Between 1 and 3% of the rare earth elements in a marine aerosol of Sah
aran origin were dissolved into surface seawater in a laboratory exper
iment. The REEs appear to fall into the category of those predominantl
y associated with the mineral aerosol (e.g. Al, Si and Fe). The interm
ediate rare earths (Eu-Er) showed slightly greater solubility than lig
ht- and heavy-rare earths which may reflect release of REEs from aeros
ol mineral coatings. Extrapolation to a global budget suggests that di
ssolved atmospheric input is equivalent to about 30-130% of rare earth
element input to the oceans by rivers.