The role of organic complexation on ambient iron chemistry in the equatorial Pacific Ocean and the response of a mesoscale iron addition experiment

We participated on the Iron‐Ex II study in the equatorial Pacific to investigate ambient iron chemistry and its response to a mesoscale iron addition experiment. As expected, dissolved iron values in the high‐nutrient, low‐chlorophyll surface waters of the South Equatorial Current (4–6°S, 105–109°W)... View More