Dipartimento di Scienze Ecologiche e Biologiche, Università della Tuscia, Via San Camillo De Lellis, 01100, Viterbo, Italy.
Laboratorio de Estudios Cristalográficos, Instituto Andaluz de Ciencias de la Tierra, CSIC-Universidad de Granada, Av. De las Palmeras 4, Armilla, Granada, Spain.
Chemistry. 2019 Mar 1;25(13):3181-3189. doi: 10.1002/chem.201803889. Epub 2018 Dec 27.
The condensation of formamide has been shown to be a robust chemical pathway affording molecules necessary for the origin of life. It has been experimentally demonstrated that condensation reactions of formamide are catalyzed by a number of minerals, including silicates, phosphates, sulfides, zirconia, and borates, and by cosmic dusts and meteorites. However, a critical discussion of the catalytic power of the tested minerals, and the geochemical conditions under which the condensation would occur, is still missing. We show here that mineral self-assembled structures forming under alkaline silica-rich solutions are excellent catalysts for the condensation of formamide with respect to other minerals. We also propose that these structures were likely forming as early as 4.4 billion years ago when the whole earth surface was a reactor, a global scale factory, releasing large amounts of organic compounds. Our experimental results suggest that the conditions required for the synthesis of the molecular bricks from which life self-assembles, rather than being local and bizarre, appears to be universal and geologically rather conventional.
甲酰胺的缩合已被证明是一种稳健的化学途径,可提供生命起源所需的分子。实验已经证明,甲酰胺的缩合反应是由许多矿物质,包括硅酸盐、磷酸盐、硫化物、氧化锆和硼酸盐,以及宇宙尘埃和陨石催化的。然而,对于测试的矿物质的催化能力,以及缩合发生的地球化学条件,仍然存在着关键性的讨论。我们在这里表明,在碱性富硅溶液中形成的矿物自组装结构是甲酰胺缩合的优良催化剂,相对于其他矿物质而言。我们还提出,这些结构可能早在 44 亿年前就已经形成,当时整个地球表面都是一个反应堆,一个全球性的工厂,释放出大量的有机化合物。我们的实验结果表明,生命自组装所需的分子积木的合成条件,不是局部的和奇特的,而是普遍的,在地质上相当常规。