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Characterizing the drivers of seedling leaf gas exchange responses to warming and altered precipitation: indirect and direct effects

机译:表征幼苗叶片气体交换对变暖和降水变化的响应:间接和直接影响

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摘要

Anthropogenic forces are projected to lead to warmer temperatures and altered precipitation patterns globally. The impact of these climatic changes on the uptake of carbon by the land surface will, in part, determine the rate and magnitude of these changes. However, there is a great deal of uncertainty in how terrestrial ecosystems will respond to climate in the future. Here, we used a fully factorial warming (four levels) by precipitation (three levels) manipulation experiment in an old-field ecosystem in the northeastern USA to examine the impact of climatic changes on leaf carbon exchange in five species of deciduous tree seedlings. We found that photosynthesis generally increased in response to increasing precipitation and decreased in response to warming. Respiration was less sensitive to the treatments. The net result was greater leaf carbon uptake in wetter and cooler conditions across all species. Structural equation modelling revealed the primary pathway through which climate impacted leaf carbon exchange. Net photosynthesis increased with increasing stomatal conductance and photosynthetic enzyme capacity (Vcmax), and decreased with increasing respiration of leaves. Soil moisture and leaf temperature at the time of measurement most heavily influenced these primary drivers of net photosynthesis. Leaf respiration increased with increasing soil moisture, leaf temperature, and photosynthetic supply of substrates. Counter to the soil moisture response, respiration decreased with increasing precipitation amount, indicating that the response to short- (i.e. soil moisture) versus long-term (i.e. precipitation amount) water stress differed, possibly as a result of changes in the relative amounts of growth and maintenance demand for respiration over time. These data (>500 paired measurements of light and dark leaf gas exchange), now publicly available, detail the pathways by which climate can impact leaf gas exchange and could be useful for testing assumptions in land surface models.
机译:人为力量预计将导致全球气温升高和降水方式改变。这些气候变化对陆地表面碳吸收的影响将部分决定这些变化的速度和幅度。但是,未来陆地生态系统如何应对气候存在很多不确定性。在这里,我们在美国东北部的一个旧田生态系统中通过降水(三级)操纵实验使用了完全因子变暖(四级),研究了气候变化对五种落叶树种幼苗叶片碳交换的影响。我们发现,光合作用通常响应于增加的降水而增加,而响应于变暖而降低。呼吸对治疗较不敏感。最终结果是在所有物种的潮湿和凉爽条件下,叶片碳吸收量更大。结构方程模型揭示了气候影响叶片碳交换的主要途径。净光合作用随气孔导度和光合酶容量(Vcmax)的增加而增加,随叶片呼吸的增加而减少。测量时的土壤水分和叶片温度对净光合作用的这些主要驱动力影响最大。叶片呼吸随着土壤湿度,叶片温度和基质光合作用的增加而增加。与土壤水分响应相反,呼吸随着降水量的增加而减少,表明对短期(即土壤水分)与长期(即降水量)水分胁迫的响应有所不同,这可能是由于土壤相对水分含量的变化所致。随着时间的流逝,呼吸的增长和维持需求。这些数据(> 500对浅色和深色烟气交换量的配对测量值)现已公开,详细说明了气候影响烟气交换的途径,可用于测试陆地表面模型中的假设。

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