Iron-Mediated Peptide Formation in Water and Liquid Sulfur Dioxide under Prebiotically Plausible Conditions**

IF 3.1 Q2 CHEMISTRY, MULTIDISCIPLINARY
Constanze Sydow, Dr. Fabian Sauer, Dr. Alexander F. Siegle, Prof. Dr. Oliver Trapp
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Abstract

Peptides have essential structural and catalytic functions in living organisms. The formation of peptides requires the overcoming of thermodynamic and kinetic barriers. In recent years, various formation scenarios that may have occurred during the origin of life have been investigated, including iron(III)-catalyzed condensations. However, iron(III)-catalysts require elevated temperatures and the catalytic activity in peptide bond forming reactions is often low. It is likely that in an anoxic environment such as that of the early Earth, reduced iron compounds were abundant, both on the Earth's surface itself and as a major component of iron meteorites. In this work, we show that reduced iron activated by acetic acid mediates efficiently peptide formation. We recently demonstrated that, compared to water, liquid sulfur dioxide (SO2) is a superior reaction medium for peptide formations. We thus investigated both and observed up to four amino acid/peptide coupling steps in each solvent. Reaction with diglycine (G2) formed 2.0 % triglycine (G3) and 7.6 % tetraglycine (G4) in 21 d. Addition of G3 and dialanine (A2) yielded 8.7 % G4. Therefore, this is an efficient and plausible route for the formation of the first peptides as simple catalysts for further transformations in such environments.

Abstract Image

益生元条件下水和液体二氧化硫中铁介导的肽形成
多肽在生物体中具有重要的结构和催化功能。多肽的形成需要克服热力学和动力学障碍。近年来,人们对生命起源期间可能发生的各种形成情景进行了研究,其中包括铁(III)催化凝聚。然而,铁(III)-催化剂需要较高的温度,并且在肽键形成反应中的催化活性通常较低。很可能在像地球早期那样的缺氧环境中,还原铁化合物丰富,无论是在地球表面还是作为铁陨石的主要成分。在这项工作中,我们证明了乙酸激活的还原铁有效地介导了肽的形成。我们最近证明,与水相比,液体二氧化硫(SO2)是生成肽的优越反应介质。因此,我们研究了这两个和观察到多达四个氨基酸/肽偶联步骤在每个溶剂。与二甘氨酸(G2)反应21 d,生成2.0%的三甘氨酸(G3)和7.6%的四甘氨酸(G4)。加入G3和二丙氨酸(A2),生成8.7%的G4。因此,这是一个有效和合理的途径,形成第一个多肽作为进一步转化的简单催化剂在这种环境中。
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CiteScore
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