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Impact of Temperature and Nutrients on Carbon: Nutrient Tissue Stoichiometry of Submerged Aquatic Plants: An Experiment and Meta-Analysis

机译:温度和养分对碳的影响:淹没水生植物的养分组织化学计量比:一项实验和荟萃分析

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Human activity is currently changing our environment rapidly, with predicted temperature increases of 1–5°C over the coming century and increased nitrogen and phosphorus inputs in aquatic ecosystems. In the shallow parts of these ecosystems, submerged aquatic plants enhance water clarity by resource competition with phytoplankton, provide habitat, and serve as a food source for other organisms. The carbon:nutrient stoichiometry of submerged aquatic plants can be affected by changes in both temperature and nutrient availability. We hypothesized that elevated temperature leads to higher carbon:nutrient ratios through enhanced nutrient-use efficiency, while nutrient addition leads to lower carbon:nutrient ratios by the luxurious uptake of nutrients. We addressed these hypotheses with an experimental and a meta-analytical approach. We performed a full-factorial microcosm experiment with the freshwater plant Elodea nuttallii grown at 10, 15, 20, and 25°C on sediment consisting of pond soil/sand mixtures with 100, 50, 25, and 12.5% pond soil. To address the effect of climatic warming and nutrient addition on the carbon:nutrient stoichiometry of submerged freshwater and marine plants we performed a meta-analysis on experimental studies that elevated temperature and/or added nutrients (nitrogen and phosphorus). In the microcosm experiment, C:N ratios of Elodea nuttallii decreased with increasing temperature, and this effect was most pronounced at intermediate nutrient availability. Furthermore, higher nutrient availability led to decreased aboveground C:P ratios. In the meta-analysis, nutrient addition led to a 25, 22, and 16% reduction in aboveground C:N and C:P ratios and belowground C:N ratios, accompanied with increased N content. No consistent effect of elevated temperature on plant stoichiometry could be observed, as very few studies were found on this topic and contrasting results were reported. We conclude that while nutrient addition consistently leads to decreased carbon:nutrient ratios, elevated temperature does not change submerged aquatic plant carbon:nutrient stoichiometry in a consistent manner. This effect is rather dependent on nutrient availability and may be species-specific. As changes in the carbon:nutrient stoichiometry of submerged aquatic plants can impact the transfer of energy to higher trophic levels, these results suggest that eutrophication may enhance plant consumption and decomposition, which could in turn have consequences for carbon sequestration.
机译:目前,人类活动正在迅速改变我们的环境,在未来的一个世纪中,预计温度将升高1-5°C,水生生态系统中的氮和磷输入量也会增加。在这些生态系统的浅层部分,被淹没的水生植物通过与浮游植物的资源竞争提高了水的清晰度,提供了栖息地,并成为其他生物的食物来源。温度和养分利用率的变化都可能影响淹没水生植物的碳:养分化学计量。我们假设升高的温度通过提高养分的利用效率导致更高的碳:养分比,而养分的添加则通过奢侈地吸收养分而导致更低的碳:养分比。我们通过实验和荟萃分析方法解决了这些假设。我们对生长在10、15、20和25°C的淡水植物Elodea nuttallii进行了全要素缩影实验,该沉积物是由池塘土壤/含100、50、25和12.5%池塘土壤的沙子混合物组成的沉积物。为了解决气候变暖和养分添加对淹没的淡水和海洋植物碳:养分化学计量的影响,我们对提高温度和/或添加养分(氮和磷)的实验研究进行了荟萃分析。在微观实验中,随着温度的升高,花生果的C:N比值​​会降低,而这种效果在中等营养水平下最为明显。此外,更高的养分利用率导致地上C:P比降低。在荟萃分析中,营养物的添加导致地上C:N和C:P比以及地下C:N比分别降低25%,22%和16%,同时氮含量增加。没有观察到高温对植物化学计量的持续影响,因为关于该主题的研究很少,并且报道了相反的结果。我们得出的结论是,尽管添加养分始终会导致碳:养分比降低,但温度升高并不会以一致的方式改变淹没水生植物碳:养分的化学计量。这种影响相当取决于养分的可获得性,并且可能是特定物种的。由于淹没水生植物碳:养分化学计量的变化会影响能量向更高营养水平的转移,因此这些结果表明富营养化可能会增加植物的消耗和分解,进而对碳固存产生影响。

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