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Sedimentary record of sources and accumulation of organic matter in Pyramid Lake, Nevada, over the past 1,000 years

机译:内华达州金字塔湖过去1000年的沉积记录和有机质积累

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摘要

ew have examined the organic matter contents of two ~210Pb-dated cores of sediment from Pyramid Lake for consequences of the historic environmental and limnological changes that have occurred since modern settlement of this region began in the 1850s. Agricultural diversion of Truckee River water has diminished the volume of this saline, terminal Lake by one-fourth since 1905. Organic C:N ratios, organic δ~13C values, and terrigenous: aquatic n-alkane ratios indicate that the proportion of land-derived organic matter in sediments has decreased as river flow has decreased.
机译:几乎没有人检查过金字塔湖中两个〜210Pb日期的沉积物核心的有机物含量,以了解自1850年代该地区开始现代定居以来发生的历史性环境和岩性变化的后果。自1905年以来,农业对特拉基河水的转移已使该盐的含量在湖的末端减少了四分之一。有机碳氮比,有机δ〜13C值以及陆源:水生正构烷烃比值表明,随着河流流量的减少,沉积物中的有机物减少。

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