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Radiocarbon Dating of Individual Lignin Phenols: A New Approach for Establishing Chronology of Late Quaternary Lake Sediments

机译:木质素苯酚的放射性碳定年:建立晚第四纪沉积物年代学的新方法

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The reliability of chronology is a prerequisite for meaningful paleoclimate reconstructions from sedimentary archives. The conventional approach of radiocarbon dating bulk organic carbon in lake sediments is often hampered by the old carbon effect, i.e., the assimilation of ancient dissolved inorganic carbon (DIC) derived from carbonate bedrocks or other sources. Therefore, radiocarbon dating is ideally performed on organic compounds derived from land plants that use atmospheric CO_(2) and rapidly delivered to sediments. We demonstrate that lignin phenols isolated from lake sediments using reversed phase high performance liquid chromatography (HPLC) can serve as effective ~(14)C dating materials for establishing chronology during the late Quaternary. We developed a procedure to purify lignin phenols, building upon a published method. By isolating lignin from standard wood reference substances, we show that our method yields pure lignin phenols and consistent ages as the consensus ages and that our procedure does not introduce radiocarbon contamination. We further demonstrate that lignin phenol ages are compatible with varve counted and macrofossil dated sediment horizons in Steel Lake and Fayetteville Green Lake. Applying the new method to lake sediment cores from Lake Qinghai demonstrates that lignin phenol ages in Lake Qinghai are consistently younger than bulk total organic carbon (TOC) ages which are contaminated by old carbon effect. We also show that the age offset between lignin and bulk organic carbon differs at different Lake Qinghai sedimentary horizons, suggesting a variable hard water effect at different times and that a uniform age correction throughout the core is inappropriate.
机译:年表的可靠性是从沉积档案中进行有意义的古气候重建的先决条件。放射性碳定年湖沉积物中大量有机碳的常规方法通常会受到旧的碳效应的阻碍,即吸收来自碳酸盐岩或其他来源的古代溶解无机碳(DIC)。因此,理想的是对使用大气CO_(2)并迅速输送到沉积物的陆地植物衍生的有机化合物进行放射性碳定年。我们证明了使用反相高效液相色谱法(HPLC)从湖泊沉积物中分离出的木质素酚可以作为有效的〜(14)C约会材料,用于在第四纪后期建立年代学。我们根据已发布的方法开发了一种纯化木质素酚的程序。通过从标准木材参考物质中分离出木质素,我们证明了我们的方法可产生纯木质素酚,并且具有与共识年龄一致的年龄,并且我们的程序不会引入放射性碳污染。我们进一步证明,木质素酚的年龄与Steel Lake和Fayetteville Green Lake中的varve计数和大型化石年代沉积物相兼容。将新方法应用于青海湖的湖泊沉积物核心表明,青海湖中木质素酚的年龄始终比被旧碳效应污染的总有机碳年龄年轻。我们还表明,在不同的青海湖沉积层位上,木质素和大量有机碳之间的年龄偏移是不同的,这表明在不同的时间出现了可变的硬水效应,并且整个岩心的统一年龄校正是不合适的。

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