Bioturbation and the δ 56 Fe signature of dissolved iron fluxes from marine sediments.

Autor: van de Velde SJ; Department of Geoscience, Environment & Society, Université Libre de Bruxelles, Av. F. Roosevelt 50, CP160/02, 1050 Brussels, Belgium.; Operational Directorate Natural Environment, Royal Belgian Institute of Natural Sciences, Rue Vautier 29, Brussels, Belgium., Dale AW; GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstr. 1-3, D-24148 Kiel, Germany., Arndt S; Department of Geoscience, Environment & Society, Université Libre de Bruxelles, Av. F. Roosevelt 50, CP160/02, 1050 Brussels, Belgium.
Jazyk: angličtina
Zdroj: Royal Society open science [R Soc Open Sci] 2023 Jan 25; Vol. 10 (1), pp. 220010. Date of Electronic Publication: 2023 Jan 25 (Print Publication: 2023).
DOI: 10.1098/rsos.220010
Abstrakt: We developed a reaction-transport model capable of tracing iron isotopes in marine sediments to quantify the influence of bioturbation on the isotopic signature of the benthic dissolved (DFe) flux. By fitting the model to published data from marine sediments, we calibrated effective overall fractionation factors for iron reduction (-1.3‰), oxidation (+0.4‰), iron-sulfide precipitation (+0.5‰) and dissolution (-0.5‰) and pyrite precipitation (-0.7‰) that agree with literature values. Results show that for bottom-water oxygen concentrations greater than 50 µM, higher bioturbation increased the benthic DFe flux and its δ 56 Fe signature. By contrast, for oxygen concentrations less than 50 µM, higher bioturbation decreased the benthic DFe flux and its δ 56 Fe signature. The expressed overall fractionation of the benthic DFe flux relative to the δ 56 Fe of the iron oxides entering the sediment ranges from -1.67‰ to 0.0‰. On a global scale, the presence of bioturbation increases sedimentary DFe release from approximately 70 G mol DFe yr -1 to approximately 160 G mol DFe yr -1 and decreases the δ 56 Fe signature of the DFe flux.
(© 2023 The Authors.)
Databáze: MEDLINE
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