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首页> 外文期刊>Global change biology >The dynamics of architectural complexity on coral reefs under climate change
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The dynamics of architectural complexity on coral reefs under climate change

机译:气候变化下珊瑚礁建筑复杂性的动态

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One striking feature of coral reef ecosystems is the complex benthic architecture which supports diverse and abundant fauna, particularly of reef fish. Reef-building corals are in decline worldwide, with a corresponding loss of live coral cover resulting in a loss of architectural complexity. Understanding the dynamics of the reef architecture is therefore important to envision the ability of corals to maintain functional habitats in an era of climate change. Here, we develop a mechanistic model of reef topographical complexity for contemporary Caribbean reefs. The model describes the dynamics of corals and other benthic taxa under climate-driven disturbances (hurricanes and coral bleaching). Corals have a simplified shape with explicit diameter and height, allowing species-specific calculation of their colony surface and volume. Growth and the mechanical (hurricanes) and biological erosion (parrotfish) of carbonate skeletons are important in driving the pace of extension/reduction in the upper reef surface, the net outcome being quantified by a simple surface roughness index (reef rugosity). The model accurately simulated the decadal changes of coral cover observed in Cozumel (Mexico) between 1984 and 2008, and provided a realistic hindcast of coral colony-scale (1-10m) changing rugosity over the same period. We then projected future changes of Caribbean reef rugosity in response to global warming. Under severe and frequent thermal stress, the model predicted a dramatic loss of rugosity over the next two or three decades. Critically, reefs with managed parrotfish populations were able to delay the general loss of architectural complexity, as the benefits of grazing in maintaining living coral outweighed the bioerosion of dead coral skeletons. Overall, this model provides the first explicit projections of reef rugosity in a warming climate, and highlights the need of combining local (protecting and restoring high grazing) to global (mitigation of greenhouse gas emissions) interventions for the persistence of functional reef habitats.
机译:珊瑚礁生态系统的一个显着特征是复杂的底栖建筑,可支持多种多样的动物群,尤其是珊瑚鱼。在世界范围内,造礁珊瑚的数量正在减少,相应的活珊瑚覆盖率随之下降,导致建筑复杂性下降。因此,了解珊瑚礁结构的动态对于设想珊瑚在气候变化时代维持功能性栖息地的能力非常重要。在这里,我们为当代加勒比海地区的珊瑚礁地形复杂性建立了一个机械模型。该模型描述了在气候驱动的干扰(飓风和珊瑚白化)下珊瑚和其他底栖生物群的动态。珊瑚具有简化的形状,具有明确的直径和高度,从而允许特定物种计算其菌落表面和体积。碳酸盐骨架的生长以及机械(飓风)和生物侵蚀(鹦嘴鱼)对于驱动上礁表面的扩展/还原速度很重要,其净结果可通过简单的表面粗糙度指数(礁皱纹)来量化。该模型准确地模拟了1984年至2008年在科苏梅尔(墨西哥)观测到的珊瑚覆盖率的年代际变化,并提供了真实的珊瑚殖民地规模(1-10m)在同一时期内改变皱纹的后兆。然后,我们预测了应对全球变暖的加勒比珊瑚礁折皱性的未来变化。在严重且频繁的热应力下,该模型预测在接下来的两到三十年中,皱纹的严重损失。至关重要的是,管理鹦鹉鱼种群的珊瑚礁能够延迟建筑复杂性的总体损失,因为放牧维持活珊瑚的好处胜过了死珊瑚骨骼的生物侵蚀。总体而言,该模型首次给出了气候变暖时珊瑚礁褶皱的明确预测,并强调了需要将局部(保护和恢复高放牧)与全球(减轻温室气体排放)的干预措施结合起来,以维持功能性珊瑚礁栖息地的持久性。

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