Sulfoquinovose (SQ; 6-deoxy-6-sulfoglucose) is the polar head group of the plant sulfolipid SQ-diacylglycerol, and SQ comprises a major proportion of the organosulfur in nature, where it is degraded by bacteria. A first degradation pathway for SQ has been demonstrated recently, a "sulfoglycolytic" pathway, in addition to the classical glycolytic (Embden-Meyerhof) pathway in Escherichia coli K-12; half of the carbon of SQ is abstracted as dihydroxyacetonephosphate (DHAP) and used for growth, whereas a C 3 -organosulfonate, 2,3-dihydroxypropane sulfonate (DHPS), is excreted. The environmental isolate Pseudomonas putida SQ1 is also able to use SQ for growth, and excretes a different C 3 -organosulfonate, 3-sulfolactate (SL). In this study, we revealed the catabolic pathway for SQ in P. putida SQ1 through differential proteomics and transcriptional analyses, by in vitro reconstitution of the complete pathway by five heterologously produced enzymes, and by identification of all four organosulfonate intermediates. The pathway follows a reaction sequence analogous to the Entner-Doudoroff pathway for glucose-6-phosphate: It involves an NAD + -dependent SQ dehydrogenase, 6-deoxy-6-sulfogluconolactone (SGL) lactonase, 6-deoxy-6-sulfogluconate (SG) dehydratase, and 2-keto-3,6-dideoxy-6-sulfogluconate (KDSG) aldolase. The aldolase reaction yields pyruvate, which supports growth of P. putida, and 3-sulfolactaldehyde (SLA), which is oxidized to SL by an NAD(P) + -dependent SLA dehydrogenase. All five enzymes are encoded in a single gene cluster that includes, for example, genes for transport and regulation. Homologous gene clusters were found in genomes of other P. putida strains, in other gamma-Proteobacteria, and in beta-and alpha-Proteobacteria, for example, in genomes of Enterobacteria, Vibrio, and Halomonas species, and in typical soil bacteria, such as Burkholderia, Herbaspirillum, and Rhizobium.bacterial biodegradation | organosulfonate | sulfolipid | 6-deoxy-6-sulfoglucose | sulfur cycle S ulfoquinovose (SQ; 6-deoxy-6-sulfoglucose) is the polar head group of the plant sulfolipids sulfoquinovosyl diacylglycerols (SQDGs), which were discovered more than 60 y ago (1). The sulfolipids are located in the photosynthetic (thylakoid) membranes of all higher plants, mosses, ferns, and algae, as well as in most photosynthetic bacteria. They are also present in some nonphotosynthetic bacteria, and SQ is in the surface layer of some archaea (2-4). SQ is continuously degraded in all environments where SQ is produced, or it would enrich in these environments. The complete degradation of SQ to, ultimately, CO 2 , concomitant with a recycling of the bound sulfur in the form of inorganic sulfate, is dominated by microbes (e.g., by soil bacteria) (2, 5-9). However, a more detailed exploration of SQ-degrading microbes, of their SQ-degradation pathways, and of the enzymes and genes involved has only recently been initiated (10-12). The common view on SQ degradation is based on the consideration that SQ is a structural analog of glucose-6...