2022
DOI: 10.3389/fmars.2022.837363
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Ocean Acidification Effect on the Iron-Gallic Acid Redox Interaction in Seawater

Abstract: 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… Show more

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Cited by 13 publications
(8 citation statements)
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“…In order to reveal whether trace •OH was produced that cannot be detected by ESR, coumarin was used as the probe to detect •OH, but the hydroxylated product (7-hydroxy coumarin) was not detected (Figure S6), indicating that negligible •OH was produced during the Fe-PC reactions even in well-oxygenated conditions. In general, ROS can be generated through the oxygenation of Fe­(II), but the oxygenation of Fe­(II) in the acidic condition is negligible; , in addition, the formation of Fe-PC complexes can protect Fe­(II) from oxidation. This is likely the main reason why ROS was not detected in this study.…”
Section: Resultsmentioning
confidence: 78%
“…In order to reveal whether trace •OH was produced that cannot be detected by ESR, coumarin was used as the probe to detect •OH, but the hydroxylated product (7-hydroxy coumarin) was not detected (Figure S6), indicating that negligible •OH was produced during the Fe-PC reactions even in well-oxygenated conditions. In general, ROS can be generated through the oxygenation of Fe­(II), but the oxygenation of Fe­(II) in the acidic condition is negligible; , in addition, the formation of Fe-PC complexes can protect Fe­(II) from oxidation. This is likely the main reason why ROS was not detected in this study.…”
Section: Resultsmentioning
confidence: 78%
“…The presence of strong Cu-binding ligands in surface seawaters stabilizes the excess of dissolved copper 21 . Carbohydrates and phenolic compounds can influence metal ion chemistry and bioavailability 2 , 22 . Catechin, sinapic acid and gallic acid were found to increase the persistence of dissolved Fe, regenerating Fe(II) in seawater from 0.05 to 11.92% 23 .…”
Section: Introductionmentioning
confidence: 99%
“…Organic matter exuded by marine microorganisms can form Fe(III) complexes that modify Fe(II) oxidation rates and promote the reduction of Fe(III) to Fe(II) in seawater. Under acidifying conditions, some research work has shown that the residence time of the reduced form of essential trace metals increases as their oxidation rate decreases (Pérez-Almeida et al, 2022;Santana-Casiano et al, 2014).…”
Section: Introductionmentioning
confidence: 99%