Chemical controls on iron distributions across the subsurface South Pacific Ocean
Iron and nitrogen are the primary nutrients that limit productivity in the ocean. While nitrogen cycling is largely controlled by biology, iron cycling is strongly determined by chemistry because iron losses are driven by abiotic formation of authigenic mineral iron. Here, we apply a mechanistic app...
| Autores: | , , , , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2026 |
| País: | España |
| Institución: | Universitat de Lleida (UdL) |
| Repositorio: | Repositori Obert UdL |
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| Acceso en línea: | https://doi.org/10.1038/s41467-026-72070-y https://hdl.handle.net/10459.1/470082 |
| Access Level: | acceso abierto |
| Palabra clave: | Iron cycling Organic matter Authigenic minerals |
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Chemical controls on iron distributions across the subsurface South Pacific OceanGledhill, M.Gosnell, K.Humphreys, M. P.Delaigue, L.Helle, N.Zhu, K.Lodeiro, PabloRey-Castro, CarlosAchterberg, E. P.Iron cyclingOrganic matterAuthigenic mineralsIron and nitrogen are the primary nutrients that limit productivity in the ocean. While nitrogen cycling is largely controlled by biology, iron cycling is strongly determined by chemistry because iron losses are driven by abiotic formation of authigenic mineral iron. Here, we apply a mechanistic approach to examine how organic matter across the dissolved-particulate size spectrum controls authigenic iron formation in subsurface waters (>250 m) of the South Pacific Ocean. We find that accounting for the chemical heterogeneity of organic matter is essential for predicting widespread authigenic iron formation. Predicted dissolved and particulate iron concentrations matched observations in the ocean interior, while discrepancies were linked to kinetic control of authigenic iron formation or inputs of particles from the seafloor. Our work shows the need to represent the complexity of abiotic interactions to better resolve the interplay of chemical and biological controls on ocean iron cyclingOpen Access funding enabled and organized by Projekt DEAL.Nature2026info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttps://doi.org/10.1038/s41467-026-72070-yhttps://hdl.handle.net/10459.1/470082reponame:Repositori Obert UdL instname:Universitat de Lleida (UdL)InglésReproducció del document publicat a https://doi.org/10.1038/s41467-026-72070-yNature Communications, 2026, vol. 17, núm. 3533, p. 1-14cc-by (c) Gledhill et al., 2026Attribution 4.0 Internationalinfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/4.0/oai:dnet:.___________::303d8fa971977ff0e304b9719f4b07ff2026-06-24T12:42:17Z |
| dc.title.none.fl_str_mv |
Chemical controls on iron distributions across the subsurface South Pacific Ocean |
| title |
Chemical controls on iron distributions across the subsurface South Pacific Ocean |
| spellingShingle |
Chemical controls on iron distributions across the subsurface South Pacific Ocean Gledhill, M. Iron cycling Organic matter Authigenic minerals |
| title_short |
Chemical controls on iron distributions across the subsurface South Pacific Ocean |
| title_full |
Chemical controls on iron distributions across the subsurface South Pacific Ocean |
| title_fullStr |
Chemical controls on iron distributions across the subsurface South Pacific Ocean |
| title_full_unstemmed |
Chemical controls on iron distributions across the subsurface South Pacific Ocean |
| title_sort |
Chemical controls on iron distributions across the subsurface South Pacific Ocean |
| dc.creator.none.fl_str_mv |
Gledhill, M. Gosnell, K. Humphreys, M. P. Delaigue, L. Helle, N. Zhu, K. Lodeiro, Pablo Rey-Castro, Carlos Achterberg, E. P. |
| author |
Gledhill, M. |
| author_facet |
Gledhill, M. Gosnell, K. Humphreys, M. P. Delaigue, L. Helle, N. Zhu, K. Lodeiro, Pablo Rey-Castro, Carlos Achterberg, E. P. |
| author_role |
author |
| author2 |
Gosnell, K. Humphreys, M. P. Delaigue, L. Helle, N. Zhu, K. Lodeiro, Pablo Rey-Castro, Carlos Achterberg, E. P. |
| author2_role |
author author author author author author author author |
| dc.subject.none.fl_str_mv |
Iron cycling Organic matter Authigenic minerals |
| topic |
Iron cycling Organic matter Authigenic minerals |
| description |
Iron and nitrogen are the primary nutrients that limit productivity in the ocean. While nitrogen cycling is largely controlled by biology, iron cycling is strongly determined by chemistry because iron losses are driven by abiotic formation of authigenic mineral iron. Here, we apply a mechanistic approach to examine how organic matter across the dissolved-particulate size spectrum controls authigenic iron formation in subsurface waters (>250 m) of the South Pacific Ocean. We find that accounting for the chemical heterogeneity of organic matter is essential for predicting widespread authigenic iron formation. Predicted dissolved and particulate iron concentrations matched observations in the ocean interior, while discrepancies were linked to kinetic control of authigenic iron formation or inputs of particles from the seafloor. Our work shows the need to represent the complexity of abiotic interactions to better resolve the interplay of chemical and biological controls on ocean iron cycling |
| publishDate |
2026 |
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2026 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
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article |
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publishedVersion |
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https://doi.org/10.1038/s41467-026-72070-y https://hdl.handle.net/10459.1/470082 |
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https://doi.org/10.1038/s41467-026-72070-y https://hdl.handle.net/10459.1/470082 |
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Inglés |
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Inglés |
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Reproducció del document publicat a https://doi.org/10.1038/s41467-026-72070-y Nature Communications, 2026, vol. 17, núm. 3533, p. 1-14 |
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cc-by (c) Gledhill et al., 2026 Attribution 4.0 International info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ |
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cc-by (c) Gledhill et al., 2026 Attribution 4.0 International http://creativecommons.org/licenses/by/4.0/ |
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openAccess |
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Nature |
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Nature |
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reponame:Repositori Obert UdL instname:Universitat de Lleida (UdL) |
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