CORDIS Project
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This project develops innovative methods to analyze phosphorus dynamics in low-oxygen marine environments, linking it to carbon cycling. By employing advanced geochemical techniques, it aims to enhance understanding of phosphorus burial processes and their implications for ocean health and historical climate change.
Phosphorus (P) is a key and often limiting nutrient for phytoplankton in the ocean. A strong positive feedback exists between marine P availability, primary production and ocean anoxia: increased production leads to ocean anoxia, which, in turn, decreases the burial efficiency of P in sediments and therefore increases the availability of P and production in the ocean.
This feedback likely plays an important role in the present-day expansion of low-oxygen waters (“dead zones”) in coastal systems…
UNIVERSITEIT UTRECHT
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