Magnetochrome- catalyzed oxidation of ferrous iron by MamP enables magnetite crystal growth in the magnetotactic bacterium AMB-1
成果类型:
Article
署名作者:
Amor, Matthieu; Chevrier, Daniel M.; Siponen, Marina I.; Egli, Ramon; Scoppola, Ernesto; Marcano, Lourdes; Li, Chenghao; Choueikani, Fadi; Faivre, Damien
署名单位:
CEA; Centre National de la Recherche Scientifique (CNRS); Aix-Marseille Universite; Ecole Normale Superieure de Lyon (ENS de LYON); Centre National de la Recherche Scientifique (CNRS); Universite Claude Bernard Lyon 1; Max Planck Society; CIC biomaGUNE; University of Oviedo; SOLEIL Synchrotron
刊物名称:
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
ISSN/ISSBN:
0027-11797
DOI:
10.1073/pnas.2410245121
发表日期:
2024-12-10
关键词:
magnetospirillum-gryphiswaldense
redox control
magnetosome biogenesis
genetic dissection
biomineralization
distinct
reveals
摘要:
Magnetotactic bacteria have evolved the remarkable capacity to biomineralize chains of magnetite [Fe(II)Fe(III)2O4] nanoparticles that align along the geomagnetic field and optimize their navigation in the environment. Mechanisms enabling magnetite formation require the complex action of numerous proteins for iron acquisition, sequestration in dedicated magnetosome organelles, and precipitation into magnetite. The MamP protein contains c- type cytochromes called magnetochrome domains that are found exclusively in magnetotactic bacteria. Ablation of magnetochromes in MamP prevents bacteria from aligning with external magnetic fields, showing their importance to maintain this biological function. MamP has been proposed, mostly from in vitro experimentations, to regulate iron redox state and maintain an Fe(II)/Fe(III) balance compatible with magnetite formation via the iron oxidase activity of magnetochromes. To test the proposed function for MamP in vivo in the magnetotactic strain Magnetospirillum magneticum (AMB)-1, we characterized the iron species in chemical MamP- mediated magnetite syntheses as well as in bacteria unable to produce MamP using a combination of physicochemical methodologies. We show that MamP has no apparent control on the speciation and oxidation state of intracellular iron or on the Fe(II)/Fe(III) balance in magnetite. We propose that MamP promotes magnetite growth by incorporating Fe(III) into preexisting magnetite seeds and that magnetite structure and stoichiometry is maintained by further equilibration with dissolved Fe(II) in magnetosome organelles.