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Organic ligands control the concentrations of dissolved iron in Antarctic sea ice

Citation

Lannuzel, D and Grotti, M and Abelmoschi, ML and Van Der Merwe, P, Organic ligands control the concentrations of dissolved iron in Antarctic sea ice, Goldschmidt2015 Abstracts, 16-21 August, Prague, Czech Republic, pp. 1766. (2015) [Conference Extract]

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Abstract

The organic complexation of iron (Fe) was assessed in 5 snow, 34 sea ice, 12 brine and 24 under-ice seawater samples collected during a time series in the East Antarctic sector in austral summer 2009. Similar to seawater, over 99% of Fe was bound to organic ligands in snow, sea ice and brines throughout the study. Dissolved organic ligand and Fe concentrations were higher in the brines and sea ice than in snow and seawater samples. In sea ice, [DFe] ranged from 2.1 to 81.0 nM and organic Fe complexing ligands ([Lt]) ranged from 4.5 to 72.1 nM, with complex stability logKFeL = 21.0-23.0. Estimated concentrations of inorganic Fe ([Fe’]) in sea ice ranged from 0.1 to 98.2 pM. In brines, [DFe] ranged from 0.3 to 34.6 nM and [Lt] ranged from 5.9 to 41.4 nM, with complex stability logKFeL=21.0-22.0. Estimated concentrations of inorganic Fe (Fe’) in brines ranged from 0.7 to 7.2 pM. Organic ligands were nearly saturated with Fe in both sea ice and brines, with positive linear relationships observed between [DFe] and [Lt]: [Lt] = 0.90 [DFe] + 4.24 (R2 = 0.93, n = 34) in sea ice and [Lt] = 1.08[DFe] + 4.86 (R2 = 0.98, n = 12) in brines. Our results therefore suggest that the organic ligands produced by sea ice algae and bacteria keep Fe in the dissolved phase therefore enhancing its availability for the sea ice algal community. When DFe concentrations become higher than the ligand concentrations, non-organically bound Fe is transferred into the particulate phase by scavenging, biological uptake or precipitation processes. As sea ice starts to melt, DFe will be released into seawater together with organic ligands, potentially increasing the residence time of Fe in Antarctic surface waters and its bio-availability for the phytoplankton community.

Item Details

Item Type:Conference Extract
Keywords:iron, sea ice, Southern Ocean
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Chemical Oceanography
Objective Division:Environment
Objective Group:Other Environment
Objective Field:Environment not elsewhere classified
Author:Lannuzel, D (Dr Delphine Lannuzel)
Author:Van Der Merwe, P (Mr Pier Van Der Merwe)
ID Code:104062
Year Published:2015
Funding Support:Australian Research Council (DE120100030)
Deposited By:IMAS Research and Education Centre
Deposited On:2015-11-02
Last Modified:2015-11-02
Downloads:0

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