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Strong Coupling of Shoot Assimilation and Soil Respiration during Drought and Recovery Periods in Beech As Indicated by Natural Abundance δ13C Measurements

机译:自然丰度δ13C测量表明山毛榉干旱和恢复期间的同化芽与土壤呼吸之间的强耦合

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摘要

Drought down-regulates above- and belowground carbon fluxes, however, the resilience of trees to drought will also depend on the speed and magnitude of recovery of these above- and belowground fluxes after re-wetting. Carbon isotope composition of above- and belowground carbon fluxes at natural abundance provides a methodological approach to study the coupling between photosynthesis and soil respiration (SR) under conditions (such as drought) that influence photosynthetic carbon isotope discrimination. In turn, the direct supply of root respiration with recent photoassimilates will impact on the carbon isotope composition of soil-respired CO2. We independently measured shoot and soil CO2 fluxes of beech saplings (Fagus sylvatica L.) and their respective δ13C continuously with laser spectroscopy at natural abundance. We quantified the speed of recovery of drought stressed trees after re-watering and traced photosynthetic carbon isotope signal in the carbon isotope composition of soil-respired CO2. Stomatal conductance responded strongly to the moderate drought (-65%), induced by reduced soil moisture content as well as increased vapor pressure deficit. Simultaneously, carbon isotope discrimination decreased by 8‰, which in turn caused a significant increase in δ13C of recent metabolites (1.5–2.5‰) and in δ13C of SR (1–1.5‰). Generally, shoot and soil CO2 fluxes and their δ13C were in alignment during drought and subsequent stress release, clearly demonstrating a permanent dependence of root respiration on recently fixed photoassimilates, rather than on older reserves. After re-watering, the drought signal persisted longer in δ13C of the water soluble fraction that integrates multiple metabolites (soluble sugars, amino acids, organic acids) than in the neutral fraction which represents most recently assimilated sugars or in the δ13C of SR. Nevertheless, full recovery of all aboveground physiological variables was reached within 4 days – and within 7 days for SR – indicating high resilience of (young) beech against moderate drought.
机译:干旱会下调地下和地下的碳通量,但是,树木对干旱的恢复力还取决于重新润湿后这些地下和地下的通量的恢复速度和幅度。自然丰度下和地下碳通量的碳同位素组成提供了一种方法学方法,用于研究在影响光合碳同位素判别的条件(例如干旱)下光合作用与土壤呼吸(SR)之间的耦合。反过来,最近的光同化物对根呼吸的直接供应将影响土壤呼吸的CO2的碳同位素组成。我们用自然丰度的激光光谱法连续独立地测量了山毛榉树苗(Fagus sylvatica L.)及其各自的δ 13 C的芽和土壤CO2通量。我们量化了再浇水后干旱胁迫树木的恢复速度,并在土壤呼吸的CO2的碳同位素组成中追踪了光合作用的碳同位素信号。气孔导度对中等干旱(-65%)有强烈的响应,这是由于土壤水分含量降低以及蒸气压赤字增加引起的。同时,碳同位素分辨力下降了8‰,这又导致最近代谢产物的δ 13 C(1.5–2.5‰)和δ 13 C显着增加。 SR(1-1.5‰)。通常,在干旱和随后的压力释放过程中,枝条和土壤中的CO2通量及其δ 13 C处于一致状态,这清楚表明根系呼吸作用永久依赖于最近固定的光同化物,而不是较老的储备物。重新浇水后,干旱信号在包含多种代谢产物(可溶性糖,氨基酸,有机酸)的水溶性部分的δ 13 C中持续的时间比在最近被吸收的中性部分中的持续时间更长。糖或SR的δ 13 C中。但是,在SR的4天内和7天内,所有地上的生理变量都已完全恢复,这表明(幼)山毛榉对中度干旱具有很高的复原力。

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