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Long-term impacts of rising sea temperature and sea level on shallow water coral communities over a ~40 year period

机译:40年来海水温度和海平面上升对浅水珊瑚群落的长期影响

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摘要

Effects of combined rising sea temperature and increasing sea level on coral reefs, both factors associated with global warming, have rarely been addressed. In this ~40 y study of shallow reefs in the eastern Indian Ocean, we show that a rising relative sea level, currently estimated at ~11 mm y−1, has not only promoted coral cover but also has potential to limit damaging effects of thermally-induced bleaching. In 2010 the region experienced the most severe bleaching on record with corals subject to sea temperatures of >31 °C for 7 weeks. While the reef flats studied have a common aspect and are dominated by a similar suite of coral species, there was considerable spatial variation in their bleaching response which corresponded with reef-flat depth. Greatest loss of coral cover and community structure disruption occurred on the shallowest reef flats. Damage was less severe on the deepest reef flat where corals were subject to less aerial exposure, rapid flushing and longer submergence in turbid waters. Recovery of the most damaged sites took only ~8 y. While future trajectories of these resilient reefs will depend on sea-level anomalies, and frequency of extreme bleaching the positive role of rising sea level should not be under-estimated.
机译:升高的海水温度和升高的海平面对珊瑚礁的综合影响,这两个与全球变暖有关的因素,很少得到解决。在这项对印度洋东部浅礁的〜40 y研究中,我们表明,目前估计为〜11 mm estimatedy -1 的相对海平面上升不仅促进了珊瑚覆盖,而且限制热致漂白破坏作用的潜力。 2010年,该地区遭受了有史以来最严重的漂白,珊瑚的海水温度超过31°C,持续了7周。虽然所研究的礁滩有一个共同的方面,并由一组类似的珊瑚物种主导,但它们的漂白反应存在相当大的空间变化,与礁滩深度相对应。在最浅的礁石滩上,珊瑚覆盖物和社区结构破坏的损失最大。在最深的珊瑚礁平地上,破坏不那么严重,在珊瑚礁上,珊瑚暴露于较少的空气中,迅速冲洗并在浑浊的水中浸没时间更长。恢复受损程度最大的站点仅需8 yy。虽然这些弹性礁石的未来轨迹将取决于海平面异常,并且极端漂白的频率不应低估海平面上升的积极作用。

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