Biogeochemical effects of atmospheric input on the ocean

The availability of iron as a nutrient for phytoplankton growth is dependent on its chemical speciation (Wells et al., 1995). Thus processes which alter iron solubility in the atmospheric aerosols have the potential to influence bioavailability 

So what is the fate of this dissolved iron in rainwater and the labile iron on aerosol surfaces upon deposition to seawater Based on the results of acid cycling 

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