Ocean Acidification Effect on the Iron-Gallic Acid Redox Interaction in Seawater
Ocean acidification impacts the iron (Fe) biogeochemistry both by its redox and its complexation reactions. This has a direct effect on the ecosystems due to Fe being an essential micronutrient. Polyphenols exudated by marine microorganisms can complex Fe(III), modifying the Fe(II) oxidation rates a...
Published in: | Frontiers in Marine Science |
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Online Access: | http://hdl.handle.net/10553/114071 https://doi.org/10.3389/fmars.2022.837363 |
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ftunivlaspalmas:oai:accedacris.ulpgc.es:10553/114071 2023-05-15T17:50:21+02:00 Ocean Acidification Effect on the Iron-Gallic Acid Redox Interaction in Seawater Pérez Almeida, María Norma González González, Aridane Santana Casiano, Juana Magdalena González Dávila, Melchor #NODATA# BU-BAS 2022 http://hdl.handle.net/10553/114071 https://doi.org/10.3389/fmars.2022.837363 eng eng Our common future ocean in the Earth system ¿ quantifying coupled cycles of carbon, oxygen, and nutrients for determining and achieving safe operating spaces with respect to tipping points Efecto de la Acidificacion Oceanica, la Temperatura y El Contenido de Materia Organica en la Persistencia de Fe(Ii) en El Oceano Atlantico Planificación Conjunta, Seguimiento y Observación, Mejora del Conocimiento y Sensibilización Ante Riesgos y Amezas del Cambio Climatico en la Macaronesia Frontiers in Marine Science 2296-7745 http://hdl.handle.net/10553/114071 doi:10.3389/fmars.2022.837363 2-s2.0-85125187222 WOS:000761553200001 Sí Frontiers in Marine Science [ISSN 2296-7745], v. 9, 837363, (Febrero 2022) 230220 Química microbiológica 2510 Oceanografía Gallic acid Iron Complexation Redox process Seawater Ocean acidification info:eu-repo/semantics/Article article 2022 ftunivlaspalmas https://doi.org/10.3389/fmars.2022.837363 2022-11-23T00:14:33Z Ocean acidification impacts the iron (Fe) biogeochemistry both by its redox and its complexation reactions. This has a direct effect on the ecosystems due to Fe being an essential micronutrient. Polyphenols exudated by marine microorganisms can complex Fe(III), modifying the Fe(II) oxidation rates as well as promoting the reduction of Fe(III) to Fe(II) in seawater. The effect of the polyphenol gallic acid (GA; 3,4,5-trihydroxy benzoic acid) on the oxidation and reduction of Fe was studied. The Fe(II) oxidation rate constant decreased, increasing the permanence of Fe(II) in solutions at nM levels. At pH = 8.0 and in the absence of gallic acid, 69.3% of the initial Fe(II) was oxidized after 10 min. With 100 nM of gallic acid (ratio 4:1 GA:Fe), and after 30 min, 37.5% of the initial Fe(II) was oxidized. Fe(III) is reduced to Fe(II) by gallic acid in a process that depends on the pH and composition of solution, being faster as pH decreases. At pH > 7.00, the Fe(III) reduction rate constant in seawater was lower than in NaCl solutions, being the difference at pH 8.0 of 1.577 × 10–5 s–1. Moreover, the change of the Fe(III) rate constant with pH, within the studied range, was higher in seawater (slope = 0.91) than in NaCl solutions (slope = 0.46). The Fe(III) reduction rate constant increased with increasing ligand concentration, being the effect higher at pH 7.0 [k′ = 1.078 × 10–4 s–1; (GA) = 250 nM] compared with that at pH 8.0 [k′ = 3.407 × 10–5 s–1; (GA) = 250 nM]. Accordingly, gallic acid reduces Fe(III) to Fe(II) in seawater, making possible the presence of Fe(II) for longer periods and favoring its bioavailability. 1,558 4,912 Q1 Q1 SCIE 10,3 Article in Journal/Newspaper Ocean acidification Universidad de Las Palmas de Gran Canaria: Acceda Frontiers in Marine Science 9 |
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Open Polar |
collection |
Universidad de Las Palmas de Gran Canaria: Acceda |
op_collection_id |
ftunivlaspalmas |
language |
English |
topic |
230220 Química microbiológica 2510 Oceanografía Gallic acid Iron Complexation Redox process Seawater Ocean acidification |
spellingShingle |
