In this paper Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction is established a link between an increase of the global temperature by $10^\circ C$ (in their simulation) and the Great Dying global extinction via a global hypoxia.
I would like to know how much the atmospheric pressure at sea level will increase when the oceans are heated $10^\circ C$
The solubility of $O_2$ in water is function of the temperature, atmospheric pressure and salinity and the paper only mention the temperature.