“…Severe decreases in nocturnal DO concentrations have been documented in Australia due to warming, which decreases oxygen solubility and increases the rate of biological oxygen consumption. In certain regions of the Caribbean, it is also known that oxygen levels may go below 2 mg/L as a result of anthropogenic eutrophication and nutrient input, and these hypoxic episodes usually last several days [ 10 , 15 , 17 , 36 , 43 , 66 ]. Acropora coral species are known to exhibit high susceptibility to climate change, including ocean warming and deoxygenation [ 10 , 15 , 27 , 34 , 67 , 68 ].…”