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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Isotopic evidence for the incorporation of methane-derived carbon into foraminifera from modern methane seeps, Hydrate Ridge, Northeast Pacific
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Isotopic evidence for the incorporation of methane-derived carbon into foraminifera from modern methane seeps, Hydrate Ridge, Northeast Pacific

机译:东北太平洋水合物山脊现代甲烷渗流中甲烷衍生碳掺入有孔虫的同位素证据

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The presence of modern methane seeps at Hydrate Ridge, offshore Oregon, provide an opportunity to study the influence of methane seeps on the ecology and geochemistry of living foraminifera. A series of cores were collected from the southern summit of Hydrate Ridge in 2002. Samples were preserved and stained to determine the delta(13)C composition of three species of live (stained) and dead benthic foraminifera: Uvigerina peregrina, Cibicidoides mckannai, and Globobulimina auriculata. Specimens were examined under light and Scanning Electron Microscopy (SEM) and exhibit no evidence of diagenesis or authigenic carbonate precipitation. Individual living foraminifera from seep sites recorded delta(13)C values from -0.4parts per thousand to -21.2parts per thousand, indicating the isotopic influence of high methane concentrations. Average delta(13)C values (calculated from single specimens) range from -1.28 to -5.64parts per thousand at seep sites, and -0.81 to -0.85parts per thousand at a control (off seep) site.Two distinct seep environments, distinguished by the presence of microbial mats or clam fields, were studied to determine environmental influences on delta(13)C values. Individual foraminifera from microbial mat sites exhibited more depleted delta(13)C values than those from clam field sites. We interpret these differences as an effect of food source and/or symbiotic microbes on foraminiferal carbon isotopic values, acting to magnify the negative delta(13)C values recorded via the DIC pool. No statistical difference was found between delta(13)C values of live vs. dead specimens. This suggests that authigenic carbonate precipitation did not play a dominant role in the observed isotopic compositions. However, a few dead specimens with extremely negative delta(13)C composition (<-12parts per thousand) do indicate potential evidence for an authigenic influence on the recorded delta(13)C composition. Copyright (C) 2004 Elsevier Ltd.
机译:俄勒冈州近海海德特里奇(Hydrate Ridge)的现代甲烷渗漏的存在,为研究甲烷渗漏对有孔有孔虫的生态和地球化学的影响提供了机会。在2002年从Hydrate Ridge的南端收集了一系列岩心。对样品进行了保存和染色,以确定三种活的(染色的)和死的底栖有孔虫的三角洲(13)C组成:Uvigerina peregrina,Cibicidoides mckannai和毛球藻。在光和扫描电子显微镜(SEM)下检查样品,没有显示成岩作用或自生碳酸盐沉淀的迹象。来自渗漏点的单个活有孔虫记录的delta(13)C值从-0.4份/千至-21.2份/千,表明高甲烷浓度的同位素影响。在不同的渗漏环境中,平均delta(13)C值(根据单个样品计算)在渗漏点处为-1.28至-5.64份/千,在对照(渗漏处)处为-0.81至-0.85份/千。为了确定环境对delta(13)C值的影响,研究了通过区分微生物垫或蛤fields场来区分。来自微生物垫位点的单个有孔虫比来自蛤field位点的那些有更多的Δ(13)C值耗尽。我们将这些差异解释为食物来源和/或共生微生物对有孔虫碳同位素值的影响,以放大通过DIC库记录的负delta(13)C值。在活样品和死样品的delta(13)C值之间未发现统计学差异。这表明自生碳酸盐沉淀在观察到的同位素组成中没有起主要作用。但是,一些具有极差的delta(13)C组成(<-12千分之一)的死标本确实表明了对所记录的delta(13)C组成有自生影响的潜在证据。版权所有(C)2004 Elsevier Ltd.

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