Seasonal iron depletion in temperate shelf seas

• Published in: Geophysical Research Letters
• Main Authors: Birchill, AJ, Milne, A, S. Woodward, EM, Harris, C, Annett, A, Rusiecka, D, Achterberg, EP, Gledhill, M, Ussher, SJ, Worsfold, PJ, Geibert, W, Lohan, MC
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Geophysical Union (AGU) 2017
• Subjects: 37 Earth Sciences; 3708 Oceanography; 3701 Atmospheric Sciences; Ross Sea
• Online Access: http://hdl.handle.net/10026.1/9969; https://doi.org/10.1002/2017GL073881

<jats:title>Abstract</jats:title><jats:p>Our study followed the seasonal cycling of soluble (SFe), colloidal (CFe), dissolved (DFe), total dissolvable (TDFe), labile particulate (LPFe), and total particulate (TPFe) iron in the Celtic Sea (NE Atlantic Ocean). Preferential uptake of SFe occurred during the spring bloom, preceding the removal of CFe. Uptake and export of Fe during the spring bloom, coupled with a reduction in vertical exchange, led to Fe deplete surface waters (<0.2 nM DFe; 0.11 nM LPFe, 0.45 nM TDFe, and 1.84 nM TPFe) during summer stratification. Below the seasonal thermocline, DFe concentrations increased from spring to autumn, mirroring NO<jats:sub>3</jats:sub><jats:sup>−</jats:sup> and consistent with supply from remineralized sinking organic material, and cycled independently of particulate Fe over seasonal timescales. These results demonstrate that summer Fe availability is comparable to the seasonally Fe limited Ross Sea shelf and therefore is likely low enough to affect phytoplankton growth and species composition.</jats:p>