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Iron persistence in a distal hydrothermal plume supported by dissolved–particulate exchange
Fitzsimmons, J.N.; John, S.G.; Marsay, C.M.; Hoffman, C.L.; Nicholas, S.L.; Toner, B.M.; German, C.R.; Sherrell, R.M. (2017). Iron persistence in a distal hydrothermal plume supported by dissolved–particulate exchange. Nature Geoscience 10(3): 195-201. http://dx.doi.org/10.1038/ngeo2900
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908, meer
Peer reviewed article  
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Trefwoord
    Marien/Kust
Auteurs  Top 
  • Fitzsimmons, J.N.
  • John, S.G.
  • Marsay, C.M.
  • Hoffman, C.L.
  • Nicholas, S.L.
  • Toner, B.M.
  • German, C.R.
  • Sherrell, R.M.
Abstract
    The largest known hydrothermal plume moves dissolved iron halfway across the Pacific. In situ measurements show that dissolved and particulate iron transport is facilitated by reversible exchange of dissolved iron onto organic compounds.
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