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盐沼植物对富营养化的响应。

Saltmarsh plant responses to eutrophication.

机构信息

Virginia Institute of Marine Science, Gloucester Point, Virginia, 23062, USA.

Department of Botany, Connecticut College, New London, Connecticut, 06320, USA.

出版信息

Ecol Appl. 2016 Dec;26(8):2647-2659. doi: 10.1002/eap.1402. Epub 2016 Oct 20.

Abstract

In saltmarsh plant communities, bottom-up pressure from nutrient enrichment is predicted to increase productivity, alter community structure, decrease biodiversity, and alter ecosystem functioning. Previous work supporting these predictions has been based largely on short-term, plot-level (e.g., 1-300 m ) studies, which may miss landscape-level phenomena that drive ecosystem-level responses. We implemented an ecosystem-scale, nine-year nutrient experiment to examine how saltmarsh plants respond to simulated conditions of coastal eutrophication. Our study differed from previous saltmarsh enrichment studies in that we applied realistic concentrations of nitrate (70-100 μM NO ), the most common form of coastal nutrient enrichment, via tidal water at the ecosystem scale (~60,000 m creeksheds). Our enrichments added a total of 1,700 kg N·creek ·yr , which increased N loading 10-fold vs. reference creeks (low-marsh, 171 g N·m ·yr ; high-marsh, 19 g N·m ·yr ). Nutrients increased the shoot mass and height of low marsh, tall Spartina alterniflora; however, declines in stem density resulted in no consistent increase in aboveground biomass. High-marsh plants S. patens and stunted S. alterniflora did not respond consistently to enrichment. Nutrient enrichment did not shift community structure, contrary to the prediction of nutrient-driven dominance of S. alterniflora and Distichlis spicata over S. patens. Our mild responses may differ from the results of previous studies for a number of reasons. First, the limited response of the high marsh may be explained by loading rates orders of magnitude lower than previous work. Low loading rates in the high marsh reflect infrequent inundation, arguing that inundation patterns must be considered when predicting responses to estuarine eutrophication. Additionally, we applied nitrate instead of the typically used ammonium, which is energetically favored over nitrate for plant uptake. Thus, the form of nitrogen enrichment used, not just N-load, may be important in predicting plant responses. Overall, our results suggest that when coastal eutrophication is dominated by nitrate and delivered via flooding tidal water, aboveground saltmarsh plant responses may be limited despite moderate-to-high water-column N concentrations. Furthermore, we argue that the methodological limitations of nutrient studies must be considered when using results to inform management decisions about wetlands.

摘要

在盐沼植物群落中,养分富化的底生压力预计会提高生产力、改变群落结构、降低生物多样性并改变生态系统功能。支持这些预测的先前工作主要基于短期、斑块尺度(例如,1-300 米)的研究,而这些研究可能会错过驱动生态系统水平响应的景观尺度现象。我们实施了一个生态系统尺度的、为期九年的养分实验,以研究盐沼植物对沿海富营养化模拟条件的响应。我们的研究与以前的盐沼富化实验不同,因为我们以潮汐水的形式在生态系统尺度上(~60000 米的小溪流域)应用了现实浓度的硝酸盐(70-100 μM 的 NO ),这是最常见的沿海养分富化形式。我们的富化总共添加了 1700 公斤 N·小溪·年,与对照小溪(低沼泽,171 克 N·米·年;高沼泽,19 克 N·米·年)相比,氮负荷增加了 10 倍。养分增加了低沼泽、高大的互花米草的地上生物量和高度;然而,茎密度的下降导致地上生物量没有一致增加。高沼泽植物 Paspalum vaginatum 和矮小的互花米草对富化的反应不一致。养分富化并没有改变群落结构,这与氮驱动互花米草和 Distichlis spicata 对 Paspalum vaginatum 优势的预测相反。我们的温和反应可能与以前研究的结果有几个原因不同。首先,高沼泽的有限响应可以用比以前工作低几个数量级的负荷率来解释。高沼泽的低负荷率反映了洪水泛滥的频率较低,这表明在预测对河口富营养化的响应时必须考虑洪水泛滥模式。此外,我们应用了硝酸盐而不是通常使用的铵盐,因为植物吸收硝酸盐比吸收硝酸盐更有利。因此,氮富化的形式,而不仅仅是 N 负荷,可能对预测植物响应很重要。总的来说,我们的结果表明,当沿海富营养化以硝酸盐为主,并通过洪水潮汐水输送时,尽管水柱中的氮浓度适中至高,地上盐沼植物的响应可能仍然有限。此外,我们认为,在利用研究结果为湿地管理决策提供信息时,必须考虑养分研究的方法学限制。

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