Dissolved iron in the vicinity of the Crozet Islands, Southern Ocean

• Published in: Deep Sea Research Part II: Topical Studies in Oceanography
• Other Authors: Planquette, H. (author), Statham, P. (author), Fones, G. (author), Charette, M. (author), Moore, C. (author), Salter, I. (author), Nedelec, F. (author), Taylor, S. (author), French, M. (author), Baker, A. (author), Mahowald, Natalie (author), Jickells, T. (author)
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier Ltd. 2007
• Subjects: Dissolved iron; Crozet Islands; Southern Ocean; HNLC; Antarctic; Kerguelen; Antarc*
• Online Access: http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-011-841; https://doi.org/10.1016/j.dsr2.2007.06.019

The annual phytoplankton bloom occurring north of the Crozet Plateau provides a rare opportunity to examine the hypothesis that natural iron fertilization can alleviate high-nutrient low-chlorophyll (HNLC) conditions normally associated with the Southern Ocean. Therefore, during CROZet natural iron bloom and EXport experiment (CROZEX), a large multidisciplinary study performed between November 2004 and January 2005, measurements of total dissolved iron (DFe⩽0.2 μm) were made on seawater from around the islands and atmospheric iron deposition estimated from rain and aerosol samples. DFe concentrations were determined by flow injection analysis with N,N-dimethyl-p-phenylenediamine dihydrochloride (DPD) catalytic spectrophotometric detection. DFe concentrations varied between 0.086 and 2.48 nM, with low values in surface waters. Enrichment of dissolved iron (>1 nM) at close proximity to the islands suggests that the plateau and the associated sediments are a source of iron. Waters farther north also appear to be affected by this input of coastal and shelf origin, although dissolved iron concentrations decrease as a function of distance to the north of the plateau with a gradient of ∼0.07 nM km−1 at the time of sampling. Using lateral and vertical diffusion coefficients derived from Ra isotope profiles and also estimates of atmospheric inputs, it was then possible to estimate a DFe concentration of ∼0.55 nM to the north of the islands prior to the bloom event, which is sufficient to initiate the bloom, the lateral island source being the largest component. A similar situation is observed for other Sub-Antarctic Islands such as Kerguelen, South Georgia, that supply dissolved iron to their surrounding waters, thus enhancing chlorophyll concentrations.