Viral burst size (BS), i.e. the number of viruses released during cell lysis, is a critical parameter for assessing the ecological and biogeochemical role of viruses in aquatic systems. Burst size is typically estimated by enumerating the viral particles in bacteria using transmission electron microscopy. Here, we review the average BS reported for different aquatic systems, present several hypotheses on the control of the BS and evaluate whether there are relationships between BS and bacterial activity parameters across systems. Based on reports from a variety of different aquatic environments, we calculated a mean BS of 24 and 34 for marine and freshwater environments, respectively. Generally, the BS increased with the trophic status of the environment and with the percentage of infected cells in marine populations. When diel dynamics were investigated or averages from large-scale environments were used, BS was positively related to bacterial production but no trend was detectable across systems. The across systems' finding that BS was significantly related to the frequency of infected cells (FIC) could be due to co-infection or superinfection. At any given site, BS seems to be influenced by a number of factors such as the size of the host cell and the viruses, the metabolic activity of the host and phage and host diversity. Thus, based on the available data collected over the past two decades on a variety of aquatic systems, some relations between BS and bacterial variables were detectable.

To elucidate the potential importance of deep-water viruses in controlling the meso-and bathypelagic picoplankton community, the abundance, decay rate, and diversity of the virioplankton community were determined in the meso-and bathypelagic water masses of the eastern part of the subtropical North Atlantic. Viral abundance averaged 1.4 ؋ 10 6 ml ؊1 at around 100 m of depth and decreased only by a factor of 2 at 3,000 to 4,000 m of depth. In contrast, picoplankton abundance decreased by 1 order of magnitude to the Lower Deep Water (LDW; 3,500-to 5,000-m depth). The virus-to-picoplankton ratio increased from 9 at about 100 m of depth to 110 in the LDW. Mean viral decay rates were 3.5 ؋ 10 ؊3 h ؊1 between 900 m and 2,750 m and 1.1 ؋ 10 ؊3 h ؊1 at 4,000 m of depth, corresponding to viral turnover times of 11 and 39 days, respectively. Pulsed-field gel electrophoresis fingerprints obtained from the viral community between 2,400 m and 4,000 m of depth revealed a maximum of only four bands from 4,000 m of depth. Based on the high viral abundance and the low picoplankton production determined via leucine incorporation, we conclude that the viral production calculated from the viral decay is insufficient to maintain the high viral abundance in the deep North Atlantic. Rather, we propose that substantial allochthonous viral input or lysogenic or pseudolysogenic production is required to maintain the high viral abundance detected in the meso-and bathypelagic North Atlantic. Consequently, deep-water prokaryotes are apparently far less controlled in their abundance and taxon richness by lytic prokaryotic phages than the high viral abundance and the virus-to-picoplankton ratio would suggest.

Viral diversity has been studied in a variety of marine habitats and spatial and seasonal changes have been documented. Most of the bacteriophages are considered host specific and are thought to affect fast growing prokaryotic phylotypes more than slow growing ones. We hypothesized that viral infection and consequently, lysis occurs in pulses with only a few prokaryotic phylotypes lysed at any given time. Thus, we propose that the newly produced viruses represent only a fraction of the viral diversity present at any given time. Virioplankton diversity was assessed by pulsed-field gel electrophoresis in the surface waters of three distinct areas of the North Sea during the spring and summer. Bulk virioplankton diversity was fairly stable in these waters. Viral diversity produced by the indigenous bacterioplankton, however, exhibited day-to-day variability with only a few bands produced at any given time. These bands frequently matched bands of the in situ virioplankton; however, bands not present in the band pattern of the in situ virioplankton community were also found. These new bands probably indicate infection and subsequent release of viruses from bacterioplankton phylotypes previously not infected by these specific viruses. Overall, our results demonstrate that viral infection and lysis are rather dynamic processes. The main targets of viral infection are changing apparently on time scales of hours to days indicating that viral infection might effectively regulate and maintain bacterioplankton diversity.

The dynamics of dissolved organic matter (DOM) and microbial activity were monitored in the coastal North Sea over an annual cycle. DOM accumulated during the spring bloom towards the summer, associated with high phytoplankton extracellular release. Accumulation of dissolved organic carbon (DOC) occurred from April to June. During this period, based on the bacterial carbon demand (BCD) of the free-living bacteria and the photosynthetic extracellular release (PER), 85 µM C were derived from sources other than direct DOC release by phytoplankton. Thereafter, from the end of August until December, the DOM concentrations decreased by about half. During this period, at least 269 µM C was removed from the system via the utilization by the bacterial community and/or sedimentation and export. Overall, our data indicate a pronounced seasonal shift in DOM sources supporting BCD. From spring to summer, BCD is almost fully supported by PER alone while in fall and winter, BCD is supported about equally by PER and by the DOM accumulated in the spring-summer period and originating presumably from a variety of DOM production mechanisms.