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Leaf nitrogen and phosphorus resorption of woody species in response to climatic conditions and soil nutrients: a meta-analysis

机译:木本植物叶片对氮和磷的吸收对气候条件和土壤养分的响应:荟萃分析

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摘要

Nutrient resorption before abscission is an important nutrient conservation mechanism regulated by climatic conditions and soil nutrients.However,our current understanding of leaf nutrient resorption is primarily derived from site-specific studies or from the use of green-leaf nutrient concentrations to represent those in soils.It remains unknown how nutrient resorption responds to natural soil-nutrient concentrations at a global scale.The effects of plant functional groups,climatic conditions,and soil nutrients and their interactions on leaf nutrient resorption are also unknown.In this study,we established a global database derived from 85 published papers,including 547 reports of nitrogen and phosphorus resorption efficiency (NRE and PRE),climatic factors (LAT,latitude;MAT,mean annual temperature;MAP,mean annual precipitation) and soil-nutrient data (STN,soil total nitrogen;STP,soil total phosphorus) across 111 research sites.The results demonstrated that mean NRE and PRE were 48.4 and 53.3%,respectively.NRE of trees was lower than those of shrubs.NRE and PRE of coniferous species were both higher than those of broad-leaved species.Evergreen species had higher PRE than did deciduous species.NRE was negatively related to STN,but PRE and STP were not related.Both NRE and PRE decreased with increasing MAT and MAP but increased with increasing LAT.Plant functional groups,climate and soil nutrients jointly explained 22 and 32% of the variations in NRE and PRE,respectively.It is important to note that climate (especially MAT) explained 12 and 29% of the variations in NRE and PRE,respectively,implying that continuing global warming will exert an increasingly profound influence on plant nutrient cycles.
机译:脱落前的养分吸收是重要的养分保护机制,受气候条件和土壤养分的调节。然而,我们目前对叶片养分吸收的了解主要来自于特定地点的研究或使用绿叶养分浓度来代表土壤中的养分。在全球范围内,养分吸收如何响应自然的土壤养分浓度仍是未知的。植物功能组,气候条件和土壤养分及其相互作用对叶片养分吸收的影响也是未知的。来自85篇已发表论文的全球数据库,其中包括547个氮磷吸收效率报告(NRE和PRE),气候因子(LAT,纬度; MAT,平均年温度; MAP,平均年降水量)和土壤养分数据(STN, 111个研究地点的土壤总氮(STP,土壤总磷)。结果表明,平均NRE和PRE为48.4 a分别为53.3%。树木的NRE低于灌木。针叶树种的NRE和PRE均高于阔叶树种。常绿树种的PRE高于落叶树种。NRE与STN负相关, NRE和PRE均随MAT和MAP的增加而降低,但随LAT的增加而升高。植物功能群,气候和土壤养分分别解释了NRE和PRE的22%和32%。需要注意的是,气候(尤其是MAT)分别解释了NRE和PRE的12%和29%的变化,这意味着持续的全球变暖将对植物养分循环产生越来越深远的影响。

著录项

  • 来源
    《林业研究(英文版)》 |2018年第4期|905-913|共9页
  • 作者

    Tao Yan; Jiaojun Zhu; Kai Yang;

  • 作者单位

    CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Shenyang 110016, People's Republic of China;

    Qingyuan Forest CERN, Chinese Academy of Sciences,Shenyang 110016, People's Republic of China;

    University of Chinese Academy of Sciences, Beijing 100049,People's Republic of China;

    CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Shenyang 110016, People's Republic of China;

    Qingyuan Forest CERN, Chinese Academy of Sciences,Shenyang 110016, People's Republic of China;

    CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Shenyang 110016, People's Republic of China;

    Qingyuan Forest CERN, Chinese Academy of Sciences,Shenyang 110016, People's Republic of China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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