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- W2034111156 abstract "In the eastern Canary islands, aeolian formations interbedded with palaeosols have been studies. The sequences cover the last 40 ka, as evidenced by one 14C accelerator analysis and several classical radiocarbon dates. As in the Sahara, at least two wet episodes characterize isotopic stage 3. A short pedogenesis corresponds to the first deglaciation step at 15 ka. After a new aeolian episode, the Holocene wet phase begins at around 10 ka. The aeolian sedimentation is of Saharian dust, in particular during the stage 3 dry episode(s). UTh and OSL dating are current." @default.
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- W2034111156 date "1996-01-01" @default.
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- W2034111156 title "Quaternary palaeoclimates in the eastern Canary islands" @default.
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