首页> 外文期刊>Plant Ecology >Annual ring widths are good predictors of changes in net primary productivity of alpine Rhododendron shrubs in the Sergyemla Mountains, southeast Tibet
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Annual ring widths are good predictors of changes in net primary productivity of alpine Rhododendron shrubs in the Sergyemla Mountains, southeast Tibet

机译:年轮宽度很好地预测了藏东南东南部塞尔吉姆拉山的高山杜鹃灌木净初级生产力的变化

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摘要

It is unclear whether annual ring widths (ARW) are good predictors of changes in net primary productivity (NPP) of trees or shrubs in cold environments. We test if the simulated NPP with inputs of observed leaf nitrogen concentration (N mass) and carbon isotope ratio (δ13C) explains altitudinal variations of ARW, relative growth rate (RGR), and maximum photosynthetic rate (P max) within a widespread woody species at moist timberline ecotones. We measured plant-level ARW and RGR, and related leaf traits (P max, N mass, δ13C etc.) for an alpine Rhododendron shrub (R. aganniphum var. schizopeplum) across ten altitudes (4,190–4,500 m) in the Sergyemla Mountains, southeast Tibet. Based on climate data available from Nyingchi station at 3,000 m, non-age-related ARW chronologies (1960–2008) for each of ten altitudes were positively correlated with June mean temperature, but related little with precipitation and other monthly mean temperatures. With increasing altitude, N mass and P max decreased and δ13C increased, resulting in decreases of observed RGR and simulated NPP. Current-year and recent 50-year-averaged ARWs were well correlated with observed RGR and P max and simulated NPP. June mean temperature explained 62 % of the altitudinal variations in observed RGR and ARW as well as simulated NPP. At moist high altitudes, ARWs can be used as predictors of changes in NPP of alpine shrubs because the low temperature in the early growing season is the primary factor limiting both ARW and NPP. This study suggests a methodology detecting the sensitivity of alpine woody species to varying climatic conditions.
机译:目前尚不清楚年轮宽度(ARW)是否能很好地预测寒冷环境中树木或灌木的净初级生产力(NPP)的变化。我们用观察到的叶氮浓度(N质量)和碳同位素比(δ13 C)的输入来测试模拟的NPP是否解释了ARW的垂直变化,相对生长率(RGR)和最大光合速率(P max )在潮湿的林线过渡带的广泛木本物种中。我们测量了高山杜鹃灌木(R. aganniphum var。schizopeplum)的植物水平ARW和RGR以及相关的叶片性状(P max ,N质量,δ13 C等)。跨越西藏东南部塞吉内姆拉山脉的十个海拔高度(4,190–4,500 m)。根据林芝站3000 m处的气候数据,十个海拔高度中与年龄无关的ARW时间序列(1960-2008年)与6月的平均温度呈正相关,而与降水和其他月平均温度的相关性则很小。随着海拔的升高,N质量和P max 降低,δ13 C升高,导致观测到的RGR和模拟NPP降低。当前和最近50年的平均ARW与观察到的RGR和P max 以及模拟的NPP密切相关。 6月的平均温度解释了所观察到的RGR和ARW以及模拟NPP的高度变化的> 62%。在潮湿的高海拔地区,ARW可以用作高山灌木NPP变化的预测指标,因为生长季节早期的低温是限制ARW和NPP的主要因素。这项研究提出了一种检测高山木本物种对不同气候条件的敏感性的方法。

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  • 来源
    《Plant Ecology》 |2012年第11期|p.1843-1855|共13页
  • 作者单位

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, 4A Datun Rd., Chaoyang District, Beijing, 100101, China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, 4A Datun Rd., Chaoyang District, Beijing, 100101, China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, 4A Datun Rd., Chaoyang District, Beijing, 100101, China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, 4A Datun Rd., Chaoyang District, Beijing, 100101, China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau R;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Alpine shrub; Carbon gain; Leaf traits; Ring-width growth; Timberline;

    机译:高山灌丛;碳吸收;叶片性状;环宽生长;林线;

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