Project Details
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Iron cycling in continental margin sediments and the nutrient and oxygen balance of the ocean

Subject Area Oceanography
Mineralogy, Petrology and Geochemistry
Term from 2016 to 2025
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 283168947
 
Final Report Year 2025

Final Report Abstract

The ICONOX project, conducted between 2016 and 2025, focused on unraveling the complex biogeochemical feedbacks between iron (Fe), nitrogen, and trace metal cycling in the water column and sediments of oxygen minimum zones. Through participation in multiple research expeditions, the project team investigated the environmental conditions under which sedimentary Fe is released into the water column, where it may support biological productivity in the surface ocean. In addition, paleo-records were analyzed to identify potential feedback mechanisms linking sedimentary Fe release or retention to carbon and nutrient cycling and oxygen consumption in the ocean's interior. These empirical findings informed the development of numerical models designed to explore how coupled cycles of Fe, nutrients, and carbon may respond to ongoing, human-driven ocean deoxygenation. The project demonstrated that the release and redistribution of Fe from sediments is a widespread phenomenon in oxygen-deficient marine environments. However, only a limited fraction of the mobilized Fe ultimately reaches the surface ocean to support primary productivity. Instead, much of it is retained or transformed within the water column or sediments. One of the key insights from the project was the identification of chemical weathering on land as a primary control on the supply of reactive Fe to marine sediments. Additionally, the transformation of silicate minerals, including their alteration, partial dissolution, and neoformation, was found to significantly influence the mobility of sedimentary Fe. Modeling results showed that sedimentary Fe release responds dynamically to decreasing oxygen concentrations in bottom waters. These findings imply that continued ocean deoxygenation could stimulate further Fe release from sediments, potentially alleviating Fe limitation in certain regions and amplifying oxygen demand in subsurface waters through enhanced biological activity. The ICONOX project thus provides important insights into how elemental cycles in the ocean are interlinked and how they may evolve under future climate conditions.

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