Iron’s irony: speciation, complexation & microbial processing of Fe in hydrothermal plumes

Abstract This review integrates vent fluid chemistry and biogeochemical processes to assess how hydrothermal systems influence oceanic iron distribution. Despite rapid precipitation of iron-bearing minerals immediately after venting, buoyant hydrothermal plumes disperse dissolved and nanoparticulate iron across thousands of kilometers, aided by slow oxidation, reversible exchanges between soluble and particulate iron, and biological interactions. These mechanisms underscore hydrothermal vents as a widespread iron source, impacting deep and surface marine ecosystems. Transport dynamics are governed by temperature, pH, microbial activity, and water-mass residence times. We investigate the controls on hydrothermal iron distribution by examining relationships between iron and pH, temperature, chlorinity and hydrogen sulfide in vent fluids, along with solubility modeling of iron(III) hydroxide and iron(II) sulfide. Finally, we highlight key research frontiers that will advance understanding of both hydrothermal processes and their role in shaping the ocean iron biogeochemical cycle.

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Publication Details

Journal
Communications Earth & Environment
Published
2025-10-17
DOI
https://doi.org/10.1038/s43247-025-02839-4
Primary Topic
Geochemistry and Elemental Analysis
Type
article
Field-Weighted Citation Impact
0.00

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article

Iron’s irony: speciation, complexation & microbial processing of Fe in hydrothermal plumes

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Communications Earth & Environment
Geochemistry and Elemental Analysis
article

Iron’s irony: speciation, complexation & microbial processing of Fe in hydrothermal plumes

Sylvia G. Sander, Andrea Koschinsky, Mirjam Perner, Charlotte Kleint, Christoph Voelker, Stefanie Böhnke-Brandt, Sinikka T. Lennartz, Laura Haffert, Alexander Diehl, Martha Gledhill, Solveig I Bühring, Ying Ye
article en

Abstract

Abstract This review integrates vent fluid chemistry and biogeochemical processes to assess how hydrothermal systems influence oceanic iron distribution. Despite rapid precipitation of iron-bearing minerals immediately after venting, buoyant hydrothermal plumes disperse dissolved and nanoparticulate iron across thousands of kilometers, aided by slow oxidation, reversible exchanges between soluble and particulate iron, and biological interactions. These mechanisms underscore hydrothermal vents as a widespread iron source, impacting deep and surface marine ecosystems. Transport dynamics are governed by temperature, pH, microbial activity, and water-mass residence times. We investigate the controls on hydrothermal iron distribution by examining relationships between iron and pH, temperature, chlorinity and hydrogen sulfide in vent fluids, along with solubility modeling of iron(III) hydroxide and iron(II) sulfide. Finally, we highlight key research frontiers that will advance understanding of both hydrothermal processes and their role in shaping the ocean iron biogeochemical cycle.

Communications Earth & EnvironmentVol. 6(1)
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), Carl von Ossietzky Universität Oldenburg (DE), University of Bremen (DE), Constructor University (DE), Christian-Albrechts-Universität zu Kiel (DE), GEOMAR Helmholtz Centre for Ocean Research Kiel (DE)
Deutsche Forschungsgemeinschaft
Openalex Percentile: Top 75%
Geochemistry and Elemental Analysis
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