DNA-based stable-isotope probing was applied to identify the active microorganisms involved in syntrophic butyrate oxidation in paddy field soil. After 14 and 21 days of incubation with [U-13 C]butyrate, the bacterial Syntrophomonadaceae and the archaeal Methanosarcinaceae and Methanocellales incorporated substantial amounts of 13 C label into their nucleic acids. Unexpectedly, members of the Planctomycetes and Chloroflexi were also labeled with 13 C by yet-unclear mechanisms.Butyrate is one of the important intermediates in the degradation of organic matter in anoxic environments (3)(4)(5)22). The degradation of butyrate to H 2 , formate, and acetate is endergonic under standard conditions. This thermodynamic barrier, however, can be overcome by the syntrophic interaction between butyrate-oxidizing bacteria and methanogenic archaea, which keep the products H 2 , formate, and acetate at low concentrations (23). A few strains involved in syntrophic butyrate oxidation have been isolated into pure cultures (e.g., see references 15, 16, and 30). These organisms represent a thermodynamically extreme lifestyle, since even in the optimum syntrophic association with methanogens, the Gibbs free energy available for syntrophic butyrate oxidizers is still close to the thermodynamic limit (⌬G 0Ј ϭ Ϫ20 kJ per reaction). Recently, genome sequences of two syntrophic butyrate oxidizers (Syntrophomonas wolfei and Syntrophus aciditrophicus) (17, 24) revealed that they have limited fermentation and respiration mechanisms but possess multiple copies of -oxidation genes and sets of reverse electron transfer machineries which are essential for the syntrophic oxidation of butyrate.Studies on natural environments, however, are very scarce (1, 5). Acetate, propionate, and butyrate are the most important intermediates during the degradation of organic residues in paddy field soils (4, 22). Only two studies known to us so far, however, have been conducted to determine the syntrophic degradation of propionate (12) and acetate (7), and none have been done on syntrophic butyrate oxidation in paddy field soil. Therefore, our objectives were to investigate syntrophic butyrate oxidation and identify the active organisms responsible for this process in a Chinese paddy field soil using nucleic acid-based stable-isotope probing (SIP), which has been proven to be powerful in linking the identities of microorganisms in environments with their specific functions (2).Soil sample and anoxic incubation. Paddy field soil was collected from an experimental station of the China National Rice Research Institute in Hangzhou, China (30 o 04Ј37ЉN, 119 o 54Ј37ЉE). The soil was a clay loam and had the following properties as measured by standard methods (18): pH 6.7, a cation exchange capacity of 14.4 cmol kg Ϫ1 , an organic C content of 24.2 g kg Ϫ1 , and a total N content of 2.3 g kg Ϫ1 . Soil was air dried and passed through 2-mm sieves. Three-gram soil samples were weighed in 15-ml serum bottles and mixed with 4.5 ml distilled anoxic water. The vials were c...