Magnetite (Fe3O4) and greigite (Fe3S4) crystals in multicellular magnetotactic prokaryotes

被引:66
作者
Lins, Ulysses
Keim, Carolina N.
Evans, Flavia F.
Farina, Marcos [1 ]
Buseck, Peter R.
机构
[1] Univ Fed Rio de Janeiro, Inst Ciencias Biomed, Ctr Ciencias Saude, BR-21941590 Rio De Janeiro, Brazil
[2] Univ Fed Rio de Janeiro, Dept Microbiol Geral, Inst Microbiol Prof Paulo de Goes, BR-21941590 Rio De Janeiro, Brazil
[3] Arizona State Univ, Dept Geol Sci, Tempe, AZ 85287 USA
[4] Arizona State Univ, Dept Chem Biochem, Tempe, AZ 85287 USA
基金
美国国家航空航天局;
关键词
biomineralization; greigite; magnetite; magnetosome; magnetotactic bacteria; magnetotactic multicellular organism; multicellular magnetotactic prokaryote; many-celled magnetotactic prokaryote; MMP;
D O I
10.1080/01490450601134317
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
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.
引用
收藏
页码:43 / 50
页数:8
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