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Seasonal changes in molecular composition of organic matter in lake sediment trap material from Nylandssjon, Sweden

机译:瑞典Nylandssjon的湖泊沉积物捕集阱中有机物分子组成的季节性变化

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The origin and degradation/preservation state of organic matter (OM) in lacustrine systems can be studied using its molecular composition. Pyrolysis gas chromatography-mass spectrometry (Py-GC-MS) allows rapid assessment of OM-rich samples and has proven a useful tool for peat, lacustrine and marine deposits, but is rarely applied specifically to lake environments prone to the formation of varves (annually laminated sediments), which are used frequently for palaeoenvironmental reconstruction. We applied Py-GC-MS to a 3.5 yr record of sediment trap samples collected from Nylandssjon in northern Sweden to determine the usefulness of the method for improving knowledge of OM dynamics in varved lakes. It appeared that seasonal variation controlled the pyrolysis fingerprints: intact polysaccharides and lignin from vascular plants, chitin from arthropods and chlorophyll from algae were concentrated in spring and summer traps, whereas winter trap samples were enriched mainly in degraded components, as OM slowly trickled down under a thick layer of ice. A secondary diagenetic process involving sulfurisation of phytadienes was recognised via isoprenoid thiophenes, with no clear seasonal trend, probably because it occurred under anoxic conditions at the lake bottom. The N-containing compounds from proteins in algae and chitin in arthropods were abundant in all samples, indicating that the dominant flux of varve OM was autochthonous in origin. We conclude that Py-GC-MS has significant potential for identifying the variability in parent material (source organisms and degradation state) and could become a valuable tool for palaeoenvironmental reconstruction from varved lake sediments. (C) 2015 Elsevier Ltd. All rights reserved.
机译:湖相系统中有机物(OM)的起源和降解/保存状态可以使用其分子组成进行研究。热解气相色谱-质谱法(Py-GC-MS)可以快速评估富含OM的样品,并已被证明是泥炭,湖相和海洋沉积物的有用工具,但很少专门用于容易形成脉脉的湖泊环境中(每年的层状沉积物),经常用于古环境重建。我们将Py-GC-MS应用于从瑞典北部的Nylandssjon收集的3.5年沉积物陷阱样品记录中,以确定该方法对改善瓦尔韦德湖中OM动力学知识的有用性。似乎季节变化控制了热解指纹:维管束中完整的多糖和木质素,节肢动物的甲壳质和藻类的叶绿素集中在春季和夏季的诱捕器中,而冬季诱捕器的样品主要富集在降解的成分中,因为OM缓慢滴入厚厚的一层冰。通过类异戊二烯噻吩可以识别出涉及植二硫醚硫化的次生成岩过程,没有明显的季节性趋势,可能是因为它发生在湖底缺氧条件下。在所有样品中,来自藻类和甲壳质中甲壳质的蛋白质中的含氮化合物均丰富,这表明瓣膜OM的主要通量是自生的。我们得出的结论是,Py-GC-MS具有确定母体材料(源生物和降解状态)变异性的巨大潜力,并可能成为从曲折的湖泊沉积物中古环境重建的有价值的工具。 (C)2015 Elsevier Ltd.保留所有权利。

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