磁选育浸矿菌种新方法的研究——磁泳分离菌种

世界无处不有磁,磁场对整个世界产生着重大的影响。本文通过大量镜检工作,观察到从酸性矿坑水中初步分离培养得到的部分细菌对外加磁场均有微弱的趋磁性。基于菌种的这种特性,设计了磁泳装置用不同的磁场梯度分离细菌,磁泳分离的方法可以初步分离出近磁、远磁茼,这两个菌群的生理特性有着很大的差异,主要体现在其对亚铁氧化和对金属高于的浸出上,远磁菌亚铁氧化活性比近磁菌高将近50％,远磁菌对铜离子的浸出效果也比近磁茼好。近磁菌在强磁性矿物培养基中生长情况较好,而远磁茼在弱磁性矿物培养基中生长情况较好。而且,在近磁茼的纯培养茼体中分离到磁性颗粒。实验结果证明。采用磁泳用于分离体内舍有磁性颗粒的细菌是可行并且有效的,这一分离技术和工艺的结合也将大大促进我国生物冶金的步伐。     

磁泳分离细菌新方法的研究

从酸性矿坑水中富集培养分离到的嗜酸氧化亚铁硫杆菌（Acidithiobacillus ferrooxidans,A.ferrooxidans）[1-2] 菌同趋磁细菌具有一定的相似性。通过显微镜观察发现,部分浸矿细菌在外加磁场的作用下具有微弱的趋磁性,基于菌种的这种特性,设计了磁泳分离仪,对其在磁场作用下泳动（磁泳）进行分析,经磁泳后的近磁、远磁菌的生理特性有较大的差异。从用涂布平板法获得的近磁菌纯培养A. ferrooxidans菌体中,分离得到纳米磁性颗粒,能谱分析表明,其主要成分为Fe和O元素。实验结果证明,A. ferrooxidans具有微弱趋磁性,采用磁泳分离该类菌体内含有磁性颗粒的细菌是可行的,这一分离技术的进一步完善和改进将为传统的微生物菌种分离提供一种新型分离技术,也将大大促进趋磁细菌的研究,而且它与浸矿工艺的结合将大大促进我国生物冶金的研究步伐。     

固体平板磁泳分离细菌新方法的研究

氧化亚铁硫杆菌（Acidithiobacillus ferrooxidans）能够在胞内形成电子致密的磁性颗粒,它的这种特性使利用氧化亚铁硫杆菌合成生物纳米磁性材料成为了可能。本课题组为了筛选出合成磁性颗粒能力强的菌株,对原有的液体磁泳进行了改进,采用了新的固体平板磁泳方法来筛选纯化目的菌株。经过磁泳分离后,细菌中含磁性颗粒的细胞比例由原始菌群的30％上升到90％,胞内含有的磁颗粒数目也由1~2颗增加至2~5颗,筛选得到的细菌在人工磁场下会进行趋磁运动。实验结果表明,氧化亚铁硫杆菌具有较弱的趋磁性,在人工磁场下会进行趋磁运动,但仅在地磁场作用下不能定向运动,利用固体平板磁泳筛选纯化含有磁性颗粒的氧化亚铁硫杆菌的方法是切实可行的,磁泳分离技术的进一步完善和改进为传统的微生物菌种分离提供了新的途径,为研究纯氧化亚铁硫杆菌菌株胞内磁性颗粒的形成条件及机理提供了前提条件,也为今后从浸矿细菌中分离筛选更多的含有磁性颗粒的菌株打下基础。     

磁分离仪分离磁性细菌的新方法

磁性细菌胞内可以产生磁性颗粒,因此具有趋磁性,基于这种特性,利用磁分离的原理,本研究开发了一种磁性细菌分离仪,提供了一种分离磁性细菌的新方法。以氧化亚铁硫杆菌为例,使用磁性细菌分离仪进行分离,可以得到强磁菌和弱磁菌。利用透射电镜观察,强磁菌胞内磁性颗粒明显多于弱磁菌;半固体平板磁泳实验也表明强磁菌趋磁性明显强于弱磁菌。各项实验结果表明磁性细菌分离仪可以有效地分离磁性细菌,这是一种分离磁性细菌的新方法,将促进磁性细菌分离培养的研究。     

趋磁细菌及磁小体的生物医学应用研究进展

近年来,趋磁细菌及其生物自身合成的磁小体由于良好的生物安全性逐渐被人们所认识,并被用于生物工程和医学应用研究。与人工化学合成磁性纳米颗粒相比,从趋磁细菌中提取的磁小体具有生物膜包被、生物相容性高、粒径均一及磁性高等优势。趋磁细菌因磁小体在其胞内呈链状排列,具有沿磁场方向泳动的能力,也被应用于各种应用研究。因此,综述了趋磁细菌及磁小体特性,并就最近的研究进展重点综述趋磁细菌和磁小体在生物工程及医学应用等领域的最新研究进展。     

