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周质细菌生物矿化硫化铜纳米颗粒。

Periplasmic Bacterial Biomineralization of Copper Sulfide Nanoparticles.

机构信息

Aix-Marseille University, French Alternative Energies and Atomic Energy Commission (CEA), French National Center for Scientific Research (CNRS), UMR7265 Institute of Biosciences and Biotechnologies of Aix-Marseille (BIAM), Saint-Paul-lez-Durance, 13108, France.

Department of Plant and Environmental Sciences, Weizmann Institute of Science, Rehovot, 7610001, Israel.

出版信息

Adv Sci (Weinh). 2022 Oct;9(28):e2203444. doi: 10.1002/advs.202203444. Epub 2022 Aug 17.

DOI:10.1002/advs.202203444
PMID:35975419
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9534983/
Abstract

Metal sulfides are a common group of extracellular bacterial biominerals. However, only a few cases of intracellular biomineralization are reported in this group, mostly limited to greigite (Fe S ) in magnetotactic bacteria. Here, a previously unknown periplasmic biomineralization of copper sulfide produced by the magnetotactic bacterium Desulfamplus magnetovallimortis strain BW-1, a species known to mineralize greigite (Fe S ) and magnetite (Fe O ) in the cytoplasm is reported. BW-1 produces hundreds of spherical nanoparticles, composed of 1-2 nm substructures of a poorly crystalline hexagonal copper sulfide structure that remains in a thermodynamically unstable state. The particles appear to be surrounded by an organic matrix as found from staining and electron microscopy inspection. Differential proteomics suggests that periplasmic proteins, such as a DegP-like protein and a heavy metal-binding protein, could be involved in this biomineralization process. The unexpected periplasmic formation of copper sulfide nanoparticles in BW-1 reveals previously unknown possibilities for intracellular biomineralization that involves intriguing biological control and holds promise for biological metal recovery in times of copper shortage.

摘要

金属硫化物是一类常见的胞外细菌生物矿化物质。然而,该类物质中仅有少数胞内生物矿化的报道,且大多局限于趋磁细菌中的磁硫铁矿(FeS)。本文报道了趋磁细菌脱硫弧菌 BW-1 细胞周质内一种未知的铜硫化物生物矿化作用,该菌已知在细胞质内矿化生成磁硫铁矿(FeS)和磁铁矿(Fe3O4)。BW-1 产生了数百个球形纳米颗粒,由 1-2nm 的亚结构组成,具有较差结晶的六方铜硫化物结构,处于热力学不稳定状态。这些颗粒似乎被一层有机基质所包围,这可从染色和电子显微镜检查中发现。差异蛋白质组学表明,周质内蛋白,如 DegP 样蛋白和重金属结合蛋白,可能参与了这一生物矿化过程。BW-1 中出乎意料的铜硫化物纳米颗粒的细胞周质形成揭示了以前未知的胞内生物矿化可能性,涉及有趣的生物控制,并有望在铜短缺时期进行生物金属回收。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/953c/9534983/90d38924a774/ADVS-9-2203444-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/953c/9534983/ee05acbe1403/ADVS-9-2203444-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/953c/9534983/9f827d5e0192/ADVS-9-2203444-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/953c/9534983/723f8c6d4eac/ADVS-9-2203444-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/953c/9534983/90d38924a774/ADVS-9-2203444-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/953c/9534983/ee05acbe1403/ADVS-9-2203444-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/953c/9534983/9f827d5e0192/ADVS-9-2203444-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/953c/9534983/723f8c6d4eac/ADVS-9-2203444-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/953c/9534983/90d38924a774/ADVS-9-2203444-g001.jpg

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Diversity of Microbial Metal Sulfide Biomineralization.微生物金属硫化物生物矿化的多样性。
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Microbe-Mediated Extracellular and Intracellular Mineralization: Environmental, Industrial, and Biotechnological Applications.
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