{"refrec":{"BRefID":391884,"RR":"<b>Deutsch, C.; Penn, J.L.; Lucey, N.</b> (2024). Climate, oxygen, and the future of marine biodiversity. <i>Ann. Rev. Mar. Sci. 16(1)</i>: 217-245. <a href=\"https://dx.doi.org/10.1146/annurev-marine-040323-095231\" target=\"_blank\">https://dx.doi.org/10.1146/annurev-marine-040323-095231</a>","BEntID":389635,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Ann. Rev. Mar. Sci. 16(1)</i>: 217-245. <a href=\"https://dx.doi.org/10.1146/annurev-marine-040323-095231\" target=\"_blank\">https://dx.doi.org/10.1146/annurev-marine-040323-095231</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Deutsch, C.; Penn, J.L.; Lucey, N.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Deutsch, C.; Penn, J.L.; Lucey, N.","Englishabstract":"The ocean enabled the diversification of life on Earth by adding O<sub>2</sub> to the atmosphere, yet marine species remain most subject to O<sub>2</sub> limitation. Human industrialization is intensifying the aerobic challenges to marine ecosystems by depleting the ocean's O<sub>2 </sub>inventory through the global addition of heat and local addition of nutrients. Historical observations reveal an ∼2% decline in upper-ocean O<sub>2 </sub>and accelerating reports of coastal mass mortality events. The dynamic balance of O<sub>2</sub> supply and demand provides a unifying framework for understanding these phenomena across scales from the global ocean to individual organisms. Using this framework, we synthesize recent advances in forecasting O<sub>2</sub> loss and its impacts on marine biogeography, biodiversity, and biogeochemistry. We also highlight three outstanding uncertainties: how long-term global climate change intensifies ocean weather events in which simultaneous heat and hypoxia create metabolic storms, how differential species O<sub>2</sub> sensitivities alter the structure of ecological communities, and how global O<sub>2 </sub>loss intersects with coastal eutrophication. Projecting these interacting impacts on future marine ecosystems requires integration of climate dynamics, biogeochemistry, physiology, and ecology, evaluated with an eye on Earth history. 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