RESUMEN
The mechanism of the metal centered reduction of metmyoglobin (MbFeIII) by sulfide species (H2S/HS-) under an argon atmosphere has been studied by a combination of spectroscopic, kinetic, and computational methods. Asymmetric S-shaped time-traces for the formation of MbFeII at varying ratios of excess sulfide were observed at pH 5.3 < pH < 8.0 and 25 °C, suggesting an autocatalytic reaction mechanism. An increased rate at more alkaline pHs points to HS- as relevant reactive species for the reduction. The formation of the sulfanyl radical (HSâ¢) in the slow initial phase was assessed using the spin-trap phenyl N-tert-butyl nitrone. This radical initiates the formation of S-S reactive species as disulfanuidyl/ disulfanudi-idyl radical anions and disulfide (HSSHâ¢-/HSSâ¢2- and HSS-, respectively). The autocatalysis has been ascribed to HSS-, formed after HSSHâ¢-/HSSâ¢2- disproportionation, which behaves as a fast reductant toward the intermediate complex MbFeIII(HS-). We propose a reaction mechanism for the sulfide-mediated reduction of metmyoglobin where only ferric heme iron initiates the oxidation of sulfide species. Beside the chemical interest, this insight into the MbFeIII/sulfide reaction under an argon atmosphere is relevant for the interpretation of biochemical aspects of ectopic myoglobins found on hypoxic tissues toward reactive sulfur species.
Asunto(s)
Sulfuro de Hidrógeno , Metamioglobina , Metamioglobina/química , Anaerobiosis , Argón , Mioglobina/química , Oxidación-Reducción , Sulfuros , CinéticaRESUMEN
Cold-adapted organisms have evolved proteins endowed with higher flexibility and lower stability in comparison to their thermophilic homologues, resulting in enhanced reaction rates at low temperatures. In this context, protein-bound water molecules were suggested to play a major role, and their weaker interactions at protein active sites have been associated with cold adaptation. In this work, we tested this hypothesis on truncated hemoglobins (a family of microbial heme-proteins of yet-unclear function) applying molecular dynamics simulations and ligand-rebinding kinetics on a protein from the Antarctic bacterium Pseudoalteromonas haloplanktis TAC125 in comparison with its thermophilic Thermobifida fusca homologue. The CO rebinding kinetics of the former highlight several geminate phases, with an unusually long-lived geminate intermediate. An articulated tunnel with at least two distinct docking sites was identified by analysis of molecular dynamics simulations and was suggested to be at the origin of the unusual geminate rebinding phase. Water molecules are present in the distal pocket, but their stabilization by TrpG8, TyrB10, and HisCD1 is much weaker than in thermophilic Thermobifida fusca truncated hemoglobin, resulting in a faster geminate rebinding. Our results support the hypothesis that weaker water-molecule interactions at the reaction site are associated with cold adaptation.
Asunto(s)
Actinomycetales/química , Frío , Hemoglobinas/química , Pseudoalteromonas/química , Sitios de Unión , Hemoglobinas/aislamiento & purificación , Cinética , Ligandos , Simulación de Dinámica MolecularRESUMEN
The reaction of hydrogen sulfide (H2S) with hemeproteins is a key physiological reaction; still, its mechanism and implications are not completely understood. In this work, we propose a combination of experimental and theoretical tools to shed light on the reaction in model system microperoxidase 11 (MP11-FeIII) and myoglobin (Mb-FeIII), from the estimation of the intrinsic binding constants of the species H2S and hydrosulfide (HS-), and the computational description of the overall binding process. Our results show that H2S and HS- are the main reactive species in Mb-FeIII and MP11-FeIII, respectively, and that the magnitude of their intrinsic binding constants are similar to most of the binding constants reported so far for hemeproteins systems and model compounds. However, while the binding of HS- to Mb-FeIII was negligible, the binding of H2S to MP11-FeIII was significant, providing a frame for a discriminated analysis of both species and revealing differential mechanistic aspects. A joint inspection of the kinetic data and the free energy profiles of the binding processes suggests that a dissociative mechanism with the release of a coordinated water molecule as rate limiting step is operative in the binding of H2S to Mb-FeIII and that the binding of HS- is prevented in the access to the protein matrix. For the MP11-FeIII case, where no access restrictions for the ligands are present, an associative component in the mechanism seems to be operative. Overall, the results suggest that if accessing the active site then both H2S and HS- are capable of binding a ferric heme moiety.
Asunto(s)
Hemoproteínas/química , Hemoproteínas/metabolismo , Sulfuros/metabolismo , Concentración de Iones de Hidrógeno , Modelos Moleculares , Unión Proteica , Conformación ProteicaRESUMEN
Hydrogen sulfide (H2S) was recently discovered as a gasotransmitter, capable of coordinating to the heme iron of hemeproteins. H2S is unique for its ability to render varying concentrations of the nucleophilic conjugate bases (HS(-) or S(2-)), either as free or bound species with expected outcomes on its further reactivity. There is no direct evidence about which species (H2S, HS(-), or S(2-)) coordinates to the iron. We performed computer simulations to address the migration and binding processes of H2S species to the hemoglobin I of Lucina pectinata, which exhibits the highest affinity for the substrate measured to date. We found that H2S is the most favorable species in the migration from the bulk to the active site, through an internal pathway of the protein. After the coordination of H2S, an array of clustered water molecules modifies the active site environment, and assists in the subsequent deprotonation of the ligand, forming Fe(III)-SH(-). The feasibility of the second deprotonation of the coordinated ligand is also discussed.