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首页> 外文期刊>Biogeosciences >Ubiquitous production of branched glycerol dialkyl glycerol tetraethers (brGDGTs) in global marine environments: a new source indicator for brGDGTs
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Ubiquitous production of branched glycerol dialkyl glycerol tetraethers (brGDGTs) in global marine environments: a new source indicator for brGDGTs

机译:在全球海洋环境中无处不在生产支链甘油二烷基甘油四醚(brGDGT):brGDGT的新来源指标

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摘要

Presumed source specificity of branched glycerol dialkyl glycerol tetraethers (brGDGTs) from bacteria thriving in soil/peat and isoprenoid GDGTs (iGDGTs) from aquatic organisms led to the development of several biomarker proxies for biogeochemical cycle and paleoenvironmental reconstructions. However, recent studies reveal that brGDGTs are also produced in aquatic environments besides soils and peat. Here we examined three cores from the Bohai Sea, and found distinct difference in brGDGT compositions varying with the distance from the Yellow River mouth. We thus propose an abundance ratio of hexamethylated to pentamethylated brGDGT (IIIa / IIa) to evaluate brGDGT sources. The compilation of globally distributed 1354 marine sediments and 589 soils shows that the IIIa / IIa ratio is generally < 0.59 in soils and 0.59-0.92 and > 0.92 in marine sediments with and without significant terrestrial inputs, respectively. Such disparity confirms the existence of two sources for brGDGTs, a terrestrial origin with lower IIIa / IIa and a marine origin with higher IIIa / IIa, which is likely attributed to a generally higher pH and the production of brGDGTs in cold deep water in marine waters. The application of the IIIa / IIa ratio to the East Siberian Arctic Shelf proves it to be a sensitive source indicator for brGDGTs, which is helpful for accurate estimation of organic carbon source and paleoclimates in marine settings.
机译:在土壤/豌豆中繁殖的细菌中支链甘油二烷基甘油四醚(brGDGTs)的来源特异性以及水生生物的类异戊二烯GDGTs(iGDGTs)的来源特异性导致了生物地球化学循环和古环境重建的几种生物标记物的发展。但是,最近的研究表明,除了土壤和泥炭外,brGDGTs也在水生环境中产生。在这里,我们检查了来自渤海的三个岩心,并发现brGDGT组成的明显差异随距黄河河口的距离而变化。因此,我们提出了六甲基化与五甲基化的brGDGT的丰度比(IIIa / IIa),以评估brGDGT的来源。全球分布的1354个海洋沉积物和589个土壤的汇编显示,在有或没有大量陆地输入的情况下,土壤中IIIa / IIa的比例通常分别<0.59,海洋沉积物中的IIIa / IIa比分别为0.59-0.92和> 0.92。这种差异证实了存在brGDGTs的两种来源,IIIa / IIa较低的陆地来源和IIIa / IIa较高的海洋来源,这可能归因于普遍较高的pH值和海水深冷水中brGDGTs的产生。 。在东西伯利亚北极大陆架上应用IIIa / IIa比值证明它是brGDGT的灵敏源指标,这有助于准确估算海洋环境中的有机碳源和古气候。

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