Arid
DOI10.1016/j.chemgeo.2017.07.030
Climatic zonation and weathering control on sediment composition (Angola)
Dinis, Pedro1; Garzanti, Eduardo2; Vermeesch, Pieter3; Huvi, Joao4
通讯作者Dinis, Pedro ; Garzanti, Eduardo
来源期刊CHEMICAL GEOLOGY
ISSN0009-2541
EISSN1878-5999
出版年2017
卷号467页码:110-121
英文摘要

Complementary mineralogical and geochemical datasets on fluvial, beach and dune samples collected along the Atlantic margin of subequatorial southwestern Africa are used to investigate the relationships between provenance and climatic controls on sediment composition and to test the reliability of different geochemical and mineralogical weathering proxies as climatic indicators. The studied N/S-trending coastal region is characterized by strong latitudinal and inland climatic gradients, and thus represents an excellent natural laboratory in which to study the effects of climatic-induced weathering on sediment composition. Although the mineralogy and geochemistry of suspended-load muds closely reflects the different weathering intensities over both latitudinal and inland climatic gradients, the composition of mud and sand samples are strongly affected by sediment provenance. Consequently, weathering parameters such as the alpha E-Al values (estimating the degree of depletion in element E relative to the UCC standard), display complex patterns of variation especially for sand samples. By assuming a typical order of bulk-sediment mobility Na > Ca > Sr > Mg > K > Ba approximate to Rb, anomalously high or low alpha(Al) values placing a specific element off the expected mobility order are considered as an indicator of source-rock control on sediment composition. The composition of detritus recycled from Meso-Cenozoic strata reflects the cumulative effect of successive sediment cycles, with recycling processes affecting to a different extent the diverse weathering proxies. In particular, alpha Na-Al appears to be more strongly affected by recycling in muds than in sands. Among all mineralogical and chemical parameters, those that correlate best with rainfall in the drainage areas are alpha Na-Al for sands, alpha Mg-Al for muds and smectite content (only in areas of low rainfall). In the geological and geomorphological setting of SW Africa these proxies turn out to be better climate estimators than the classical weathering indices CIA or WIP. This case study reminds us to carefully consider source-rock control and mixing with recycled detritus when drawing inferences on climatic conditions based on weathering indices.


英文关键词Weathering geochemistry Clay mineralogy Arid tropical climate Humid equatorial climate Angolan passive margin
类型Article
语种英语
国家Portugal ; Italy ; England ; Angola
收录类别SCI-E
WOS记录号WOS:000408048800010
WOS关键词SOUTH-ATLANTIC-OCEAN ; SOURCE-ROCK CONTROL ; CONGO CRATON ; GRAIN-SIZE ; TRACE-ELEMENTS ; PROVENANCE ; EVOLUTION ; AFRICA ; MARGIN ; GEOCHEMISTRY
WOS类目Geochemistry & Geophysics
WOS研究方向Geochemistry & Geophysics
来源机构University of London
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/198080
作者单位1.Univ Coimbra, MARE Marine & Environm Sci Ctr, Dept Ciencias Terra, P-3030790 Coimbra, Portugal;
2.Univ Milano Bicocca, Dept Earth & Environm Sci, I-20126 Milan, Italy;
3.UCL, London WC1E 6BT, England;
4.Univ Katiavala Bwila, Marine & Environm Sci Ctr, Benguela, Angola
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Dinis, Pedro,Garzanti, Eduardo,Vermeesch, Pieter,et al. Climatic zonation and weathering control on sediment composition (Angola)[J]. University of London,2017,467:110-121.
APA Dinis, Pedro,Garzanti, Eduardo,Vermeesch, Pieter,&Huvi, Joao.(2017).Climatic zonation and weathering control on sediment composition (Angola).CHEMICAL GEOLOGY,467,110-121.
MLA Dinis, Pedro,et al."Climatic zonation and weathering control on sediment composition (Angola)".CHEMICAL GEOLOGY 467(2017):110-121.
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