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The Autotrophic Core: An Ancient Network of 404 Reactions Converts H2, CO2, and NH3 into Amino Acids, Bases, and Cofactors.
Wimmer, Jessica L E; Vieira, Andrey do Nascimento; Xavier, Joana C; Kleinermanns, Karl; Martin, William F; Preiner, Martina.
Afiliação
  • Wimmer JLE; Department of Biology, Institute for Molecular Evolution, Heinrich-Heine-University of Düsseldorf, 40225 Düsseldorf, Germany.
  • Vieira ADN; Department of Biology, Institute for Molecular Evolution, Heinrich-Heine-University of Düsseldorf, 40225 Düsseldorf, Germany.
  • Xavier JC; Department of Biology, Institute for Molecular Evolution, Heinrich-Heine-University of Düsseldorf, 40225 Düsseldorf, Germany.
  • Kleinermanns K; Department of Chemistry, Institute for Physical Chemistry, Heinrich-Heine-University of Düsseldorf, 40225 Düsseldorf, Germany.
  • Martin WF; Department of Biology, Institute for Molecular Evolution, Heinrich-Heine-University of Düsseldorf, 40225 Düsseldorf, Germany.
  • Preiner M; Department of Biology, Institute for Molecular Evolution, Heinrich-Heine-University of Düsseldorf, 40225 Düsseldorf, Germany.
Microorganisms ; 9(2)2021 Feb 23.
Article em En | MEDLINE | ID: mdl-33672143
ABSTRACT
The metabolism of cells contains evidence reflecting the process by which they arose. Here, we have identified the ancient core of autotrophic metabolism encompassing 404 reactions that comprise the reaction network from H2, CO2, and ammonia (NH3) to amino acids, nucleic acid monomers, and the 19 cofactors required for their synthesis. Water is the most common reactant in the autotrophic core, indicating that the core arose in an aqueous environment. Seventy-seven core reactions involve the hydrolysis of high-energy phosphate bonds, furthermore suggesting the presence of a non-enzymatic and highly exergonic chemical reaction capable of continuously synthesizing activated phosphate bonds. CO2 is the most common carbon-containing compound in the core. An abundance of NADH and NADPH-dependent redox reactions in the autotrophic core, the central role of CO2, and the circumstance that the core's main products are far more reduced than CO2 indicate that the core arose in a highly reducing environment. The chemical reactions of the autotrophic core suggest that it arose from H2, inorganic carbon, and NH3 in an aqueous environment marked by highly reducing and continuously far from equilibrium conditions. Such conditions are very similar to those found in serpentinizing hydrothermal systems.
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Texto completo: 1 Base de dados: MEDLINE Idioma: En Ano de publicação: 2021 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Idioma: En Ano de publicação: 2021 Tipo de documento: Article