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首页> 外文期刊>Global change biology >Simulated climate change decreases nutrient resorption from senescing leaves
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Simulated climate change decreases nutrient resorption from senescing leaves

机译:模拟气候变化降低了Sencing Leave的营养物吸收

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Nutrient resorption is the process whereby plants recover nutrients from senescing leaves and reallocate them to storage structures or newer tissues. Elemental resorption of foliar N and P has been shown to respond to temperature and precipitation, but we know remarkably little about the influence of warming and drought on the resorption of these and other essential plant macro- and micronutrients, which could alter the ability of species to recycle their nutrients. We conducted a 5 year manipulative field study to simulate predicted climate change conditions and studied the effects of warming (W), rainfall reduction (RR), and their combination (W+RR) on nutrient resorption efficiency in five coexisting shrub species in a semiarid shrubland. Both mature and senesced leaves showed significant reductions in their nutrient contents and an altered stoichiometry in response to climate change conditions. Warming (W, W+RR) reduced mature leaf N, K, Ca, S, Fe, and Zn and senesced leaf N, Ca, Mg, S, Fe, and Zn contents relative to ambient temperature conditions. Warming increased mature leaf C/N ratios and decreased N/P and C/P ratios and increased senesced leaf C/N and C/P ratios. Furthermore, W and W+RR reduced nutrient resorption efficiencies for N (6.3%), K (19.8%), S (70.9%) and increased Ca and Fe accumulation in senesced leaves (440% and 35.7%, respectively) relative to the control treatment. Rainfall reduction decreased the resorption efficiencies of N (6.7%), S (51%), and Zn (46%). Reductions in nutrient resorption efficiencies with warming and/or rainfall reduction were rather uniform and consistent across species. The negative impacts of warming and rainfall reduction on foliar nutrient resorption efficiency will likely cause an impairment of plant nutrient budgets and fitness across coexisting native shrubs in this nutrient-poor habitat, with probable implications for key ecosystem functions such as reductions in nutrient retention in vegetation, litter decomposition, and nutrient cycling rates.
机译:营养吸收是植物从衰老叶中恢复营养物的过程,并将它们重新分配给储存结构或更新组织。叶酸N和P的元素再吸收已被证明可以响应温度和降水,但我们对温暖和干旱的影响非常少了解这些和其他必需植物的吸收,这可能改变物种的能力回收他们的营养素。我们进行了一个5年的操纵田间研究,以模拟预测的气候变化条件,并研究了温暖(W),降雨量减少(RR)和它们的组合(W + RR)在半干旱中共存灌木种类的营养吸收效率的影响灌木丛。成熟和院长的叶片均响应于气候变化条件显示出营养物质内容物和改变的化学计量的显着降低。相对于环境温度条件,变暖(W,W + RR)降低成熟的叶片N,K,Ca,S,Fe和Zn和Sinesced Lea,Ca,Ca,Mg,S,Fe和Zn含量。升温成熟的成熟叶片C / N比率和下降N / P和C / P比率,并且增加了叶片C / N和C / P比率。此外,W和W + RR降低了N(6.3%),K(19.8%),S(70.9%),并增加了参赛叶(分别为440%和35.7%)增加了CA和Fe积累的营养吸收效率控制治疗。降雨降低降低了N(6.7%),S(51%)和Zn(46%)的吸收效率。减少营养吸收效率的减少和/或降雨减少的营养吸收效率相当均匀,跨种类一致。变暖和降雨降雨对叶面养分吸收效率的负面影响可能会导致植物营养预算和适应在这种营养疾病的栖息地中的植物营养预算和适应性,这对关键生态系统功能有可能影响,例如植被中养分保留的营养保留,凋落物分解和营养循环速率。

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