胞增殖分化的调节者

肠道干细胞(intestinal stem cells, ISCs)是肠道各类上皮细胞的来源,通过平衡增殖与分化维持肠道稳态。同时,肠道菌群及其代谢物在维持宿主肠道稳态中也发挥着重要作用。随着技术的发展,研究者认识到ISCs与肠道菌群之间存在相互作用。研究表明,ISCs对上皮细胞亚型的调控影响肠道菌群的组成,并且肠道菌群及其代谢物也影响ISCs介导的上皮发育。本文阐述了ISCs分化对肠道菌群的影响,重点总结了肠道菌群及其代谢物调控ISCs增殖分化的研究进展,从菌群调控ISCs的角度探讨肠道损伤的治疗思路,并对未来可能的研究方向进行讨论。     

二苯醚类除草剂的微生物降解研究进展

二苯醚类除草剂是一类广谱、高效、高选择性的除草剂,广泛应用于大豆、花生等农田一年生和多年生阔叶杂草的防除。由于该类除草剂不易降解,多年连续使用会导致其在土壤环境中的大量积累。本文概述了二苯醚类除草剂的基本结构及其对生物的影响,总结了降解二苯醚类除草剂的微生物种类、降解途径和降解过程中关键酶及其基因,分析了影响微生物降解二苯醚类除草剂的因素,对二苯醚类除草剂微生物降解未来的研究方向进行了展望,为深入研究二苯醚类除草剂的生物降解提供参考。     

不同预处理对小鼠粪样菌群高通量测序分析结果的影响

应用高通量测序技术比较不同预处理对小鼠粪样菌群结构的影响,以期为后续相关研究提供参考依据。采集昆明小鼠新鲜粪样,分为原始粪样组、生理盐水处理组和PBS处理组,提取粪样DNA,采用Illumina MiSeq平台进行测序对3组样本的16S rRNA V3~V4区基因文库进行生物信息学分析。结果显示,3组样本拥有共同的OTUs 188个,不同预处理对粪样微生物多样性和丰度产生影响,生理盐水处理组、PBS处理组和原始粪样组分别检出14、11、12个门,3组样本共有门11个;分别检出24、21、21个纲,3组样本共有纲20个;分别检出62、55、59个科,3组样本共有科26个;分别检出147、126、137个属,3组样本共有属117个。总体来看,生理盐水处理组微生物多样性和丰度相对最高,原始粪样组次之,PBS处理组最低。粪样经生理盐水处理后,能在一定程度上提高肠道菌群检测的准确性。     

Contemporary issues,current best practice and ways forward in soil protist ecology

Soil protists are increasingly studied due to a release from previous methodological constraints and the acknowledgement of their immense diversity and functional importance in ecosystems. However, these studies often lack sufficient depth in knowledge, which is visible in the form of falsely used terms and false- or over-interpreted data with conclusions that cannot be drawn from the data obtained. As we welcome that also non-experts include protists in their still mostly bacterial and/or fungal-focused studies, our aim here is to help avoid some common errors. We provide suggestions for current terms to use when working on soil protists, like protist instead of protozoa, predator instead of grazer, microorganisms rather than microflora and other terms to be used to describe the prey spectrum of protists. We then highlight some dos and don'ts in soil protist ecology including challenges related to interpreting 18S rRNA gene amplicon sequencing data. We caution against the use of standard bioinformatic settings optimized for bacteria and the uncritical reliance on incomplete and partly erroneous reference databases. We also show why causal inferences cannot be drawn from sequence-based correlation analyses or any sampling/monitoring, study in the field without thorough experimental confirmation and sound understanding of the biology of taxa. Together, we envision this work to help non-experts to more easily include protists in their soil ecology analyses and obtain more reliable interpretations from their protist data and other biodiversity data that, in the end, will contribute to a better understanding of soil ecology.     

