4.5 Review

The role of geochemistry and energetics in the evolution of modern respiratory complexes from a proton-reducing ancestor

Journal

BIOCHIMICA ET BIOPHYSICA ACTA-BIOENERGETICS
Volume 1857, Issue 7, Pages 958-970

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.bbabio.2016.01.010

Keywords

Complex I; Hydrogenase; Membrane complexes; Ion pumping; Archaea; Sulfur; Methanogens

Funding

  1. Biological and Electron Transfer and Catalysis EFRC, an Energy Frontiers Research Center - U.S. Department of Energy, Office of Science [DE-SC0012518]
  2. U.S. Department of Energy, Division of Chemical Sciences, Geosciences, and Biosciences, Office of Basic Energy Sciences [DE-FG05-95ER20175]

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Complex I or NADH quinone oxidoreductase (NUO) is an integral component of modern day respiratory chains and has a close evolutionary relationship with energy-conserving [NiFe]-hydrogenases of anaerobic microorganisms. Specifically, in all of biology, the quinone-binding subunit of Complex I, NuoD, is most closely related to the proton-reducing, H-2-evolving [NiFe]-containing catalytic subunit, MbhL, of membrane-bound hydrogenase (MBH), to the methanophenzine-reducing subunit of a methanogenic respiratory complex (FPO) and to the catalytic subunit of an archaeal respiratory complex (MBX) involved in reducing elemental sulfur (S degrees). These complexes also pump ions and have at least 10 homologous subunits in common. As electron donors, MBH and MBX use ferredoxin (Fd), FPO uses either Fd or cofactor F-420, and NUO uses either Fd or NADH. In this review, we examine the evolutionary trajectory of these oxidoreductases from a proton-reducing ancestral respiratory complex (ARC). We hypothesize that the diversification of ARC to MBH, MBX, FPO and eventually NUO was driven by the larger energy yields associated with coupling Fd oxidation to the reduction of oxidants with increasing electrochemical potential, including protons, S degrees and membrane soluble organic compounds such as phenazines and quinone derivatives. Importantly, throughout Earth's history, the availability of these oxidants increased as the redox state of the atmosphere and oceans became progressively more oxidized as a result of the origin and ecological expansion of oxygenic photosynthesis. ARC-derived complexes are therefore remarkably stable respiratory systems with little diversity in core structure but whose general function appears to have co-evolved with the redox state of the biosphere. This article is part of a Special Issue entitled Respiratory Complex I, edited by Volker Zickermann and Ulrich Brandt. (C) 2016 Elsevier B.V. All rights reserved.

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