From Anoxic to Oxic Earth: Detectability of Atmospheric Biosignatures across Stellar Hosts with ELT/ANDES
arXiv:2610.41621
Abstract
Earth's atmosphere evolved from an anoxic, methane-bearing Archean state through Proterozoic oxygenation to the O-rich modern atmosphere. However, most biosignature detectability studies focus on modern Earth, leaving earlier atmospheric states comparatively unexplored. We investigate how atmospheric evolution and stellar environments influence the detectability of O, CH, HO, and CO, and their potential to distinguish anoxic from oxygenated atmospheres. We construct two complementary photochemical grids: representative Archean, Proterozoic, and modern-Earth scenarios around the Sun, and four geological epochs (3.9, 2.0, 0.8 Ga, and modern Earth) across FGKM hosts. Combining one-dimensional photochemical modeling, high-resolution transmission spectral simulations, and instrument-noise modeling, we assess molecular detectability with ELT/ANDES under optimistic photon-noise-limited conditions. For solar-host Archean and Proterozoic models, CH requires approximately 33 and 42 transits, respectively, to reach the adopted 5 criterion, whereas O remains below 3 within the observing limits. Modern-Earth O reaches 3 after approximately 38 transits. Across the FGKM grid, O does not reach 5 for the 3.9 Ga models. However, For the M3V, K2V, and M8V proxies, modern-Earth O reaches 5 in 9, 15, and 20 transits, respectively, whereas CH requires 11, 12, and 28 transits at 3.9 Ga and only 2--4 transits across the oxygenated epochs. These results reveal a strong O detectability contrast around M and K-dwarfs, but not Sun-like hosts in the YJH bands. Robust biosignature interpretation requires complementary molecular constraints, including informative non-detections, within the context of atmospheric evolution and stellar environment.
arXiv commentSubmitted to AAS (31 pages, 20 figures). Comments are most welcome