School of Environmental and Life Sciences, University of Newcastle, Chittaway Road, Newcastle, NSW 2308, Australia; Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, University Drive, Townsville, QLD 4810, Australia.
Climate Change Cluster, University of Technology Sydney, PO Box 123, Broadway, NSW 2007, Australia.
Curr Biol. 2019 Aug 19;29(16):2723-2730.e4. doi: 10.1016/j.cub.2019.06.077. Epub 2019 Aug 8.
Severe marine heatwaves have recently become a common feature of global ocean conditions due to a rapidly changing climate [1, 2]. These increasingly severe thermal conditions are causing an unprecedented increase in the frequency and severity of mortality events in marine ecosystems, including on coral reefs [3]. The degradation of coral reefs will result in the collapse of ecosystem services that sustain over half a billion people globally [4, 5]. Here, we show that marine heatwave events on coral reefs are biologically distinct to how coral bleaching has been understood to date, in that heatwave conditions result in an immediate heat-induced mortality of the coral colony, rapid coral skeletal dissolution, and the loss of the three-dimensional reef structure. During heatwave-induced mortality, the coral skeletons exposed by tissue loss are, within days, encased by a complex biofilm of phototrophic microbes, whose metabolic activity accelerates calcium carbonate dissolution to rates exceeding accretion by healthy corals and far greater than has been documented on reefs under normal seawater conditions. This dissolution reduces the skeletal density and hardness and increases porosity. These results demonstrate that severe-heatwave-induced mortality events should be considered as a distinct biological phenomenon from bleaching events on coral reefs. We also suggest that such heatwave mortality events, and rapid reef decay, will become more frequent as the intensity of marine heatwaves increases and provides further compelling evidence for the need to mitigate climate change and instigate actions to reduce marine heatwaves.
由于气候变化迅速,近年来严重的海洋热浪已成为全球海洋状况的常见特征[1,2]。这些日益严重的热条件导致海洋生态系统中死亡率事件的频率和严重程度以前所未有的速度增加,包括珊瑚礁[3]。珊瑚礁的退化将导致维持着全球超过 5 亿人口的生态系统服务崩溃[4,5]。在这里,我们表明,珊瑚礁上的海洋热浪事件在生物学上与迄今为止人们所理解的珊瑚白化有所不同,因为热浪条件会导致珊瑚群体立即因热而死亡,珊瑚骨骼迅速溶解,以及三维珊瑚礁结构的丧失。在热浪引起的死亡过程中,组织损失暴露的珊瑚骨骼在几天内就会被一层复杂的光养微生物生物膜所包围,其代谢活动加速了碳酸钙的溶解,速度超过了健康珊瑚的沉积速度,远远超过了在正常海水条件下记录的珊瑚礁上的溶解速度。这种溶解降低了骨骼的密度和硬度,增加了孔隙度。这些结果表明,严重热浪引起的死亡事件应被视为与珊瑚礁白化事件不同的独特生物学现象。我们还建议,随着海洋热浪强度的增加,这种热浪死亡率事件和快速的珊瑚礁衰退将变得更加频繁,这为需要缓解气候变化和采取行动减少海洋热浪提供了进一步的有力证据。