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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Microbial production of long-chain n-alkanes: Implication for interpreting sedimentary leaf wax signals
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Microbial production of long-chain n-alkanes: Implication for interpreting sedimentary leaf wax signals

机译:长链的微生物生产 n - alkanes:解释沉积叶蜡信号的含义

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Highlights?Microbial production rates ofn-alkanes in peaty soils were determined.?Anaerobic microbes only produce 19short-chain lengthn-alkanes.?Aerobic microbes produce long-chainn-alkanes (e.g.,n-C29) by up to 0.1%/yr.?Microbes can complicate the application of leaf-waxes in paleo-climate studies.AbstractRelative distributions as well as compound-specific carbon and hydrogen isotope ratios of long-chain C25to C33n-alkanes in sediments provide important paleoclimate and paleoenvironmental information. These compounds in aquatic sediments are generally attributed to leaf waxes produced by higher plants. However, whether microbes, such as fungi and bacteria, can make a significant contribu
机译:<![cdata [ 亮点 n 鞘膜的斜朗的微生物生产率是确定。 Anaerobic Microbes仅生产<?c 19 短链长度 n -allanes。 有氧微生物产生长链 n - alkanes(例如, n -c 29 < / ce:inf>)高达0.1%/ yr。 微生物可以复杂化普赖诺叶蜡的应用-Celimate。 抽象 相对分布以及长链C 25 to c 33 n - 沉积物中的alalanes提供重要的古古怪和古环境信息。水生沉积物中的这些化合物通常归因于由高等植物产生的叶蜡。但是,是否微生物,如真菌和细菌,可以产生重要的贡献

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