In all ecosystems, bacteria are the most numerous organisms and through the
m flows a large fraction of annual primary production. In the past decade w
e have learned a great deal about some of the factors that regulate bacteri
a and their activities, and how these activities, in turn, alter ecosystem-
level processes. Here I review three areas in which recent progress has bee
n made with particular reference to pelagic ecosystems: the problem of bact
erial cell dormancy; the effect of solar radiation on organic matter labili
ty; and, the maintenance of net heterotrophy. In a system in which grazing
is the major source of mortality for bacteria, bacterial cell dormancy is s
omething of a paradox. I argue that the degree to which bacteria are grazed
by flagellates (highly selective grazers) versus other grazers (cladoceran
s, bivalves) may explain the degree and variation in the proportion of acti
ve cells which recent evidence shows to be large. Another factor affecting
bacterial activity that has come to the fore in recent years is solar radia
tion. Irradiation, especially in the ultra-violet range has long been thoug
ht of as simply deleterious to some bacteria. A wealth of newer evidence sh
ows that refractory dissolved organic compounds may be converted into micro
bially labile compounds by solar radiation in several wavebands. This inter
action between irradiation and organic matter (photolysis) may explain, in
part, how dissolved organic carbon (C) may be refractory in the dark enviro
nment of the soil but become labile in the illumunated surface waters of la
kes or rivers. The newer evidence shows that aquatic ecosystems, at least o
ligotrophic ones, are significantly subsidized by terrestrially-produced or
ganic matter. I review here multiple lines of evidence that suggest that fr
eshwater ecosystems are predominantly systems which respire more organic C
than they produce by photosynthesis, and are therefore net heterotrophic. W
hile net heterotrophy is an interesting exception for terrestrial ecosystem
s, it appears to be commonplace for aquatic systems and represents an impor
tant linkage between terrestrial and aquatic ecosystems.