Articles | Volume 17, issue 5
https://doi.org/10.5194/bg-17-1327-2020
© Author(s) 2020. 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-17-1327-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
16 Mar 2020
Research article |
| 16 Mar 2020
| 16 Mar 2020
Fe(II) stability in coastal seawater during experiments in Patagonia, Svalbard, and Gran Canaria
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
Carolina Santana-González
Instituto de Oceanografía y Cambio Global, IOCAG, Universidad de Las
Palmas de Gran Canaria, ULPGC, Las Palmas, Spain
Julian Gallego-Urrea
Department of Marine Sciences, Kristineberg Marine Research Station, University of Gothenburg, Gothenburg, Sweden
Nicolas Sanchez
Norwegian University of Science and Technology, Trondheim, Trondheim, Norway
Eric P. Achterberg
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
Murat V. Ardelan
Norwegian University of Science and Technology, Trondheim, Trondheim, Norway
Martha Gledhill
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
Melchor González-Dávila
Instituto de Oceanografía y Cambio Global, IOCAG, Universidad de Las
Palmas de Gran Canaria, ULPGC, Las Palmas, Spain
Linn Hoffmann
Department of Chemistry, University of Otago, Dunedin, New Zealand
Øystein Leiknes
Norwegian University of Science and Technology, Trondheim, Trondheim, Norway
Juana Magdalena Santana-Casiano
Instituto de Oceanografía y Cambio Global, IOCAG, Universidad de Las
Palmas de Gran Canaria, ULPGC, Las Palmas, Spain
Tatiana M. Tsagaraki
Department of Biological Sciences, University of Bergen, Bergen, Norway
David Turner
Department of Marine Sciences, University of Gothenburg, Gothenburg, Sweden
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Cited
13 citations as recorded by crossref.
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- Novel ionic reverse mixed micelle supramolecules in dispersive liquid-liquid microextraction for the successive/individual sensitive speciation analysis of iron in natural water by UV–Vis spectrophotometry N. Meeravali et al. 10.1016/j.microc.2021.105986
- Particulate Trace Metal Sources, Cycling, and Distributions on the Southwest African Shelf A. Al‐Hashem et al. 10.1029/2022GB007453
- A mosaic of phytoplankton responses across Patagonia, the southeast Pacific and the southwest Atlantic to ash deposition and trace metal release from the Calbuco volcanic eruption in 2015 M. Vergara-Jara et al. 10.5194/os-17-561-2021
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- Atmospheric Iron and Aluminium Deposition and Sea-Surface Dissolved Iron and Aluminium Concentrations in the South China Sea off Malaysia Borneo (Sarawak Waters) F. Idrus et al. 10.33736/bjrst.4166.2021
- Dissolved and particulate iron redox speciation during the LOHAFEX fertilization experiment L. Laglera et al. 10.1016/j.marpolbul.2022.114161
- Northern High-Latitude Organic Soils As a Vital Source of River-Borne Dissolved Iron to the Ocean R. Krachler & R. Krachler 10.1021/acs.est.1c01439
- Molecular Mechanisms for Iron Uptake and Homeostasis in Marine Eukaryotic Phytoplankton R. Lampe et al. 10.1146/annurev-micro-041222-023252
- The biological uptake of dissolved iron in the changing Daya Bay, South China Sea: Effect of pH and DO B. Wang et al. 10.1016/j.marpolbul.2022.113635
- From the Ocean to the Lab—Assessing Iron Limitation in Cyanobacteria: An Interface Paper A. Hunnestad et al. 10.3390/microorganisms8121889
12 citations as recorded by crossref.
- Dissolved Fe(II) and its oxidation rates in the Kuroshio area, subarctic Pacific, and Bering Sea H. Obata et al. 10.2343/geochemj.GJ24006
- Experiment design and bacterial abundance control extracellular H<sub>2</sub>O<sub>2</sub> concentrations during four series of mesocosm experiments M. Hopwood et al. 10.5194/bg-17-1309-2020
- Biogeochemical feedbacks may amplify ongoing and future ocean deoxygenation: a case study from the Peruvian oxygen minimum zone K. Wallmann et al. 10.1007/s10533-022-00908-w
- Novel ionic reverse mixed micelle supramolecules in dispersive liquid-liquid microextraction for the successive/individual sensitive speciation analysis of iron in natural water by UV–Vis spectrophotometry N. Meeravali et al. 10.1016/j.microc.2021.105986
- Particulate Trace Metal Sources, Cycling, and Distributions on the Southwest African Shelf A. Al‐Hashem et al. 10.1029/2022GB007453
- A mosaic of phytoplankton responses across Patagonia, the southeast Pacific and the southwest Atlantic to ash deposition and trace metal release from the Calbuco volcanic eruption in 2015 M. Vergara-Jara et al. 10.5194/os-17-561-2021
- Correlation of pesticide ecotoxicity with clay mineral dispersion effect on adsorption and ozonation – An approach through impact assessment on Lemna minor A. Benghaffour et al. 10.1016/j.clay.2023.107001
- Atmospheric Iron and Aluminium Deposition and Sea-Surface Dissolved Iron and Aluminium Concentrations in the South China Sea off Malaysia Borneo (Sarawak Waters) F. Idrus et al. 10.33736/bjrst.4166.2021
- Dissolved and particulate iron redox speciation during the LOHAFEX fertilization experiment L. Laglera et al. 10.1016/j.marpolbul.2022.114161
- Northern High-Latitude Organic Soils As a Vital Source of River-Borne Dissolved Iron to the Ocean R. Krachler & R. Krachler 10.1021/acs.est.1c01439
- Molecular Mechanisms for Iron Uptake and Homeostasis in Marine Eukaryotic Phytoplankton R. Lampe et al. 10.1146/annurev-micro-041222-023252
- The biological uptake of dissolved iron in the changing Daya Bay, South China Sea: Effect of pH and DO B. Wang et al. 10.1016/j.marpolbul.2022.113635
1 citations as recorded by crossref.
Latest update: 23 Nov 2024
Short summary
Fe is an essential micronutrient. Fe(III)-organic species are thought to account for > 99 % of dissolved Fe in seawater. Here we quantified Fe(II) during experiments in Svalbard, Gran Canaria, and Patagonia. Fe(II) was always a measurable fraction of dissolved Fe up to 65 %. Furthermore, when Fe(II) was allowed to decay in the dark, it remained present longer than predicted by kinetic equations, suggesting that Fe(II) is a more important fraction of dissolved Fe in seawater than widely recognized.
Fe is an essential micronutrient. Fe(III)-organic species are thought to account for 99 % of...
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