| 總結: | Methane formation in methanogenic Archaea is catalyzed by methyl-coenzyme M reductase (MCR) and takes place via the reduction of methyl-coenzyme M (CH₃-S-CoM) with coenzyme B (HS-CoB) to methane and the heterodisulfide CoM-S-S-CoB. MCR harbors the nickel porphyrinoid conenzyme F⠄₃₀ as a prosthetic group, which has to be in the Ni(I) oxidation state for the enzyme to be active. To date no intermediates in the catalytic cycle of MCR<sub>red1</sub> (red for reduced Ni) have been identified. Here, we report a detailed characterization of MCR<sub>red1</sub> ("m" for methyl-coenzyme M), which is the complex of MCR<sub>red1a</sub> ("a" for absence of substrate) with CH₃-S-CoM. Using continuous-wave and pulse electron paramagnetic resonance spectroscopy in combination with selective isotope labeling (¹³C and ²H) of CH₃-S-CoM, it is shown that CH₃-S-CoM binds in the active site of MCR such that it thioether sulfur is weakly coordinated to the Ni(I) of F⠄₃₀. The complex is stable until the addition of the second substrate, HS-CoB. Results from EPR spectroscopy, along with quantum mechanical calculations, are used to characterize the electronic and geometric structure of this complex, which can be regarded as the first intermediate in the catalytic mechanism.
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