Contribution of Electroactive Humic Substances to the Iron‐Binding Ligands Released During Microbial Remineralization of Sinking Particles

• Published in: Geophysical research letters 2020-04, Vol.47 (7), p.n/a
• Main Authors: Whitby, Hannah, Bressac, Matthieu, Sarthou, Géraldine, Ellwood, Michael J., Guieu, Cécile, Boyd, Philip W.
• Format: Article
• Language: English
• Subjects: Binding; Biodegradation; Biodiversity and Ecology; Biogeochemistry; Carbon sequestration; Chemical analysis; Climate change; Climate change influences; Composition; degradation; Drawdown; Earth Sciences; Environmental Sciences; Euphotic zone; Food chains; Geochemistry; humic; Humic substances; Incubators; Iron; ligand; Ligands; Low concentrations; Microbial degradation; Microorganisms; Mineral nutrients; Nutrients; Ocean models; Ocean, Atmosphere; Oceanography; Oceans; particle; Particulate flux; Regeneration; Regeneration (biological); remineralisation; Remineralization; Replenishment; Sciences of the Universe; Seawater; Sinking; Survival; Upper ocean; Water analysis; Water circulation; Water column
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1029/2019GL086685

Iron is a key micronutrient in seawater, but concentrations would be negligible without the presence of organic ligands. The processes influencing the ligand pool composition are poorly constrained, limiting our understanding of the controls on dissolved iron distributions. To address this, the release of iron and iron‐binding ligands during the microbial remineralization of sinking particles was investigated by deploying in situ particle interceptor/incubator devices at subsurface sites in the Mediterranean Sea and Subantarctic. Analyses revealed that the pool of released ligands was largely dominated by electroactive humic substances (74 ± 28%). The release of ligands during remineralization ensured that concurrently released iron remained in solution, which is crucial for iron regeneration. This study presents compelling evidence of the key role of humic ligands in the subsurface replenishment of dissolved iron and thus on the wider oceanic dissolved iron inventory, which ultimately controls the magnitude of iron resupplied to the euphotic zone. Plain Language Summary Microscopic plants and animals in seawater require nutrients to survive. One of these key nutrients is iron, dissolved in seawater at very low concentrations. The growth of around half of the microscopic life in the upper ocean is dependent on the availability of this dissolved iron. These organisms form the bottom of the food chain, and their growth is linked to marine productivity and the drawdown of carbon into the deep ocean, in turn influencing climate change. Because iron tends to not dissolve easily in seawater, it must bind with compounds known as ligands, which help keep iron dissolved. However, processes controlling the composition of this ligand pool are poorly understood. As material sinks through the water column, it is broken down by marine microbes, releasing iron and ligands. Here we have studied the release of iron, ligands, and a specific type of ligand known as humic substances, during the microbial degradation of sinking particles. By doing this, we have identified a large fraction of the released ligand pool. This furthers our understanding of the processes controlling dissolved iron concentrations and distributions in ocean waters, providing key information for biogeochemical modeling and for calculating carbon sequestration in seawater. Key Points Electroactive humic substances contribute significantly to iron‐binding ligands released during microbial decomposition o