Acidthiobacillus ferrooxidans中磁小体的提取

At.f和趋磁细菌在生理特性和生长环境有一定的相似性,而且镜检发现At.f具有趋磁性,所以本文采用了趋磁细菌中磁小体的提取方法尝试提取At.f中的磁小体,用超声波破碎At.f后,以磁铁吸取其体内的磁性颗粒,经过检测,发现其体内确实存在含铁元素的磁性颗粒。提取粗样品经过电镜分析,证实其体内存在着少量由脂质包裹的磁小体。磁小体悬浮液经过蔗糖密度梯度离心纯化后,对其作透射电镜,可以清晰的看到磁小体。实验结果表明,At.f体内存在少量的磁小体,正是由于磁小体的存在,才使得At.f在外加磁场作用下发生磁生物效应。这是首次发现从酸性矿坑水分离的At.f具有趋磁性,并从中提取到了磁小体,可以利用At.f的趋磁性将其按照不同磁性进行分离,从而获得活性高的、对不同磁性矿物有特异性的高效浸矿菌种。     

两株不同来源的嗜酸氧化亚铁硫杆菌对黄铜矿浸出的研究

为了比较两株不同来源的嗜酸氧化亚铁硫杆菌菌株在不同培养基中的亚铁氧化活性和黄铜矿浸出能力,本研究采用了分离自广东梅山酸性矿坑水中的菌株M1和标准菌株ATCC 23270,对其在9K培养基中的亚铁氧化活性和矿物培养基中氧化还原电位以及浸矿效率进行了测定,该矿物培养基中黄铜矿来自广东梅山.研究结果表明,菌株M1在9K培养基中需5天才能将亚铁完全氧化.而ATCC 23270只需4天,但是菌株MI的铜离子浸出效率(38%)却高于ATCC 23270(31%),浸出30天后,菌株M1浸矿体系的氧化还原电位从最初348 mV上升到520 mV,而ATCC 23270上升较小,仅从最初350 mV上升到491 mV.氧化还原电位的变化说明从广东梅山分离得到的菌株M1在浸矿体系中亚铁氧化活性比ATCC 23270更高.菌株M1比长期实验室培养的标准菌株ATCC 23270更适合当地矿物的微生物浸出,因而在生物浸出工艺中,应考虑采用分离或富集当地原生菌株来进行浸矿.     

细菌磁的生物技术开发和利用

细菌磁的生物技术开发和利用任修海（上海大学生物工程系,上海２０１８００）磁细菌即向磁性细菌沿地球磁力线移动,其细菌内含有自身合成的生物磁颗粒,这些颗粒细小均匀,外被生物膜,呈链状排列。最近在磁细菌的分离及培养技术上获得许多进展,为细菌磁的大规模生产奠...     

磁细菌与细菌磁颗粒的特点及应用研究

概述了磁细菌的特点及由磁细菌所产生的细菌磁颗粒的晶体成分、形态特征、磁颗粒膜的特点以及细菌磁颗粒在信息贮存、磁性细胞制备、基因研究、生物活性物质载体、免疫检测以及在污水处理、矿物分选等方面的应用研究。     

趋磁细菌及其应用于生物导航的研究进展

趋磁性细菌是一种由于体内含有对磁场具有敏感性的磁小体,而能够沿着磁力线运动的特殊细菌,本文综述了趋磁细菌的分布、分类、特性、磁小体研究以及趋磁细菌在生物导航方面的研究进展。     

趋磁细菌的磁小体

趋磁细菌是一类对磁场有趋向性反应的细菌,其菌体能吸收外界环境中铁元素并在体内合成包裹有膜的纳米磁性颗粒Fe₃O₄或Fe₃O_{3S4晶体即磁小体。综述了趋磁细菌的磁小体生物矿化的条件,以及趋磁细菌的铁离子吸收、磁小体囊泡的形成、铁离子的转运到磁小体囊泡及囊泡中受控的Fe3O4生物矿化的分子生物学和生物化学等方面的研究进展,重点介绍了趋磁细菌磁小体合成机制的研究进展及未来研究磁小体的发展方向。}     

Reduced Efficiency of Magnetotaxis in Magnetotactic Coccoid Bacteria in Higher than Geomagnetic Fields

Magnetotactic bacteria are microorganisms that orient and migrate along magnetic field lines. The classical model of polar magnetotaxis predicts that the field-parallel migration velocity of magnetotactic bacteria increases monotonically with the strength of an applied magnetic field. We here test this model experimentally on magnetotactic coccoid bacteria that swim along helical trajectories. It turns out that the contribution of the field-parallel migration velocity decreases with increasing field strength from 0.1 to 1.5 mT. This unexpected observation can be explained and reproduced in a mathematical model under the assumption that the magnetosome chain is inclined with respect to the flagellar propulsion axis. The magnetic disadvantage, however, becomes apparent only in stronger than geomagnetic fields, which suggests that magnetotaxis is optimized under geomagnetic field conditions. It is therefore not beneficial for these bacteria to increase their intracellular magnetic dipole moment beyond the value needed to overcome Brownian motion in geomagnetic field conditions.     

