%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Labatut, M.
%A Lacan, F.
%A Pradoux, C.
%A Chmeleff, J.
%A Radic, A.
%A Murray, J. W.
%A Poitrasson, Franck
%A Johansen, A. M.
%A Thil, F.
%T Iron sources and dissolved-particulate interactions in the seawater of the Western Equatorial Pacific, iron isotope perspectives
%D 2014
%L fdi:010062691
%G ENG
%J Global Biogeochemical Cycles
%@ 0886-6236
%K iron isotopes ; particles ; equatorial Pacific ; Papua New Guinea ; seawater ; GEOTRACES
%K PACIFIQUE OUEST ; ZONE EQUATORIALE ; PAPOUASIE NOUVELLE GUINEE
%M ISI:000344797500003
%N 10
%P 1044-1065
%R 10.1002/2014gb004928
%U https://www.documentation.ird.fr/hor/fdi:010062691
%> https://www.documentation.ird.fr/intranet/publi/2014/12/010062691.pdf
%V 28
%W Horizon (IRD)
%X This work presents iron isotope data in the western equatorial Pacific. Marine aerosols and top core margin sediments display a slightly heavy Fe isotopic composition (Fe-56) of 0.330.11 (2SD) and 0.140.07, respectively. Samples reflecting the influence of Papua New Guinea runoff (Sepik River and Rabaul volcano water) are characterized by crustal values. In seawater, Fe is mainly supplied in the particulate form and is found with a Fe-56 between -0.49 and 0.34 +/- 0.07 parts per thousand. The particulate Fe seems to be brought mainly by runoff and transported across continental shelves and slopes. Aerosols are suspected to enrich the surface Vitiaz Strait waters, while hydrothermal activity likely enriched New Ireland waters. Dissolved Fe isotopic ratios are found between -0.03 and 0.53 +/- 0.07 parts per thousand. They are almost systematically heavier than the corresponding particulate Fe, and the difference between the signature of both phases is similar for most samples with Fe-56(DFe-PFe)=+0.27 +/- 0.25 parts per thousand (2SD). This is interpreted as an equilibrium isotopic fractionation revealing exchange fluxes between both phases. The dissolved phase being heavier than the particles suggests that the exchanges result in a net nonreductive release of dissolved Fe. This process seems to be locally significantly more intense than Fe reductive dissolution documented along reducing margins. It may therefore constitute a very significant iron source to the ocean, thereby influencing the actual estimation of the iron residence time and sinks. The underlying processes could also apply to other elements.
%$ 032 ; 064