New Phenotype and Mineralization of Biogenic Iron Oxide in Magnetotactic Bacteria

Many magnetotactic bacteria (MTB) biomineralize magnetite crystals that nucleate and grow inside intracellular membranous vesicles originating from invaginations of the cytoplasmic membrane. The crystals together with their surrounding membranes are referred to as magnetosomes. Magnetosome magnetite...

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Main Authors: Walid Baaziz, Corneliu Ghica, Jefferson Cypriano, Fernanda Abreu, Karine Anselme, Ovidiu Ersen, Marcos Farina, Jacques Werckmann
Format: Article
Language:English
Published: MDPI AG 2021-11-01
Series:Nanomaterials
Subjects:
Online Access:https://www.mdpi.com/2079-4991/11/12/3189
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author Walid Baaziz
Corneliu Ghica
Jefferson Cypriano
Fernanda Abreu
Karine Anselme
Ovidiu Ersen
Marcos Farina
Jacques Werckmann
author_facet Walid Baaziz
Corneliu Ghica
Jefferson Cypriano
Fernanda Abreu
Karine Anselme
Ovidiu Ersen
Marcos Farina
Jacques Werckmann
author_sort Walid Baaziz
collection DOAJ
description Many magnetotactic bacteria (MTB) biomineralize magnetite crystals that nucleate and grow inside intracellular membranous vesicles originating from invaginations of the cytoplasmic membrane. The crystals together with their surrounding membranes are referred to as magnetosomes. Magnetosome magnetite crystals nucleate and grow using iron transported inside the vesicle by specific proteins. Here, we tackle the question of the organization of magnetosomes, which are always described as constituted by linear chains of nanocrystals. In addition, it is commonly accepted that the iron oxide nanocrystals are in the magnetite-based phase. We show, in the case of a wild species of coccus-type bacterium, that there is a double organization of the magnetosomes, relatively perpendicular to each other, and that the nanocrystals are in fact maghemite. These findings were obtained, respectively, by using electron tomography of whole mounts of cells directly from the environment and high-resolution transmission electron microscopy and diffraction. Structure simulations were performed with the MacTempas software. This study opens new perspectives on the diversity of phenotypes within MTBs and allows to envisage other mechanisms of nucleation and formation of biogenic iron oxide crystals.
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spelling doaj.art-0b95ac6b99584f5e9eba10cc0927dc502023-11-23T09:49:06ZengMDPI AGNanomaterials2079-49912021-11-011112318910.3390/nano11123189New Phenotype and Mineralization of Biogenic Iron Oxide in Magnetotactic BacteriaWalid Baaziz0Corneliu Ghica1Jefferson Cypriano2Fernanda Abreu3Karine Anselme4Ovidiu Ersen5Marcos Farina6Jacques Werckmann7Institut de Physique et Chimie des Matériaux de Strasbourg (IPCMS), University of Strasbourg, 23 rue du Loess BP 43, CEDEX 2, 67034 Strasbourg, FranceNational Institute of Materials Physics, Atomistilor 405A, 077125 Magurele, RomaniaInstituto de Microbiologia Paulo de Góes, Universidade Federal do Rio de Janeiro, Avenida Carlos Chagas Filho, 373, CCS, UFRJ, Rio de Janeiro 21941-902, BrazilInstituto de Microbiologia Paulo de Góes, Universidade Federal do Rio de Janeiro, Avenida Carlos Chagas Filho, 373, CCS, UFRJ, Rio de Janeiro 21941-902, BrazilInstitut de Science des Matériaux de Mulhouse, University of Haute Alsace, 68057 Mulhouse, FranceInstitut de Physique et Chimie des Matériaux de Strasbourg (IPCMS), University of Strasbourg, 23 rue du Loess BP 43, CEDEX 2, 67034 Strasbourg, FranceInstituto de Ciências Biomédicas, Universidade Federal do Rio de Janeiro, Rio de Janeiro 21941-902, BrazilInstituto de Ciências Biomédicas, Universidade Federal do Rio de Janeiro, Rio de Janeiro 21941-902, BrazilMany magnetotactic bacteria (MTB) biomineralize magnetite crystals that nucleate and grow inside intracellular membranous vesicles originating from invaginations of the cytoplasmic membrane. The crystals together with their surrounding membranes are referred to as magnetosomes. Magnetosome magnetite crystals nucleate and grow using iron transported inside the vesicle by specific proteins. Here, we tackle the question of the organization of magnetosomes, which are always described as constituted by linear chains of nanocrystals. In addition, it is commonly accepted that the iron oxide nanocrystals are in the magnetite-based phase. We show, in the case of a wild species of coccus-type bacterium, that there is a double organization of the magnetosomes, relatively perpendicular to each other, and that the nanocrystals are in fact maghemite. These findings were obtained, respectively, by using electron tomography of whole mounts of cells directly from the environment and high-resolution transmission electron microscopy and diffraction. Structure simulations were performed with the MacTempas software. This study opens new perspectives on the diversity of phenotypes within MTBs and allows to envisage other mechanisms of nucleation and formation of biogenic iron oxide crystals.https://www.mdpi.com/2079-4991/11/12/3189magnetotactic bacteriaphenotypemagnetitemaghemiteelectron microscopyEDS
spellingShingle Walid Baaziz
Corneliu Ghica
Jefferson Cypriano
Fernanda Abreu
Karine Anselme
Ovidiu Ersen
Marcos Farina
Jacques Werckmann
New Phenotype and Mineralization of Biogenic Iron Oxide in Magnetotactic Bacteria
Nanomaterials
magnetotactic bacteria
phenotype
magnetite
maghemite
electron microscopy
EDS
title New Phenotype and Mineralization of Biogenic Iron Oxide in Magnetotactic Bacteria
title_full New Phenotype and Mineralization of Biogenic Iron Oxide in Magnetotactic Bacteria
title_fullStr New Phenotype and Mineralization of Biogenic Iron Oxide in Magnetotactic Bacteria
title_full_unstemmed New Phenotype and Mineralization of Biogenic Iron Oxide in Magnetotactic Bacteria
title_short New Phenotype and Mineralization of Biogenic Iron Oxide in Magnetotactic Bacteria
title_sort new phenotype and mineralization of biogenic iron oxide in magnetotactic bacteria
topic magnetotactic bacteria
phenotype
magnetite
maghemite
electron microscopy
EDS
url https://www.mdpi.com/2079-4991/11/12/3189
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