Geochemical and mineralogical evidence for Sahara and Sahel dust additions to Quaternary soils on Lanzarote, eastern Canary Islands, Spain

被引:48
|
作者
Muhs, Daniel R. [1 ]
Budahn, James [1 ]
Skipp, Gary [1 ]
Prospero, Joseph M. [2 ]
Patterson, DeAnna [3 ]
Bettis, E. Arthur, III [4 ]
机构
[1] US Geol Survey, Fed Ctr, Denver, CO 80225 USA
[2] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Miami, FL 33149 USA
[3] ATA Serv Inc, Lakewood, CO 80228 USA
[4] Univ Iowa, Dept Geosci, Iowa City, IA 52242 USA
基金
美国国家科学基金会;
关键词
EQUATORIAL NORTH-ATLANTIC; EARLY HUMAN OCCUPATION; DEEP-SEA SEDIMENTS; AFRICAN DUST; CHRONOMETRICAL EVIDENCE; ISOTOPIC COMPOSITION; TROPICAL ATLANTIC; WIND REGIMES; WEST-AFRICA; ND;
D O I
10.1111/j.1365-3121.2010.00949.x
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Africa is the most important source of dust in the world today, and dust storms are frequent on the nearby Canary Islands. Previous workers have inferred that the Sahara is the most important source of dust to Canary Islands soils, with little contribution from the Sahel region. Soils overlying a late Quaternary basalt flow on Lanzarote, Canary Islands, contain, in addition to volcanic minerals, quartz and mica, exotic to the island's bedrock. Kaolinite in the soils also likely has an exotic origin. Trace-element geochemistry shows that the soils are derived from varying proportions of locally derived basalt and African dust. Major-element geochemistry, clay mineralogy and interpretation of satellite imagery suggest that dust additions to the Canary Islands come not only from the Sahara Desert, but also from the Sahel region.
引用
收藏
页码:399 / 410
页数:12
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