Department of Marine Biology and Ecology, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL, USA.
Department of Marine and Environmental Sciences, Halmos College of Natural Sciences and Oceanography, Nova Southeastern University, Dania Beach, FL, USA.
Mar Pollut Bull. 2018 Aug;133:717-733. doi: 10.1016/j.marpolbul.2018.06.002. Epub 2018 Jun 22.
Coral populations and structural coral reefs have undergone severe reductions and losses respectively over large parts of the Galápagos Islands during and following the 1982-83 El Niño event. Coral tissue loss amounted to 95% across the Archipelago. Also at that time, all coral reefs in the central and southern islands disappeared following severe degradation and eventual collapse due primarily to intense bioerosion and low recruitment. Six sites in the southern islands have demonstrated low to moderate coral community (scattered colonies, but no carbonate framework) recovery. The iconic pocilloporid reef at Devil's Crown (Floreana Island) experienced recovery to 2007, then severe mortality during a La Niña cooling event, and is again (as of 2017) undergoing rapid recovery. Notable recovery has occurred at the central (Marchena) and northern islands (Darwin and Wolf). Of the 17 structural reefs first observed in the mid-1970s, the single surviving reef (Wellington Reef) at Darwin Island remains in a positive growth mode. The remainder either degraded to a coral community or was lost. Retrospective analyses of the age structure of corals killed in 1983, and isotopic signatures of the skeletal growth record of massive corals suggest the occurrence of robust coral populations during at least a 500-year period before 1983. The greatest potential threats to the recovery and persistence of coral reefs include: ocean warming and acidification, bioerosion, coral diseases, human population growth (increasing numbers of residents and tourists), overfishing, invasive species, pollution, and habitat destruction. Such a diverse spectrum of disturbances, acting alone or in combination, are expected to continue to cause local and archipelago-wide mortality and degradation of the coral reef ecosystem.
在 1982-1983 年厄尔尼诺事件期间和之后,加拉帕戈斯群岛的大部分地区珊瑚数量和珊瑚礁结构都经历了严重的减少和损失。整个群岛的珊瑚组织损失达到了 95%。当时,由于强烈的生物侵蚀和低繁殖率,中部和南部岛屿的所有珊瑚礁都严重退化,最终消失。在南部的六个地点,珊瑚群落(零星的殖民地,但没有碳酸盐框架)已经显示出低到中度的恢复。恶魔之冠(费尔南迪纳岛)标志性的石珊瑚礁在经历了 2007 年的恢复后,又在拉尼娜冷却事件中遭受了严重的死亡,截至 2017 年,它又在迅速恢复。中部(马切纳)和北部岛屿(达尔文和沃尔夫)也有显著的恢复。在 20 世纪 70 年代中期首次观察到的 17 个结构珊瑚礁中,达尔文岛上唯一幸存的珊瑚礁(惠灵顿礁)仍处于正增长模式。其余的要么退化到珊瑚群落,要么消失了。对 1983 年死亡珊瑚的年龄结构的回顾性分析,以及巨珊瑚骨骼生长记录的同位素特征表明,在 1983 年之前的至少 500 年期间,珊瑚种群曾经非常繁盛。对珊瑚礁恢复和持续存在的最大潜在威胁包括:海洋变暖与酸化、生物侵蚀、珊瑚疾病、人口增长(居民和游客人数增加)、过度捕捞、入侵物种、污染和生境破坏。如此多样化的干扰因素,单独或组合作用,预计将继续导致局部和全岛范围内的珊瑚礁生态系统的死亡和退化。