趋磁细菌运动特性的研究进展

细菌的运动性是影响其生存及致病的一个关键条件,同时也为合成和开发仿生运动体、微型机器人等提供了有效的模型。趋磁细菌具有胞内磁小体从而能够感知磁场的变化,进而影响其运动行为。目前,这种外部磁场与生物体的远程响应模式已在环境、医疗、材料等领域有广泛应用。因此,聚焦于趋磁细菌的运动特性,综述了趋磁细菌运动行为的表征、运动机理以及应用等方面的最新研究进展,并对该领域的发展和面临的挑战进行了展望。     

Killing of Staphylococcus aureus via Magnetic Hyperthermia Mediated by Magnetotactic Bacteria

Staphylococcus aureus is a common hospital and household pathogen. Given the emergence of antibiotic-resistant derivatives of this pathogen resulting from the use of antibiotics as general treatment, development of alternative therapeutic strategies is urgently needed. Here, we assess the feasibility of killing S. aureus cells in vitro and in vivo through magnetic hyperthermia mediated by magnetotactic bacteria that possess magnetic nanocrystals and demonstrate magnetically steered swimming. The S. aureus suspension was added to magnetotactic MO-1 bacteria either directly or after coating with anti-MO-1 polyclonal antibodies. The suspensions were then subjected to an alternating magnetic field (AMF) for 1 h. S. aureus viability was subsequently assessed through conventional plate counting and flow cytometry. We found that approximately 30% of the S. aureus cells mixed with uncoated MO-1 cells were killed after AMF treatment. Moreover, attachment between the magnetotactic bacteria and S. aureus increased the killing efficiency of hyperthermia to more than 50%. Using mouse models, we demonstrated that magnetic hyperthermia mediated by antibody-coated magnetotactic MO-1 bacteria significantly improved wound healing. These results collectively demonstrated the effective eradication of S. aureus both in vitro and in vivo, indicating the potential of magnetotactic bacterium-mediated magnetic hyperthermia as a treatment for S. aureus-induced skin or wound infections.     

Newly isolated but uncultivated magnetotactic bacterium of the phylum Nitrospirae from Beijing, China

Magnetotactic bacteria (MTB) in the phylum Nitrospirae synthesize up to hundreds of intracellular bullet-shaped magnetite magnetosomes. In the present study, a watermelon-shaped magnetotactic bacterium (designated MWB-1) from Lake Beihai in Beijing, China, was characterized. This uncultivated microbe was identified as a member of the phylum Nitrospirae and represents a novel phylogenetic lineage with ≥6% 16S rRNA gene sequence divergence from all currently described MTB. MWB-1 contained 200 to 300 intracellular bullet-shaped magnetite magnetosomes and showed a helical swimming trajectory under homogeneous magnetic fields; its magnetotactic velocity decreased with increasing field strength, and vice versa. A robust phylogenetic framework for MWB-1 and all currently known MTB in the phylum Nitrospirae was constructed utilizing maximum-likelihood and Bayesian algorithms, which yielded strong evidence that the Nitrospirae MTB could be divided into four well-supported groups. Considering its population densities in sediment and its high numbers of magnetosomes, MWB-1 was estimated to account for more than 10% of the natural remanent magnetization of the surface sediment. Taken together, the results of this study suggest that MTB in the phylum Nitrospirae are more diverse than previously realized and can make important contributions to the sedimentary magnetization in particular environments.     

Characterization of Bacterial Magnetotactic Behaviors by Using a Magnetospectrophotometry Assay

