Chasing iron bioavailability in the Southern Ocean: Insights from Phaeocystis antarctica and iron speciation

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 bio...

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Bibliographic Details
Main Authors: Fourquez, Marion, Janssen, David J., Conway, Tim M., Cabanes, Damien, Ellwood, Michael J., Sieber, Matthias, Trimborn, Scarlett, Hassler, Christel
Format: Article in Journal/Newspaper
Language:English
Published: AAAS 2023
Subjects:
Southern Ocean
Antarc*
Antarctica
Online Access:https://hdl.handle.net/20.500.11850/621914
https://doi.org/10.3929/ethz-b-000621914
Description
Summary: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 (<1 to ~200% compared to free inorganic Fe') than previously thought, with higher bioavailability found near glacial sources. The degree of bioavailability varied regardless of in situ dFe concentration and depth, challenging the consensus that sole dFe concentrations can be used to predict Fe uptake in modeling studies. Further, our data suggest a disproportionately major role of biologically mediated ligands and encourage revisiting the role of humic substances in influencing marine Fe biogeochemical cycling in the SO. Last, we describe a linkage between in situ dFe bioavailability and isotopic signatures that, we anticipate, will stimulate future research. ISSN:2375-2548

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