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First Calibration and Application of Leaf Wax n-Alkane Biomarkers in Loess-Paleosol Sequences and Modern Plants and Soils in Armenia

机译:黄土古糖醇序列和现代植物和土壤中叶蜡N-烷烃生物标志物的首先校准和应用

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摘要

Interpreting paleoenvironmental conditions by means of n-alkane biomarker analyses is challenging because results depend on different influencing factors. Thus, regional calibration of n-alkane patterns is needed because of different plant chemo-taxonomic behavior. We investigated for the first-time leaf wax-derived n-alkane biomarkers from modern plants, litter, top soils, and two recently discovered loess-paleosol sequences (LPSs) in Armenia (Lesser Caucasus). Our results on modern samples show a promising discrimination power based on n-alkane chain length nC33 (probably nC31)) for grasses and herbs versus nC29 for deciduous trees, despite the large interplant variability within vegetation groups. In contrast with other Loess records in Europe, where Late Pleistocene environments are ranging from tundra-like (glacial) to deciduous forest habitats (interglacial), our results from two Armenian LPSs suggest a transition from humid-steppe biome or forest-steppe vegetation dominating during interglacial periods, to semi-desert shrubs species more adapted to the enhanced aridity during glacial periods.
机译:通过N-烷烃的生物标志物分析解释古环境状况是挑战性的,因为结果取决于不同的影响因素。因此,由于不同的植物化疗 - 分类行为,因此需要N-烷烃图案的区域校准。我们调查了来自现代植物,垃圾,顶部土壤的第一次叶片蜡衍生的N-烷烃生物标志物,以及最近发现的亚美尼亚的黄土古糖序列(LPSS)(较小的高加索)。我们在现代样品上的结果表明,尽管植被群体中具有较大的植物可变异性,但是,现代样品上的基于N-烷基链长度NC33(可能NC31)的判别能力为基于N-烷烃链长度NC33(可能NC31))。与欧洲的其他黄土记录相比,迟到的更加优越的环境从苔原(冰川)到落叶林栖息地(中间峡谷),我们的两个亚美尼亚LPS的结果表明了从湿草原生物群系或森林 - 草原植被的过渡在冰川期间,在半沙漠灌木期间,在冰川期间更适应增强的炎症。

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