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Palaeoenvironmental Changes Inferred from Biological Remains in Short Lake Sediment Cores from the Central Alps and Dolomites

机译:从中部阿尔卑斯山和白云岩的短湖沉积岩芯中的生物残留推断出的古环境变化

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摘要

In this paper we review research on eutrophication, acidification and climate change based on studies of lake sediments in the Alps. Studies on fossil diatoms, chrysophytes, plant pigments, Cladocera and carbonaceous particles in a number of high altitude lakes in Italy and Switzerland have been used to track environmental changes. We present an original study on fossil Cladocera in sediment cores from 29 lakes that have shown changes in biodiversity from the pre-industrial period (ca. pre AD 1850) to the present. These data show that altitude, ca. 60 years of acidification impacts and fish stocking are the most important factors that affect their distribution and abundance. We review further case studies from two morphometrically and chemically different lakes (Tovel and Paione Superiore). Their lake sediment records span 400 and 150 years, respectively; multi-core, multi-proxy analyses show their pH, trophic and climatic evolution over time.
机译:本文基于阿尔卑斯山湖泊沉积物的研究,回顾了富营养化,酸化和气候变化的研究。在意大利和瑞士的许多高海拔湖泊中,对化石硅藻,金藻,植物色素,角藻和含碳颗粒的研究已用于追踪环境变化。我们目前对29个湖泊沉积岩心中的克拉克多化石进行了一项原始研究,这些研究表明,从工业化前时期(约公元1850年)到现在,生物多样性发生了变化。这些数据表明,海拔高度约为60年的酸化影响和鱼类放养是影响其分布和丰度的最重要因素。我们将从两个形态和化学上不同的湖泊(Tovel和Paione Superiore)中回顾更多的案例研究。他们的湖泊沉积物记录分别为400年和150年。多核,多代理分析显示了它们的pH值,营养和气候随时间的变化。

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