230220 Química microbiológica 2510 Oceanografía Gallic acid Iron Complexation Redox process Seawater Ocean acidification Pérez Almeida, María Norma González González, Aridane Santana Casiano, Juana Magdalena González Dávila, Melchor Ocean Acidification Effect on the Iron-Gallic Acid Redox Interaction in Seawater |
topic_facet |
230220 Química microbiológica 2510 Oceanografía Gallic acid Iron Complexation Redox process Seawater Ocean acidification |
description |
Ocean acidification impacts the iron (Fe) biogeochemistry both by its redox and its complexation reactions. This has a direct effect on the ecosystems due to Fe being an essential micronutrient. Polyphenols exudated by marine microorganisms can complex Fe(III), modifying the Fe(II) oxidation rates as well as promoting the reduction of Fe(III) to Fe(II) in seawater. The effect of the polyphenol gallic acid (GA; 3,4,5-trihydroxy benzoic acid) on the oxidation and reduction of Fe was studied. The Fe(II) oxidation rate constant decreased, increasing the permanence of Fe(II) in solutions at nM levels. At pH = 8.0 and in the absence of gallic acid, 69.3% of the initial Fe(II) was oxidized after 10 min. With 100 nM of gallic acid (ratio 4:1 GA:Fe), and after 30 min, 37.5% of the initial Fe(II) was oxidized. Fe(III) is reduced to Fe(II) by gallic acid in a process that depends on the pH and composition of solution, being faster as pH decreases. At pH > 7.00, the Fe(III) reduction rate constant in seawater was lower than in NaCl solutions, being the difference at pH 8.0 of 1.577 × 10–5 s–1. Moreover, the change of the Fe(III) rate constant with pH, within the studied range, was higher in seawater (slope = 0.91) than in NaCl solutions (slope = 0.46). The Fe(III) reduction rate constant increased with increasing ligand concentration, being the effect higher at pH 7.0 [k′ = 1.078 × 10–4 s–1; (GA) = 250 nM] compared with that at pH 8.0 [k′ = 3.407 × 10–5 s–1; (GA) = 250 nM]. Accordingly, gallic acid reduces Fe(III) to Fe(II) in seawater, making possible the presence of Fe(II) for longer periods and favoring its bioavailability. 1,558 4,912 Q1 Q1 SCIE 10,3 |
author2 |
#NODATA# BU-BAS |
format |
Article in Journal/Newspaper |
author |
Pérez Almeida, María Norma González González, Aridane Santana Casiano, Juana Magdalena González Dávila, Melchor |
author_facet |
Pérez Almeida, María Norma González González, Aridane Santana Casiano, Juana Magdalena González Dávila, Melchor |
author_sort |
Pérez Almeida, María Norma |
title |
Ocean Acidification Effect on the Iron-Gallic Acid Redox Interaction in Seawater |
title_short |
Ocean Acidification Effect on the Iron-Gallic Acid Redox Interaction in Seawater |
title_full |
Ocean Acidification Effect on the Iron-Gallic Acid Redox Interaction in Seawater |
title_fullStr |
Ocean Acidification Effect on the Iron-Gallic Acid Redox Interaction in Seawater |
title_full_unstemmed |
Ocean Acidification Effect on the Iron-Gallic Acid Redox Interaction in Seawater |
title_sort |
ocean acidification effect on the iron-gallic acid redox interaction in seawater |
publishDate |
2022 |
url |
http://hdl.handle.net/10553/114071 https://doi.org/10.3389/fmars.2022.837363 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Frontiers in Marine Science [ISSN 2296-7745], v. 9, 837363, (Febrero 2022) |
op_relation |
Our common future ocean in the Earth system ¿ quantifying coupled cycles of carbon, oxygen, and nutrients for determining and achieving safe operating spaces with respect to tipping points Efecto de la Acidificacion Oceanica, la Temperatura y El Contenido de Materia Organica en la Persistencia de Fe(Ii) en El Oceano Atlantico Planificación Conjunta, Seguimiento y Observación, Mejora del Conocimiento y Sensibilización Ante Riesgos y Amezas del Cambio Climatico en la Macaronesia Frontiers in Marine Science 2296-7745 http://hdl.handle.net/10553/114071 doi:10.3389/fmars.2022.837363 2-s2.0-85125187222 WOS:000761553200001 Sí |
op_doi |
https://doi.org/10.3389/fmars.2022.837363 |
container_title |
Frontiers in Marine Science |
container_volume |
9 |
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1766157064354136064 |