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Fluxes and distribution of dissolved iron in the eastern (sub-) tropical North Atlantic Ocean
Rijkenberg, M.J.A.; Steigenberger, S.; Powell, C.F.; van Haren, H.; Patey, M.D.; Baker, A.R.; Achterberg, E.P. (2012). Fluxes and distribution of dissolved iron in the eastern (sub-) tropical North Atlantic Ocean. Global Biogeochem. Cycles 26.
In: Global Biogeochemical Cycles. American Geophysical Union: Washington, DC. ISSN 0886-6236, more
Peer reviewed article  

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  • Rijkenberg, M.J.A., more
  • Steigenberger, S.
  • Powell, C.F.
  • van Haren, H., more
  • Patey, M.D.
  • Baker, A.R.
  • Achterberg, E.P.

    Aeolian dust transport from the Saharan/Sahel desert regions is considered the dominant external input of iron (Fe) to the surface waters of the eastern (sub-) tropical North Atlantic Ocean. To test this hypothesis, we investigated the sources of dissolved Fe (DFe) and quantified DFe fluxes to the surface ocean in this region. In winter 2008, surface water DFe concentrations varied between <0.1 nM and 0.37 nM, with an average of 0.13 +/- 0.07 nM DFe (n = 194). A strong correlation between mixed layer averaged concentrations of dissolved aluminum (DAl), a proxy for dust input, and DFe indicated dust as a source of DFe to the surface ocean. The importance of Aeolian nutrient input was further confirmed by an increase of 0.1 nM DFe and 0.05 mu M phosphate during a repeat transect before and after a dust event. An exponential decrease of DFe with increasing distance from the African continent, suggested that continental shelf waters were a source of DFe to the northern part of our study area. Relatively high Fe: C ratios of up to 3 x 10(-5) (C derived from apparent oxygen utilization (AOU)) indicated an external source of Fe to these African continental shelf waters. Below the wind mixed layer along 12 degrees N, enhanced DFe concentrations (>1.5 nM) correlated positively with apparent oxygen utilization (AOU) and showed the importance of organic matter remineralization as an DFe source. As a consequence, vertical diffusive mixing formed an important Fe flux to the surface ocean in this region, even surpassing that of a major dust event.

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