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首页> 外文期刊>Frontiers in Marine Science >Marine Heatwave Hotspots in Coral Reef Environments: Physical Drivers, Ecophysiological Outcomes, and Impact Upon Structural Complexity
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Marine Heatwave Hotspots in Coral Reef Environments: Physical Drivers, Ecophysiological Outcomes, and Impact Upon Structural Complexity

机译:珊瑚礁环境中的海洋热浪热点:物理驱动因素,生态生理结果及其对结构复杂性的影响

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A changing climate is driving increasingly common and prolonged marine heatwaves (MHWs) and these extreme events have now been widely documented to severely impact marine ecosystems globally. However MHWs have rarely recently been considered when examining temperature-induced degradation of coral reef ecosystems. Here we consider extreme, localised thermal anomalies, nested within broader increases in sea surface temperature, which fulfil the definitive criteria for MHWs. These acute and intense events, referred to here as MHW hotspots, are not always well represented in the current framework used to describe coral bleaching, but do have distinct ecological outcomes, including widespread bleaching and rapid mass mortality of putatively thermally tolerant coral species. The physical drivers of these localised hotspots are discussed here, and in doing so we present a comprehensive theoretical framework that links the biological responses of the coral photo-endosymbiotic organism to extreme thermal stress and ecological changes on reefs associated after MHW hotspots. We describe how the rapid onset of high temperatures drives immediate heat-stress induced cellular damage, overwhelming mechanisms that would otherwise mitigate the impact of gradually accumulated thermal stress. The warm environment, and increased light penetration of the coral skeleton due to the loss of coral tissues, coupled with coral tissue decay support rapid microbial growth in the skeletal microenvironment, resulting in the widely unrecognised consequence of rapid decay and degeneration of the coral skeletons. This accelerated degeneration of the coral skeletonson a reef scale hinder the recovery of coral populations and increase the likelihood of phase shifts towards algal dominance. We suggest that MHW hotspots, through driving rapid heat-induced mortality, compromise reefs’ structural frameworks to the detriment of long term recovery. We propose that MHW hotspots be considered as a distinct class of thermal stress events in coral reefs, and that the current framework used to describe coral bleaching and mass mortality be expanded to include these. We urge further research into how coral mortality affects bioerosion by coral endoliths.
机译:气候变化正驱动着越来越普遍和延长的海洋热浪(MHW),并且这些极端事件现已得到广泛记录,对全球海洋生态系统产生了严重影响。但是,在检查温度引起的珊瑚礁生态系统退化时,很少有人考虑使用MHW。在这里,我们考虑了极端的局部热异常,这些异常嵌套在海表温度的更大范围内,可以满足MHW的确定标准。这些急性和强烈事件在这里被称为MHW热点,在用于描述珊瑚褪色的当前框架中并不总是能很好地体现出来,但是它们确实具有独特的生态结果,包括广泛的褪色和推定耐热的珊瑚物种的快速大量死亡。这里讨论了这些局部热点的物理驱动因素,在此过程中,我们提出了一个综合的理论框架,该框架将珊瑚光内共生生物的生物学响应与MHW热点后相关的珊瑚礁的极端热应力和生态变化联系起来。我们描述了高温的快速发作如何驱动立即的热应激诱导的细胞损伤,而压倒性的机制将减轻逐渐积累的热应激的影响。由于珊瑚组织的丧失,温暖的环境以及增加的珊瑚骨骼的光穿透性,再加上珊瑚组织的腐烂,在骨骼微环境中支持了微生物的快速生长,从而导致人们普遍认识到珊瑚骨骼迅速腐烂和退化的后果。珊瑚骨架上的珊瑚骨骼的这种加速退化阻碍了珊瑚种群的恢复,并增加了向藻类优势相转变的可能性。我们建议,MHW热点通过推动快速的热致死亡,损害礁石的结构框架,损害长期恢复。我们建议将MHW热点视为珊瑚礁中的一类独特的热应力事件,并应将用于描述珊瑚褪色和大规模死亡的当前框架扩展到这些范围。我们敦促对珊瑚死亡率如何影响珊瑚残体对生物侵蚀的影响进行进一步研究。

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