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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Influence of vegetation type on n-alkane composition and hydrogen isotope values from a high latitude ombrotrophic bog
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Influence of vegetation type on n-alkane composition and hydrogen isotope values from a high latitude ombrotrophic bog

机译:植被型对高纬度脉冲沼泽N-烷烃组成和氢同位素值的影响

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The composition and hydrogen isotope values of leaf wax components can be powerful tools in reconstructing past climate and environments. However, interpretation of past environmental conditions from such components in sediments is complicated by species-specific influences and there is a need to better understand how vegetation type affects leaf wax composition and isotope ratios in modern environments. In this study we analyzed leaf wax (n-alkane) distributions and hydrogen isotope values of plants from a high latitude ombrotrophic bog in northern Norway. The isotopic analysis of surface water was also conducted on samples from 15 lakes along a ca. 150 km transect to contextualize the bog water isotopic composition and constrain fractionation factors among n-alkane homologues. We identified 14 different plant types growing on the bog surface, including mosses, graminoids and other herbs, sub-shrubs and a tree. n-Alkanes from the leaves of the modern plants had average chain lengths from 25 to 30.5, with a variety of distributions, and with the dominant compound of longer chain lengths (C-27, C-29, or C-31). SD values of n-C-25 to n-C-33 for the vegetation samples ranged from -197 parts per thousand, to -116 parts per thousand, with an average of -162 parts per thousand. The data also revealed that the SD values for the homologues for half of the vegetation types had ranges that were = 20 parts per thousand. Using the average isotopic value of bog water samples, -60%, we calculated apparent fractionation factors that ranged from -66 parts per thousand, to -134 parts per thousand (avg. -108 +/- 22 parts per thousand), similar to other sites across Europe and to a global data compilation. Our results demonstrate the range of species-specific influences on leaf wax composition and isotopic values at this site and presumably other ombrotrophic bog environments, and provide a dataset to help evaluate the influence of vegetation type on regional sedimentary leaf wax
机译:叶蜡组分的组成和氢同位素值可以是重建过去气候和环境的强大工具。然而,对沉积物中这些组分的过去的环境条件的解释是由物种特异性影响复杂化,并且需要更好地了解植被类型如何影响现代环境中的叶蜡组合物和同位素比。在这项研究中,我们分析了挪威北部高纬度令人障碍沼泽植物的叶蜡(N-烷烃)分布和氢同位素值。表面水的同位素分析也在沿着15湖的样品上进行。 150公里的横断面介绍沼泽水同位素组合物,并约束N-烷烃同源物中的分馏因子。我们鉴定了14种不同的植物类型在沼泽表面上生长,包括苔藓,禾本科和其他草药,亚灌木和树。现代植物叶片的N-烷烃的平均链长度为25至30.5,具有多种分布,以及较长链长的主要化合物(C-27,C-29或C-31)。对于植被样品的N-C-25至N-C-33的SD值范围为-197份,至-116份百分之一,平均为-162份。数据还显示,一半的植被类型的同源物的SD值具有& = 20‰的范围。使用沼水样的平均同位素值,-60%,我们计算出明显的分馏因子,范围为-66份每千份,至-134份每千份(AVG。-108 +/-22份),类似于欧洲的其他网站和全球数据编译。我们的结果证明了该网站上叶蜡组合物和同位素值的物种特异性影响范围,并且可能是其他令人越来越令人障碍沼泽环境,并提供数据集,以帮助评估植被类型对区域沉积叶蜡的影响

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