On the Role of Dust‐Deposited Lithogenic Particles for Iron Cycling in the Tropical and Subtropical Atlantic

Lithogenic material deposited as dust is one of the major sources of trace metals to the ocean, particularly in the tropical and subtropical Atlantic. On the other hand, it can also act as a scavenging surface for iron. Here we studied this double role of lithogenic material in the marine iron cycle by adding a new scheme for describing particle dynamics into a global biogeochemistry and ecosystem model including particle aggregation and disaggregation of two particle size classes and scavenging on both organic and lithogenic particles. Considering the additional scavenging of iron on lithogenic particles, the modeled dissolved iron concentration is reduced significantly in the tropical and subtropical Atlantic, bringing the model much closer to observations. This underlines the necessity to consider the double role of dust particles as iron source and sink in studies on the marine iron cycle in high dust regions and with changing dust fluxes. Key Points Dust particles and particle dynamics were added in a global biogeochemical model Dust particles are considered both as iron source and scavengers Modeled dissolved iron in high dust regions is significantly reduced due to additional scavenging on dust