Pseudomonas putida DS1 is able to utilize dimethyl sulfone as a sulfur source. Expression of the sfnFG operon responsible for dimethyl sulfone oxygenation is directly regulated by a 54 -dependent transcriptional activator, SfnR, which is encoded within the sfnECR operon. We investigated the transcription mechanism for the sulfate starvation-induced expression of these sfn operons. Using an in vivo transcription assay and in vitro DNAbinding experiments, we revealed that SfnR negatively regulates the expression of sfnECR by binding to the downstream region of the transcription start point. Additionally, we demonstrated that a LysR-type transcriptional regulator, CysB, directly activates the expression of sfnECR by binding to its upstream region. CysB is a master regulator that controls the sulfate starvation response of the sfn operons, as is the case for the sulfonate utilization genes of Escherichia coli, although CysB DS1 appeared to differ from that of E. coli CysB in terms of the effect of O-acetylserine on DNA-binding ability. Furthermore, we investigated what effector molecules repress the expression of sfnFG and sfnECR in vivo by using the disruptants of the sulfate assimilatory genes cysNC and cysI. The measurements of mRNA levels of the sfn operons in these gene disruptants suggested that the expression of sfnFG is repressed by sulfate itself while the expression of sfnECR is repressed by the downstream metabolites in the sulfate assimilatory pathway, such as sulfide and cysteine. These results indicate that SfnR plays a role independent of CysB in the sulfate starvation-induced expression of the sfn operons.Sulfur, an essential element for bacterial growth, is assimilated from a range of sources. The preferred sulfur source for bacteria is inorganic sulfate, but in soil environments, sulfate may not be freely available because inorganic sulfate constitutes less than 5% of the total sulfur (1). The remainder is largely in the form of sulfate esters and carbon-bound sulfur such as peptides/amino acids and sulfonates (1). Volatile organic sulfur compounds, for example, dimethyl sulfide (DMS) and methanethiol, are also widely distributed in the environment because they are emitted from oceans (2), freshwater sediments (28, 29), and soils (26, 31). Thus, several soil bacterial species have developed a number of systems that allow the use of these organosulfur compounds.Metabolic use of these organosulfur compounds, especially alkanesulfonates, taurine, and alkanesulfate ester, has been extensively investigated in Escherichia coli and Pseudomonas spp. (reviewed in reference 19). Bacterial organosulfur assimilation is mediated by the sulfate starvation response, which involves a set of proteins synthesized by several species of bacteria when the supply of their preferred sulfur sources, such as inorganic sulfate, cysteine, and thiosulfate, is limited. These proteins are known as sulfate starvation-induced (SSI) proteins and include enzymes and transport systems for scavenging sulfur from organic compounds (19...