Franchi Marco, Gallori Enzo
Department of Animal Biology and Genetics, University of Florence. Via Romana 17, 50125 Florence, Italy.
Gene. 2005 Feb 14;346:205-14. doi: 10.1016/j.gene.2004.11.002.
The involvement of clay surfaces in the origin of the first genetic molecules on Earth has long been suggested. However, the formation of these polymers was not sufficient by itself to initiate the evolutionary process leading to the appearance of life. These macromolecules had to persist in primeval habitats so that their biological potentiality could be expressed. In this study, we assess the possibility of development of the RNA world on a clay substrate by investigating the capacity of different RNA molecules adsorbed/bound on the clay minerals montmorillonite (M) and kaolinite (K) to persist in the presence of a degrading agent (RNase-A), to interact specifically with complementary RNA strands, and to transmit the information contained in their nucleotide sequences. The RNase-A degradation of clay-adsorbed 23S rRNA from Escherichia coli was significantly slower (75-80%) than that observed for free rRNA, and the complete digestion of nucleic acid in the presence of clay was obtained in 2 vs. 1 h. Clay-adsorbed Poly[A] homopolymer was able to recognize the complementary Poly[U] homopolymer present in the surrounding water solution and to establish a specific interaction (association) with it, possibly leading to the formation of double strands. Reverse transcription and amplification (RT-PCR) amplification of free and clay-adsorbed 16S indicated that the presence of clay particles partially reduced the efficiency and processivity of reverse transcriptase but did not inhibit its activity, demonstrating that clay-adsorbed RNA is still available for enzymatic replication. These findings indicate that primordial genetic molecules adsorbed on clay minerals would have been protected against degrading agents present in the environment and would have been in the right conditions to undergo evolutionary processes.
长期以来,人们一直认为黏土表面与地球上首批遗传分子的起源有关。然而,这些聚合物的形成本身并不足以启动导致生命出现的进化过程。这些大分子必须在原始栖息地中持续存在,以便其生物潜力能够得以表达。在本研究中,我们通过研究吸附/结合在黏土矿物蒙脱石(M)和高岭石(K)上的不同RNA分子在降解剂(核糖核酸酶A)存在的情况下持续存在的能力、与互补RNA链特异性相互作用的能力以及传递其核苷酸序列中所含信息的能力,来评估在黏土底物上发展RNA世界的可能性。来自大肠杆菌的黏土吸附23S rRNA的核糖核酸酶A降解明显比游离rRNA慢(75 - 80%),在有黏土存在的情况下,核酸在2小时内完全消化,而游离rRNA则需1小时。黏土吸附的聚腺苷酸均聚物能够识别周围水溶液中存在的互补聚尿苷酸均聚物,并与之建立特异性相互作用(缔合),这可能导致双链的形成。游离和黏土吸附的16S的逆转录和扩增(RT - PCR)表明,黏土颗粒的存在部分降低了逆转录酶的效率和持续合成能力,但并未抑制其活性,这表明黏土吸附的RNA仍可用于酶促复制。这些发现表明,吸附在黏土矿物上的原始遗传分子本可以免受环境中降解剂的破坏,并且处于适合经历进化过程的条件。