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Recovery of a northern New England salt marsh plant community from winter icing

机译:从冬季结冰中恢复新英格兰北部盐沼植物群落

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High latitude salt marsh plant communities are frequently exposed to conspicuous winter ice disturbances, which trigger secondary succession. In this paper, we document the recovery of a northern New England salt marsh from a severe winter icing event in 1998. Ice disturbances that killed plants but that left the underlying peat intact recovered rapidly. However, ice damage that killed plants and removed the underlying peat, led to areas of physiologically harsh edaphic conditions, specifically waterlogged and anoxic soils that limited plant recolonization. A transplant experiment revealed that only the most stress-tolerant plants were capable of invading the most stressful portions of ice disturbances. A second experiment that artificially dried disturbance patches accelerated patch recovery. These data suggest that recovery from intense ice disturbance is dependent on stress-tolerant plants invading edaphically harsh disturbances, eventually facilitating the recolonization of the community. This process likely takes longer than a decade for full recovery to occur in the areas where both plants and the peat base are removed.
机译:高纬度盐沼植物群落经常遭受明显的冬季冰雪干扰,从而引发继发演替。在本文中,我们记录了1998年严重的冬季结冰事件后新英格兰北部盐沼的恢复。冰灾使植物死亡,但使下层泥炭完好无损地得以迅速恢复。但是,冰冻破坏了植物并去除了潜在的泥炭,导致了生理条件恶劣的土壤条件,特别是浸水和缺氧的土壤,限制了植物的重新定殖。一项移植实验表明,只有最耐胁迫的植物才能够入侵最严重的冰干扰部分。人工干燥干扰补丁的第二个实验可加快补丁恢复。这些数据表明,从强烈的冰干扰中恢复依赖于耐应力植物入侵入侵的严重干扰,最终促进了社区的重新定殖。要完全恢复植物和泥炭基地均已消失的地区,此过程可能要花费十年以上的时间。

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