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RNA’s tendency to break down is a serious challenge for the RNA-world hypothesis, but it is not by itself a disproof. The key question is whether early environments could form, concentrate, protect and copy RNA quickly enough for useful molecules to persist. RNA’s present-day roles show that it can carry information and help catalyze reactions; they do not establish how the first RNA-based system arose.
What “RNA instability” means
RNA is hydrolytically unstable: water can break chemical bonds in its sugar-phosphate backbone, shortening or destroying a strand. Chemical reactions that alter its bases can also change the information it carries. These are related but distinct problems. A strand might remain intact while a base changes, or its backbone might break before its sequence is copied.
How quickly degradation happens depends on conditions such as temperature and pH. A lifetime measured in one laboratory environment therefore cannot be treated as a universal lifetime for RNA on the early Earth. The relevant origin-of-life question is whether a particular setting could let formation and copying compete with degradation.
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What the recent lifetime estimates do—and do not—show
In a 2026 critical reassessment, Royal J. Truman reports an estimated ribose half-life of about 300 days at 25°C and an RNA phosphodiester-bond half-life of about four years under the paper’s referenced conditions. From the per-bond estimate, the paper argues that a 1,000-nucleotide strand would have a half-life of roughly 1.5 days.
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That strand figure is an extrapolation based on the paper’s assumptions, not an established lifetime for every long RNA molecule or every plausible prebiotic environment. The estimates are the reassessment’s analysis, not a settled field-wide value; the short-strand lifetime should be read as an argument about how cumulative bond-breaking could matter, rather than a universal clock for the RNA world.
Why base damage is a separate issue
RNA’s bases do not all have the same stability. A 1998 PNAS study considered cytosine hydrolysis to uracil and reported a cytosine hydrolysis rate constant of 4.1 × 10⁻⁵ yr⁻¹ at 0°C in its steady-state model. That number concerns a particular base-conversion process under the model’s conditions. It is not a measured half-life for intact RNA, nor does it tell us how long an RNA strand would survive in a prebiotic setting.
How proposed early environments might help
Reviews discuss several settings that could alter the balance among degradation, concentration, polymer formation and copying. These are possible mechanisms, not demonstrated end-to-end solutions: no single setting in the available evidence establishes that RNA could form, persist and replicate as a self-sustaining system.
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|---|---|---|
| Mineral surfaces | Could retain or concentrate molecules and provide a surface on which reactions occur. | How well the setting supports polymerization, protects strands from hydrolysis and enables copying together is not established here. |
| Evaporating ponds and wet-dry cycling | Drying could concentrate building blocks; cycling could alternate conditions relevant to reactions and strand use. | The balance between useful concentration or polymer formation and damage during repeated cycles remains uncertain. |
| Freezing-thawing compartments | Freezing could concentrate solutes in remaining liquid regions, potentially changing reaction conditions and persistence. | A complete route from concentrated ingredients to sustained template copying has not been demonstrated. |
| Thermal gradients and other non-equilibrium settings | Differences across space or time could create varied conditions for reactions, strand separation or concentration. | The available reviews treat these as candidate models, not as a quantitatively ranked or proven resolution to instability. |
The comparison is qualitative: the cited reviews identify possible effects and research settings, but do not provide a like-for-like quantitative ranking of their ability to support prebiotic RNA copying.
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Could another genetic polymer have come first?
Concerns about RNA synthesis and persistence have motivated proposals for an earlier genetic polymer that later gave way to RNA. Suggested candidates include TNA, PNA and pyranosyl-RNA. These proposals explore whether a different chemistry might have been easier to form or more stable under some conditions; naming a candidate is not evidence that it was the historical precursor.
An IUPAC review by S. G. Srivatsan (2004) notes that the difficulty of explaining de novo nucleic-acid synthesis and RNA’s hydrolytic instability has prompted serious discussion of biopolymers resembling nucleic acids preceding the RNA world. That is a statement of an open scientific question, not proof that such a precursor existed.
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What instability means for the RNA-world hypothesis
The hypothesis is not simply that modern RNA can function. RNA’s genetic and catalytic roles—including catalysis by ribosomal RNA—make an RNA-based stage chemically plausible as a concept. But demonstrating what RNA can do now does not reconstruct the prebiotic sequence that produced it or show that an early RNA system could sustain itself.
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Instability therefore sharpens the origin problem: a viable account must explain not only how RNA’s components and strands formed, but also how strands persisted long enough to copy and evolve despite hydrolysis and other damage. Neither “RNA was impossible” nor “environmental cycling solved the problem” follows from the evidence described here.
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