Abstract. Rivers discharge a notable amount of dissolved Fe
(1.5×109 mol yr−1) to coastal waters but are still not considered
important sources of bioavailable Fe to open marine waters. The reason is
that the vast majority of particular and dissolved riverine Fe is considered
to be lost to the sediment due to aggregation during estuarine mixing.
Recently, however, several studies demonstrated relatively high stability of
riverine Fe to salinity-induced aggregation, and it has been proposed that
organically complexed Fe (Fe-OM) can “survive” the salinity gradient,
while Fe (oxy)hydroxides are more prone to aggregation and selectively
removed. In this study, we directly identified, by X-ray absorption
spectroscopy, the occurrence of these two Fe phases across eight boreal
rivers draining into the Baltic Sea and confirmed a significant but
variable contribution of Fe-OM in relation to Fe (oxy)hydroxides among river
mouths. We further found that Fe-OM was more prevalent at high flow
conditions in spring than at low flow conditions during autumn and that
Fe-OM was more dominant upstream in a catchment than at the river mouth. The
stability of Fe to increasing salinity, as assessed by artificial mixing
experiments, correlated well to the relative contribution of Fe-OM,
confirming that organic complexes promote Fe transport capacity. This study
suggests that boreal rivers may provide significant amounts of potentially
bioavailable Fe beyond the estuary, due to organic matter complexes.