L-2-Halo acid dehalogenase catalyzes the stereospecific hydrolytic dehalogenation of L-2-halo acids, with inversion of the C2-configuration. Seven L-2-halo acid dehalogenases from various bacterial strains are significantly similar to one another in their amino acid sequences (36-70% identity), and they are supposed to catalyze the reaction through the same mechanism. To identify catalytically important residues, we mutated all the 36 highly conserved charged and polar amino acid residues of L-2-halo acid dehalogenase from Pseudomonas sp. YL, which consists of 232 amino acid residues, by replacement of D by N, E by Q, R by K, and vice versa, S and T by A, Y and W by F, M by L, and H by N. We found that the replacement of D10, K151, S175, D180, R41, S118, T14, Y157, and N177 led to a significant loss in the enzyme activity or an increase in the Km value for the substrate, showing their involvement in the catalysis. The roles of these residues are discussed.
Aims: The objective of this study was to investigate the changes in the indigenous bacterial community structure for assessing the impact of biostimulation on spilled oil.
Methods and Results: Changes in the bacterial community structure were monitored by denaturing gradient gel electrophoresis (DGGE) and clone library methods based on 16S rRNA gene (rDNA) sequences. The results of DGGE, coupled with the use of the Shannon index and principal component analysis (PCA) and clone library analyses, were consistent. In the treated (fertilized) area, one operational taxonomic unit (OTU) became dominant during the fertilization period, and it was most closely related to Pseudomonas putida.
Conclusions: The bacterial community structure in the treated area was markedly different from that in the control (non‐fertilized) area during the fertilization period, but in the two areas it became similar at 14 weeks after the end of fertilization.
Significance and Impact of the Study: The results suggest that the bacterial community structure was disrupted by the biostimulation treatment, but that it recovered immediately after the end of fertilization.
Chlorine isotope fractionation during reductive dechlorination of trichloroethene (TCE) and tetrachloroethene (PCE) to cis-1,2-dichloroethene (cDCE) by anaerobic bacteria was investigated. The changes in the 37Cl/35Cl ratio observed during the one-step reaction (TCE to cDCE) can be explained by the regioselective elimination of chlorine accompanied by the Rayleigh fractionation. The fractionation factors (alpha) of the TCE dechlorination by three kinds of anaerobic cultures were approximately 0.994-0.995 at 30 degrees C. The enrichment of 37Cl in the organic chlorine during the two-step reaction (PCE to cDCE) can be explained by the random elimination of one chlorine atom in the PCE molecule followed by the regioselective elimination of one chlorine atom in the TCE molecule. The fractionation factors for the first step of the PCE dechlorination with three kinds of anaerobic cultures were estimated to be 0.987-0.991 at 30 degrees C using a mathematical model. Isotope fractionation during the first step would be the primary factor for the chlorine isotope fractionation during the PCE dechorination to cDCE. The developed models can be utilized to evaluate the fractionation factors of regioselective and multistep reactions.
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