Dissolved organic matter utilization and oxygen uptake in algal-bacterial microcosms.
Under closed laboratory conditions, at non-limiting nutrient levels, the biomass of Anabaena variabilis, Anacystis nidulans, Chlorella pyrenoidosa, and Selanastrum capricornutum increased with increasing levels of dissolved organic matter (DOM) as a result of bacterially produced carbon dioxide (CO2) and (or) cofactors. Oxygen (O2) produced as a result of algal photosynthesis was sufficient to supply the najority of O2 required by the bacterial community. The percentage of DOM utilized by bacteria which was subsequently incorporated into algal biomass varied with individual species indicating that the association between individual algal species and the bacterial microbiota varied. Under natural conditions bacteria could provide CO2 and (or) cofactors for algal photosynthesis which in turn supplies O2 for bacterial respiration. This mutualistic association in aquatic environments could result in an increase in planktonic and epiphytic algal biomass if other nutrients are available.
D001419:Bacteria / Q000254:growth & development / Q000378:metabolism*; D002244:Carbon / Q000378:metabolism*; D002245:Carbon Dioxide / Q000378:metabolism; D056890:Eukaryota / Q000254:growth & development / Q000378:metabolism*; D010101:Oxygen Consumption; D013045:Species Specificity; D013559:Symbiosis; D014871:Water Microbiology
D002245:Carbon Dioxide; D002244:Carbon