Velthuis Mandy, van Deelen Emma, van Donk Ellen, Zhang Peiyu, Bakker Elisabeth S
Department of Aquatic Ecology, Netherlands Institute of EcologyWageningen, Netherlands.
Department of Biology, Utrecht UniversityUtrecht, Netherlands.
Front Plant Sci. 2017 May 4;8:655. doi: 10.3389/fpls.2017.00655. eCollection 2017.
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 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 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.
当前,人类活动正在迅速改变我们的环境,预计在未来一个世纪气温将升高1 - 5°C,水生生态系统中的氮和磷输入也会增加。在这些生态系统的浅水区,沉水植物通过与浮游植物竞争资源来提高水体透明度,提供栖息地,并作为其他生物的食物来源。沉水植物的碳:养分化学计量比可能会受到温度和养分有效性变化的影响。我们假设,温度升高通过提高养分利用效率导致碳:养分比升高,而添加养分则通过养分的奢侈吸收导致碳:养分比降低。我们通过实验和元分析方法来验证这些假设。我们用淡水植物进行了一项全因子微观实验,该植物在由池塘土壤/沙子混合物组成的沉积物上生长,池塘土壤含量分别为100%、50%、25%和12.5%,温度设置为10°C、15°C、20°C和25°C。为了研究气候变暖和添加养分对沉水淡水和海洋植物碳:养分化学计量比的影响,我们对升高温度和/或添加养分(氮和磷)的实验研究进行了元分析。在微观实验中,随着温度升高,[植物名称]的C:N比降低,这种效应在中等养分有效性时最为明显。此外,较高的养分有效性导致地上部分C:P比降低。在元分析中,添加养分导致地上部分C:N和C:P比以及地下部分C:N比分别降低25%、22%和16%,同时氮含量增加。由于关于这个主题的研究很少且结果相互矛盾,因此未观察到温度升高对植物化学计量比有一致的影响。我们得出结论,虽然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沉水植物的碳:养分化学计量比。这种效应相当程度上取决于养分有效性,并且可能具有物种特异性。由于沉水植物碳:养分化学计量比的变化会影响能量向更高营养级的传递,这些结果表明富营养化可能会增强植物的消耗和分解,进而可能对碳固存产生影响。