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Journal of Geophysical Research: Oceans

Dissolved trace metals (Ni, Zn, Co, Cd, Pb, Al, and Mn) around the Crozet Islands, Southern Ocean

Authors

  • Maxi Castrillejo,

    Corresponding author
    1. National Oceanography Centre of Southampton, University of Southampton, Southampton, UK
    2. Institut de Ciència i Tecnologia Ambientals, Universitat Autònoma de Barcelona, Bellaterra, Spain
    • Corresponding author: M. Castrillejo, National Oceanography Centre of Southampton, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK. (mcastrillejo.sci@gmail.com)

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  • Peter J. Statham,

    1. National Oceanography Centre of Southampton, University of Southampton, Southampton, UK
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  • Gary R. Fones,

    1. School of Earth and Environment Sciences, University of Portsmouth, Portsmouth, UK
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  • Hélène Planquette,

    1. Laboratoire des Sciences de l'Environnement Marin, Institut Universitaire Européen de la Mer, France
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  • Farah Idrus,

    1. National Oceanography Centre of Southampton, University of Southampton, Southampton, UK
    2. Faculty of Resources Science and Technology Department of Aquatic Science, University Malaysia Sarawak, Sarawak, Malaysia
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  • Keiron Roberts

    1. National Oceanography Centre of Southampton, University of Southampton, Southampton, UK
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Abstract

[1] A phytoplankton bloom shown to be naturally iron (Fe) induced occurs north of the Crozet Islands (Southern Ocean) every year, providing an ideal opportunity to study dissolved trace metal distributions within an island system located in a high nutrient low chlorophyll (HNLC) region. We present water column profiles of dissolved nickel (Ni), zinc (Zn), cobalt (Co), cadmium (Cd), lead (Pb), aluminium (Al), and manganese (Mn) obtained as part of the NERC CROZEX program during austral summer (2004–2005). Two stations (M3 and M1) were sampled downstream (north) of Crozet in the bloom area and near the islands, along with a control station (M2) in the HNLC zone upstream (south) of the islands. The general range found was for Ni, 4.64–6.31 nM; Zn, 1.59–7.75 nM; Co, 24–49 pM; Cd, 135–673 pM; Pb, 6–22 pM; Al, 0.13–2.15 nM; and Mn, 0.07–0.64 nM. Vertical profiles indicate little island influence to the south with values in the range of other trace metal deprived regions of the Southern Ocean. Significant removal of Ni and Cd was observed in the bloom and Zn was moderately correlated with reactive silicate (Si) indicating diatom control over the internal cycling of this metal. Higher concentrations of Zn and Cd were observed near the islands. Pb, Al, and Mn distributions also suggest small but significant atmospheric dust supply particularly in the northern region.

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