Aubineau, Jeremie, Chi Fru, Ernest ![]() ![]() |
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Abstract
Models describing banded iron formation deposition beneath oxygenated Paleoproterozoic marine shelf waters assume that microaerophilic iron-oxidizing microorganisms were significant contributors. However, direct evidence for this mechanism is lacking, and it remains unclear how associated primary organic biomass and biogenic iron oxyhydroxides transformed into organic carbon-poor iron oxide/carbonate-rich bands in banded iron formations. Here we explore in situ modern Zetaproteobacterial iron-oxidizing mats thriving in the Lucky Strike hydrothermal vent field to develop an empirical model that explains the potential contribution of iron-based metabolisms to deposition of rocks resembling banded iron formations. Petrographic, mineralogical, and geochemical data suggest that abundant production of Zetaproteobacterial stalks nucleates and drives spontaneous biotic/abiotic ferrihydrite precipitation in the mats. Subsequent early diagenetic anaerobic microbial oxidation of dead biomass as the mats aged, coupled to microbial reduction of iron oxyhydroxides/oxides, generates ferrous carbonates and mixed valence magnetite. Collectively, this forms crystalline iron-rich organic carbon-lean 13C-depleted layers reminiscent of Precambrian banded iron formation microbands.
Item Type: | Article |
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Date Type: | Published Online |
Status: | Published |
Schools: | Schools > Earth and Environmental Sciences |
Publisher: | Nature Research |
ISSN: | 2662-4435 |
Date of First Compliant Deposit: | 7 April 2025 |
Date of Acceptance: | 18 March 2025 |
Last Modified: | 07 May 2025 10:46 |
URI: | https://orca.cardiff.ac.uk/id/eprint/177440 |
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