Semicontinuous cultures were used to assess the effect of aqueous Fe(II) re
moval on the dissimilatory reduction of crystalline Fe(III) oxides by Shewa
nella alga strain BrY. Aqueous phase replacement in semicontinuous cultures
(average residence time of 9 or 18 days) resulted in a 2-3-fold increase i
n the cumulative amount of Fe(II) produced from synthetic goethite reductio
n over a 2-month incubation period, compared to parallel batch cultures. A
more modest (maximum 30%) but significant stimulation of natural subsoil Fe
(III) oxide reduction was observed. The extended Fe(III) reduction resulted
from enhanced generation of aqueous Fe(II) which was periodically removed
from the cultures. A concomitant stimulation of bacterial protein productio
n was detected, which suggested that Fe(II) removal also promoted bacterial
growth. A simulation model in which Fe(II) sorption to the solid-phase res
ulted in blockage of surface reduction sites captured the contrasting behav
ior of the batch vs semicontinuous Gt reduction systems. Our findings indic
ate that elimination of Fe(II) via advective transport could play a signifi
cant role in governing the rate and extent of microbial Fe(III) oxide reduc
tion in sedimentary environments.