I. Hamels et al., Uncoupling of bacterial production and flagellate grazing in aquatic sediments: a case study from an intertidal flat, AQUAT MIC E, 25(1), 2001, pp. 31-42
In contrast to planktonic ecosystems, the fate of bacterial production in a
quatic sediments is still largely unclear. In this study, we identified the
factors regulating the impact of flagellate grazing on benthic bacterial p
roduction for a sandy and a silty intertidal sediment. Flagellate grazing r
ates were estimated using fluorescently labelled sediment to prevent distur
bance of in situ bacterial density and community composition and to account
for grazing on attached bacteria. Since flagellate cell size was quite div
erse, the grazing rates were determined for 4 size classes. Bacterial produ
ction was measured simultaneously with grazing estimates. Bacterial density
and production increased with decreasing median grain size of the sediment
. Bacterial production was strongly related to the chlorophyll a content of
the sediment, indicating resource control of bacterial production. In cont
rast to bacteria, flagellate biomass decreased with decreasing median grain
size of the sediment. Pairwise comparison of grazing rates between the 2 s
ites showed that grazing rates were significantly higher at the sandy site.
This suggests that the effect of sediment composition on flagellate biomas
s may be mediated by an influence of sediment characteristics on flagellate
ingestion rates, The negative relation of bacterial production and the pos
itive relation of flagellate biomass and grazing rates with median grain si
ze resulted in a significant positive relation between the impact of flagel
late grazing on bacterial production and the median grain size of the sedim
ent. These results amount to an uncoupling of flagellate grazing and bacter
ial production in fine sediments. Our results as well as results from previ
ous studies suggest that grazing by flagellates is not an important fate of
bacterial production in aquatic sediments, except for sandy sediments duri
ng periods of low bacterial production.