4.7 Article

Elemental composition of biogenic sediments reveals palaeoclimatic changes during the Late Weichselian in a Central European river valley: A statistical approach

期刊

CATENA
卷 200, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.catena.2021.105188

关键词

Geochemistry; Multivariate statistics; Lithogeochemical facies; River valley; Environmental changes; Late Weichselian

资金

  1. National Science Centre (NCN) [2011/01/B/ST10/04905]

向作者/读者索取更多资源

The study analyzed the lithological and geochemical characteristics of sediment fillings in a small river valley in Central Europe during the Late Weischselian period. It found differentiation in composition and grain-size properties due to changes in hydroclimatic conditions and geology. The sediments, mainly mineral or organic-mineral, contained high levels of lithophilic elements such as Na, K, and Mg, indicating mechanical denudation processes in the Grabia River valley during the Late Weischselian period.
Five sections of sediment from mire infillings located in different part of the catchment small river valley in central Europe were studied by lithological and geochemical analysis in order to examine the response of aquatic ecosystems to the environment changes during Late Weischselian (LW). Differentiation of geochemical composition and grain-size properties in biogenic deposits is being considered as a result of change hydroclimatic conditions and geology structure in individual parts of the catchment. The principal component analysis (PCA) and clustered by hierarchical method (HCA) were chosen to create the lithogeochemical facies and their chronostratigraphy variability. Biogenic sediments of the studied river mires, regardless of the location in a given reach of the valley, are represents mainly by mineral or organic-mineral lithogeochemial facies with increased of lithophilic elements (Na, K and Mg). Similar chemical composition of gyttja and peat sediments in almost all periods of LW, indicate the strongly mechanical denudation processes in the Grabia River valley. The major process, conditioning the development of the mires (in it type and rate sedimentation), was the variable terrigenous material input which are related to its variable dynamic of floods. The higher than expected chemical denudation probably a result of specific groundwater flow direction and dissolving vari-grained sands and silts, which build plains in the central part of the study catchment. The number and thickness of individual lithogeochemical facies are caused by differences in the potential volume of the hydrologically active zone and geological conditions of the emerge or disappear permafrost.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据