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Epsilon-Fe(2)O(3) is a novel intermediate for magnetite biosynthesis in magnetotactic bacteria
BACKGROUND: Natural biological magnetite nanoparticles are widely distributed from microorganisms to humans. It is found to be very important in organisms, especially in navigation. Moreover, purified magnetite nanoparticles also have potential applications in bioengineering and biomedicine. Magneto...
Autores principales: | , , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
BioMed Central
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6679552/ https://www.ncbi.nlm.nih.gov/pubmed/31388439 http://dx.doi.org/10.1186/s40824-019-0162-1 |
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author | Wen, Tong Zhang, Yunpeng Geng, Yuanyuan Liu, Junquan Basit, Abdul Tian, Jiesheng Li, Ying Li, Jilun Ju, Jing Jiang, Wei |
author_facet | Wen, Tong Zhang, Yunpeng Geng, Yuanyuan Liu, Junquan Basit, Abdul Tian, Jiesheng Li, Ying Li, Jilun Ju, Jing Jiang, Wei |
author_sort | Wen, Tong |
collection | PubMed |
description | BACKGROUND: Natural biological magnetite nanoparticles are widely distributed from microorganisms to humans. It is found to be very important in organisms, especially in navigation. Moreover, purified magnetite nanoparticles also have potential applications in bioengineering and biomedicine. Magnetotactic bacteria (MTB) is considered one of the most abundant species around the world which can form intracellular membrane enveloped magnetic nanoparticles, referred to as magnetosomes. To our knowledge, the biomineralization of magnetosome in MTB involves a serious of genes located on a large unstable genomic region named magnetosome island, which specially exists in MTB. The magnetite core of magnetosome formed via a Fe (III) ion intermediates, for instance, α-Fe(2)O(3) and ferrihydrite. Though the biosynthesis of magnetosome represents a general biomineralization mechanism of biogenic magnetite, knowledge of magnetosome biosynthesis and biomineralization remains very limited. METHOD: Cells used in this study were cultured in a 7.5-L bioreactor, samples for intermediate capture were taken each certain time interval after the generation of magnetosome biosynthesis condition. High-resolution transmission electron microscopy were used to analyze the detailed structure of magnetosomes. The parameters of the crystal structures were obtained by Fast Fourier Transform analyses. RESULTS: In this study, we identified a novel intermediate phase, ε-Fe(2)O(3), during the magnetite maturation process in MTB via kinetic analysis. Unlike α-Fe(2)O(3), which has been reported as a precursor during magnetosome biosynthesis in MTB before, ε-Fe(2)O(3), due to its thermal instability, is a rare phase with scarce natural abundance. This finding confirmed that ε-Fe(2)O(3) is an important novel intermediate during the biomineralization of magnetosome in MTB, and shed new light on the magnetosome biosynthesis pathway. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1186/s40824-019-0162-1) contains supplementary material, which is available to authorized users. |
format | Online Article Text |
id | pubmed-6679552 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2019 |
publisher | BioMed Central |
record_format | MEDLINE/PubMed |
spelling | pubmed-66795522019-08-06 Epsilon-Fe(2)O(3) is a novel intermediate for magnetite biosynthesis in magnetotactic bacteria Wen, Tong Zhang, Yunpeng Geng, Yuanyuan Liu, Junquan Basit, Abdul Tian, Jiesheng Li, Ying Li, Jilun Ju, Jing Jiang, Wei Biomater Res Research Article BACKGROUND: Natural biological magnetite nanoparticles are widely distributed from microorganisms to humans. It is found to be very important in organisms, especially in navigation. Moreover, purified magnetite nanoparticles also have potential applications in bioengineering and biomedicine. Magnetotactic bacteria (MTB) is considered one of the most abundant species around the world which can form intracellular membrane enveloped magnetic nanoparticles, referred to as magnetosomes. To our knowledge, the biomineralization of magnetosome in MTB involves a serious of genes located on a large unstable genomic region named magnetosome island, which specially exists in MTB. The magnetite core of magnetosome formed via a Fe (III) ion intermediates, for instance, α-Fe(2)O(3) and ferrihydrite. Though the biosynthesis of magnetosome represents a general biomineralization mechanism of biogenic magnetite, knowledge of magnetosome biosynthesis and biomineralization remains very limited. METHOD: Cells used in this study were cultured in a 7.5-L bioreactor, samples for intermediate capture were taken each certain time interval after the generation of magnetosome biosynthesis condition. High-resolution transmission electron microscopy were used to analyze the detailed structure of magnetosomes. The parameters of the crystal structures were obtained by Fast Fourier Transform analyses. RESULTS: In this study, we identified a novel intermediate phase, ε-Fe(2)O(3), during the magnetite maturation process in MTB via kinetic analysis. Unlike α-Fe(2)O(3), which has been reported as a precursor during magnetosome biosynthesis in MTB before, ε-Fe(2)O(3), due to its thermal instability, is a rare phase with scarce natural abundance. This finding confirmed that ε-Fe(2)O(3) is an important novel intermediate during the biomineralization of magnetosome in MTB, and shed new light on the magnetosome biosynthesis pathway. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1186/s40824-019-0162-1) contains supplementary material, which is available to authorized users. BioMed Central 2019-08-02 /pmc/articles/PMC6679552/ /pubmed/31388439 http://dx.doi.org/10.1186/s40824-019-0162-1 Text en © The Author(s). 2019 Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated. |
spellingShingle | Research Article Wen, Tong Zhang, Yunpeng Geng, Yuanyuan Liu, Junquan Basit, Abdul Tian, Jiesheng Li, Ying Li, Jilun Ju, Jing Jiang, Wei Epsilon-Fe(2)O(3) is a novel intermediate for magnetite biosynthesis in magnetotactic bacteria |
title | Epsilon-Fe(2)O(3) is a novel intermediate for magnetite biosynthesis in magnetotactic bacteria |
title_full | Epsilon-Fe(2)O(3) is a novel intermediate for magnetite biosynthesis in magnetotactic bacteria |
title_fullStr | Epsilon-Fe(2)O(3) is a novel intermediate for magnetite biosynthesis in magnetotactic bacteria |
title_full_unstemmed | Epsilon-Fe(2)O(3) is a novel intermediate for magnetite biosynthesis in magnetotactic bacteria |
title_short | Epsilon-Fe(2)O(3) is a novel intermediate for magnetite biosynthesis in magnetotactic bacteria |
title_sort | epsilon-fe(2)o(3) is a novel intermediate for magnetite biosynthesis in magnetotactic bacteria |
topic | Research Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6679552/ https://www.ncbi.nlm.nih.gov/pubmed/31388439 http://dx.doi.org/10.1186/s40824-019-0162-1 |
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