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Atmospheric iron deposition and sea-surface dissolved iron concentrations in the eastern Atlantic Ocean

Sarthou, G., Baker, A.R., Blain, S., Achterberg, E.P., Boye, M., Bowie, A.R., Croot, P., Laan, P., De Baar, H.J.W., Jickells, T.D. and Worsfold, P.J. (2003) Atmospheric iron deposition and sea-surface dissolved iron concentrations in the eastern Atlantic Ocean Deep Sea Research Part I: Oceanographic Research Papers, 50, (10-11), pp. 1339-1352. (doi:10.1016/S0967-0637(03)00126-2).

Record type: Article


Atmospheric iron and underway sea-surface dissolved (<0.2 m) iron (DFe) concentrations were investigated along a north–south transect in the eastern Atlantic Ocean (27°N/16°W–19°S/5°E). Fe concentrations in aerosols and dry deposition fluxes of soluble Fe were at least two orders of magnitude higher in the Saharan dust plume than at the equator or at the extreme south of the transect. A weaker source of atmospheric Fe was also observed in the South Atlantic, possibly originating in southern Africa via the north-easterly outflow of the Angolan plume. Estimations of total atmospheric deposition fluxes (dry plus wet) of soluble Fe suggested that wet deposition dominated in the intertropical convergence zone, due to the very high amount of precipitation and to the fact that a substantial part of Fe was delivered in dissolved form. On the other hand, dry deposition dominated in the other regions of the transect (73–97%), where rainfall rates were much lower. Underway sea-surface DFe concentrations ranged 0.02–1.1 nM. Such low values (0.02 nM) are reported for the first time in the Atlantic Ocean and may be (co)-limiting for primary production. A significant correlation (Spearman's RHO=0.862, p<0.01) was observed between mean DFe concentrations and total atmospheric deposition fluxes, confirming the importance of atmospheric deposition on the iron cycle in the Atlantic. Residence time of DFe in the surface waters relative to atmospheric inputs were estimated in the northern part of our study area (17±8 to 28±16 d). These values confirmed the rapid removal of Fe from the surface waters, possibly by colloidal aggregation.

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Published date: 2003
Keywords: Dissolved iron, Aerosol iron, Sea surface, Iron supply, Atmospheric (wet and dry) deposition, Residence time


Local EPrints ID: 12535
ISSN: 0967-0637
PURE UUID: 8b4f8748-b155-4a3d-b562-59bfb82ad7f7

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Date deposited: 26 Nov 2004
Last modified: 17 Jul 2017 17:02

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Author: G. Sarthou
Author: A.R. Baker
Author: S. Blain
Author: E.P. Achterberg
Author: M. Boye
Author: A.R. Bowie
Author: P. Croot
Author: P. Laan
Author: H.J.W. De Baar
Author: T.D. Jickells
Author: P.J. Worsfold

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