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In situ produced branched glycerol dialkyl glycerol tetraethers in suspended particulate matter from the Yenisei River, Eastern Siberia

机译:从东西伯利亚的叶尼塞河原位生成悬浮颗粒物中的支链甘油二烷基甘油四醚

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摘要

Soil-derived branched glycerol dialkyl glycerol tetraethers (brGDGTs) in marine river fan sediments have a potential use for determining changes in the mean annual temperature (MAT) and pH of the river watershed soils. Prior to their incorporation in marine sediments, the compounds are transported to the marine system by rivers. However, emerging evidence suggests that the brGDGTs in freshwater systems can be derived from both soil run-off and in situ production. The production of brGDGTs in the river system can complicate the interpretation of the brGDGT signal delivered to the marine system. Therefore, we studied the distribution of brGDGT lipids in suspended particulate matter (SPM) of the Yenisei River. Chromatographic improvements allowed quantification of the recently described hexamethylated brGDGT isomer, characterized by having two methyl groups at the 6/6 ' instead of the 5/5 ' positions, in an environmental dataset for the first time. This novel compound was the most abundant brGDGT in SPM from the Yenisei. Its fractional abundance correlated well with that of the 6-methyl isomer of the hexamethylated brGDGT that contains one cyclopentane moiety. The Yenisei River watershed is characterized by large differences in MAT (>11 degrees C) as it spans a large latitudinal range (46-73 degrees N), which would be expected to be reflected in brGDGT distributions of its soils. However, the brGDGT distributions in its SPM show little variation. Furthermore, the reconstructed pH values are high compared to the watershed soil pH. We, therefore, hypothesize that the brGDGTs in the Yenisei River SPM are predominantly produced in situ and not primarily derived from erosion of soil. This accounts for the absence of a change in the temperature signal, as the river water temperature is more stable. Using a lake calibration, the reconstructed temperature values agree with the mean summer temperatures (MST) recorded. The brGDGTs delivered to the sea by the Yenisei River during this season are thus not soil-derived, possibly complicating the use of brGDGTs in marine sediments for palaeoclimate reconstructions.
机译:海洋河扇沉积物中土壤衍生的支链甘油二烷基甘油四醚(brGDGTs)具有潜在用途,可用于确定河流流域土壤的年均温度(MAT)和pH值变化。在将它们掺入海洋沉积物中之前,这些化合物会通过河流运到海洋系统。但是,新的证据表明,淡水系统中的brGDGTs可以来自土壤径流和原位生产。河流系统中brGDGT的产生会使传递到海洋系统的brGDGT信号的解释复杂化。因此,我们研究了叶尼塞河的悬浮颗粒物(SPM)中brGDGT脂质的分布。色谱方面的改进允许首次描述环境数据集中最近描述的六甲基化brGDGT异构体,其特征是在6/6'位置而不是5/5'位置具有两个甲基。这种新型化合物是叶尼塞酵母中SPM中最丰富的brGDGT。它的分数丰度与含有一个环戊烷部分的六甲基化brGDGT的6-甲基异构体高度相关。叶尼塞河流域的特征是MAT(> 11摄氏度)的巨大差异,因为它横跨一个较大的纬度范围(北纬46-73摄氏度),有望在其土壤的brGDGT分布中得到反映。但是,其SPM中的brGDGT分布几乎没有变化。此外,与流域土壤的pH值相比,重建的pH值较高。因此,我们假设叶尼塞河SPM中的brGDGT主要是原位产生的,而不是主要来自土壤侵蚀。由于河水温​​度更稳定,这说明温度信号没有变化。使用湖泊校准,重建的温度值与记录的夏季平均温度(MST)一致。因此,叶尼塞河在这一季节向海洋输送的brGDGTs不是土壤来源的,这可能会使brGDGTs在海洋沉积物中用于古气候重建。

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