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首页> 外文期刊>Rapid Communications in Mass Spectrometry: RCM >Leaf transition from heterotrophy to autotrophy is recorded in the intraleaf C, H and O isotope patterns of leaf organic matter
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Leaf transition from heterotrophy to autotrophy is recorded in the intraleaf C, H and O isotope patterns of leaf organic matter

机译:从异常对自触发的叶片过渡记录在叶片有机物的巢莴苣C,H和O同位素模式中

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摘要

Rationale Quantitatively relating(13)C/C-12,H-2/H-1 and(18)O/O-16 ratios of plant alpha-cellulose and(2)H/H-1 ofn-alkanes to environmental conditions and metabolic status should ideally be based on the leaf, the plant organ most sensitive to environmental change. The fact that leaf organic matter is composed of isotopically different heterotrophic and autotrophic components means that it is imperative that one be able to disentangle the relative heterotrophic and autotrophic contributions to leaf organic matter. Methods We tackled this issue by two-dimensional sampling of leaf water and alpha-cellulose, and specificn-alkanes from greenhouse-grown immature and mature and field-grown mature banana leaves, taking advantage of their large areas and thick waxy layers. Leaf water, alpha-cellulose andn-alkane isotope ratios were then characterized using elemental analysis isotope ratio mass spectrometry (IRMS) or gas chromatography IRMS. A three-member (heterotrophy, autotrophy and photoheterotrophy) conceptual linear mixing model was then proposed for disentangling the relative contributions of the three trophic modes. Results We discovered distinct spatial leaf water, alpha-cellulose andn-alkane isotope ratio patterns that varied with leaf developmental stages. We inferred from the conceptual model that, averaged over the leaf blade, only 20% of alpha-cellulose in banana leaf is autotrophically laid down in both greenhouse-grown and field-grown banana leaves, while approximately 60% and 100% ofn-alkanes are produced autotrophically in greenhouse-grown and field-grown banana leaves, respectively. There exist distinct lateral (edge to midrib) gradients in autotrophic contributions of alpha-cellulose andn-alkanes. Conclusions Efforts to establish quantitative isotope-environment relationships should take into account the fact that the evaporative leaf water(18)O and(2)H enrichment signal recorded in autotrophically laid down alpha-cellulose is significantly diluted by the heterotrophically formed alpha-cellulose. The delta H-2 value of field-grown mature banana leafn-alkanes is much more sensitive than alpha-cellulose as a recorder of the growth environment. Quantitative isotope-environment relationship based on greenhouse-grownn-alkane delta H-2 values may not be reliable.
机译:理论定量相关(13)C / C-12,H-2 / H-1和(18)O / O-16的植物α-纤维素的比率和(2)H / H-1的烷烃与环境条件和代谢状态理想地应基于叶子,植物器官对环境变化最敏感。叶有机物由同位素不同的异养和自养成品组成的事实是指必须使得能够解开对叶有机质的相对异养和自养贡献。方法通过叶水和α-纤维素的二维取样,以及来自温室生长的未成熟和成熟和野外成熟的香蕉叶的特异性烷烃,利用它们的大面积和厚蜡质层来解决这一问题。然后使用元素分析同位素比质谱(IRMS)或气相色谱IRMS表征叶水,α-纤维素Andn-烷烃同位素比。然后提出了一种三个成员(异营养,自触发和光检查器)概念线性混合模型,用于解除三种营养模式的相对贡献。结果我们发现了与叶发育阶段变化的明显的空间叶片水,α-纤维素AndN-烷烃同位素比例。从概念模型推断,在叶片上平均,香蕉叶中只有20%的α-纤维素在温室生长和田间生长的香蕉叶中自动铺设,而大约60%和100%的烷烃分别以温室生长和野外生长的香蕉叶为自身繁殖。在α-纤维素Andn-烷烃的自养贡献中存在明显的横向(边缘到MIDRIB)梯度。结论建立定量同位素环境关系的努力应考虑到蒸发叶片水(18)o和(2)H浓缩信号在自营形成的α-纤维素中显着稀释。现场生长的成熟香蕉叶烷基烷烃的ΔH-2值比α-纤维素更敏感,作为生长环境的记录器。基于温室生成的烷烃δH-2值的定量同位素环境关系可能不可靠。

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  • 作者单位

    Shaanxi Univ Sci &

    Technol Sch Chem &

    Chem Engn Isotop Chem Biol Weiyang Univ Pk Xian 710021 Peoples R China;

    MNR Third Inst Oceanol Lab Marine &

    Coastal Geol 178 Daxue Rd Xiamen 361005 Peoples R China;

    Shenzhen Univ Sch Life &

    Marine Sci 3688 Nanhai Rd Shenzhen 518060 Peoples R China;

    Shaanxi Univ Sci &

    Technol Sch Chem &

    Chem Engn Isotop Chem Biol Weiyang Univ Pk Xian 710021 Peoples R China;

    Shaanxi Univ Sci &

    Technol Sch Chem &

    Chem Engn Isotop Chem Biol Weiyang Univ Pk Xian 710021 Peoples R China;

    Shaanxi Univ Sci &

    Technol Sch Chem &

    Chem Engn Isotop Chem Biol Weiyang Univ Pk Xian 710021 Peoples R China;

    Shaanxi Univ Sci &

    Technol Sch Chem &

    Chem Engn Isotop Chem Biol Weiyang Univ Pk Xian 710021 Peoples R China;

    Shaanxi Univ Sci &

    Technol Sch Chem &

    Chem Engn Isotop Chem Biol Weiyang Univ Pk Xian 710021 Peoples R China;

    Shaanxi Univ Sci &

    Technol Sch Chem &

    Chem Engn Isotop Chem Biol Weiyang Univ Pk Xian 710021 Peoples R China;

    MNR Third Inst Oceanol Lab Marine &

    Coastal Geol 178 Daxue Rd Xiamen 361005 Peoples R China;

    Swiss Fed Inst Forest Snow &

    Landscape Res CH-8903 Birmensdorf Switzerland;

    Shaanxi Univ Sci &

    Technol Sch Chem &

    Chem Engn Isotop Chem Biol Weiyang Univ Pk Xian 710021 Peoples R China;

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  • 正文语种 eng
  • 中图分类 分析化学;
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