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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Leaf water deuterium enrichment shapes leaf wax n-alkane δD values of angiosperm plants II: Observational evidence and global implications
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Leaf water deuterium enrichment shapes leaf wax n-alkane δD values of angiosperm plants II: Observational evidence and global implications

机译:叶水氘富集塑造被子植物叶蜡的正构烷烃δD值II:观测证据和全球意义

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Leaf wax n-alkanes are long-chain hydrocarbons that can persist in sedimentary records over geological timescales. Since their hydrogen isotopic composition (expressed as a δD value) can be correlated to the δD values of precipitation, leaf wax n-alkane δD values have been advocated as new and powerful proxies for paleohydrological research. The exact type of hydrological information that is recorded in the δD values of leaf wax n-alkanes remains, however, unclear. In a companion paper we provide experimental evidence showing that the δD values of leaf wax n-alkanes of angiosperm plants grown under controlled environmental conditions not only reflect δD values of precipitation - as has often been assumed - but that evaporative deuterium (D)-enrichment of leaf water has an additional critical effect on their δD values. Here we present a detailed observational study that illustrates that evaporative D-enrichment of leaf water also affects the δD values of leaf wax n-alkanes in plants from natural ecosystems along a 1500. km climate gradient in Northern Australia. Based on global simulations of leaf water D-enrichment we show that the effects of evaporative D-enrichment of leaf water on leaf wax n-alkane δD values is relevant in all biomes but that it is particularly important in arid environments. Given the combined influence of precipitation δD values and leaf water D-enrichment we argue that leaf wax n-alkane δD values contain an integrated signal that can provide general hydrological information, e.g. on the aridity of a catchment area. We also suggest that more specific hydrological information and even plant physiological information can be obtained from leaf wax n-alkanes if additional indicators are available to constrain the plant- and precipitation-derived influences on their δD values. As such, our findings have important implications for the interpretation of leaf wax n-alkane δD values from paleohydrological records. In addition, our investigations open the door to employ δD values of leaf wax n-alkanes as new ecohydrological proxies in contemporary plant and ecosystem sciences.
机译:叶蜡正构烷烃是长链烃,可以在地质时标上保留在沉积记录中。由于它们的氢同位素组成(表示为δD值)可以与降水的δD值相关,因此人们提倡叶蜡正烷烃δD值是古水文学研究的新的有力代表。叶蜡正构烷烃的δD值记录的确切水文信息类型仍然不清楚。在随附的论文中,我们提供了实验证据,表明在受控环境条件下生长的被子植物的叶蜡正构烷烃的δD值不仅反映了降水的δD值(通常认为是),而且蒸发性氘(D)富集叶水对其δD值具有额外的关键影响。在这里,我们提供了一项详细的观察性研究,该研究表明,叶水的蒸发D富集也会影响北澳大利亚州1500公里气候梯度下自然生态系统中植物中叶蜡正构烷烃的δD值。基于叶水D富集的全球模拟,我们显示了叶水蒸发D富集对叶蜡正构烷烃δD值的影响在所有生物群落中都相关,但在干旱环境中尤为重要。考虑到降水δD值和叶水D富集的综合影响,我们认为叶蜡正构烷烃δD值包含可以提供一般水文信息的综合信号,例如在一个集水区的干旱。我们还建议,如果可以使用其他指标来限制植物和降水对它们的δD值的影响,则可以从叶蜡正构烷烃中获得更具体的水文信息,甚至植物生理信息。因此,我们的发现对从古水文记录中解释叶蜡正构烷烃的δD值具有重要意义。此外,我们的研究为利用叶蜡正构烷烃的δD值作为当代植物和生态系统科学中的新生态水文代理打开了大门。

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