Atmospheric Supply of Hydrogen Cyanide Is Not the Rate-limiting Step for Prebiotic Chemistry across Rocky Exoplanets
Gergely Friss, Paul I. Palmer, Marrick Braam, Ken Rice

TL;DR
This study models atmospheric hydrogen cyanide (HCN) delivery to early Earth-like planets, finding it is generally abundant and not the limiting factor for prebiotic chemistry, thus increasing prospects for life elsewhere.
Contribution
It demonstrates that atmospheric HCN supply is robust across various conditions and unlikely to limit prebiotic chemistry on rocky exoplanets.
Findings
Atmospheric HCN delivery exceeds meteoritic sources in baseline conditions.
Higher C/O ratios and closer orbiting M-dwarfs increase atmospheric HCN delivery.
HCN delivery is not the rate-limiting step for prebiotic chemistry on rocky exoplanets.
Abstract
Hydrogen cyanide (HCN) is crucial for the RNA World hypothesis, forming biomolecules essential for early life. Life likely emerged around 4 billion years ago during the early Archean Eon, a period on Earth with a fainter sun, frequent impacts, and a weakly reducing atmosphere. Warm little ponds (WLPs) are hypothetical protective aqueous environments that help explain the emergence and evolution of fragile prebiotic chemistry in such a hostile environment. WLPs need to undergo cycles of evaporation and rehydration, concentrating prebiotic molecules that increase the likelihood of (de-)polymerisation and forming early RNA molecules. We use a 1-D model of atmospheric chemistry to compare atmospheric HCN delivery to WLPs with exogenous sources. Using early Archean Earth as our baseline, we examine the sensitivity of atmospheric HCN delivery to the atmospheric C/O ratio, semi-major axis,…
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