Literature DB >> 25461840

[FeFe]- and [NiFe]-hydrogenase diversity, mechanism, and maturation.

John W Peters1, Gerrit J Schut2, Eric S Boyd3, David W Mulder4, Eric M Shepard5, Joan B Broderick5, Paul W King4, Michael W W Adams2.   

Abstract

The [FeFe]- and [NiFe]-hydrogenases catalyze the formal interconversion between hydrogen and protons and electrons, possess characteristic non-protein ligands at their catalytic sites and thus share common mechanistic features. Despite the similarities between these two types of hydrogenases, they clearly have distinct evolutionary origins and likely emerged from different selective pressures. [FeFe]-hydrogenases are widely distributed in fermentative anaerobic microorganisms and likely evolved under selective pressure to couple hydrogen production to the recycling of electron carriers that accumulate during anaerobic metabolism. In contrast, many [NiFe]-hydrogenases catalyze hydrogen oxidation as part of energy metabolism and were likely key enzymes in early life and arguably represent the predecessors of modern respiratory metabolism. Although the reversible combination of protons and electrons to generate hydrogen gas is the simplest of chemical reactions, the [FeFe]- and [NiFe]-hydrogenases have distinct mechanisms and differ in the fundamental chemistry associated with proton transfer and control of electron flow that also help to define catalytic bias. A unifying feature of these enzymes is that hydrogen activation itself has been restricted to one solution involving diatomic ligands (carbon monoxide and cyanide) bound to an Fe ion. On the other hand, and quite remarkably, the biosynthetic mechanisms to produce these ligands are exclusive to each type of enzyme. Furthermore, these mechanisms represent two independent solutions to the formation of complex bioinorganic active sites for catalyzing the simplest of chemical reactions, reversible hydrogen oxidation. As such, the [FeFe]- and [NiFe]-hydrogenases are arguably the most profound case of convergent evolution. This article is part of a Special Issue entitled: Fe/S proteins: Analysis, structure, function, biogenesis and diseases.
Copyright © 2014 Elsevier B.V. All rights reserved.

Entities:  

Keywords:  Bifurcation; Carbon monoxide; Cyanide; Hydrogen oxidation; Iron-sulfur; Proton reduction

Mesh:

Substances:

Year:  2014        PMID: 25461840     DOI: 10.1016/j.bbamcr.2014.11.021

Source DB:  PubMed          Journal:  Biochim Biophys Acta        ISSN: 0006-3002


  108 in total

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Journal:  Proc Natl Acad Sci U S A       Date:  2018-06-18       Impact factor: 11.205

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Authors:  Ming-Hsi Chiang; Vladimir Pelmenschikov; Leland B Gee; Yu-Chiao Liu; Chang-Chih Hsieh; Hongxin Wang; Yoshitaka Yoda; Hiroaki Matsuura; Lei Li; Stephen P Cramer
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Authors:  Thomas D Mand; William W Metcalf
Journal:  Microbiol Mol Biol Rev       Date:  2019-09-18       Impact factor: 11.056

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Journal:  Inorg Chem       Date:  2017-05-18       Impact factor: 5.165

9.  Molecular Evidence for an Active Microbial Methane Cycle in Subsurface Serpentinite-Hosted Groundwaters in the Samail Ophiolite, Oman.

Authors:  Emily A Kraus; Daniel Nothaft; Blake W Stamps; Kaitlin R Rempfert; Eric T Ellison; Juerg M Matter; Alexis S Templeton; Eric S Boyd; John R Spear
Journal:  Appl Environ Microbiol       Date:  2021-01-04       Impact factor: 4.792

10.  Iron-Sulfur Cluster States of the Hydrogenase Maturase HydF.

Authors:  Eric M Shepard; Amanda S Byer; Joan B Broderick
Journal:  Biochemistry       Date:  2017-08-30       Impact factor: 3.162

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