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Nutrient distribution in East Antarctic summer sea ice: a potential iron contribution from glacial basal melt
Duprat, L.; Corkill, M.; Genovese, C.; Townsend, A.T.; Moreau, S.; Meiners, K.M.; Lannuzel, D. (2020). Nutrient distribution in East Antarctic summer sea ice: a potential iron contribution from glacial basal melt. JGR: Oceans 125(12): e2020JC016130. https://dx.doi.org/10.1029/2020JC016130
In: Journal of Geophysical Research-Oceans. AMER GEOPHYSICAL UNION: Washington. ISSN 2169-9275; e-ISSN 2169-9291, meer
Peer reviewed article  
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Trefwoord
    Marien/Kust
Author keywords
    East Antarctica; iron; platelet ice; sea ice; summer
Auteurs  Top 
  • Duprat, L.
  • Corkill, M.
  • Genovese, C.
  • Townsend, A.T.
  • Moreau, S.
  • Meiners, K.M.
  • Lannuzel, D.
Abstract
    Antarctic sea ice can incorporate high levels of iron (Fe) during its formation and has been suggested as an important source of this essential micronutrient to Southern Ocean surface waters during the melt season. Over the last decade, a limited number of studies have quantified the Fe pool in Antarctic sea ice, with a focus on late winter and spring. Here we study the distribution of operationally defined dissolved and particulate Fe from nine sites sampled between Wilkes Land and King George V Land during austral summer 2016/2017. Results point toward a net heterotrophic sea-ice community, consistent with the observed nitrate limitation (<1 μM). We postulate that the recycling of the high particulate Fe pool in summer sea ice supplies sufficient (∼3 nM) levels of dissolved Fe to sustain ice algal growth. The remineralization of particulate Fe is likely favored by high concentrations of exopolysaccharides (113–16,290 μg xeq L−1) which can serve as a hotspot for bacterial activity. Finally, results indicate a potential relationship between glacial meltwater discharged from the Moscow University Ice Shelf and the occurrence of Fe-rich (∼4.3 μM) platelet ice in its vicinity. As climate change is expected to result in enhanced Fe-rich glacial discharge and changes in summer sea-ice extent and quality, the processes influencing Fe distribution in sea ice that persists into summer need to be better constrained.
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