土壤大气甲烷氧化菌研究进展

土壤微生物催化是大气中痕量甲烷(约1.8ppmv)氧化的唯一生物途径。目前的研究表明好氧土壤中存在专性和选择性大气甲烷氧化菌2种类型:前者(USCα和USCγ)广泛分布于各种好氧旱地土壤,其甲烷氧化酶对低浓度甲烷亲和力极高,属真正的寡营养型,但至今尚未获得该种类的纯培养菌株。后者属于传统甲烷氧化菌Methylocystis/Methylosinus属,广泛分布于各种周期性排放高浓度甲烷的土壤环境中。该属大部分菌株含有亲和力不同的2套甲烷单加氧酶系统,其中的高亲和力甲烷单加氧酶使这些菌株可以在相当长的时间内(3个月)保持大气浓度甲烷氧化活性,但其生长和繁殖还需依赖于土壤内部阶段性产生的高浓度甲烷。本文详细阐述了2类大气甲烷氧化菌的发现历程及其可能的生存策略,最后系统梳理了几种关键的环境因子(土壤温度及湿度、土壤pH、植被、土地利用及氮输入)对大气甲烷氧化菌群落结构和甲烷氧化活性的影响,提出并展望了土壤大气甲烷氧化菌研究的重要方向。     

新型产甲烷古菌研究进展

产甲烷古菌是一类能利用简单化合物产生甲烷气体的厌氧菌。近年来,随着测序技术的不断发展,科学家结合宏基因组学和其他技术先后发现了众多之前未被报道的新型产甲烷古菌。基因组分析等研究发现这几类新型产甲烷古菌具有独特的甲烷代谢通路以及广泛的生态分布,科学家推测它们在全球生态调节以及碳循环中可能起到了不可忽视的作用。然而,这些新型产甲烷古菌大部分尚未通过传统培养方法获得纯培养菌株,其确切的生理代谢机制和生态功能还有待深入研究。为了更加系统地了解这些新型产甲烷古菌,本文从它们的分类、系统发育地位、代谢机制、生态分布以及分离培养等方面进行了综述,并对新型产甲烷古菌未来的研究方向进行了展望。     

基于甲烷氧化菌的脱氮技术研究进展

甲烷氧化菌利用甲烷作为唯一碳源和能源,在氧化甲烷的过程中能有效地实现脱氮,该过程分为好氧甲烷氧化耦合反硝化(aerobic methane oxidation coupled to denitrification,AME-D)和厌氧甲烷氧化耦合反硝化(anaerobic methane oxidation coupled to denitrification,ANME-D),在碳循环和氮循环的研究中具有重要意义。本文通过总结近年来有关甲烷氧化菌的分类与分布,阐述AME-D和ANME-D的基本原理、影响因素和应用情况,提出相应的研究方向,以期为甲烷氧化菌在污水脱氮中的应用提供参考。     

微生物甲烷氧化反硝化耦合反应研究进展

甲烷氧化反硝化耦合过程是连接碳循环和氮循环的重要桥梁.该过程的深入研究有助于完善人们对全球碳氮生物化学循环的认识.甲烷作为反硝化外加气体碳源,既能调控大气甲烷平衡,有效减缓由甲烷引起的温室效应,又能降低反硝化工艺中因投入外加碳源带来的成本.因此近年来甲烷氧化反硝化耦合反应及其机理研究倍受关注.本文主要讨论了好氧和厌氧两种类型的甲烷氧化反硝化过程,重点对其微生物耦合反应机理及其影响因素进行了综述,同时指出了其工程化应用存在的问题,并对其应用前景提出展望.
     

好氧甲烷氧化菌生态学研究进展

好氧甲烷氧化菌是一群以甲烷为碳源和能源的细菌。好氧甲烷氧化菌在自然环境中分布广泛,人类已从土壤、淡水和海洋沉积、泥炭沼泽、热泉、海水和南极环境分离到甲烷氧化菌的纯培养。好氧甲烷氧化菌可分为14个属,包括研究较为深入的隶属于变形菌门Alpha和Gamma纲的细菌,以及属于疣微菌门的极端嗜热嗜酸甲烷氧化菌。最近,好氧甲烷氧化菌还被发现存在于苔藓类植物（尤其是泥炭苔藓）共生体中,兼性营养好氧甲烷氧化菌也被发现。本文通过对好氧甲烷氧化菌的分类、生理生化特征、分子生物学检测方法以及微生物生态学中的研究成果的总结与分析,以及对甲烷氧化菌研究所面临的问题进行讨论,以期为今后进一步开展好氧甲烷氧化菌及其在碳循环中的作用研究提供参考。     

