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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Environmental influence on the biohopanoid composition of recent sediments
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Environmental influence on the biohopanoid composition of recent sediments

机译:环境对最近沉积物生物类类胡萝卜素成分的影响

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摘要

Bacteriohopanepolyols are the biological precursors of extended hopane biomarkers which are ubiquitous in the geosphere. The abundance and composition of these biohopanoids were determined for modem sediments from eight depositional environments by GC-MS analysis of hopanols derived from a side-chain cleavage reaction (periodic acid and sodium borohydride) of the bacteriohopanepolyols. We report quantitative data for bacteriohopanetetrol (BHT), composite tetrafunctionalised biohopanoids, pentafunctionalised biohopanoids and hexafunctionalised biohopanoids. BHT was found in concentrations higher than previously reported (up to ca. 1500 mu g/g TOC), but comprised only a relatively small proportion (0-26%) of the total biohopanoids in all except one sample. Composite tetrafunctionalised biohopanoids were the dominant group of bacteriohopanepolyols in all other sediments, and are likely to be a major source of the geologically occurring extended hopanes. Hexafunctionalised biohopanoids were most abundant in lake sediments, particularly two small highly productive stratified lakes (where they comprised 20-40% of total biohopanoids). This feature is interpreted to be due to greater contribution to the organic matter of these sediments from Type I methanotrophic bacteria (which produce dominantly hexafunctionalised biohopanoids), consistent with the environmental settings. In the marine environments where sulphate reduction is dominant, hexafunctionalised biohopanoids are relatively minor constituents (2-6% of total biohopanoids). These data comprise the first clear demonstration that bacteriohopanepolyols vary in composition between depositional environments, and have the potential to preserve specific bacterial source information in sedimentary organic matter. Copyright (C) 2000 Elsevier Science Ltd. [References: 45]
机译:细菌型庚烷多元醇是扩展的hop烷生物标志物的生物前体,后者在地球圈中无处不在。通过GC-MS分析衍生自细菌类六醇多元醇的侧链裂解反应(高碘酸和硼氢化钠)的酒酚的GC-MS分析,确定了来自八个沉积环境的现代沉积物中这些生物类胡萝卜素的丰度和组成。我们报告细菌紫杉醇(BHT),复合四官能生物类胡萝卜素,五官能生物类胡萝卜素和六官能生物类胡萝卜素的定量数据。发现BHT的浓度高于先前报道的浓度(最高约1500μg / g TOC),但除一个样品外,在所有生物类胡萝卜素中仅占相对较小的比例(0-26%)。复合四官能化生物类人猿是所有其他沉积物中细菌类人猿多元醇的主要组,并且很可能是地质上扩展的hop烷的主要来源。六官能化生物类胡萝卜素在湖泊沉积物中含量最高,尤其是两个小型高产分层湖泊(它们占生物类胡萝卜素总量的20-40%)。解释此特征是由于与环境设置一致,这些I型甲烷营养细菌(主要产生六官能化的生物类类生物)对这些沉积物的有机物有较大贡献。在硫酸盐还原占主导地位的海洋环境中,六官能化生物类胡萝卜素的含量相对较小(占总生物类胡萝卜素的2-6%)。这些数据首次清楚地表明,细菌六聚多元醇的组成在沉积环境之间会发生变化,并且有可能在沉积有机物中保存特定的细菌来源信息。版权所有(C)2000 Elsevier Science Ltd. [参考:45]

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