Abstract. Microbial consumption of phytoplankton-derived organic
carbon in the pelagic food web is an important component of the global C
cycle. We studied C cycling in two phytoplankton–bacteria systems
(non-axenic cultures of a dinoflagellate Apocalathium malmogiense and a cryptophyte Rhodomonas marina) in two
complementary experiments. In the first experiment we grew phytoplankton and
bacteria in nutrient-replete conditions and followed C processing at early
exponential growth phase and twice later when the community had grown
denser. Cell-specific primary production and total community respiration
were up to 4 and 7 times higher, respectively, in the A. malmogiense treatments. Based on
the optical signals, accumulating dissolved organic C (DOC) was degraded
more in the R. marina treatments, and the rate of bacterial production to primary
production was higher. Thus, the flow of C from phytoplankton to bacteria
was relatively higher in R. marina treatments than in A. malmogiense treatments, which was further
supported by faster 14C transfer from phytoplankton to bacterial
biomass. In the second experiment we investigated consumption of the
phytoplankton-derived DOC by bacteria. DOC consumption and transformation,
bacterial production, and bacterial respiration were all higher in R. marina
treatments. In both experiments A. malmogiense supported a bacterial community
predominated by bacteria specialized in the utilization of less labile DOC
(class Bacteroidia), whereas R. marina supported a community predominated by
copiotrophic Alpha- and Gammaproteobacteria. Our findings suggest that large
dinoflagellates cycle relatively more C between phytoplankton biomass and
the inorganic C pool, whereas small cryptophytes direct relatively more C to
the microbial loop.