Magnetotactic bacteria have the unique capacity of synthesizing intracellular single-domain magnetic particles called magnetosomes. The magnetosomes are usually organized in a chain that allows the bacteria to align and swim along geomagnetic field lines, a behavior called magnetotaxis. Two mechanisms of magnetotaxis have been described. Axial magnetotactic cells swim in both directions along magnetic field lines. In contrast, polar magnetotactic cells swim either parallel to the geomagnetic field lines toward the North Pole (north seeking) or antiparallel toward the South Pole (south seeking). In this study, we used a magnetospectrophotometry (MSP) assay to characterize both the axial magnetotaxis of “Magnetospirillum magneticum” strain AMB-1 and the polar magnetotaxis of magneto-ovoid strain MO-1. Two pairs of Helmholtz coils were mounted onto the cuvette holder of a common laboratory spectrophotometer to generate two mutually perpendicular homogeneous magnetic fields parallel or perpendicular to the light beam. The application of magnetic fields allowed measurements of the change in light scattering resulting from cell alignment in a magnetic field or in absorbance due to bacteria swimming across the light beam. Our results showed that MSP is a powerful tool for the determination of bacterial magnetism and the analysis of alignment and swimming of magnetotactic bacteria in magnetic fields. Moreover, this assay allowed us to characterize south-seeking derivatives and non-magnetosome-bearing strains obtained from north-seeking MO-1 cultures. Our results suggest that oxygen is a determinant factor that controls magnetotactic behavior.Magnetotactic bacteria are morphologically, metabolically, and phylogenetically diverse prokaryotes (1, 11). They synthesize unique intracellular organelles, the magnetosomes, which are single-domain magnetic crystals of the mineral magnetite or greigite enveloped by membranes. Magnetosomes are usually organized in a chain(s) within the cell and cause the cell to align along geomagnetic field lines while it swims. The highest numbers of magnetotactic bacteria are generally found at, or just below, the oxic-anoxic transition zone (OATZ) or redoxocline in aquatic habitats (1). Early studies showed that Northern Hemisphere magnetotactic bacteria swim preferentially northward in parallel with the geomagnetic field lines (north seeking [NS]) (2) and that those from the Southern Hemisphere swim preferentially antiparallel to the geomagnetic field lines to the magnetic South Pole (south seeking [SS]) (4). The geomagnetic field is inclined downward from horizontal in the Northern Hemisphere and upward in the Southern Hemisphere, with the inclination magnitude increasing from the equator to the poles. Therefore, magnetotaxis might guide cells in each hemisphere downward to less-oxygenated regions of aquatic habitats, where they would presumably stop swimming until conditions change (1). A recent study reported the coexistence of both NS and SS magnetotactic bacteria in the Northern Hemisphere, which conflicts with the prevalent model of the adaptive value of magnetotaxis (14).Under laboratory conditions, magnetotactic bacteria form microaerophilic bands of cells in oxygen-gradient medium. In fact, magnetotaxis and aerotaxis work together in these bacteria, and the behavior observed has been referred to as “magnetoaerotaxis.” Two different magnetoaerotactic mechanisms, termed polar and axial, are found in different bacterial species (6). The magnetotactic bacteria, principally the magnetotactic cocci, that swim persistently in one direction along the magnetic field (NS or SS) are polar magnetoaerotactic. Magnetotactic bacteria, especially the freshwater spirilla, that swim in either direction along the magnetic field lines with frequent, spontaneous reversals of swimming direction without turning around are axial magnetoaerotactic. For polar magnetotactic bacteria, the magnetic field provides an axis and a direction for motility, whereas for axial magnetotactic bacteria, the magnetic field provides only an axis of motility. The two mechanisms can best be seen in flattened capillary tubes containing suspensions of cells in reduced medium in a magnetic field oriented parallel to the capillary. An oxygen gradient forms along the tube, beginning at the ends of the capillary, with one oriented parallel and the other antiparallel to the magnetic field (1). Band formation by axial magnetoaerotactic cells, such as Magnetospirillum magnetotacticum cells, occurs at both ends of the capillary. Rotation of the magnetic field by 180° after the formation of the bands causes the cells in both bands to rotate 180°, but the bands remain intact. In contrast, band formation by polar magnetoaerotactic cells, such as the marine cocci, occurs only at the end of the capillary for which the magnetic field and the oxygen concentration gradient are oriented opposite to each other. Rotation of the magnetic field by 180° after the formation of the band causes the cells in the band to rotate 180° and swim away, resulting in the dispersal of the band (1). In this study, we developed a magnetospectrophotometry (MSP) assay that provides an alternative method for the quantitative and versatile characterization of the two magnetotactic mechanisms. Using this assay, we demonstrated the effect of artificial magnetic fields on the generation of homogeneous NS or SS magnetotactic bacterial populations.     

响应面法优化Fe~(2+)的微生物氧化条件

氧化亚铁钩端螺旋菌(Leptospirillum ferrooxidans,L.f)是一种极端嗜酸,专性自养氧化铁的细菌,能够耐受较低pH和较高的温度,被广泛应用于生物浸矿和环境治理。氧化亚铁钩端螺旋体菌的生物浸矿效率与其对Fe~(2+)氧化速率相关,因此,本文采用响应面法,通过建立二次多项式回归方程考察pH、温度、Fe~(2+)浓度及转速四个培养因素对Fe~(2+)氧化速率的影响。结果显示在pH为2.25、温度为32℃、初始Fe~(2+)浓度为175.36 mmol/L、转数为165 r/min时,Fe~(2+)最高氧化速率为0.2911 g/Lh。