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首页> 外文期刊>Frontiers in Microbiology >Magnetotactic Coccus Strain SHHC-1 Affiliated to Alphaproteobacteria Forms Octahedral Magnetite Magnetosomes
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Magnetotactic Coccus Strain SHHC-1 Affiliated to Alphaproteobacteria Forms Octahedral Magnetite Magnetosomes

机译:变形蛋白形式的八面体磁铁矿磁致趋化球菌菌株SHHC-1

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摘要

Magnetotactic bacteria (MTB) are morphologically and phylogenetically diverse prokaryotes. They can form intracellular chain-assembled magnetite (Fe_(3)O_(4)) or greigite (Fe_(3)S_(4)) nanocrystals each enveloped by a lipid bilayer membrane called a magnetosome. Magnetotactic cocci have been found to be the most abundant morphotypes of MTB in various aquatic environments. However, knowledge on magnetosome biomineralization within magnetotactic cocci remains elusive due to small number of strains that have been cultured. By using a coordinated fluorescence and scanning electron microscopy method, we discovered a unique magnetotactic coccus strain (tentatively named SHHC-1) in brackish sediments collected from the estuary of Shihe River in Qinhuangdao city, eastern China. It phylogenetically belongs to the Alphaproteobacteria class. Transmission electron microscopy analyses reveal that SHHC-1 cells formed many magnetite-type magnetosomes organized as two bundles in each cell. Each bundle contains two parallel chains with smaller magnetosomes generally located at the ends of each chain. Unlike most magnetotactic alphaproteobacteria that generally form magnetosomes with uniform crystal morphologies, SHHC-1 magnetosomes display a more diverse variety of crystal morphology even within a single cell. Most particles have rectangular and rhomboidal projections, whilst others are triangular, or irregular. High resolution transmission electron microscopy observations coupled with morphological modeling indicate an idealized model—elongated octahedral crystals, a form composed of eight {111} faces. Furthermore, twins, multiple twins and stack dislocations are frequently observed in the SHHC-1 magnetosomes. This suggests that biomineralization of strain SHHC-1 magnetosome might be less biologically controlled than other magnetotactic alphaproteobacteria. Alternatively, SHHC-1 is more sensitive to the unfavorable environments under which it lives, or a combination of both factors may have controlled the magnetosome biomineralization process within this unique MTB.
机译:趋磁细菌(MTB)在形态和系统发育上都是原核生物。它们可以形成细胞内链组装的磁铁矿(Fe_(3)O_(4))或钙铁矿(Fe_(3)S_(4))纳米晶体,每个纳米晶体都被称为磁性小体的脂质双层膜包裹。趋磁球菌是在各种水生环境中最丰富的MTB形态型。然而,由于已经培养了少量菌株,因此在趋磁球菌中关于磁小体生物矿化的知识仍然难以捉摸。通过协同荧光和扫描电子显微镜方法,我们在中国东部秦皇岛市石河河口收集的微咸沉积物中发现了一种独特的趋磁球菌菌株(暂定为SHHC-1)。它在系统发育上属于Alphaproteobacteria类。透射电子显微镜分析表明,SHHC-1细胞形成许多磁铁矿型磁小体,每个小室中组织成两个束。每个束包含两条平行链,较小的磁小体通常位于每条链的末端。与通常形成具有均匀晶体形态的磁小体的大多数趋磁α蛋白细菌不同,SHHC-1磁小体即使在单个细胞内也显示出更多样化的晶体形态。大多数粒子具有矩形和菱形的投影,而其他粒子则是三角形或不规则的。高分辨率透射电子显微镜观察与形态学建模相结合,显示出一种理想化的模型-细长的八面体晶体,该晶体由八个{111}面组成。此外,在SHHC-1磁小体中经常观察到双胞胎,多胞胎和堆叠错位。这表明SHHC-1磁小体的生物矿化作用可能比其他趋磁α变形细菌的生物控制少。另外,SHHC-1对它所处的不利环境更为敏感,或者这两个因素的组合可能已经控制了这种独特MTB中的磁小体生物矿化过程。

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