3-氰基吡啶水合酶产生菌的筛选及其酶形成条件

应用富集培养和梯度底物浓度定向筛选技术,从长期被腈化物污染的土壤中筛选到一株产 3-氰基吡啶水合酶(3-cyanopyridine hydratase)活性较高的马红球菌(Rhodococcus e-qui)SHB-121.研究了该菌3-氰基吡啶水合酶的最适形成条件.在最适条件下,酶的比活力达5.3u/mg干细胞,比在初筛条件下的酶活力提高95倍,而在其细胞内共存的尼克酰胺(烟酰胺)水解酶活力很低.     

CHARACTERIZATION AND BIOLOGICAL IMPLICATIONS OF SCYTONEMIN,A CYANOBACTERIAL SHEATH PIGMENT1

Scytonemin, the yellow-brown pigment of cyanobacterial (blue-green algal) extracellular sheaths, was found in species thriving in habitats exposed to intense solar radiation. Scytonemin occurred predominantly in sheaths of the outermost parts or top layers of cyanobacterial mats, crusts, or colonies. Scytonemin appears to be a single compound identified in more than 30 species of cyanobacteria from cultures and natural populations. It is lipid soluble and has a prominent absorption maximum in the near-ultraviolet region of the spectrum (384 nm in acetone; ca. 370 nm in vivo) with a long tail extending to the infrared region. Microspectrophotometric measurements of the transmittance of pigmented sheaths and the quenching of ultraviolet excitation of phycocyanin fluorescence demonstrate that the pigment was effective in shielding the cells from incoming near-ultraviolet-blue radiation, but not from green or red light. High light intensity (between 99 and 250 μmol photon · m^?2· S^?1, depending on species) promoted the synthesis of scytonemin in cultures of cyanobacteria. In cultures, high light intensity caused reduction in the specific content of Chl a and phycobilins, increase in the ratio of total carotenoids to Chl a, and scytonemin increase. UV-A (320–400 nm) radiation was very effective in eliciting scytonemin synthesis. Scytonemin production was physiological and not due to a mere photochemical conversion. These results strongly suggest that scytonemin production constitutes an adaptive strategy of photoprotection against short-wavelength solar irradiance.     

Soil-surface carbon dioxide efflux and microbial biomass in relation to tree density 13 years after a stand replacing fire in a lodgepole pine ecosystem

The effects of fire on soil‐surface carbon dioxide (CO₂) efflux, F_S, and microbial biomass carbon, C_mic, were studied in a wildland setting by examining 13‐year‐old postfire stands of lodgepole pine differing in tree density (< 500 to > 500 000 trees ha^?1) in Yellowstone National Park (YNP). In addition, young stands were compared to mature lodgepole pine stands (～110‐year‐old) in order to estimate ecosystem recovery 13 years after a stand replacing fire. Growing season F_S increased with tree density in young stands (1.0 µmol CO₂ m^?2 s^?1 in low‐density stands, 1.8 µmol CO₂ m^?2 s^?1 in moderate‐density stands and 2.1 µmol CO₂ m^?2 s^?1 in high‐density stands) and with stand age (2.7 µmol CO₂ m^?2 s^?1 in mature stands). Microbial biomass carbon in young stands did not differ with tree density and ranged from 0.2 to 0.5 mg C g^?1 dry soil over the growing season; C_mic was significantly greater in mature stands (0.5–0.8 mg C g^?1 dry soil). Soil‐surface CO₂ efflux in young stands was correlated with biotic variables (above‐ground, below‐ground and microbial biomass), but not with abiotic variables (litter and mineral soil C and N content, bulk density and soil texture). Microbial biomass carbon was correlated with below‐ground plant biomass and not with soil carbon and nitrogen, indicating that plant activity controls not only root respiration, but C_mic pools and overall F_S rates as well. These findings support recent studies that have demonstrated the prevailing importance of plants in controlling rates of F_S and suggest that decomposition of older, recalcitrant soil C pools in this ecosystem is relatively unimportant 13 years after a stand replacing fire. Our results also indicate that realistic predictions and modeling of terrestrial C cycling must account for the variability in tree density and stand age that exists across the landscape as a result of natural disturbances.