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首页> 外文期刊>Global change biology >Temperature and precipitation controls over leaf- and ecosystem-level CO2 flux along a woody plant encroachment gradient.
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Temperature and precipitation controls over leaf- and ecosystem-level CO2 flux along a woody plant encroachment gradient.

机译:木本植物入侵梯度下叶片和生态系统水平的CO 2 通量的温度和降水控制。

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Conversion of grasslands to woodlands may alter the sensitivity of CO2 exchange of individual plants and entire ecosystems to air temperature and precipitation. We combined leaf-level gas exchange and ecosystem-level eddy covariance measurements to quantify the effects of plant temperature sensitivity and ecosystem temperature responses within a grassland and mesquite woodland across seasonal precipitation periods. In so doing, we were able to estimate the role of moisture availability on ecosystem temperature sensitivity under large-scale vegetative shifts. Optimum temperatures (Topt) for net photosynthetic assimilation (A) and net ecosystem productivity (NEP) were estimated from a function fitted to A and NEP plotted against air temperature. The convexities of these temperature responses were quantified by the range of temperatures over which a leaf or an ecosystem assimilated 50% of maximum NEP ( Omega 50). Under dry pre- and postmonsoon conditions, leaf-level Omega 50 in C3 shrubs were two-to-three times that of C4 grasses, but under moist monsoon conditions, leaf-level Omega 50 was similar between growth forms. At the ecosystems-scale, grassland NEP was more sensitive to precipitation, as evidenced by a 104% increase in maximum NEP at monsoon onset, compared to a 57% increase in the woodland. Also, woodland NEP was greater across all temperatures experienced by both ecosystems in all seasons. By maintaining physiological function across a wider temperature range during water-limited periods, woody plants assimilated larger amounts of carbon. This higher carbon-assimilation capacity may have significant implications for ecosystem responses to projected climate change scenarios of higher temperatures and more variable precipitation, particularly as semiarid regions experience conversions from C4 grasses to C3 shrubs. As regional carbon models, CLM 4.0, are now able to incorporate functional type and photosynthetic pathway differences, this work highlights the need for a better integration of the interactive effects of growth form/functional type and photosynthetic pathway on water resource acquisition and temperature sensitivity.Digital Object Identifier http://dx.doi.org/10.1111/j.1365-2486.2011.02599.x
机译:草地向林地的转化可能会改变单个植物和整个生态系统的CO 2 交换对气温和降水的敏感性。我们将叶级气体交换和生态系统级涡动协方差测量相结合,以量化季节性降水期间草原和豆科灌木林内植物温度敏感性和生态系统温度响应的影响。通过这样做,我们能够估计大规模植被转移下水分供应对生态系统温度敏感性的作用。净光合同化( A )和净生态系统生产力(NEP)的最佳温度( T opt )是根据与 A 和NEP对空气温度作图。这些温度响应的凸度通过叶片或生态系统吸收最大NEP(Omega 50 )的50%的温度范围来量化。在季风前后,干旱的条件下,C 3 灌木中叶水平的欧米茄 50 是C 4 草的二至三倍,但是在潮湿的季风条件下,叶片水平的欧米茄 50 在生长形式之间相似。在生态系统范围内,草原NEP对降水更加敏感,季风开始时最大NEP增加了104%,而林地增加了57%,这证明了这一点。此外,在两个季节所有生态系统经历的所有温度下,林地NEP都更大。通过在缺水时期在更宽的温度范围内维持生理功能,木本植物吸收了大量的碳。更高的碳同化能力可能会对生态系统对预计的高温和更多降水的气候变化情景的反应产生重大影响,尤其是在半干旱地区经历了C 4 草向C 3 < / sub>灌木。随着区域碳模型CLM 4.0现在能够合并功能类型和光合途径差异,这项工作凸显了需要更好地整合生长形式/功能类型与光合途径对水资源获取和温度敏感性的相互作用。数字对象标识符http://dx.doi.org/10.1111/j.1365-2486.2011.02599.x

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