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

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 fraction...

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Detalles Bibliográficos
Autores principales: van de Velde, Sebastiaan J., Dale, Andrew W., Arndt, Sandra
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society 2023
Materias:
Earth and Environmental Science
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9874279/
https://www.ncbi.nlm.nih.gov/pubmed/36704258
http://dx.doi.org/10.1098/rsos.220010

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9874279/
https://www.ncbi.nlm.nih.gov/pubmed/36704258
http://dx.doi.org/10.1098/rsos.220010

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