Ocean warming reduces O₂ solubility and increases organismal O₂ demand, endangering marine life. Coastal ecosystems, however, experience O₂ supersaturation during peak daytime temperatures due to metabolic cycles. Recent discoveries show that this environmental supersaturation can reduce the vulnerability of tropical species to warming by satisfying their oxygen requirements. To test whether this also occurs within the cnidarian holobiont, we elevated internal O₂ in Cassiopea andromeda at nighttime (i.e. holobiont respiration prevails on Symbiodniaceae O₂ production) relying on bell pulsation for ventilation, then experimentally subjected them to thermal stress (+1°C day^-1). Though ecologically unrealistic, this approach verified our hypothesis and eliminated confounding factors. Holobionts were exposed to either constant levels of 100% air saturation (100AS) or nighttime supersaturation (NSS; where 100% air saturation transitioned to O₂ supersaturation at nighttime). At sublethal temperatures, supersaturation mitigated reductions in holobiont size of ~ 10.37% (-33.418% ± 0.345 under 100AS vs -23.039% ± 0.687 under NSS). Supersaturation alleviated chlorophyll-a loss by 42.73% until 34°C, when counteraction of this process could not be sustained due to excessive thermal stress. Supersaturation also enriched potentially beneficial bacterial taxa of the microbiome and selected a more consistent bacterial community. Although modest, the detected effects show that a O₂ surplus increased the resistance of the holobionts to thermal stress.