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Didehydroaspartate Modification in Methyl-CoenzymeM Reductase Catalyzing Methane Formation

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Wagner,  T.
Department-Independent Research Group Microbial Protein Structure, Max Planck Institute for Terrestrial Microbiology, Max Planck Society;

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Kahnt,  J.
Department of Ecophysiology, Max Planck Institute for Terrestrial Microbiology, Max Planck Society;

Ermler,  U.
Max Planck Society;

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Shima,  S.
Department-Independent Research Group Microbial Protein Structure, Max Planck Institute for Terrestrial Microbiology, Max Planck Society;

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Citation

Wagner, T., Kahnt, J., Ermler, U., & Shima, S. (2016). Didehydroaspartate Modification in Methyl-CoenzymeM Reductase Catalyzing Methane Formation. Angewandte Chemie-International Edition, 55(36), 10630-10633. doi:10.1002/anie.201603882.


Cite as: https://hdl.handle.net/21.11116/0000-0007-BBD3-8
Abstract
All methanogenic and methanotrophic archaea known to date contain methyl-coenzyme M reductase (MCR) that catalyzes the reversible reduction of methyl-coenzyme M to methane. This enzyme contains the nickel porphinoid F430 as a prosthetic group and, highly conserved, a thioglycine and four methylated amino acid residues near the active site. We describe herein the presence of a novel post-translationally modified amino acid, didehydroaspartate, adjacent to the thioglycine as revealed by mass spectrometry and high-resolution X-ray crystallography. Upon chemical reduction, the didehydroaspartate residue was converted into aspartate. Didehydroaspartate was found in MCR I and II from Methanothermobacter marburgensis and in MCR of phylogenetically distantly related Methanosarcina barkeri but not in MCR I and II of Methanothermobacter wolfeii, which indicates that didehydroaspartate is dispensable but might have a role in fine-tuning the active site to increase the catalytic efficiency.