The chemistry and bioavailability of Ag contribute to its high toxicit
y in marine and estuarine waters. Silver is unusual, in that both the
dominant speciation reaction in seawater and the processes important i
n sorbing Ag in sediments favour enhanced bioavailability. Formation o
f a stable chloro complex favours dispersal of dissolved Ag, and the a
bundant chloro complex is available to biota. Sequestration by sedimen
ts also occurs, but with relatively slow kinetics. Amorphous aggregate
d coatings enhance Ag accumulation in sediments, as well as Ag uptake
from sediments by deposit feeders. In estuaries, the bioaccumulation o
f Ag increases 56-fold with each unit of increased Ag concentration in
sediments. Toxicity for sensitive marine species occurs at absolute c
oncentrations as low as those observed for any non-alkylated metal, pa
rtly because bioaccumulation increases so steeply with contamination.
The environmental window of tolerance to Ag in estuaries could be narr
ower than for many elements.