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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Investigating the carbon isotope composition and leaf wax n-alkane concentration of C-3 and C-4 plants in Stiffkey saltmarsh, Norfolk, UK
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Investigating the carbon isotope composition and leaf wax n-alkane concentration of C-3 and C-4 plants in Stiffkey saltmarsh, Norfolk, UK

机译:研究英国诺福克郡斯蒂夫盐沼中C-3和C-4植物的碳同位素组成和叶蜡正构烷烃浓度

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The carbon isotope composition of terrestrial plants records valuable ecophysiological and palaeoecological information. However, interspecies variability in C-13/C-12, at both the bulk and compound-specific (CS) level, requires further exploration across a range of ecosystem types. Here, we present bulk and n-alkane delta C-13 values, and n-alkane concentrations, from seven plants (C-3 and C-4) growing in a temperate UK saltmarsh. Inter-and intra-species variation in n-alkane delta C-13 values among C-3 plants ranged from 8%(n-C-31) to 10% (n-C-27) across the 2011 and 2012 growing seasons, exceeding variability in bulk tissue (7%). In contrast, the C-4 monocot showed <2% seasonal shifts in bulk and CS values. As a result of the variability in our CS data, we calculate that n-alkane based C-3/C-4 reconstructions in temperate saltmarshes have a maximum uncertainty of similar to 11%. For dicots and succulents, seasonal bulk and CS delta C-13 trends diverged, while for C-3 and C-4 monocots, bulk and CS values followed similar temporal patterns. Fractionation between bulk and n-alkane carbon isotope values varied from -4 to -10% for C-3 plants, and reached -13% for the C-4 monocot. We explain discrepancies between bulk and n-alkane delta C-13 values by referring to possible interspecies variation in salinity adaptation, which may influence the partitioning of pyruvate, shifting the isotopic composition of lipid biomarkers. These findings open new avenues for empirical studies to further understand the metabolic processes fractionating carbon during the synthesis of n-alkanes, enhancing interpretation of the biomarker signal from the geological record. (C) 2016 Elsevier Ltd. All rights reserved.
机译:陆地植物的碳同位素组成记录了宝贵的生态生理和古生态信息。然而,无论是在总体上还是在特定化合物(CS)水平上,C-13 / C-12的种间变异都需要在一系列生态系统类型上进行进一步的探索。在这里,我们介绍了在温带英国盐沼中生长的七种植物(C-3和C-4)的总体和正构烷烃δC-13值以及正构烷烃浓度。在2011年和2012年的生长季节中,C-3植物中正构烷烃δC-13的种间和种内变化范围从8%(nC-31)到10%(nC-27),超过了批量变化的范围组织(7%)。相反,C-4单子叶植物的散装和CS值显示小于2%的季节性变化。由于CS数据的可变性,我们计算出在温带盐沼中基于正构烷烃的C-3 / C-4重建物的最大不确定性接近11%。对于双子叶植物和肉质植物,季节性体积和CS三角洲的C-13趋势有所不同,而对于C-3和C-4单子叶植物,体积和CS值遵循类似的时间模式。对于C-3植物,本体和正构烷烃碳同位素值之间的分级范围从-4到-10%不等,而对于C-4单子叶植物则达到-13%。我们通过参考盐度适应性的可能物种间差异来解释本体和正构烷烃δC-13值之间的差异,这可能会影响丙酮酸的分配,从而改变脂质生物标志物的同位素组成。这些发现为实证研究开辟了新途径,以进一步了解正构烷烃合成过程中碳分离的代谢过程,从而增强了对地质记录中生物标志物信号的解释。 (C)2016 Elsevier Ltd.保留所有权利。

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