Deep-branching magnetotactic bacteria form intracellular carbonates enriched in trace metals

Intracellular biomineralization is a hallmark of animals and algae, yet among prokaryotes, it has traditionally been associated with a limited range of lineages and minerals. This study reveals that magnetotactic bacteria (MTB) from both the <i>Pseudomonadota</i> and the deep-branching <i>Nitrospirota</i> phyla are capable of intracellularly forming carbonate granules enriched in diverse divalent cations, including environmentally scarce trace metals Ba²⁺ and Ni²⁺, and biologically essential Mg²⁺. These findings significantly expand the known taxonomic and functional diversity of prokaryotic intracellular calcifiers. By integrating electron microscopy, metagenomics, and structural protein modeling, we propose a potential metal-selective transport system that facilitates trace element accumulation and carbonate precipitation. This work establishes a previously underappreciated role for MTB in trace metal biogeochemical cycling (i.e., Ba²⁺ and Ni²⁺) and suggests that intracellular calcification may be a more widespread bacterial trait than previously assumed.

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Publication Details

Journal
mSystems
Published
2025-11-12
DOI
https://doi.org/10.1128/msystems.01131-25
Citations
1
Primary Topic
Geomagnetism and Paleomagnetism Studies
Type
article
Field-Weighted Citation Impact
0.81
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article

Deep-branching magnetotactic bacteria form intracellular carbonates enriched in trace metals

Yinzhao Wang, Fanqi Meng, Z. Cao, Yongxin Pan et al.
1 citations
mSystems
Geomagnetism and Paleomagnetism Studies
0.81
article

Deep-branching magnetotactic bacteria form intracellular carbonates enriched in trace metals

Yinzhao Wang, Fanqi Meng, Z. Cao, Yongxin Pan, Kelei Zhu, Jinhua Li, Rongrong Zhang, Chaoqun Zhang, Peiyu Liu, Andrew P. Roberts
article en
1 citations

Abstract

Intracellular biomineralization is a hallmark of animals and algae, yet among prokaryotes, it has traditionally been associated with a limited range of lineages and minerals. This study reveals that magnetotactic bacteria (MTB) from both the <i>Pseudomonadota</i> and the deep-branching <i>Nitrospirota</i> phyla are capable of intracellularly forming carbonate granules enriched in diverse divalent cations, including environmentally scarce trace metals Ba²⁺ and Ni²⁺, and biologically essential Mg²⁺. These findings significantly expand the known taxonomic and functional diversity of prokaryotic intracellular calcifiers. By integrating electron microscopy, metagenomics, and structural protein modeling, we propose a potential metal-selective transport system that facilitates trace element accumulation and carbonate precipitation. This work establishes a previously underappreciated role for MTB in trace metal biogeochemical cycling (i.e., Ba²⁺ and Ni²⁺) and suggests that intracellular calcification may be a more widespread bacterial trait than previously assumed.

mSystemsVol. 10(12)
King University (US), Australian National University (AU), Planetary Science Institute (US), Shanghai Jiao Tong University (CN), Peking University (CN), Institute of Geology and Geophysics (AZ), Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (CN), Qingdao National Laboratory for Marine Science and Technology (CN), Institute of Geology and Geophysics (CN), Division of Materials Science and Engineering (AU), University of Chinese Academy of Sciences (CN), Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (CN)
Openalex Percentile: Top 22%
Geomagnetism and Paleomagnetism Studies
0.81
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