Articles | Volume 21, issue 22
https://doi.org/10.5194/bg-21-5233-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-21-5233-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
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25 Nov 2024
Research article | Highlight paper |
| 25 Nov 2024
| 25 Nov 2024
Microbial strong organic-ligand production is tightly coupled to iron in hydrothermal plumes
Joint Institute for the Study of Atmosphere and Ocean, University of Washington, 3737 Brooklyn Avenue NE, Seattle, WA 98195, USA
Cooperative Institute for Climate, Ocean, and Ecosystem Studies, University of Washington, 3737 Brooklyn Avenue NE, Seattle, WA 98195, USA
School of Oceanography, University of Washington, 1501 NE Boat Street, Seattle, WA 98195, USA
Patrick J. Monreal
CORRESPONDING AUTHOR
School of Oceanography, University of Washington, 1501 NE Boat Street, Seattle, WA 98195, USA
Earth Systems Program, Stanford University, 473 Via Ortega, Stanford, CA 94305, USA
Justine B. Albers
Department of Ecology, Evolution, and Marine Biology, University of California, Santa Barbara, CA 93106, USA
Alastair J. M. Lough
Department of Ocean and Earth Sciences, National Oceanography Centre, University of Southampton, European Way, Southampton SO14 3ZH, UK
Alyson E. Santoro
Department of Ecology, Evolution, and Marine Biology, University of California, Santa Barbara, CA 93106, USA
Travis Mellett
School of Oceanography, University of Washington, 1501 NE Boat Street, Seattle, WA 98195, USA
College of Marine Science, University of South Florida, 140 7th Avenue South, St. Petersburg, FL 33701, USA
Kristen N. Buck
College of Marine Science, University of South Florida, 140 7th Avenue South, St. Petersburg, FL 33701, USA
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 2651 SW Orchard Ave., Corvallis, OR 97331, USA
Alessandro Tagliabue
Department of Earth, Ocean, and Ecological Sciences, University of Liverpool, 4 Brownlow Street, Liverpool l69 3GP, UK
Maeve C. Lohan
Department of Ocean and Earth Sciences, National Oceanography Centre, University of Southampton, European Way, Southampton SO14 3ZH, UK
Joseph A. Resing
Joint Institute for the Study of Atmosphere and Ocean, University of Washington, 3737 Brooklyn Avenue NE, Seattle, WA 98195, USA
Cooperative Institute for Climate, Ocean, and Ecosystem Studies, University of Washington, 3737 Brooklyn Avenue NE, Seattle, WA 98195, USA
School of Oceanography, University of Washington, 1501 NE Boat Street, Seattle, WA 98195, USA
Randelle M. Bundy
School of Oceanography, University of Washington, 1501 NE Boat Street, Seattle, WA 98195, USA
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Co-editor-in-chief
In their study, Hoffmann and co-workers provide new exciting data on the role of organic ligands in supporting elevated dissolved iron in hydrothermal vent plumes. The authors were able to detect siderophores (including amphiphilic types) in hydrothermal plumes at different sites along a 1,700 km section of the Mid-Atlantic Ridge, pointing to microbial utilization of siderophores to access particulate hydrothermal iron.
In their study, Hoffmann and co-workers provide new exciting data on the role of organic ligands...
Short summary
Hydrothermally derived iron can be transported kilometers away from deep-sea vents, representing a significant flux of vital micronutrients to the ocean. However, the mechanisms that support the stabilization of dissolved iron remain elusive. Using electrochemical, spectrometry, and genomic methods, we demonstrated that strong ligands exert an important control on iron in plumes, and high-affinity iron-binding siderophores were identified in several hydrothermal plume samples for the first time.
Hydrothermally derived iron can be transported kilometers away from deep-sea vents, representing...
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