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- W4386813093 endingPage "166993" @default.
- W4386813093 startingPage "166993" @default.
- W4386813093 abstract "Microbial Fe(III) reduction is a key component of the iron cycle in natural environments. However, the susceptibility of Fe(III) (hydr)oxides to microbial reduction varies depending on the mineral's crystallinity, and the type of Fe(III) (hydr)oxide in turn will affect the composition of the microbial community. We created microcosm reactors with microbial communities from four different sources (soil, surface water, groundwater, and aerosols), three Fe(III) (hydr)oxides (lepidocrocite, goethite, and hematite) as electron acceptors, and acetate as an electron donor to investigate the shaping effect of Fe(III) mineral type on the development of microbial communities. During a 10-month incubation, changes in microbial community composition, Fe(III) reduction, and acetate utilization were monitored. Overall, there was greater reduction of lepidocrocite than of goethite and hematite, and the development of microbial communities originating from the same source diverged when supplied with different Fe(III) (hydr)oxides. Furthermore, each Fe(III) mineral was associated with unique taxa that emerged from different sources. This study illustrates the taxonomic diversity of Fe(III)-reducing microbes from a broad range of natural environments." @default.
- W4386813093 created "2023-09-18" @default.
- W4386813093 creator A5022824022 @default.
- W4386813093 creator A5026192569 @default.
- W4386813093 creator A5050142136 @default.
- W4386813093 creator A5067279479 @default.
- W4386813093 date "2023-12-01" @default.
- W4386813093 modified "2023-09-30" @default.
- W4386813093 title "Effects of Fe(III) (hydr)oxide mineralogy on the development of microbial communities originating from soil, surface water, groundwater, and aerosols" @default.
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