A Plausible Prebiotic Path to Nucleosides: Ribosides and Related Aldosides Generated from Ribulose, Fructose, and Similar Abiotic Precursors

Abiotic formation of hexoses and disaccharides in aqueous microdroplets

Understanding the chemical reactions that led to the origin of life is a fundamental challenge of chemistry. The formose reaction, an abiotic pathway to monosaccharides, provides a mechanism of sugar formation from simple aldehydes and ketones. However, the reaction requires the addition of base, metal catalysts, and is prone to side reactions, leaving questions about how such processes could have occurred on a primitive Earth. The abiotic formation of more complex sugars, such as disaccharides also require catalysts, and remains underexplored compared to other classes of biomolecules. This study investigates the role of microdroplets in the formation of hexoses and their subsequent condensation reactions to produce disaccharides, without the need for catalysts. The microdroplet-mediated synthesis of fructose and sorbose from glyceraldehyde or dihydroxyacetone, as well as that of disaccharides from various pentoses or hexoses, was monitored via mass spectrometery. Products were confirmed by high resolution mass spectrometry and tandem mass spectrometry. The product distribution of glucose disaccharides was determined by matching the relative intensities of product ions to a mixture of six disaccharide and showed a maximum yield of 9.4% or 1.7 µg min-1 emitter. This study demonstrates the abiotic formation of monosaccharides and disaccharides, such as xylobiose and maltose, providing a possible link between prebiotic sugar synthesis and extant carbohydrate biochemistry. Hexose formation and disaccharide synthesis are driven by the unique air water interface of microdroplets, where partial solvation, pH extremes, and fast mass transfer kinetics enable abiotic transformations.

Molecular Modeling on Duplexes with Threose-Based TNA and TPhoNA Reveals Structural Basis for Different Hybridization Affinity toward Complementary Natural Nucleic Acids

Synthetic nucleic acids, also defined as xenobiotic nucleic acids (XNAs), opened an avenue to address the limitations of nucleic acid therapeutics and the development of alternative carriers for genetic information in biotechnological applications. Two related XNA systems of high interest are the α-l-threose nucleic acid (TNA) and (3'-2') phosphonomethyl threosyl nucleic acid (tPhoNA), where TNAs show potential in antisense applications, whereas tPhoNAs are investigated for their predisposition toward orthogonal genetic systems. We present predictions on helical models of TNA and tPhoNA chemistry in homoduplexes and in complex with native ribose chemistries. A stretched right-handed helical structure with a sugar puckering preference for the 4'3'T (C3'- endo/C4'- exo) and O4'1'T (C1'- endo/O4'- exo) is found for the in silico model of dsTNA, while for the in silico model of dstPhoNA a B-type structure is found with a sugar puckering preference for O4'1'T (C1'- endo/O4'- exo). Simulations with complementary DNA and RNA provided insight into the distinct pairing capabilities of TNA and tPhoNA.

Emergent ribozyme behaviors in oxychlorine brines indicate a unique niche for molecular evolution on Mars

Mars is a particularly attractive candidate among known astronomical objects to potentially host life. Results from space exploration missions have provided insights into Martian geochemistry that indicate oxychlorine species, particularly perchlorate, are ubiquitous features of the Martian geochemical landscape. Perchlorate presents potential obstacles for known forms of life due to its toxicity. However, it can also provide potential benefits, such as producing brines by deliquescence, like those thought to exist on present-day Mars. Here we show perchlorate brines support folding and catalysis of functional RNAs, while inactivating representative protein enzymes. Additionally, we show perchlorate and other oxychlorine species enable ribozyme functions, including homeostasis-like regulatory behavior and ribozyme-catalyzed chlorination of organic molecules. We suggest nucleic acids are uniquely well-suited to hypersaline Martian environments. Furthermore, Martian near- or subsurface oxychlorine brines, and brines found in potential lifeforms, could provide a unique niche for biomolecular evolution.

Abiotic Ribose Synthesis Under Aqueous Environments with Various Chemical Conditions

Ribose is the defining sugar in ribonucleic acid (RNA), which is often proposed to have carried the genetic information and catalyzed the biological reactions of the first life on Earth. Thus, abiological processes that yield ribose under prebiotic conditions have been studied for decades. However, aqueous environments required for the formation of ribose from materials available in quantity under geologically reasonable models, where the ribose formed is not immediately destroyed, remain unclear. This is due in large part to the challenge of analysis of carbohydrates formed under a wide range of aqueous conditions. Thus, the formation of ribose on prebiotic Earth has sometimes been questioned. We investigated the quantitative effects of pH, temperature, cation, and the concentrations of formaldehyde and glycolaldehyde on the synthesis of diverse sugars, including ribose. The results suggest a range of conditions that produce ribose and that ribose could have formed in constrained aquifers on prebiotic Earth.

Chapter 4: A Geological and Chemical Context for the Origins of Life on Early Earth

Within the first billion years of Earth's history, the planet transformed from a hot, barren, and inhospitable landscape to an environment conducive to the emergence and persistence of life. This chapter will review the state of knowledge concerning early Earth's (Hadean/Eoarchean) geochemical environment, including the origin and composition of the planet's moon, crust, oceans, atmosphere, and organic content. It will also discuss abiotic geochemical cycling of the CHONPS elements and how these species could have been converted to biologically relevant building blocks, polymers, and chemical networks. Proposed environments for abiogenesis events are also described and evaluated. An understanding of the geochemical processes under which life may have emerged can better inform our assessment of the habitability of other worlds, the potential complexity that abiotic chemistry can achieve (which has implications for putative biosignatures), and the possibility for biochemistries that are vastly different from those on Earth.

One-Pot Formation of Pairing Proto-RNA Nucleotides and Their Supramolecular Assemblies

Most contemporary theories for the chemical origins of life include the prebiotic synthesis of informational polymers, including strong interpretations of the RNA World hypothesis. Existing challenges to the prebiotic emergence of RNA have encouraged exploration of the possibility that RNA was preceded by an ancestral informational polymer, or proto-RNA, that formed more easily on the early Earth. We have proposed that the proto-nucleobases of proto-RNA would have readily formed glycosides with ribose and that these proto-nucleosides would have formed base pairs as monomers in aqueous solution, two properties not exhibited by the extant nucleosides or nucleotides. Here we demonstrate that putative proto-nucleotides of the model proto-nucleobases barbituric acid and melamine can be formed in the same one-pot reaction with ribose-5-phosphate. Additionally, the proto-nucleotides formed in these reactions spontaneously form assemblies that are consistent with the presence of Watson-Crick-like base pairs. Together, these results provide further support for the possibility that heterocycles closely related to the extant bases of RNA facilitated the prebiotic emergence of RNA-like molecules, which were eventually replaced by RNA over the course of chemical and biological evolution.