首页> 外文期刊>Ecology: A Publication of the Ecological Society of America >Causal mechanisms of soil organic matter decomposition: deconstructing salinity and flooding impacts in coastal wetlands
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Causal mechanisms of soil organic matter decomposition: deconstructing salinity and flooding impacts in coastal wetlands

机译:土壤有机质分解的因果机制:沿海湿地解构盐度和洪水冲击

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Coastal wetlands significantly contribute to global carbon storage potential. Sea-level rise and other climate-change-induced disturbances threaten coastal wetland sustainability and carbon storage capacity. It is critical that we understand the mechanisms controlling wetland carbon loss so that we can predict and manage these resources in anticipation of climate change. However, our current understanding of the mechanisms that control soil organic matter decomposition, in particular the impacts of elevated salinity, are limited, and literature reports are contradictory. In an attempt to improve our understanding of these complex processes, we measured root and rhizome decomposition and developed a causal model to identify and quantify the mechanisms that influence soil organic matter decomposition in coastal wetlands that are impacted by sea-level rise. We identified three causal pathways: (1) a direct pathway representing the effects of flooding on soil moisture, (2) a direct pathway representing the effects of salinity on decomposer microbial communities and soil biogeochemistry, and (3) an indirect pathway representing the effects of salinity on litter quality through changes in plant community composition over time. We used this model to test the effects of alternate scenarios on the response of tidal freshwater forested wetlands and oligohaline marshes to short-and long-term climate-induced disturbances of flooding and salinity. In tidal freshwater forested wetlands, the model predicted less decomposition in response to drought, hurricane salinity pulsing, and long-term sea-level rise. In contrast, in the oligohaline marsh, the model predicted no change in response to drought and sea-level rise, and increased decomposition following a hurricane salinity pulse. Our results show that it is critical to consider the temporal scale of disturbance and the magnitude of exposure when assessing the effects of salinity intrusion on carbon mineralization in coastal wetlands. Here, we identify three causal mechanisms that can reconcile disparities between long-term and short-term salinity impacts on organic matter decomposition.
机译:沿海湿地显着促进全球碳储存潜力。海平面上升和其他气候变化诱导的扰动威胁沿海湿地可持续性和碳储存能力。我们理解控制湿地碳损失的机制至关重要,以便我们可以预测气候变化的预测和管理这些资源。然而,我们目前对控制土壤有机物质分解的机制,特别是升高盐度的影响,有限,文献报告是矛盾的。为了改善我们对这些复杂过程的理解,我们测量了根和根茎分解,并开发了一种因果模型,以确定和量化影响受海平面上升影响的沿海湿地中的土壤有机质分解的机制。我们确定了三种因果通路:(1)一种直接途径,代表洪水淹没对土壤水分的影响,(2)代表盐度对分解微生物群落和土壤生物地球化学影响的直接途径,以及代表效果的间接途径随着时间的推移通过植物群落构成变化的垃圾质量盐度。我们使用该模型来测试替代方案对潮汐淡水森​​林湿地和寡酒植物沼泽对短期和长期气候诱导的洪水和盐度的响应的影响。在潮汐淡水森​​林湿地中,该模型响应干旱,飓风盐度脉冲和长期海平面上升预测不太分解。相比之下,在寡核苷酸沼泽中,该模型预测了对干旱和海平面升高的响应的变化,并且在飓风盐度脉冲后增加分解。我们的研究结果表明,在评估盐度侵扰对沿海湿地碳矿化的影响时,考虑扰动的时间量表和暴露程度至关重要。在这里,我们确定三种因果机制,可以在有机物质分解对长期和短期盐度影响之间调和之间的差异。

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