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Nutrient resorption in tropical savanna forests and woodlands of central Brazil

机译:巴西中部热带稀树草原森林和林地的养分吸收

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Nutrient limitation in Brazilian savanna (known as cerrado) presumably causes trees to maximize nutrient resorption from senesced leaves to reduce their dependence on nutrient availability. To assess patterns between nutrient resorption and soil fertility, we measured community-level nitrogen (N), phosphorus (P), and potassium (K) concentrations in mature and senesced leaves and soil fertility in the upper 50 cm soil layer in structurally diverse cerrado ecosystems in the Cuiaba Basin (CB) and Pantanal (PAN) of Mato Grosso, Brazil. Foliar nutrient concentration data were used to estimate resorption efficiency and proficiency, and correlation was used to determine whether resorption efficiency and proficiency varied across soil fertility gradients. We found that N and P resorption proficiency (NRP and PRP, respectively) and P resorption efficiency (PRE) increased significantly as total soil N (NRP) and extractable P (PRP and PRE) declined. In contrast, K resorption efficiency (KRE) declined as soil sand content and bulk density increased, which was likely due to a reduction in soil water-holding capacity. Leaf N/P ratios indicate potential N limitation and/or N + P co-limitation for ecosystems in the PAN and P limitation and/or N + P co-limitation for ecosystems in the CB, while trends in leaf N/K ratios indicate possible K or K + P co-limitation for the CB only. Our results illustrate that cerrado forests and woodlands have highly variable nutrient resorption capacities that vary predictably across soil fertility or textural gradients and indicate that cerrado communities have flexible nutrient resorption that can reduce their dependence on soil nutrient availability
机译:巴西稀树草原(称为塞拉多)的营养限制可能导致树木最大限度地从衰老的叶片中吸收养分,以减少其对养分利用率的依赖。为了评估养分吸收与土壤肥力之间的关系,我们测量了成熟和衰老叶片中社区水平的氮(N),磷(P)和钾(K)浓度以及结构多样的塞拉多50 cm土层上部的土壤肥力巴西马托格罗索州库亚巴盆地(CB)和潘塔纳尔(PAN)的生态系统。叶面养分浓度数据用于估算吸收效率和熟练程度,相关性用于确定土壤肥力梯度之间的吸收效率和熟练程度是否有所不同。我们发现,随着土壤总氮(NRP)和可提取磷(PRP和PRE)的下降,氮和磷的吸收能力(分别为NRP和PRP)和P吸收效率(PRE)显着提高。相反,随着土壤含沙量和堆积密度的增加,钾的吸收效率(KRE)下降,这很可能是由于土壤持水量降低所致。叶片N / P比表明PAN中生态系统的潜在N限制和/或N + P共同限制,以及CB中生态系统的P限制和/或N + P共同限制,而叶片N / K比的趋势表明仅对CB可能的K或K + P共限制。我们的结果表明,塞拉多森林和林地的养分吸收能力变化很大,在土壤肥力或质地梯度之间变化可预测,并且表明塞拉多群落具有灵活的养分吸收能力,可以减少对土壤养分有效性的依赖

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