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首页> 外文期刊>Global change biology >Effects of climate change on labile and structural carbon in Douglas-fir needles as estimated by delta C-13 and C-area measurements
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Effects of climate change on labile and structural carbon in Douglas-fir needles as estimated by delta C-13 and C-area measurements

机译:气候变化对道格拉斯冷杉针中不稳定碳和结构碳的影响,通过δC-13和C面积测量估算

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Models of photosynthesis, respiration, and export predict that foliar labile carbon (C) should increase with elevated CO2 but decrease with elevated temperature. Sugars, starch, and protein can be compared between treatments, but these compounds make up only a fraction of the total labile pool. Moreover, it is difficult to assess the turnover of labile carbon between years for evergreen foliage. Here, we combined changes in foliar C-area (C concentration on an areal basis) as needles aged with changes in foliar isotopic composition (delta(13) C) caused by inputs of (13) C-depleted CO2 to estimate labile and structural C in needles of different ages in a four-year, closed-chamber mesocosm experiment in which Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) seedlings were exposed to elevated temperature (ambient + 3.5 degreesC) and CO2 (ambient + 179 ppm). Declines in delta (13) C of needle cohorts as they aged indicated incorporation of newly fixed labile or structural carbon. The delta (13) C calculations showed that new C was 41 +/- 2% and 28 +/- 3% of total needle carbon in second- and third-year needles, respectively, with higher proportions of new C in elevated than ambient CO2 chambers (e.g. 42 +/- 2% vs. 37 +/- 6%, respectively, for second-year needles). Relative to ambient CO2 , elevated CO2 increased labile C in both first- and second-year needles. Relative to ambient temperature, elevated temperature diminished labile C in second-year needles but not in first-year needles, perhaps because of differences in sink strength between the two needle age classes. We hypothesize that plant-soil feedbacks on nitrogen supply contributed to higher photosynthetic rates under elevated temperatures that partly compensated for higher turnover rates of labile C. Strong positive correlations between labile C and sugar concentrations suggested that labile C was primarily determined by carbohydrates. Labile C was negatively correlated with concentrations of cellulose and protein. Elevated temperature increased foliar %C, possibly due to a shift of labile constituents from low %C carbohydrates to relatively high %C protein. Decreased sugar concentrations and increased nitrogen concentrations with elevated temperature were consistent with this explanation. Because foliar constituents that vary in isotopic signature also vary in concentrations with leaf age or environmental conditions, inferences of c (i) /c (a) values from delta (13) C of bulk leaf tissue should be done cautiously. Tracing of (13) C through foliar carbon pools may provide new insight into foliar C constituents and turnover. [References: 42]
机译:光合作用,呼吸作用和出口的模型预测,叶面不稳定碳(C)随CO2升高而增加,但随温度升高而降低。可以在处理之间比较糖,淀粉和蛋白质,但这些化合物仅占总不稳定成分的一小部分。此外,很难评估常绿叶片多年间不稳定碳的转化率。在这里,我们结合了针叶的C面积变化(以面积为单位的C浓度)与由于(13)贫C的二氧化碳的输入引起的叶同位素组成变化(δ(13)C)的变化,以估计不稳定和结构在一项为期四年的封闭室中观试验中,将不同年龄的针叶中的碳暴露在其中,道格拉斯冷杉(Pseudotsuga menziesii(Mirb。)Franco)幼苗暴露于高温(环境+ 3.5摄氏度)和CO2(环境+ 179 ppm)下)。随着年龄增长,针头队列的增量(13)C下降表明新加入了不稳定的固定碳或结构碳。 δ(13)C计算表明,第二年和第三年针头的新碳分别占总针头碳的41 +/- 2%和28 +/- 3%,并且升高的新C的比例比环境中的高二氧化碳室(例如,二年级针头分别为42 +/- 2%和37 +/- 6%)。相对于环境中的CO2,升高的CO2增加了第一年和第二年针头中的不稳定C。相对于环境温度,升高的温度降低了二年级针头的不稳定C值,但不降低了第一年级针头的不稳定C值,这可能是由于两个年龄段的针头的沉陷强度不同所致。我们假设植物土壤对氮供应的反馈有助于提高高温下的光合作用速率,从而部分补偿了不稳定碳的较高周转率。不稳定碳与糖浓度之间的强正相关性表明,不稳定碳主要由碳水化合物决定。不稳定碳与纤维素和蛋白质的浓度呈负相关。升高的温度增加了叶面%C的含量,这可能是由于不稳定成分从低%C的碳水化合物转移到了相对较高的%C的蛋白质造成的。随着温度升高,糖浓度降低和氮浓度升高与该解释一致。由于同位素特征不同的叶成分也随着叶龄或环境条件的变化而变化,因此应谨慎地根据大叶组织的δ(13)C推断c(i)/ c(a)值。通过叶碳库追踪(13)C可能会提供有关叶C成分和周转的新见解。 [参考:42]

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