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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Conservative composition of n-alkane biomarkers in Sphagnum species: implications for palaeoclimate reconstruction in ombrotrophic peat bogs
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Conservative composition of n-alkane biomarkers in Sphagnum species: implications for palaeoclimate reconstruction in ombrotrophic peat bogs

机译:泥炭藓物种中正构烷烃生物标志物的保守组成:对全营养泥炭沼泽古气候重建的影响

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摘要

The n-alkane distributions from total lipDE extracts often modern Sphagnum moss species, collected from a suite of ombrotrophic bogs across Europe, were determined using gas chromatography/mass spectrometry (GC/MS). n-Alkane distributions are reported for the first time for Sphagnum balticum, S. majus, S. angustifolium and S. lindbergii, which are all dominated by C-23 with the exception of S. lindbergii, which exhibits a bimodal distribution with C-23 and C-31 as the major homologues. The distributions for indivDEual species generally agree with published compositions, confirming the conservative nature of the n-alkane compositions, which provDEe a basis for differentiating the n-C-23 and n-C-25 dominated species. Investigations of the variation in n-C-23-C-25 and n-C-23-C-3, ratios of Sphagnum species, using the new and published n-alkane distributions, reveal that intra-species variation is generally minor. Critically, the distributions and ratios for most species do not vary among the sites studied, suggesting that they are conservative tracers for a given species, despite differences in growth conditions. In contrast, inter-species variation exists, allowing differentiation of indivDEual Sphagnum species based on vegetation biomarkers, specifically the C-25 n-alkane in S. fuscum and the n-C-23-C-25 ratio. Biomarker stratigraphic analysis of a 150 cm peat core (Kontolanrahka Bog, Finland) reveal shifts in the n-C-23-C-25 ratio, which track changes in the abundance of S. fuscum in the macrofossil record. This supports the application of n-alkane biomarkers in peat archives for tracking past shifts in indivDEual Sphagnum species abundance. This will be particularly important where fossil plant remains are highly degraded in, or absent from, peat records.
机译:使用气相色谱/质谱法(GC / MS)测定了从整个欧洲的一组营养缺陷型沼泽中收集的总的lipDE提取物(通常是现代泥炭藓类)的正构烷烃分布。首次报道了pha草,S。majus,S。angustifolium和S. lindbergii的正构烷烃分布,除了S. lindbergii与C-呈双峰分布外,其余均由C-23占据主导地位。 23和C-31为主要同源物。单个物种的分布通常与已公布的组成一致,这证实了正构烷烃组成的保守性,这为区分n-C-23和n-C-25占优势的物种提供了基础。使用新的和已发布的正构烷烃分布对泥炭藓物种的n-C-23 / n-C-25和n-C-23 / n-C-3比率的变化进行调查后,发现种内变化通常较小。至关重要的是,大多数物种的分布和比率在所研究的地点之间没有变化,这表明尽管生长条件不同,但它们是给定物种的保守示踪剂。相反,存在种间变异,从而允许基于植被生物标志物,特别是镰刀菌中的C-25正构烷烃和n-C-23 / n-C-25比值,对不同的泥炭藓属植物进行区分。 150厘米泥炭岩心的生物标志物地层分析(芬兰Kontolanrahka沼泽)揭示了n-C-23 / n-C-25比值的变化,该变化追踪了大化石记录中的镰刀菌丰度变化。这支持正构烷烃生物标记物在泥炭档案中的应用,以追踪过去泥炭物种丰富度的变化。当化石植物的残留物在泥炭记录中高度退化或缺失时,这一点尤其重要。

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