How would ocean fertilization increase carbon dioxide uptake by phytoplankton?
Ocean fertilization is a proposed geoengineering technique that aims to enhance the natural ability of phytoplankton to absorb carbon dioxide from the atmosphere.21
The process works by introducing nutrients—specifically iron or nitrates—into surface waters where primary productivity is currently low. By stimulating these blooms, the phytoplankton photosynthesize atmospheric carbon dioxide into new organic tissues.21
The intended mechanism for long-term carbon sequestration is that, upon death, these phytoplankton sink to the ocean floor, effectively transporting the carbon they absorbed out of the surface cycle. Ideally, a portion of this organic material would eventually be stored as sedimentary rock. However, the effectiveness of this method remains a subject of scientific debate, as some studies suggest that much of the carbon may be consumed by zooplankton near the surface or returned to the atmosphere through upwelling rather than reaching the seafloor.21