Adenosine triphosphate (ATP) is a multifunctional small molecule, necessary for all modern Earth life, which must be a component of the last universal common ancestor (LUCA). However, the relatively complex structure of ATP causes doubts about its accessibility on prebiotic Earth. In this paper, based on previous studies on the synthesis of ATP components, a plausible prebiotic pathway yielding this key molecule is constructed, which relies on terrestrial volcanism to provide the required materials and suitable conditions.

How the ribonucleic acid (RNA) world transited to the deoxyribonucleic acid (DNA) world has remained controversial in evolutionary biology. At a certain time point in the transition from the RNA world to the DNA world, \'RNA replicons\', in which RNAs produce proteins to replicate their coding RNA, and \'DNA replicons\', in which DNAs produce RNA to synthesize proteins that replicate their coding DNA, can be assumed to coexist. The coexistent state of RNA replicons and DNA replicons is desired for experimental approaches to determine how the DNA world overtook the RNA world. We constructed a mini-RNA replicon in Escherichia coli. This mini-RNA replicon encoded the β subunit, one of the subunits of the Qβ replicase derived from the positive-sense single-stranded Qβ RNA phage and is replicated by the replicase in E. coli. To maintain the mini-RNA replicon persistently in E. coli cells, we employed a system of α complementation of LacZ that was dependent on the Qβ replicase, allowing the cells carrying the RNA replicon to grow in the lactose minimal medium selectively. The coexistent state of the mini-RNA replicon and DNA replicon (E. coli genome) was successively synthesized. The coexistent state can be used as a starting system to experimentally demonstrate the transition from the RNA-protein world to the DNA world, which will contribute to progress in the research field of the origin of life.

We report a prebiotically relevant solution to the N1-ribosylation of pyrimidine nucleobases, a well-known challenge to the RNA world hypothesis. We found that the presence of metal cations and clay minerals enable the previously unachievable direct ribosylation of uracil. Spectroscopy and chromatography analyses confirmed the formation of ribosylated uracil. The method can be extended to the ribosylation of 2-pyrimidinone. These findings are also compatible with the metal-doped-clay model, developed by our lab for the unified route of the selection of ribose and subsequent syntheses of nucleotide and RNA.

Homochirality is a feature of life, but its origin is still disputed. Recent theories indicate that the origin of homochirality coincided with that of the RNA world, but proteins have not yet been incorporated into the story. Ribosome is considered a living fossil that survived the RNA world and records the oldest interaction between RNA and proteins. Inspired by several ribosome-related findings, we propose a hypothesis as follows: the substrate chirality preference of some primitive peptide synthesis ribozymes can mediate the chirality transmission from RNA to protein. In return, the chiral preference of protective peptide-RNA interaction can bring these ribozymes an evolutionary advantage and facilitate the expansion of enantiomeric excess in peptides. Monte Carlo simulation results show that this system\'s chemistry model is plausible. This model can be further tested through investigation of the chirality preference for the interactions between d/l-ribose-composed rRNA homologs and l/d-amino acid-composed peptides.

The origin of life is a field full of controversies, not only because of our vague understanding concerning the relevant issues, but also, perhaps more often, owing to our dim conceptual framework throughout the whole field. To improve this situation, an in-depth conceptual dissection is presented here. It is elucidated that, at its core, the origin of life has three aspects. The facts involved in the process are taken as the historical aspect, which is destined to be uncertain and often irrelevant to debate regarding details. The rules involved include two distinct aspects: chemical mechanisms operated in the whole process, while evolutionary mechanisms joined in only after the emergence of the first Darwinian entities - and then accounted for the subsequent buildup of complexity (this cannot be explained solely by natural selection). Basically, we can ask about the possibility of any assumed event in the origin of life: \'Is it evolutionarily plausible, chemically feasible, and historically likely?\' Clues from any of the three aspects may be quite valuable in directing our explorations on the other two. This conceptual dissection provides a clearer context for the field, which may even be more useful than any sort of specific research.