Pseudomonas brassicacearum-Induced Biotite Weathering: Role of Iron Homeostasis and Two Siderophores

Soil bacteria play a crucial role in enhancing mineral weathering, thereby facilitating the release of mineral structural ions into the environment. Pseudomonas brassicacearum NFM421, a root-isolated bacterium, produces two different siderophores in the form of pyoverdine and ornicorrugatin. We stud...

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Published inEnvironmental science & technology Vol. 59; no. 16; pp. 7973 - 7982
Main Authors Girard, Tom, Basile-Doelsch, Isabelle, Fochesato, Sylvain, Duvivier, Adrien, Doelsch, Emmanuel, Heulin, Thierry, Achouak, Wafa
Format Journal Article
LanguageEnglish
Published United States American Chemical Society 29.04.2025
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Summary:Soil bacteria play a crucial role in enhancing mineral weathering, thereby facilitating the release of mineral structural ions into the environment. Pseudomonas brassicacearum NFM421, a root-isolated bacterium, produces two different siderophores in the form of pyoverdine and ornicorrugatin. We studied the interaction between this bacterium and biotitea natural iron-bearing phyllosilicateto assess the factors governing siderophore-mediated biogenic weathering. We demonstrated that bacterial Fe is an essential factor driving biotite weathering. Our findings suggested that the lipopeptidic siderophore ornicorrugatin might be more effective than pyoverdine as an iron-bearing mineral weathering agent. This secondary siderophore’s production is maintained even when the iron requirement of the bacteria is fulfilled. Moreover, we observed that another mechanism requiring direct physical contact might enable P. brassicacearum to acquire iron structural ions from soil minerals.
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ISSN:0013-936X
1520-5851
1520-5851
DOI:10.1021/acs.est.4c07951