FEMS MicrobiologyLetters 90 ( 199212111-2114 c~ ~) 1992 Federalionof European MicrobiologicalSocieties11378-1(197/92/$115.1111 Published by Elsevier FEMSLE 04751 Dehalogenation of trichlorofluoromethane (CFC-11) by Methanosarcina barkeri U t e E. K r o n e a n d R u d o l f K. T h a u e r Lahoratorium filr Mikrobh~h~gie der Phi~ipps-Unicersitiit. Karl-con-Frisch-Str,,ts.~e. 3550 Marburg. F.R.G. Received t~sOctober 1901 Accepted28 October 1991 Key words: Halomethane degradation; Reductive dehalogenation: Methanogenic bacteria; Anaerobic archaebacteria; Methanohacterium barkeri i. S U M M A R Y Methanobacterium barkeri was found to cat- alyze the reductive dehalogenation of trich!~3rofluoromethane ( C F C - I I ) , also known as F R E O N 11. Products detected were CHFCI,, CH2FCI, CO and fluoride. 2. INTRODUCTION Trichlorofluoromethane (CFC-II), also known as F R E O N 11, is a volatile compound that has been widely used as a foam-blowing agent, as an aerosol propellant, and as a refrigerant. Because of its high stability it has accumulated in the atmosphere, with adverse effects on the ozone layer [1] and on the climate [2]. It persists in the atmosphere for as many as 40-45 years [3]. The Correspondence to: R. Thauer, Laborato~ium fiir Mikrobiolo- gie der Phillips-Universir;.it, Karl-von-Frisch-Strasse.3550 Marburg, F.R.G. only major known decomposition of CFC-II appears to be its photolysis in the lower stratosphere [3,4]. We rcport here that CFC-II is biodegradable by reductive dehalogenation. It has already been known that many anaerobic bacteria can catalyze the reductive dehalogenation of CCI 4 to CHCI 3, CH2CI 2, and CH3CI [5-10]. Evidence is available that corrinoids are involved in the catalytic mechanism [11,12]. This evidence is based on the two observations that (i) the ability of bacteria to dehalogenate CCI 4 correlates with the presence of high concentrations of corrinoids in the microorganisms; and (ii) corrineids such as aquocobalamin catalyze the reduction of CCI 4 to CHCI~, CH2CI 2, CH3CI, and CO with titanium(liD citrate or with dithiothreitol as electron donor [11,13]. Recently it was found that corrinoids can also catalyze the reductive dehalogenation of CFC-I 1 [13]. Products detectcd were CO and fluoride in an 1 to 1 stoichiomctry, and CHFCI 2, CH2FCI, CH3F, C2F2CI 2, C2F2CI4, and formate in minor amounts. The product pattern indicates that the corrinoid-mediated reduction of the chlorofluoro- 2(12 carbon involves the intermediacy of dihalocarbones. CFCI 3 + 2 [ H ] --, CFCI + 2HCI ( 1) CFCI + H , O - , C O + H F + HCI (2) The above mentioned findings promp!,:d an investigation to determine w h e t h c r anaerobic bacteria that can mediate the reductive dehalogenation of CCI 4 can also degrade CFC-I 1. For our studies we selected Methanosarchta barkeri. This organism is a strictly anaerobic m e t h a n o g e n i c archaebacterium which is very a b u n d a n t in anaer- A 7.0 O o 6.0 E 7i ,o obic e n v i r o n m e n t s [14}. Methanosarchm species are known to have a relatively high dchalogenation capacity [10,1215-17] and to contain high concentrations of corrinoids [18]. 