While microbial aquatic communities are dominated numerically by viruses, both bacterioplankton and phytoplankton play a basal role in the carbon cycle, producing and mineralizing organic matter and driving CO 2 concentrations. Both weak and strong relationships between these 2 microbial groups have been reported for temperate ecosystems. However, data from the tropics and sub-tropics are still scarce, and no consistent pattern regarding the structural microbial connections in these aquatic environments is known so far. We examined bacteria-phytoplankton abundance relationships for tropical freshwaters in comparison to well-studied temperate aquatic ecosystems. We present data on bacterioplankton and phytoplankton abundances in a large data set (1644 samples; lakes, rivers, and reservoirs) from sampling throughout an extensive gradient of latitude (3°N to 33°S) and longitude (35°to 70°W) in tropical waters. We found a generally weak, but significant, relationship between bacterioplankton and phytoplankton abundances and between bacterioplankton and chlorophyll. However, analyzing system by system, we observed an increase in the strength of the relationships (expressed by the determination coefficient, r 2 ), from 0.05 to 0.17 (bacterioplankton and phytoplankton abundances) and from 0.09 to 0.44 (bacterial abundance and chl a). Our data suggest that the in-system ecological drivers (e.g. water temperature, trophic state, and flushing characteristics, i.e. lentic or lotic) determine the bacterioplankton abundance patterns more than other factors such as latitude or system typology. In a global perspective, the comparison between non-tropical and tropical/sub-tropical freshwaters showed that a lower proportion of phytoplankton carbon is transformed into bacterial carbon in the tropics.
KEY WORDS: Microbial dynamics · Bacterial-phytoplankton coupling · Tropical waters
Resale or republication not permitted without written consent of the publisherAquat Microb Ecol 60: [261][262][263][264][265][266][267][268][269][270][271][272] 2010 plankton and fish through bacterial biomass (Cole et al. 2006). It is generally believed that autochthonous DOM from phytoplankton is more available for bacterial consumption than allochthonous terrestrial DOC (Kritzberg et al. 2005). Bacteria rapidly assimilate phytoplanktonic carbon compared to terrestrial DOC (Chen & Wangersky 1996). In tropical freshwaters, for instance, humic substances are an important energy source for aquatic bacteria (Amado et al. 2006), but this source is probably not very relevant as a carbon source for bacterial production, since consumption of humic substances appears to be mostly channeled through microbial respiration (Farjalla et al. 2009).The dependence of bacterioplankton on autochthonous carbon has been supported by positive relationships between phytoplankton (expressed as chlorophyll a [chl a], cell numbers, or biovolume) and heterotrophic bacteria (expressed as numbers or biomass, Bird & Kalff 1984, Stewart & Fritsen 2004 or production, W...