Department of Ecology, Evolution, and Marine Biology, University of California, Santa Barbara, California, USA.
Environmental Data Science Innovation & Inclusion Lab (ESIIL), University of Colorado Boulder, Boulder, Colorado, USA.
Glob Chang Biol. 2024 Sep;30(9):e17504. doi: 10.1111/gcb.17504.
Ecosystem responses to disturbance depend on the nature of the perturbation and the ecological legacies left behind, making it critical to understand how climate-driven changes in disturbance regimes modify resilience properties of ecosystems. For coral reefs, recent increases in severe marine heat waves now co-occur with powerful storms, the historic agent of disturbance. While storms kill coral and remove their skeletons, heat waves bleach and kill corals but leave their skeletons intact. Here, we explored how the material legacy of dead coral skeletons modifies two key ecological processes that underpin coral reef resilience: the ability of herbivores to control macroalgae (spatial competitors of corals), and the replenishment of new coral colonies. Our findings, grounded by a major bleaching event at our long-term study locale, revealed that the presence of structurally complex dead skeletons reduced grazing on turf algae by 80%. For macroalgae, browsing was reduced by >40% on less preferred (unpalatable) taxa, but only by ~10% on more preferred taxa. This enabled unpalatable macroalgae to reach ~45% cover in 2 years. By contrast, herbivores prevented macroalgae from becoming established on adjacent reefs that lacked skeletons. Manipulation of unpalatable macroalgae revealed that the cover reached after 1 year (20%) reduced recruitment of corals by 50%. The effect of skeletons on juvenile coral growth was contingent on the timing of settlement relative to the disturbance. If corals settled directly after bleaching (before macroalgae colonized), dead skeletons enhanced colony growth by 34%, but this benefit was lost if corals colonized dead skeletons a year after the disturbance once macroalgae had proliferated. These findings underscore how a material legacy from a changing disturbance regime can alter ecosystem resilience properties by disrupting key trophic and competitive interactions that shape post-disturbance community dynamics.
生态系统对干扰的响应取决于扰动的性质和遗留的生态特征,因此了解气候驱动的干扰格局变化如何改变生态系统的恢复力特性至关重要。对于珊瑚礁而言,最近海洋热浪的严重程度不断增加,与强大风暴同时发生,而风暴是干扰的历史因素。虽然风暴会杀死珊瑚并去除它们的骨骼,但热浪会使珊瑚白化并杀死它们,而其骨骼仍然完好无损。在这里,我们探讨了死珊瑚骨骼的物质遗留在支撑珊瑚礁恢复力的两个关键生态过程中的作用:食草动物控制大型藻类(珊瑚的空间竞争者)的能力,以及新珊瑚殖民地的补充。我们的研究结果基于我们的长期研究地点的一次重大白化事件,发现结构复杂的死骨骼的存在将食草动物对草皮藻类的摄食减少了约 80%。对于大型藻类,在不太受欢迎(不可口)的分类群上的摄食减少了 >40%,但在更受欢迎的分类群上只减少了约 10%。这使得不可口的大型藻类在 2 年内达到了约 45%的覆盖率。相比之下,食草动物阻止了没有骨骼的相邻珊瑚礁上的大型藻类的定植。对不可口大型藻类的操纵表明,1 年后达到的覆盖率(约 20%)使珊瑚的繁殖减少了 50%。骨骼对幼年珊瑚生长的影响取决于与干扰有关的定居时间。如果珊瑚在白化后直接定居(在大型藻类定植之前),死骨骼会使珊瑚虫的生长增加 34%,但如果珊瑚在干扰后一年在骨骼上定居,而大型藻类已经大量繁殖,这种好处就会消失。这些发现强调了变化的干扰格局如何通过破坏塑造干扰后群落动态的关键营养和竞争相互作用来改变生态系统的恢复力特性。