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Characterization of magnetotactic bacteria and their magnetosomes isolated from Tieshan iron ore in Hubei Province of China

机译:湖北铁山铁矿中趋磁细菌及其磁小体的表征

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摘要

Several magnetotactic bacteria (MTB) have been isolated from iron cap belt, surface soil of intermediate belt and "primary iron ore belt" of Tieshan iron ore in Hubei Province, China. These magnetotactic bacteria were cultivated in enrichment medium at room temperature (25-30℃), with oxygen concentration of 5 -10% under the field of a permanent magnet. The magnetotactic bacteria were cocci or rods. They contained two or more magnetosomes under transmission electron microscope (TEM H-7000 FA), and the magnetosomes were in the shapes of rounded, triangular, rectangular and irregular. Energy spectrum analysis with Jeol 2000 transmission electron microscope (JEM2000FXII) equipped with energy dispersive system (EDS) controlled by Oxford Instruments Analytical system (INCA) showed that iron oxides were the main component of the magnetic particles.
机译:从湖北铁山铁矿的铁帽带,中间带表层土壤和“初级铁矿带”中分离出了几种趋磁细菌。这些趋磁细菌在室温(25-30℃)下于富集培养基中培养,在永久磁铁的磁场下,氧浓度为5 -10%。趋磁细菌是球菌或棒。在透射电子显微镜(TEM H-7000 FA)下,它们包含两个或多个磁小体,并且磁小体呈圆形,三角形,矩形和不规则形状。使用配备有牛津仪器分析系统(INCA)控制的能量分散系统(EDS)的Jeol 2000透射电子显微镜(JEM2000FXII)进行的能谱分析表明,氧化铁是磁性颗粒的主要成分。

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