细菌好氧反硝化研究进展

阐述了好氧反硝化细菌的种类及有关性质 ,并从电子理论、氧的浓度、反硝化酶系等方面对细菌好氧反硝化的作用机制进行了探讨 ,对细菌好氧反硝化的研究概况、进展及其研究意义和目前存在的问题作了较为详细的介绍。     

双膦酸盐对抗骨质疏松的研究进展

双膦酸盐是目前治疗骨质疏松的有效药物,能导致破骨细胞凋亡,从而使骨密度增加.本文对双膦酸盐的结构特点,抗骨质疏松作用的细胞学机制,在临床上的应用以及近年来国内外对双膦酸盐抗骨质疏松方面的研究状况做一综述,为今后的研究提供参考.     

微生物厌氧甲烷氧化反硝化研究进展

厌氧甲烷氧化反硝化过程(Denitrifying anaerobic methane oxidation,DAMO)以甲烷为电子供体进行反硝化作用,在实现废水脱氮处理的同时,可有效削减温室气体甲烷的排放,从而减缓全球温室效应。相关机制研究集中在逆向产甲烷途径耦合反硝化和亚硝酸盐依赖型厌氧甲烷氧化(nitrite-dependent anaerobic methane oxidation,n-damo)两个方面。鉴于厌氧甲烷氧化反硝化过程对全球碳氮物质循环的重要意义,本文对近年来厌氧甲烷氧化反硝化过程的研究进展进行了概述,着重阐述了有关厌氧甲烷氧化反硝化微生物富集培养物,特别是含Candidatus Methylomirabilis oxyfera(M.oxyfera)富集培养物的微生物特性、甲烷氧化反硝化的机理以及影响因子。在此基础上,探讨了厌氧甲烷氧化反硝化过程未来的研究方向和工业化应用前景。     

导电材料强化微生物直接种间电子传递产甲烷的研究进展

厌氧条件下,微生物可以通过厌氧代谢产生甲烷(CH4),由此衍生的厌氧消化技术可实现能源的回收利用.产CH4的关键步骤是刺激发酵细菌和产甲烷古菌之间的有效电子转移,电活性微生物可以取代传统的氢/甲酸盐实现直接种间电子传递,其电子传递效率更高.添加导电材料可以促进直接种间电子传递并提高CH4产率,是一种更有效的强化电子传递...     

氢营养型产甲烷代谢途径研究进展

产甲烷古菌是一类极端厌氧的古菌域微生物,可以利用CO_2、甲醇、乙酸等简单化合物产甲烷并获得能量。目前能够培养的氢营养型(CO_2/H_2)产甲烷古菌的种类较多,而且在三类产甲烷代谢类型中,氢营养型产甲烷途径的产能效率最高,并具有多种模式的特殊能量利用系统。近年来,随着质谱、光谱和晶体技术的发展与运用,人们对产甲烷代谢途径的研究进一步深入,尤其是对氢营养型产甲烷途径的生化机制有了新的认识,揭示了产甲烷古菌在能量极限条件下独特、高效的能量利用模式。本文从能量储存、代谢途径、蛋白功能与催化机制等方面概述产甲烷古菌利用CO_2/H_2产甲烷的详细过程,并对产甲烷古菌代谢途径的研究方向与技术发展进行展望。     

Recent advances toward the bioconversion of methane and methanol in synthetic methylotrophs

