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Geochemistry of recent lacustrine sediments from Fildes Peninsula, King George Island, maritime Antarctica

机译:南极海域乔治王岛菲尔德斯半岛最近湖相沉积物的地球化学

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摘要

Comprehensive geochemical analyses (bulk parameters, major and trace elements, organic matter, mineralogy and particle analysis) were carried out on sediments from seven lakes on Fildes Peninsula, King George Island. The resulting compositional dataset was subjected to principal component analysis and cluster analysis. The results showed that four different lacustrine sedimentary environments can be distinguished: i) lakes 1 and 2 with relatively high values of secondary aluminous clay minerals, ii) lake 4 with anthropogenic enrichment of Co, Cu and Zn, iii) lake 7 with relatively high values of Ba and P and a high zeolite content, and iv) all the other studied lakes. Our results indicate moderate chemical weathering in all lacustrine sediments and that the distance to the glacial ice margin is one of the most important factors influencing the chemical weathering in the area. Furthermore, depositional processes have little influence on the geochemistry of the investigated elements and that local bedrock is the main source of sediments in the lakes on Fildes Peninsula.
机译:对乔治岛国王菲尔德斯半岛上七个湖的沉积物进行了全面的地球化学分析(主要参数,主要和微量元素,有机质,矿物学和颗粒分析)。对所得组成数据集进行主成分分析和聚类分析。结果表明,可以区分四种不同的湖相沉积环境:i)含铝次生粘土矿物含量较高的湖泊1和2,ii)人为富集Co,Cu和Zn的湖泊4,iii)相对较高的湖泊7 Ba和P值较高且沸石含量高; iv)所有其他研究的湖泊。我们的结果表明,所有湖相沉积物中的化学风化程度均中等,并且距冰川冰缘的距离是影响该地区化学风化的最重要因素之一。此外,沉积过程对所研究元素的地球化学影响很小,并且局部基岩是菲尔德斯半岛湖泊中沉积物的主要来源。

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