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首页> 外文期刊>Biogeosciences Discussions >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:全球海洋环境中的支链甘油二烷基甘油四乙醚(BRGDGTS)的生产:BRGDGTS的新源指标

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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:从水生生物中蓬松蓬松蓬松蓬松的分枝甘油二烷基甘油四乙酯(BRGDGTS)的推测源特异性导致了用于生物地球化学循环和古环境重建的几种生物标志物代理的发育。然而,最近的研究表明,除了土壤和泥炭之外,BRGDGTS也在水生环境中产生。在这里,我们从渤海检查了三个核心,发现BRGDGT组合物不同,随着黄河口的距离而变化。因此,我们提出了六甲基化与五甲基化的BRGDGT(IIIaβ/β)的丰富比以评估BRGDGT来源。全球分布的1354海洋沉积物和589个土壤的汇编表明,IIIa?/?IIa比例一般是β0.59的土壤和0.59-0.92和α0.92分别有和没有显着的陆地投入的海洋沉积物。这种差异证实了BRGDGTS的两个来源,陆地源性较低的陆地来源?/?IIa和患有更高IIIa的海洋源性,其可能归因于通常更高的pH和在寒冷深处的BRGDGTS的生产海水中的水。 IIIa的应用α/?IIA比率与东西伯利亚北极货架证明,它是BRGDGTS的敏感源指标,这有助于准确估计海洋环境中的有机碳源和古趋势。

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