Intracellular magnetite biomineralization in bacteria proceeds by a distinct pathway involving membrane-bound ferritin and an iron(II) species

被引：109

作者：

Faivre, Damien

Boettger, Lars H.

Matzanke, Berthold F.

Schueler, Dirk

机构：

[1] Univ Munich, Dept Biol, D-80638 Munich, Germany

[2] Max Planck Inst Marine Microbiol, Dept Microbiol, D-28359 Bremen, Germany

[3] Univ Lubeck, Inst Phys, D-23538 Lubeck, Germany

[4] Univ Lubeck, Isotopes Lab, D-23538 Lubeck, Germany

[5] Max Planck Inst Colloids & Interfaces, Abt Biomat, D-14424 Potsdam, Germany

来源：

ANGEWANDTE CHEMIE-INTERNATIONAL EDITION | 2007年 / 46卷 / 44期

关键词：

biomineralization; magnetic properties; magnetotactic bacteria; Mossbauer spectroscopy; reaction mechanisms;

D O I：

10.1002/anie.200700927

中图分类号：

O6 [化学];

学科分类号：

0703 ;

摘要：

A time-resolved study of magnetite formation in magnetotactic bacteria has shown that magnetite biomineralization proceeds first by coprecipitation of Fe2+ and Fe3+ ions and then via small magnetite crystallites (see picture) within invaginating magnetosomes associated with the cell membrane, which further develop into mature crystals after magnetosome vesicles are released from the cell membrane. (Figure Presented) © 2007 Wiley-VCH Verlag GmbH & Co. KGaA.

引用

页码：8495 / 8499

页数：5

共 19 条

[1] Magnetosome formation in prokaryotes [J].