Articles | Volume 17, issue 13
https://doi.org/10.5194/bg-17-3685-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-3685-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The control of hydrogen sulfide on benthic iron and cadmium fluxes in the oxygen minimum zone off Peru
Anna Plass
CORRESPONDING AUTHOR
GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstraße
1–3, 24148 Kiel, Germany
Christian Schlosser
GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstraße
1–3, 24148 Kiel, Germany
Stefan Sommer
GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstraße
1–3, 24148 Kiel, Germany
Andrew W. Dale
GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstraße
1–3, 24148 Kiel, Germany
Eric P. Achterberg
GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstraße
1–3, 24148 Kiel, Germany
Florian Scholz
CORRESPONDING AUTHOR
GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstraße
1–3, 24148 Kiel, Germany
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Latest update: 23 Nov 2024
Short summary
We compare the cycling of Fe and Cd in sulfidic sediments of the Peruvian oxygen minimum zone. Due to the contrasting solubility of their sulfide minerals, the sedimentary Fe release and Cd burial fluxes covary with spatial and temporal distributions of H2S. Depending on the solubility of their sulfide minerals, sedimentary trace metal fluxes will respond differently to ocean deoxygenation/expansion of H2S concentrations, which may change trace metal stoichiometry of upwelling water masses.
We compare the cycling of Fe and Cd in sulfidic sediments of the Peruvian oxygen minimum zone....
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