It is found that carbon export fluxes to the deep ocean from a highly productive, naturally iron-fertilized region of the sub-Antarctic Southern Ocean are two to three times larger than the carbon export fluxes from an adjacent high-nutrient low-chlorophyll area not fertilized by iron. These findings support the hypothesis that increased iron supply to the glacial sub-Antarctic may have directly enhanced carbon export to the deep ocean.
- Raymond T. Pollard
- Ian Salter
- Mike V. Zubkov
