The development of iron crust lateritic systems in Burkina Faso, West Africa examined with in-situ-produced cosmogenic nuclides

Erik Thorson Brown, Didier L. Bourl`es, Fabrice Colin, Zakaria Sanfo, Grant M. Raisbeck, Françoise Yiou

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We have investigated the development of iron crust laterites on the stable West African Craton in northern Burkina Faso using cosmogenic radionuclides produced in situ in quartz veins and pebbles. Lateritic soils develop in tectonically stable, slowly eroding, tropical environments and are a major component of the Earth's surface. To examine processes affecting laterite formation, we determined 10Be and 26Al in samples of quartz from three sites representing two sequential and connected iron crust laterite systems. Results from outcropping quartz veins suggest that the mean erosion rate in this region is about 3-8 m Myr-1. In addition, data from quartz cobbles and pebbles incorporated in iron crusts demonstrate that depth-dependent distributions of these nuclides may be used to distinguish surfaces undergoing burial from those undergoing erosive loss. Results from sections of the lowland lateritic system are consistent with mean accumulation rates of a few metres per million years. Quartz cobbles, presently at depths of a few metres in a paleochannel filled with rapidly deposited fluvial-colluvial material, have 10Be distributions that suggest that the lowland lateritic surface may have formed during an erosive episode, presumably associated with a wetter climate, roughly 300 kyr BP. These results illustrate the practicality and the potential of the use of in-situ-produced cosmogenic nuclides for understanding the history of formation of laterites and for differentiating between systems formed through in-situ chemical weathering and mechanical transport.

Original languageEnglish (US)
Pages (from-to)19-33
Number of pages15
JournalEarth and Planetary Science Letters
Issue number1-4
StatePublished - Jun 1994

Bibliographical note

Funding Information:
Discussion with Bruno Boulange, Georges Grandin and Ed Brook and reviews by James Arnold, George Brimhall and Robert Stallard greatly improved the quality of this work. We thank Jacques Lestringuez and Dominique De-boffle for their continuing expertise in AMS measurements and Professor Bernard Platevoet for providing access to sample preparation facilities. This work was supported by INSU through the DBT Programme (DBTF l/01). Tandetron operation is supported by the CNRS, CEA and IN,P,. Logistic support was from the ORSTOM Centre, Ouagadougou, Burkina Faso.


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