We investigated the constraints on sulWde uptake by bacterial ectosymbionts on the marine peritrich ciliate Zoothamnium niveum by a combination of experimental and numerical methods. Protists with symbionts were collected on large blocks of mangrove-peat. The blocks were placed in a Xow cell with Xow adjusted to in situ velocity. The water motion around the colonies was then characterized by particle tracking velocimetry. This shows that the feather-shaped colony of Z. niveum generates a unidirectional Xow of seawater through the colony with no recirculation. The source of the feeding current was the free-Xowing water although the size of the colonies suggests that they live partly submerged in the diVusive boundary layer. We showed that the Wltered volume allows Z. niveum to assimilate suYcient sulWde to sustain the symbiosis at a few micromoles per liter in ambient concentration. Numerical modeling shows that sulWde oxidizing bacteria on the surfaces of Z. niveum can sustain 100-times higher sulWde uptake than bacteria on Xat surfaces, such as microbial mats. The study demonstrates that the Wlter feeding zooids of Z. niveum are preadapted to be prime habitats for sulWde oxidizing bacteria due to Z. niveum's habitat preference and due to the feeding current. Z. niveum is capable of exploiting low concentrations of sulWde in near norm-oxic seawater. This links its otherwise dissimilar habitats and makes it functionally similar to invertebrates with thiotrophic symbionts in Wltering organs.