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Water Relations Link Carbon and Oxygen Isotope Discrimination to Phloem Sap Sugar Concentration in Eucalyptus globulus

机译:水关系将桉树球茎中韧皮部汁液糖的浓度与碳氧同位素的鉴别联系起来

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摘要

A strong correlation was previously observed between carbon isotope discrimination (Δ13C) of phloem sap sugars and phloem sap sugar concentration in the phloem-bleeding tree Eucalyptus globulus Labill. (J. Pate, E. Shedley, D. Arthur, M. Adams [1998] Oecologia 117: 312–322). We hypothesized that correspondence between these two parameters results from covarying responses to plant water potential. We expected Δ13C to decrease with decreasing plant water potential and phloem sap sugar concentration to increase, thereby maintaining turgor within sieve tubes. The hypothesis was tested with analyses of E. globulus trees growing on opposite ends of a rainfall gradient in southwestern Australia. The Δ13C of phloem sap sugars was closely related to phloem sap sugar concentration (r = −0.90, P < 0.0001, n = 40). As predicted, daytime shoot water potential was positively related to Δ13C (r = 0.70, P < 0.0001, n = 40) and negatively related to phloem sap sugar concentration (r = −0.86, P < 0.0001, n = 40). Additional measurements showed a strong correspondence between predawn shoot water potential and phloem sap sugar concentration measured at midday (r = −0.87, P < 0.0001, n = 30). The Δ13C of phloem sap sugars collected from the stem agreed well with that predicted from instantaneous measurements of the ratio of intercellular to ambient carbon dioxide concentrations on subtending donor leaves. In accordance, instantaneous ratio of intercellular to ambient carbon dioxide concentrations correlated negatively with phloem sap sugar concentration (r = −0.91, P < 0.0001, n = 27). Oxygen isotope enrichment (Δ18O) in phloem sap sugars also varied with phloem sap sugar concentration (r = 0.91, P < 0.0001, n = 39), consistent with predictions from a theoretical model of Δ18O. We conclude that drought induces correlated variation in the concentration of phloem sap sugars and their isotopic composition in E. globulus.
机译:先前曾观察到韧皮部树液糖的碳同位素鉴别(Δ 13 C)与韧皮部出血树桉树Labill中韧皮部树液糖浓度之间存在强相关性。 (J. Pate,E. Shedley,D. Arthur,M.Adams [1998] Oecologia 117:312-322)。我们假设这两个参数之间的对应关系来自对植物水势的共变响应。我们预计Δ 13 C随植物水势的降低而降低,韧皮部汁液中糖的浓度升高,从而保持筛管内的膨胀。通过分析在澳大利亚西南部降雨梯度的相对两端生长的E. globulus树对这一假设进行了检验。韧皮树汁糖的Δ 13 C与韧皮树汁糖的浓度密切相关(r = -0.90,P <0.0001,n = 40)。如预测的那样,白天芽水势与Δ 13 C正相关(r = 0.70,P <0.0001,n = 40),与韧皮树汁糖浓度呈负相关(r = -0.86,P < 0.0001,n = 40)。其他测量结果显示,黎明前的芽水势与韧皮部汁液糖浓度在中午之间有很强的对应性(r = -0.87,P <0.0001,n = 30)。从茎中收集的韧皮部树液糖的Δ 13 C与瞬时测量供体叶片上细胞间与周围二氧化碳浓度之比所预测的相符。因此,细胞间与周围二氧化碳浓度的瞬时比值与韧皮部汁液糖浓度呈负相关(r = -0.91,P <0.0001, n = 27)。韧皮树汁糖中的氧同位素富集(Δ 18 O)也随韧皮树汁糖浓度的变化而变化( r = 0.91, P <0.0001,< em> n = 39),与Δ 18 O的理论模型的预测一致。我们得出结论,干旱导致 E中韧皮部汁液糖的浓度及其同位素组成发生相关变化。 globulus

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