Exploring Mechanisms of Biotic Chlorinated Alkane Reduction: Evidence of Nucleophilic Substitution (S2) with Vitamin B.

Chlorinated alkanes are notorious groundwater contaminants. Their natural reductive dechlorination by microorganisms involves reductive dehalogenases (RDases) containing cobamide as a cofactor. However, underlying mechanisms of reductive dehalogenation have remained uncertain. Here, observed products, radical trap experiments, UV-vis, and mass spectra demonstrate that (i) reduction by cobalamin (vitamin B) involved chloroalkyl-cobalamin complexes (ii) whose formation involved a second-order nucleophilic substitution (S2). Dual element isotope analysis subsequently linked insights from our model system to microbial reductive dehalogenation. Identical observed isotope effects in reduction of trichloromethane by CF and cobalamin ( CF, ε = -27.9 ± 1.7‰; ε = -4.2 ± 0.‰; λ = 6.6 ± 0.1; cobalamin, ε = -26.0 ± 0.9‰; ε = -4.0 ± 0.2‰; λ = 6.5 ± 0.2) indicated the same underlying mechanism, as did identical isotope effects in the reduction of 1,2-dichloroethane by and cobalamin (, ε = -33.0 ± 0.4‰; ε = -5.1 ± 0.1‰; λ = 6.5 ± 0.2; cobalamin, ε = -32.8 ± 1.7‰; ε = -5.1 ± 0.2‰; λ = 6.4 ± 0.2). In contrast, a different, non-S2 reaction was evidenced by different isotope effects in reaction of 1,2-dichloroethane with (ε = -23.0 ± 2.0‰; ε = -12.0 ± 0.8‰; λ = 1.9 ± 0.02) illustrating a diversity of biochemical reaction mechanisms manifested even within the same class of enzymes (RDases). This study resolves open questions in our understanding of bacterial reductive dehalogenation and, thereby, provides important information on the biochemistry of bioremediation.