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首页> 外文期刊>Coral reefs: journal of the International Society for Reef Studies >Coral bleaching impacts from back-to-back 2015-2016 thermal anomalies in the remote central Indian Ocean
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Coral bleaching impacts from back-to-back 2015-2016 thermal anomalies in the remote central Indian Ocean

机译:珊瑚漂白从遥远的中央印度洋中的回归2015-2016热异常的影响

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摘要

Studying scleractinian coral bleaching and recovery dynamics in remote, isolated reef systems offers an opportunity to examine impacts of global reef stressors in the absence of local human threats. Reefs in the Chagos Archipelago, central Indian Ocean, suffered severe bleaching and mortality in 2015 following a 7.5 maximum degree heating weeks (DHWs) thermal anomaly, causing a 60% coral cover decrease from 30% cover in 2012 to 12% in April 2016. Mortality was taxon specific, with Porites becoming the dominant coral genus post-bleaching because of an 86% decline in Acropora from 14 to 2% cover. Spatial heterogeneity in Acropora mortality across the Archipelago was significantly negatively correlated with variation in DHWs and with chlorophyll-a concentrations. In 2016, a 17.6 maximum DHWs thermal anomaly caused further damage, with 68% of remaining corals bleaching in May 2016, and coral cover further declining by 29% at Peros Banhos Atoll (northern Chagos Archipelago) from 14% in March 2016 to 10% in April 2017. We therefore document back-to-back coral bleaching and mortality events for two successive years in the remote central Indian Ocean. Our results indicate lower coral mortality in 2016 than 2015 despite a more severe thermal anomaly event in 2016. This could be caused by increased thermal resistance and resilience within corals surviving the 2015 thermal anomaly; however, high bleaching prevalence in 2016 suggests there remained a high sensitivity to bleaching. Similar coral mortality and community change were seen in the Chagos Archipelago following the 1998 global bleaching event, from which recovery took 10 yr. This relatively rapid recovery suggests high reef resiliency and indicates that the Archipelago's lack of local disturbances will increase the probability that the reefs will again recover over time. However, as the return time between thermal anomaly events becomes shorter, this ability to recover will become increasingly compromised.
机译:在遥控器中研究巩膜珊瑚珊瑚漂白和恢复动态,提供了在没有当地人类威胁的情况下检查全球珊瑚礁压力源的影响。在7.5个最高度加热周(DHWS)热异常后,2015年,印度印度洋,中央印度洋,中部海洋,中央印度洋,遭受严重漂白和死亡率的珊瑚礁,导致2012年2012年的30%覆盖率降低了60%的珊瑚盖。死亡率是分类群特异性,Porites成为漂白后冠状珊瑚属的主要珊瑚属,因为Acropora下降的86%从14%到2%的封面下降。在群岛上的Acropora死亡率中的空间异质性与DHWs的变异和叶绿素 - 一种浓度显着呈负相关。 2016年,17.6最高DHW热异常引起了进一步的损害,占剩余珊瑚漂白的伤害2016年5月,珊瑚盖在2016年3月14%的佩罗斯巴哥·阿马拉格(Northern Chagos Archipelago)进一步下降了29%至10%因此,在2017年4月。因此,我们在偏远的中央印度洋中举行了两年连续几年的回报珊瑚漂白和死亡事件。尽管2016年,我们的结果表明2016年的珊瑚死亡率低于2015年,这可能是由于2016年更严重的热量异常事件。这可能是由于珊瑚内的热阻和恢复力增加源于2015年的热异常;然而,2016年的高漂白普遍性表明仍然存在对漂白的高敏感性。在1998年全球漂白事件之后,在1998年的全球漂白事件之后,在克拉索斯群岛中看到了类似的珊瑚死亡率和社区变革,从中恢复到10年。这种相对快速的恢复表明高礁弹性,表明群岛缺乏局部紊乱将增加珊瑚礁再次随着时间的推移恢复的可能性。然而,随着热异常事件之间的返回时间变短,这种恢复能力将变得越来越受到损害。

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