Heterotrophic bacteria perform two major functions in the transformation of
organic matter: They produce new bacterial biomass (bacterial secondary pr
oduction [BP]), and they respire organic C to inorganic C (bacterial respir
ation [BR]). For planktonic bacteria, a great deal has been learned about B
P and its regulation during the past several decades but far less has been
learned about BR. Our lack of knowledge about BR limits our ability to unde
rstand the role of bacteria in the carbon cycle of aquatic ecosystems. Bact
erial growth efficiency (BGE) is the amount of new bacterial biomass produc
ed per unit of organic C substrate assimilated and is a way to relate BP an
d BR: BGE = (BP)/(BP + BR). Estimates of BGE for natural planktonic bacteri
a range from <0.05 to as high as 0.6, but little is known about what might
regulate this enormous range. In this paper we review the physiological and
ecological bases of the regulation of BGE. Further, we assemble the litera
ture of the past 30 years for which both BP and BR were measured in natural
planktonic ecosystems and explore the relationship between BGE and BP. Alt
hough the relationship is variable, BGE varies systematically with BP and t
he trophic richness of the ecosystem. In the most dilute, oligotrophic syst
ems, BGE is as low as 0.01; in the most eutrophic systems, it plateaus near
0.5. Planktonic bacteria appear to maximize carbon utilization rather than
BGE. A consequence of this strategy is that maintenance energy costs (and
therefore maintenance respiration) seems to be highest in oligotrophic syst
ems.