  We investigate the chemical stability of CO2-dominated atmospheres of
desiccated M dwarf terrestrial exoplanets using a 1-dimensional photochemical
model. Around Sun-like stars, CO2 photolysis by Far-UV (FUV) radiation is
balanced by recombination reactions that depend on water abundance. Planets
orbiting M dwarf stars experience more FUV radiation, and could be depleted in
water due to M dwarfs' prolonged, high-luminosity pre-main sequences (Luger &
Barnes 2015). We show that, for water-depleted M dwarf terrestrial planets, a
catalytic cycle relying on H2O2 photolysis can maintain a CO2 atmosphere.
However, this cycle breaks down for atmospheric hydrogen mixing ratios <1 ppm,
resulting in ~40% of the atmospheric CO2 being converted to CO and O2 on a time
scale of 1 Myr. The increased O2 abundance leads to high O3 concentrations, the
photolysis of which forms another CO2-regenerating catalytic cycle. For
atmospheres with <0.1 ppm hydrogen, CO2 is produced directly from the
recombination of CO and O. These catalytic cycles place an upper limit of ~50%
on the amount of CO2 that can be destroyed via photolysis, which is enough to
generate Earth-like abundances of (abiotic) O2 and O3. The conditions that lead
to such high oxygen levels could be widespread on planets in the habitable
zones of M dwarfs. Discrimination between biological and abiotic O2 and O3 in
this case can perhaps be accomplished by noting the lack of water features in
the reflectance and emission spectra of these planets, which necessitates
observations at wavelengths longer than 0.95 microns.
