Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, People's Republic of China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, People's Republic of China.
Appl Environ Microbiol. 2019 Jul 1;85(14). doi: 10.1128/AEM.00731-19. Print 2019 Jul 15.
Magnetotactic bacteria (MTB) are phylogenetically diverse prokaryotes that are able to biomineralize intracellular, magnetic chains of magnetite or greigite nanocrystals called magnetosomes. Simultaneous characterization of MTB phylogeny and biomineralization is crucial but challenging because most MTB are extremely difficult to culture. We identify a large rod, bean-like MTB (tentatively named WYHR-1) from freshwater sediments of Weiyang Lake, Xi'an, China, using a coupled fluorescence and scanning electron microscopy approach at the single-cell scale. Phylogenetic analysis of 16S rRNA gene sequences indicates that WYHR-1 is a novel genus from the class. Transmission electron microscope observations reveal that WYHR-1 cells contain tens of magnetite magnetosomes that are organized into a single chain bundle along the cell long axis. Mature WYHR-1 magnetosomes are bullet-shaped, straight, and elongated along the [001] direction, with a large flat end terminated by a {100} face at the base and a conical top. This crystal morphology is distinctively different from bullet-shaped magnetosomes produced by other MTB in the class and the phylum. This indicates that WYHR-1 may have a different crystal growth process and mechanism from other species, which results from species-specific magnetosome biomineralization in MTB. Magnetotactic bacteria (MTB) represent a model system for understanding biomineralization and are also studied intensively in biogeomagnetic and paleomagnetic research. However, many uncultured MTB strains have not been identified phylogenetically or investigated structurally at the single-cell level, which limits comprehensive understanding of MTB diversity and their role in biomineralization. We have identified a novel MTB strain, WYHR-1, from a freshwater lake using a coupled fluorescence and scanning electron microscopy approach at the single-cell scale. Our analyses further indicate that strain WYHR-1 represents a novel genus from the class. In contrast to bullet-shaped magnetosomes produced by other MTB in the class and the phylum, WYHR-1 magnetosomes are bullet-shaped, straight, and highly elongated along the [001] direction, are terminated by a large {100} face at their base, and have a conical top. Our findings imply that, consistent with phylogenetic diversity of MTB, bullet-shaped magnetosomes have diverse crystal habits and growth patterns.
磁细菌(MTB)是具有不同进化背景的原核生物,能够在体内生物矿化形成磁铁矿或纤铁矿纳米晶体的磁性链,称为磁小体。同时对 MTB 的系统发育和生物矿化进行特征分析至关重要,但也极具挑战性,因为大多数 MTB 极难培养。我们使用荧光和扫描电子显微镜联用的单细胞尺度方法,从中国西安未央湖的淡水沉积物中鉴定出一种大型棒状、豆形的 MTB(暂命名为 WYHR-1)。16S rRNA 基因序列的系统发育分析表明,WYHR-1 是一个新属,属于 纲。透射电子显微镜观察显示,WYHR-1 细胞内含有数十个磁小体,这些磁小体沿细胞长轴排列成单个链束。成熟的 WYHR-1 磁小体呈子弹状,笔直,沿 [001] 方向拉长,较大的平面端在底部终止于一个 {100} 面,顶端呈锥形。这种晶体形态与 纲和 门中其他 MTB 产生的子弹形磁小体明显不同。这表明 WYHR-1 可能具有与其他物种不同的晶体生长过程和机制,这是由于 MTB 中特定物种的磁小体生物矿化所致。磁细菌(MTB)是研究生物矿化的典型系统,在生物地磁和古地磁研究中也受到了广泛关注。然而,许多未培养的 MTB 菌株在系统发育上尚未得到鉴定,在单细胞水平上的结构也未得到研究,这限制了对 MTB 多样性及其在生物矿化中作用的全面了解。我们使用荧光和扫描电子显微镜联用的单细胞尺度方法,从一个淡水湖中鉴定出一种新型 MTB 菌株,WYHR-1。我们的分析进一步表明,WYHR-1 菌株代表了一个新属,属于 纲。与 纲和 门中其他 MTB 产生的子弹形磁小体不同,WYHR-1 的磁小体呈子弹状,笔直,沿 [001] 方向高度拉长,底部终止于一个大的 {100} 面,顶端呈锥形。我们的发现表明,与 MTB 的系统发育多样性一致,子弹形磁小体具有不同的晶体习性和生长模式。