Abundant natural gas reserves, along with increased biogas production, have prompted recent interest in harnessing methane as an industrial feedstock for the production of liquid fuels and chemicals. Methane can either be used directly for fermentation or first oxidized to methanol via biological or chemical means. Methanol is advantageous due to its liquid state under normal conditions. Methylotrophy, defined as the ability of microorganisms to utilize reduced one-carbon compounds like methane and methanol as sole carbon and energy sources for growth, is widespread in bacterial communities. However, native methylotrophs lack the extensive and well-characterized synthetic biology toolbox of platform microorganisms like Escherichia coli, which results in slow and inefficient design-build-test cycles. If a heterologous production pathway can be engineered, the slow growth and uptake rates of native methylotrophs generally limit their industrial potential. Therefore, much focus has been placed on engineering synthetic methylotrophs, or non-methylotrophic platform microorganisms, like E. coli, that have been engineered with synthetic methanol utilization pathways. These platform hosts allow for rapid design-build-test cycles and are well-suited for industrial application at the current time. In this review, recent progress made toward synthetic methylotrophy (including methanotrophy) is discussed. Specifically, the importance of amino acid metabolism and alternative one-carbon assimilation pathways are detailed. A recent study that has achieved methane bioconversion to liquid chemicals in a synthetic E. coli methanotroph is also briefly discussed. We also discuss strategies for the way forward in order to realize the industrial potential of synthetic methanotrophs and methylotrophs.     

Phylogenetic and enzymatic diversity of deep subseafloor aerobic microorganisms in organics- and methane-rich sediments off Shimokita Peninsula

"A meta-enzyme approach" is proposed as an ecological enzymatic method to explore the potential functions of microbial communities in extreme environments such as the deep marine subsurface. We evaluated a variety of extra-cellular enzyme activities of sediment slurries and isolates from a deep subseafloor sediment core. Using the new deep-sea drilling vessel "Chikyu", we obtained 365 m of core sediments that contained approximately 2% organic matter and considerable amounts of methane from offshore the Shimokita Peninsula in Japan at a water depth of 1,180 m. In the extra-sediment fraction of the slurry samples, phosphatase, esterase, and catalase activities were detected consistently throughout the core sediments down to the deepest slurry sample from 342.5 m below seafloor (mbsf). Detectable enzyme activities predicted the existence of a sizable population of viable aerobic microorganisms even in deep subseafloor habitats. The subsequent quantitative cultivation using solid media represented remarkably high numbers of aerobic, heterotrophic microbial populations (e.g., maximally 4.4 x 10(7) cells cm(-3) at 342.5 mbsf). Analysis of 16S rRNA gene sequences revealed that the predominant cultivated microbial components were affiliated with the genera Bacillus, Shewanella, Pseudoalteromonas, Halomonas, Pseudomonas, Paracoccus, Rhodococcus, Microbacterium, and Flexibacteracea. Many of the predominant and scarce isolates produced a variety of extra-cellular enzymes such as proteases, amylases, lipases, chitinases, phosphatases, and deoxyribonucleases. Our results indicate that microbes in the deep subseafloor environment off Shimokita are metabolically active and that the cultivable populations may have a great potential in biotechnology.     

瘤胃甲烷调控方法评述

反刍动物释放的甲烷不仅消耗6％～10％的能量摄入,而且是重要的温室效应气体。过去20多年以来,研究人员围绕瘤胃甲烷生成及其调控展开了大量的研究,目前采取的主要措施包括：（1）提供电子释放新途径;（2）利用疫苗、生物控制剂（噬菌体和细菌素）以及化学抑制剂等抑制产甲烷菌,以及（3）去原虫、添加植物提取物或有机酸等促进产乙酸菌增加,降低产甲烷菌可利用的氢。瘤胃生态系统是一个复杂的生态系统,能够将复杂碳水化合物转化成为挥发性脂肪酸,这个过程部分依赖于甲烷的生成和氢的消耗。因此,虽然各种调控措施能够在短期内抑制甲烷生成,但瘤胃微生态系统能够恢复原有的甲烷生成水平,这表明我们对瘤胃中氢代谢仍然认识不足。进一步提高对瘤胃内氢和甲烷生成的微生物生化机制的了解,有助于我们找到有效的甲烷调控措施。     

好氧反硝化菌的研究进展

综述了好氧反硝化菌的种类和特性、好氧反硝化菌的反硝化作用机制和影响因素.好氧反硝化菌主要包括假单胞菌属(Pseudomonas)、产碱杆菌属(Alcaligenes)、副球菌属(Para-coccus)和芽孢杆菌属(Bacillus)等,属好氧或兼性好氧异养微生物.好氧反硝化菌能在好氧条件下进行反硝化,其主要产物是N2O,并可将铵态氮直接转化成气态产物.催化好氧反硝化菌反硝化作用的硝酸盐还原酶是周质酶而不是膜结合酶.溶解氧和C/N往往是影响好氧反硝化菌反硝化作用的主要因素.介绍了间歇曝气法、选择性培养基法等好氧反硝化菌的主要分离筛选方法.概述了好氧反硝化菌在水产养殖、废水生物处理、降解有机污染物以及对土壤氮素损失的影响方面的研究进展.     

