Ocean fertilisation has been proposed as a strategy to increase the biological capacity of the oceans to absorb carbon dioxide from the atmosphere. This is done by introducing iron into the oceans to increase productivity, thereby stimulating phytoplankton blooms and consequently increasing carbon uptake. This strategy has been heavily criticised for its low carbon sequestration potential and potentially far-reaching ecological consequences. It is not possible to fully predict the effects of this strategy in advance. The risks include a significant reduction in biodiversity through a massive die-off of fish and marine plants, which could trigger an alarming chain of cascading effects.
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