Division of Geological and Planetary Science and Division of Engineering and Applied Science, California Institute of Technology, Pasadena, California 91125.
Appl Environ Microbiol. 1991 Nov;57(11):3248-54. doi: 10.1128/aem.57.11.3248-3254.1991.
The presence of a narrow shape and size distribution for magnetite crystals within magnetotactic organisms suggests strongly that there are species-specific mechanisms that control the process of biomineralization. In order to explore the extent of this control, cultures of Aquaspirillum magnetotacticum in the exponential growth phase were exposed to increasing magnetic pulses with the aim of separating cell populations on the basis of their magnetic coercivities. Isothermal remanent magnetization and anhysteretic remanent magnetization studies were performed with freeze-dried magnetic cells after the remagnetization treatment. Subpopulations of A. magnetotacticum that showed an increase in coercivity correlated with the intensity of the magnetic pulses were isolated. After successive subcultures of the remaining north-seeking cells, a maximum bulk coercivity (H(b)) of 40 mT was obtained after treatment with a 55-mT pulse. Although we obtained A. magnetotacticum variants displaying higher coercivities than the wild-type strain, changes in crystal size or shape of the magnetite crystals were below reliable detection limits with transmission electron microscopy. Attempts to shift the coercivity towards higher values caused it to decrease, a change which was accompanied by an increase in magnetostatic interactions of the magnetosome chains as well as an increase in the cell population displaying an abnormal distribution of the magnetosome chains. Ultrastructural analyses of cells and magnetosomes revealed the appearance of cystlike bodies which occasionally contained magnetosomes. The increase in cystlike cells and abnormal magnetosome chains when higher magnetic pulses were used suggested that magnetosomes were collapsing because of stronger interparticle magnetostatic forces.
在磁趋性生物体内磁铁矿晶体的形状和尺寸分布较窄,这强烈表明存在控制生物矿化过程的特定物种机制。为了探究这种控制的程度,将处于指数生长期的趋磁细菌(Aquaspirillum magnetotacticum)暴露于递增的磁场脉冲中,目的是基于其磁矫顽力分离细胞群体。对经过再磁化处理后的冻干磁性细胞进行等温剩磁和非磁滞剩磁研究。显示矫顽力增加的趋磁细菌(Aquaspirillum magnetotacticum)亚群与磁场脉冲强度相关,被分离出来。对剩余的寻北细胞进行连续亚培养后,在用 55 mT 脉冲处理后获得了最大的体磁矫顽力(H(b))为 40 mT。尽管我们获得了显示出比野生型菌株更高矫顽力的趋磁细菌(Aquaspirillum magnetotacticum)变体,但通过透射电子显微镜,磁铁矿晶体的尺寸或形状变化低于可靠的检测极限。试图将矫顽力推向更高值会导致其降低,这种变化伴随着磁晶体内磁静磁相互作用的增加以及显示磁晶体内异常分布的细胞群体的增加。细胞和磁小体的超微结构分析显示出偶尔含有磁小体的囊泡样体的出现。当使用更高的磁场脉冲时,囊泡样细胞和异常磁小体链的增加表明,由于更强的粒子间磁静电力,磁小体正在崩溃。