Amylase activity in substrate deficiency aerobic granules

Immunohistochemical staining was applied together with the multicolor fluorescent scheme to demonstrate the amylase activity for polysaccharide hydrolysis in stored or starved aerobic granules that are in substrate deficiency. If sufficient nutrients were present, α-amylase and β-amylase were found close to the surface layer of the original granules. Following storage or starvation during which most external nutrients were depleted, the α-amylase and β-amylase were distributed over the entire granule interior, suggesting endogenous respiration at the core of the granule. In particular, the fluorescent intensities of α-amylase and β-amylase were enriched 5–20 μm from the edge of the internal cavity, suggesting the strong correlation between polysaccharide hydrolysis and the formation of interior cavities. The secreted amylase was located near the living cells, suggesting that the polysaccharide hydrolysis is restricted to local environment that occurs near the functional strains. Internal hydrolysis within the core, for the case of both proteins and polysaccharides should correspond in principle to the loss of granule stability.     

Changes during aerobic exposure of wheat silages

Aerobic stability is an important characteristic of silages because they are exposed to air during storage and feedout. The objective of the current study was to investigate changes that occur in wheat silages during aerobic exposure. Silages of whole crop wheat harvested at the flowering, milk and dough stages of maturity were prepared in 1.5 L anaerobic glass jars. Three months after ensiling, silages were subjected to a 7-day aerobic stability test. The silages of wheat harvested at the flowering stage were the most stable upon aerobic exposure, but had the largest fermentation losses. Silages of milk-stage wheat were unstable upon aerobic exposure, and had large amounts of CO₂ and heating, large yeast populations, decreased amounts of fermentation products and decreased dry matter (DM) and neutral detergent fiber (NDF) digestibility (from 667 to 572 g/kg DM and from 597 to 558 g/kg DM, following 7-day aerobic exposure, respectively). Silages of dough-stage wheat had relatively low fermentation losses and were quite stable for at least 4 days of aerobic exposure. Silage samples from the center of commercial bunker silos, and from areas adjacent to the walls of the silos, were judged to be of good quality. Samples from the shoulders of bunker silos were spoiled with higher pH (P<0.05), higher ash content and lower DM and NDF digestibility compared with samples from the center of the silos and areas near the walls (6.8 vs. 4.0, 19.0 vs. 7.8, 477 g/kg DM vs. 634 g/kg DM and 230 g/kg DM vs. 487 g/kg DM, respectively).     

Relationship of aerobic and anaerobic parameters with 400 m front crawl swimming performance

The aims of the present study were to investigate the relationship of aerobic and anaerobic parameters with 400 m performance, and establish which variable better explains long distance performance in swimming. Twenty-two swimmers (19.1±1.5 years, height 173.9±10.0 cm, body mass 71.2±10.2 kg; 76.6±5.3% of 400 m world record) underwent a lactate minimum test to determine lactate minimum speed (LMS) (i.e., aerobic capacity index). Moreover, the swimmers performed a 400 m maximal effort to determine mean speed (S400m), peak oxygen uptake (V.O2PEAK) and total anaerobic contribution (C_ANA). The C_ANA was assumed as the sum of alactic and lactic contributions. Physiological parameters of 400 m were determined using the backward extrapolation technique (V.O2PEAK and alactic contributions of C_ANA) and blood lactate concentration analysis (lactic anaerobic contributions of C_ANA). The Pearson correlation test and backward multiple regression analysis were used to verify the possible correlations between the physiological indices (predictor factors) and S400m (independent variable) (p < 0.05). Values are presented as mean ± standard deviation. Significant correlations were observed between S400m (1.4±0.1 m·s^-1) and LMS (1.3±0.1 m·s^-1; r = 0.80), V.O2PEAK (4.5±3.9 L·min^-1; r = 0.72) and C_ANA (4.7±1.5 L·O₂; r= 0.44). The best model constructed using multiple regression analysis demonstrated that LMS and V.O2PEAK explained 85% of the 400 m performance variance. When backward multiple regression analysis was performed, C_ANA lost significance. Thus, the results demonstrated that both aerobic parameters (capacity and power) can be used to predict 400 m swimming performance.