Schlikker Manon Laura, Brabender Max, Schwander Loraine, Garcia Garcia Carolina, Burmeister Maximillian, Metzger Sabine, Moran Joseph, Martin William F
Institute of Molecular Evolution, Heinrich Heine University Düsseldorf, Germany.
Institut de Science et d'Ingénierie, Supramoléculaires (ISIS), CNRS UMR 7006, Université de Strasbourg, France.
FEBS J. 2024 Dec 19. doi: 10.1111/febs.17357.
Serpentinizing hydrothermal vents are likely sites for the origin of metabolism because they produce H as a source of electrons for CO reduction while depositing zero-valent iron, cobalt, and nickel as catalysts for organic reactions. Recent work has shown that solid-state nickel can catalyze the H-dependent reduction of CO to various organic acids and their reductive amination with H and NH to biological amino acids under the conditions of H-producing hydrothermal vents and that amino acid synthesis from NH, H, and 2-oxoacids is facile in the presence of Ni. Such reactions suggest a metallic origin of metabolism during early biochemical evolution because single metals replace the function of over 130 enzymatic reactions at the core of metabolism in microbes that use the acetyl-CoA pathway of CO fixation. Yet solid-state catalysts tether primordial amino synthesis to a mineral surface. Many studies have shown that pyridoxal catalyzes transamination reactions without enzymes. Here we show that pyridoxamine, the NH-transferring intermediate in pyridoxal-dependent transamination reactions, is generated from pyridoxal by reaction with NH (as little as 5 mm) and H (5 bar) on Ni as catalyst at pH 11 and 80 °C within hours. These conditions correspond to those in hydrothermal vents undergoing active serpentinization. The results indicate that at the origin of metabolism, pyridoxamine provided a soluble, organic amino donor for aqueous amino acid synthesis, mediating an evolutionary transition from NH-dependent amino acid synthesis on inorganic surfaces to pyridoxamine-dependent organic reactions in the aqueous phase.
蛇纹石化热液喷口可能是新陈代谢起源的场所,因为它们产生氢气作为还原二氧化碳的电子来源,同时沉积零价铁、钴和镍作为有机反应的催化剂。最近的研究表明,在产生氢气的热液喷口条件下,固态镍可以催化氢气依赖的二氧化碳还原为各种有机酸,并将其与氢气和氨气还原胺化生成生物氨基酸,并且在镍存在的情况下,由氨气、氢气和2-氧代酸合成氨基酸很容易。这些反应表明在早期生化进化过程中新陈代谢起源于金属,因为单一金属取代了利用乙酰辅酶A固定二氧化碳途径的微生物中130多种核心代谢酶促反应的功能。然而,固态催化剂将原始氨基酸合成与矿物表面联系在一起。许多研究表明,吡哆醛可以在没有酶的情况下催化转氨反应。在这里我们表明,吡哆胺是吡哆醛依赖的转氨反应中转移氨基的中间体,在pH值为11、80℃的条件下,以镍为催化剂,与氨气(低至5毫米)和氢气(5巴)反应,数小时内即可由吡哆醛生成。这些条件与正在进行活跃蛇纹石化的热液喷口的条件相符。结果表明,在新陈代谢起源时,吡哆胺为水相氨基酸合成提供了一种可溶性有机氨基供体,介导了从无机表面上依赖氨气的氨基酸合成到水相中依赖吡哆胺的有机反应的进化转变。