{"refrec":{"BRefID":323330,"RR":"<b>Hughes, D.J.; Alderdice, R.; Cooney, C.; Kühl, M.; Pernice, M.; Voolstra, C.R.; Suggett, D.J.</b> (2020). Coral reef survival under accelerating ocean deoxygenation. <i>Nat. Clim. Chang. 10(4)</i>: 296-307. <a href=\"https://dx.doi.org/10.1038/s41558-020-0737-9\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-020-0737-9</a>","BEntID":316802,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 10(4)</i>: 296-307. <a href=\"https://dx.doi.org/10.1038/s41558-020-0737-9\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-020-0737-9</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Hughes, D.J.; Alderdice, R.; Cooney, C.; Kühl, M.; Pernice, M.; Voolstra, C.R.; Suggett, D.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Hughes, D.J. <i>et al.</i>","Englishabstract":"Global warming and local eutrophication simultaneously lower oxygen (O<SUB>2</SUB>) saturation and increase biological O<SUB>2</SUB> demands to cause deoxygenation. Tropical shallow waters, and their coral reefs, are particularly vulnerable to extreme low O<SUB>2</SUB> (hypoxia) events. These events can drive mass mortality of reef biota; however, they currently remain unaccounted for when considering coral reef persistence under local environmental alterations and global climatic change. In this Perspective, we integrate existing biological, ecological and geochemical evidence to consider how O<SUB>2</SUB> availability and hypoxia affect reef biota, with particular focus on the ecosystem architects, reef-building corals, that operate as both O<SUB>2</SUB> consumers and producers. 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