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首页> 外文期刊>Geomicrobiology journal >Magnetite (Fe3O4) and greigite (Fe3S4) crystals in multicellular magnetotactic prokaryotes
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Magnetite (Fe3O4) and greigite (Fe3S4) crystals in multicellular magnetotactic prokaryotes

机译:多细胞趋磁原核生物中的磁铁矿(Fe3O4)和钙铁矿(Fe3S4)晶体

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摘要

Magnetotactic bacteria produce iron oxides, iron sulfides or both in organelles called magnetosomes. Most of these bacteria are unicellular and biomineralize magnetite (Fe3O4). In contrast, multicellular magnetotactic prokaryotes (MMPs) consisting of several gram-negative cells have only been known to crystallize the magnetic iron sulfide greigite (Fe3S4). In this work, we describe MMPs that mineralize magnetite in bullet-shaped crystals. Another unusual aspect is that magnetite occurs either as the only crystals or together with greigite crystals. MMPs containing only greigite in the magnetosomes occur in the same environment. These findings show that morphology, ultrastructure, and behavior are the main characteristics of the MMPs, not the type of magnetic crystal biomineralized in the magnetosomes.
机译:趋磁细菌在称为磁小体的细胞器中产生氧化铁,硫化铁或二者兼有。这些细菌大多数是单细胞的且生物矿化的磁铁矿(Fe3O4)。相比之下,仅由几个革兰氏阴性细胞组成的多细胞趋磁原核生物(MMP)才能使磁性硫化铁钙铁矿(Fe3S4)结晶。在这项工作中,我们描述了在子弹形晶体中矿化磁铁矿的MMP。另一个不寻常的方面是磁铁矿要么作为唯一的晶体出现,要么与钙铁矿晶体一起出现。磁小体中仅含有钙铁矿的MMP在同一环境中发生。这些发现表明形态,超微结构和行为是MMP的主要特征,而不是在磁小体中生物矿化的磁性晶体的类型。

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