Microscale physiological and ecological studies of aquatic cyanobacteria: macroscale implications.

Cyanobacteria have had a profound and unparalleled biogeochemical impact on the earth's biosphere. As the first oxygenic phototrophs, cyanobacteria were responsible for the transition from anaerobic to aerobic life. Ironically, molecular oxygen (O2) is inhibitory to critical components of cyanobacterial metabolism, including photosynthesis and nitrogen fixation. Cyanobacteria have developed a great variety of biochemical, structural, and biotic adaptations ensuring optimal growth and proliferation in diverse oxic environments to counter this difficult situation. Structurally, cyanobacteria reveal remarkable diversity, including the formation of highly differentiated, O2-deplete cells (heterocysts), multicellularity as trichomes, and aggregates, that, among N2-fixing genera, facilitate division of labor between aerobic and anaerobic processes. Cyanobacteria enjoy unique consortial and symbiotic associations with other microorganisms, higher plants, and animals, in which O2 consumption is closely coupled in time and space to its production. Because as prokaryotes they are devoid of O2-consuming organelles (e.g., mitochondria), cyanobacteria have developed alternative strategies for locally protecting O2-sensitive processes, including consortial relationships with other microorganisms. Specific organic compounds released by cyanobacteria are capable of chemotactically attracting bacterial consorts, which in turn attach to the host cyanobacteria, consume O2, and recycle inorganic nutrients within the cyanobacterial "phycosphere." Multicellularity and aggregation lead to localized O2 gradients and hypoxic/anoxic microzones in which O2-sensitive processes can coexist. Microscale partitioning of O2-producing and O2-inhibited processes promotes contiguous and effective metabolite and nutrient exchange between these processes in oxygenated waters, representing a bulk of the world's oceanic and freshwater ecosystems.