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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Conifers are a major source of sedimentary leaf wax n-alkanes when dominant in the landscape: Case studies from the Paleogene
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Conifers are a major source of sedimentary leaf wax n-alkanes when dominant in the landscape: Case studies from the Paleogene

机译:针叶树是在景观中占主导地位时的沉积叶蜡N-烷烃的主要来源:古烯的案例研究

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Plant wax n-alkanes are valuable paleoclimate proxies because their carbon (delta C-13) and hydrogen (delta H-2) isotopes track biological and environmental processes. Angiosperms produce higher concentrations of n-alkanes than conifers, with some exceptions. Vegetation source is significant because in similar climates, both taxa produce n-alkanes with unique delta C-13 and delta H-2 values due to different physiological strategies. To test whether conifers contribute significantly to sediment n-alkanes and result in distinctive isotopic signatures, we collected sediment samples from a suite of Paleogene paleobotanical sites in North America with high and low conifer abundances. To disentangle the source of sediment nalkanes, we measured the delta C-13 values of nonsteroidal triterpenoids (angiosperm biomarkers) and tricyclic diterpenoids (conifer biomarkers) to determine angiosperm and conifer end member delta C-13 values. We then compared these end member values to n-alkane delta C-13 values for each site to estimate their major taxon sources. At sites dominated by conifer macrofossils, delta C-13 values of n-alkanes indicate a conifer source. At mixed conifer and angiosperm sites, conifer contributions increased with increasing nalkane chain length. At sites where conifers were not as abundant as angiosperms, the delta C-13 values of n-alkanes indicate a predominant angiosperm source with some sites showing a conifer contribution to n-C-33 and n-C-35 alkanes. This suggests that conifers in the Paleogene contributed to longer chain nalkanes (n-C-33 and n-C-35) even when not the dominant taxa, but this likely differs for other geographic locations and taxa. This new approach allows unique floral information to be extracted when chain length is carefully considered in the absence of other paleobotanical data and necessitates having some paleovegetation constraints when interpreting carbon and hydrogen isotopes of plant wax-derived n-alkanes. (C) 2020 Elsevier Ltd. All rights reserved.
机译:植物蜡N-烷烃是有价值的古娱乐代理,因为它们的碳(Delta C-13)和氢气(Delta H-2)同位素轨道轨道轨道生物和环境方法。贪婪植物产生高于针叶树的浓度高浓度的N-烷烃,具有一些例外。植被源是显着的,因为在类似的气候中,由于不同的生理策略,这两个出征的速率都会产生具有独特的Delta C-13和Delta H-2值的N-烷烃。为了测试针叶树是否有助于沉积N-烷烃并导致具有独特同位素签名,我们从北美的一套古古古孤植物中收集沉积物样品,高低针织品。为了解开沉积物Nalkanes的来源,我们测量了非甾体三萜类化合物(Angiosperm Biomarkers)和三环二萜类(针叶树生物标志物)的Delta C-13值,以确定有aniosperm和针叶树末端构件δc-13值。然后,我们将这些最终成员值与每个部位的N-alkane Delta C-13值进行比较,以估计其主要的分类源。在由针叶树大甲酰胺主导地位的位点,N形烷烃的Delta C-13值表示针叶树源。在混合针叶树和高管植物位点,随着脱烷烃链长度的增加,针叶树贡献增加。在针叶树不是高血管植物的基地,N-烷烃的δC-13值表明了具有一些位点的主要的高血管源,显示针叶树对N-C-33和N-C-35烷烃的贡献。这表明古雄地区的针叶树也有助于较长的苯烷烃(N-C-33和N-C-35)即使不是主要的分类群,但这可能对其他地理位置和分类群不同。这种新方法允许在不存在其他古蝴蝶族数据的情况下仔细考虑链长时提取独特的花卉信息,并且在解释植物蜡衍生的N-烷烃的碳和氢同位素时需要具有一些古植被约束。 (c)2020 elestvier有限公司保留所有权利。

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