Contribution of electroactive humic substances to the iron-binding ligands released during microbial remineralisation of sinking particles
|Author(s)||Whitby Hannah1, 2, Bressac Matthieu3, 4, Sarthou Geraldine2, Ellwood Michael J.5, Guieu Cécile4, 6, Boyd Philip W.3, 7|
|Affiliation(s)||1 : University of Liverpool; Liverpool ,UK
2 : CNRS, Université de Brest, IRD, Ifremer, UMR 6539 LEMAR, IUEM; Technopôle Brest Iroise, Place Nicolas Copernic; Plouzané, France
3 : Institute for Marine and Antarctic Studies, University of Tasmania; Hobart Tasmania, Australia
4 : Sorbonne Université, CNRS, Laboratoire d'Océanographie de Villefranche, LOV; Villefranche-sur-mer ,France
5 : Research School of Earth Sciences, Australian National University; Canberra, ACT ,Australia
6 : The Center for Prototype Climate Modeling; New York University in Abu Dhabi; Abu Dhabi ,UAE
7 : Antarctic Climate and Ecosystems Collaborative Research Center; University of Tasmania; Hobart Tasmania, Australia
|Source||Geophysical Research Letters (00948276) (American Geophysical Union (AGU)), 2020-04 , Vol. 47 , N. 7 , P. e2019GL086685 (11p.)|
|Keyword(s)||Iron, ligand, humic, remineralisation, particle, degradation|
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 remineralisation of sinking particles was investigated by deploying in situ particle interceptor/incubator devices at subsurface sites in the Mediterranean Sea and Subantarctic. Analyses revealed the pool of released ligands was largely dominated by electroactive humic substances (74 ± 28%). The release of ligands during remineralisation 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 modelling and for calculating carbon sequestration in seawater.