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Sea-level rise and storm surges structure coastal forests into persistence and regeneration niches

机译:海平面上升和风暴潮将沿海森林结构化为持久性和再生利基

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摘要

The retreat of coastal forests as sea level rises is well documented; however, the mechanisms which control this retreat vary with the physical and biological setting of the interface between tidal marsh and forest. Tidal flooding and saltwater intrusion as well as flooding and wind associated with storms can kill trees. Even if these processes do not kill stands, they may halt regeneration because seedlings are more sensitive to stress. We present a case study of a coastal pine forest on the Delmarva Peninsula, United States. This forest contains a persistent but nonregenerating zone of mature trees, the size of which is related to the sea level rise experienced since forest establishment. The transgression of coastal forest and shrub or marsh ecosystems is an ecological ratchet: sea-level rise pushes the regeneration boundary further into the forest while extreme events move the persistence boundary up to the regeneration boundary.
机译:有证据表明,随着海平面上升,沿海森林的退缩;但是,控制这种退缩的机制因潮汐沼泽和森林之间的界面的物理和生物环境而异。潮汐洪水和咸水入侵,以及与暴风雨有关的洪水和风能杀死树木。即使这些过程不会杀死林分,但由于幼苗对压力更敏感,它们可能会停止再生。我们目前以美国Delmarva半岛上的沿海松树林为例。该森林包含一个成熟树木的持久但非再生区,其大小与自森林建立以来经历的海平面上升有关。沿海森林和灌木或沼泽生态系统的越境活动是生态棘手的问题:海平面上升将再生边界进一步推入森林,而极端事件将持久性边界移至再生边界。

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