<div>Outstanding questions about the RNA world hypothesis for the emergence of life</div><div>on Earth concern the stability and self-replication of prebiotic aqueous RNA.</div><div>Recent experimental work has suggested that solid substrates and low</div><div>temperatures could help resolve these issues. Here, we use classical molecular</div><div>dynamics simulations to explore the possibility that the substrate is ice itself. We</div><div>find that at -20 C, a quasi-liquid layer at the air/ice interface solvates a short (8-</div><div>nucleotide) RNA strand such that phosphate groups tend to anchor to specific</div><div>points of the underlying crystal lattice, lengthening the strand. Hydrophobic bases,</div><div>meanwhile, tend to migrate to the air/ice interface. Further, contacts between</div><div>solvent water and ribose 2-OH’ groups are found to occur less frequently for RNA</div><div>on ice than for aqueous RNA at the same temperature; this reduces the likelihood</div><div>of deprotonation of the 2-OH’ and its subsequent nucleophilic attack on the</div><div>phosphate diester. The implied enhanced resistance to hydrolysis, in turn, could</div><div>increase opportunities for polymerization and self-copying. These findings thus</div><div>offer the possibility of a role for an ancient RNA world on ice distinct from that</div><div>considered in extant elaborations of the RNA world hypothesis. This work is, to the</div><div>best of our knowledge, the first molecular dynamics study of RNA on ice</div>