3. M A T E R I A L S A N D M E T H O D S Methanosarcbta barkeri (strain Fusaro) (DSM 804) was from the Deutsche Sammlung von Mikroorganismen (Braunschweig, F.R.G.). The archaebacterium was grown on methanol and harvested at the end of the exponential phase as I O ~ j 1.8 with N2i I B 1.2 CHFCl2 g o.6 5.0 -~ c~ ~e 0 --~A~t--"-~" j_CO A 4.0 r 0 20 40 60 0 Time (min) i i , i 40 20 , , 60 Time (min) D 6.0 4.0 CHFCI2 S' ~o 3.0 E C,HFCI "2 -~ ~ a_ 4.0 3 /.," m 2.0 o /~Fluoride /" / " 1.0 ,~ Fluoride ~ 2.0 V 0 0 6 12 Protein ( m g / m l ) 6 12 CFC- 11 (/~mol/vial) Fig. 1. Reductive dehalogenation of CFC-I I by cell suspensions of Me,ham~sarcina barkeri. (A) Rate of CFC-I I ¢ons,~mption: (B) rate of products formation: (C) protein dependence: (D) CFC-I 1 dependence. For assay conditions see MATERIAI,SAND METI-tODS. 0 2~)3 described [19]. Cell suspensions (5 mg p r o t e i n / m l or as indicated) were anaerobically prepared in 25 mM imidazole/phosphate pH 7.0 containing 5 mM dithiothreitol, 2 mM MgCI_,, 411 mM NaCI and 2/.tM resazqrin. The dehalogenation assays were performed at 37°C in the dark in 120-ml serum vials containing 10 ml cell suspension and 11)0% H e (or 1110% N_, where indicated) at 1.5 x 105 Pa as gas phase. The reaction, which was n:n under continuous shaking at 250 rpm, was started by the addition of 6.7 t~mol CFC-II in methanolic solution (or of the amounts indicated). At 15-rain time intervals 0.3-ml samples of the head space were withdrawn and analyzed by gas chromatography [13]. 4. RESULTS AND DISCUSSION Cell suspensions of M. barked grown on methanol were found to degrade CFC-II in the presence of H 2 (Fig. IA), which the organism can use as electron donor via an active hydrogenase [20,21]. CHFCI z, fluoride, and CO were found as products (Fig. IB). CH_,FCI was detected in minute amounts (not shown). The rate of product formation increased linearly with the protein concentration (Fig. IC) and hyperbolically with the CFC-11 concentration (Fig. ID). From Fig. ID an apparent K m for CFC-I1 of approximately 10l~ ppm in the gas phase (6 p.mol per vial) was estimated. The specific rates (apparent V~,,~)were 100 nmol CFC-11 consumed per h per mg protein, and 66 nmol CHFCI 2, 16 nmol fluoride, and 3 nmol CO formed per h per mg protein. Carbon monoxide, which is converted to CO2 and H 2 by the organism via an active CO dehydrogenase [22], could substitute for H 2 as electron donor in CFC-I 1 reduction (data not shown). CFC-11 v, as net degraded in the absence of either H., or CO (Fig. 1A). Cells denatured by incubation at 100°C for 20 rain were unable to catalyze the reduction of CFC-I 1 with H 2 or CO. Th~ specific rate of CFC-II degradation was half that of CCI 4 reduction to CHCI 3 and twice that of CHC! 3 reduction to CHzCI 2 by M. barked. Degradation of CFC-12 (diehlorodifluoro- methane) occurred at less than 5% the rate at which CFC- 1 I was dehalogenated. CFC-II completely inhibited mcthanogenesis in M barked at the concentrations tested in the dehalogenation experiments. An apparent K, of 51) l~pm in the gas phase was determined. It is clear that CFC-I I is highly toxic for the organism. However, at the concentrations prevailing in the atmosphere (approx. 0.2 ppb) [23], no inhibition of methanogenesis was observed. Based on the apparent K m of 1000 ppm the rate of CFC-II dehalogenation will be very low at these concer,trations. It has yet to be determined whether this low rate is of biogeochemical significance Methanogenie soils and sediments have to be considered as possible sinks. Because of the long tropospheric lifetime, even minor dehalogenation rates could have a long-term i~,pact on the amount of CFC-I 1 that reaches the.stratosphere. ACKNOWLEDGEMENTS This work was supported by the Deutsche Forschungsgemeinschaft and by the Fonds der Chemischen industrie. We thank Dr. H.C. Friedmann, University of Chicago, and Dr. H.P.C. 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