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首页> 外文期刊>Global change biology >Increased temperature and precipitation interact to affect root production, mortality, and turnover in a temperate steppe: implications for ecosystem C cycling
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Increased temperature and precipitation interact to affect root production, mortality, and turnover in a temperate steppe: implications for ecosystem C cycling

机译:温度和降水的增加会影响温带草原的根系产量,死亡率和周转率:对生态系统碳循环的影响

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Fine root production and turnover play important roles in regulating carbon (C) cycling in terrestrial ecosystems. In order to examine effects of climate change on root production and turnover, a field experiment with increased temperature and precipitation had been conducted in a semiarid temperate steppe in northern China since April 2005. Experimental warming decreased annual root production, mortality, and mean standing crop by 10.3%, 12.1%, 7.0%, respectively, while root turnover was not affected in 2006 and 2007 by the warming. Annual root production and turnover was 5.9% and 10.3% greater in the elevated than ambient precipitation plots. Changes in root production and mortality in response to increased temperature and precipitation could be largely attributed to the changes in gross ecosystem productivity (GEP) and belowground/aboveground C allocation. There were significant interactive effects of warming and increased precipitation on root productivity, mortality, and standing crop. Experimental warming had positive and negative effects on the three root variables (root production, mortality, standing crop) under ambient and increased precipitation, respectively. Increased precipitation stimulated and suppressed the three root variables in the unwarmed and warmed subplots, respectively. The positive dependence of soil respiration and ecosystem respiration upon root productivity and mortality highlights the important role of root dynamics in ecosystem C cycling. The nonadditive effects of increased temperature and precipitation on root productivity, mortality, and standing crop observed in this study are critical for model projections of climate-ecosystem feedbacks. These findings indicate that carbon allocation is a focal point for future research and that results from single factor experiments should be treated with caution because of factor interactions.
机译:优良的根系生产和周转在调节陆地生态系统中的碳(C)循环中起着重要作用。为了研究气候变化对根系产量和周转量的影响,自2005年4月以来,在中国北方的半干旱温带草原上进行了温度和降水增加的田间试验。试验性变暖降低了每年的根系产量,死亡率和平均单季产量分别增长了10.3%,12.1%和7.0%,而2006年和2007年的变暖并未影响根的周转。与高海拔降水区相比,高架区的年生根产量和周转量分别高5.9%和10.3%。随着温度和降水的增加,根系产量和死亡率的变化可能主要归因于生态系统总生产力(GEP)和地下/地上碳分配的变化。变暖和降水增加对根系生产力,死亡率和站立作物具有显着的交互作用。实验性增温分别对环境和增加降水量下的三个根系变量(根系产量,死亡率,站立作物)产生正向和负向影响。降水增加分别刺激和抑制了未加热和加热子图中的三个根变量。土壤呼吸和生态系统呼吸对根系生产力和死亡率的正相关性凸显了根系动力学在生态系统C循环中的重要作用。在这项研究中观察到的温度和降水增加对根系生产力,死亡率和站立作物的非累加效应对于气候-生态系统反馈的模型预测至关重要。这些发现表明,碳分配是未来研究的重点,由于因素相互作用,单因素实验的结果应谨慎对待。

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