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Dissolved iron (dFe) availability limits the uptake of atmospheric CO2 by the Southern Ocean (SO) biological pump. Hence, any change in bioavailable dFe in this region can directly influence climate. On the basis of Fe uptake experiments with Phaeocystis antarctica, we show that the range of dFe bioavailability in natural samples is wider (
Athanasios Nenes, Kalliopi Violaki, Christos Panagiotopoulos
Berend Smit, Wendy Lee Queen, Christopher Patrick Ireland, Andres Adolfo Ortega Guerrero, Jordi Espin Marti, Fatma Pelin Uran, Nency Patricio Domingues, Miriam Jasmin Pougin