School of Chemical Sciences, University of Illinois, 600 S Mathews Ave., MC-712, Box 68-6, Urbana, IL 61801, USA.
Orig Life Evol Biosph. 2010 Jun;40(3):303-17. doi: 10.1007/s11084-010-9207-0. Epub 2010 Mar 7.
We investigate a proposed origins of life scenario involving the clay montmorillonite and its catalytic role in forming oligonucleotides from activated mononucleotides. Clay and mineral surfaces are important for concentrating the reactants and for promoting nucleotide polymerization reactions. Using classical molecular dynamics methods we provide atomic details of reactant conformations prior to polynucleotide formation, lending insight into previously reported experimental observations of this phenomenon. The simulations clarify the catalytic role of metal ions, demonstrate that reactions leading to correct linkages take place primarily in the interlayer, and explain the observed sequence selectivity in the elongation of the chain. The study comparing reaction probabilities involving L- and D-chiral forms of the reactants has found enhancement of homochiral over heterochiral products when catalyzed by montmorillonite.
我们研究了一个涉及粘土蒙脱石及其在激活单核苷酸形成寡核苷酸中的催化作用的生命起源假设场景。粘土和矿物表面对于反应物的浓缩和促进核苷酸聚合反应很重要。使用经典的分子动力学方法,我们提供了多核苷酸形成前反应物构象的原子细节,深入了解了先前报道的这一现象的实验观察结果。模拟结果阐明了金属离子的催化作用,表明导致正确键合的反应主要发生在层间,并且解释了在链延伸过程中观察到的序列选择性。比较涉及反应物 L-和 D-手性形式的反应概率的研究发现,当由蒙脱石催化时,同手性产物相对于异手性产物的增强。