There's more to life than O$_2$: Simulating the detectability of a range of molecules for ground-based high-resolution spectroscopy of transiting terrestrial exoplanets
Authors: Miles H. Currie, Victoria S. Meadows, Kaitlin C. Rasmussen
AI-generated Key Points
- Exoplanet research has focused on finding life beyond our solar system
- Detection of biosignatures, such as atmospheric oxygen (O$_2$), is a promising avenue for finding Earth-like planets orbiting M dwarf stars
- O$_2$ alone does not necessarily indicate the presence of life, additional molecules are needed to provide context and rule out false positives
- Simulations were used to explore the detectability of a range of molecules for ground-based high-resolution spectroscopy of transiting terrestrial exoplanets using extremely large ground-based telescopes (ELTs)
- CH$_4$, CO$_2$, O$_2$, NIR and H$_2$O 0.9 $\mu m $ bands are the most accessible molecules for terrestrial planets transiting a range of M dwarf hosts using an E-ELT, TMT or GMT sized telescope
- ELTs have the potential to reveal two biosignature pairs and detect the molecules necessary to discriminate biological and false positive origins for O$_2$
- Some molecules such as N$_2$ may not be detectable with ELTs
- Continued development of techniques for telluric line subtraction and closer transit targets is needed to fully realize the potential of ELT observations in detecting biosignatures on exoplanets
Abstract: Within the next decade, atmospheric O$_2$ on Earth-like M dwarf planets may be accessible with visible--near-infrared, high spectral resolution extremely large ground-based telescope (ELT) instruments. However, the prospects for using ELTs to detect environmental properties that provide context for O$_2$ have not been thoroughly explored. Additional molecules may help indicate planetary habitability, rule out abiotically generated O$_2$, or reveal alternative biosignatures. To understand the accessibility of environmental context using ELT spectra, we simulate high-resolution transit transmission spectra of previously-generated evolved terrestrial atmospheres. We consider inhabited pre-industrial and Archean Earth-like atmospheres, and lifeless worlds with abiotic O$_2$ buildup from CO$_2$ and H$_2$O photolysis. All atmospheres are self-consistent with M2V--M8V dwarf host stars. Our simulations include explicit treatment of systematic and telluric effects to model high-resolution spectra for GMT, TMT, and E-ELT configurations for systems 5 and 12 pc from Earth. Using the cross-correlation technique, we determine the detectability of major species in these atmospheres: O$_2$, O$_3$, CH$_4$, CO$_2$, CO, H$_2$O, and C$_2$H$_6$. Our results suggest that CH$_4$ and CO$_2$ are the most accessible molecules for terrestrial planets transiting a range of M dwarf hosts using an E-ELT, TMT, or GMT sized telescope, and that the O$_2$ NIR and H$_2$O 0.9 $\mu$m bands may also be accessible with more observation time. Although this technique still faces considerable challenges, the ELTs will provide access to the atmospheres of terrestrial planets transiting earlier-type M-dwarf hosts that may not be possible using JWST.
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