Researchers have reported that regional iron variations in the oceans is up to 10,000 times. Iron, key for ocean plant plankton growth, shows larger variations than previously recognised, with implications for models of climate. Microscopic marine plants, phytoplankton, lock up atmospheric carbon dioxide, but a lack of iron limits photosynthesis. This observation is expected to improve ocean-climate models.
Photosynthetic life is limited by low availability of iron in as much as one third of Earth's surface oceans. The problem for phytoplankton is particularly acute around the Southern Ocean. Dr Will Homoky from the Universities of Southampton and South Carolina said, "Iron acts like a giant lever on marine life, storing carbon. It switches on growth of microscopic marine plants, which extract carbon dioxide from our atmosphere and lock it away in the ocean."
In separate studies, scientists have previously added iron to the ocean in iron-limited areas, which typically generates large blooms of phytoplankton. This has been suggested by some as a possible geoengineering solution to capture carbon from the atmosphere and transfer it to the ocean. It remains unclear what the fate of phytoplankton carbon, at the base of the food chain is, and the role of iron for fertilising the oceans is a developing field of research.
Dr Homoky said, "Satellite images of the oceans show less phytoplankton growth in the eastern South Atlantic off the African coast, than in the western South Atlantic, off South America. Our primary hypothesis is that there are more micronutrients like iron being mixed into the surface ocean from the south African continent than from South America." The key to understanding these variations is now to understand how elements mix into the surface of the ocean, and how this in turn changes ocean life and potentially locks up atmospheric carbon dioxide.