A sequence of fluvial and aeolian deposits (desert loess) and palaeosoils covering the last 60 ka in the Opuwo basin (Kaokoland/Kunene Region, Namibia) based on luminescence dating

Arid and semi-arid areas are lacking in fossils for the reconstruction of the Quaternary climate. Therefore, sediments from ephemeral rivers are a welcome climatic archive in Namibia. Restrictions concerning the palaeoclimatic evidence lie in the fact that the sediments examined usually reflect the...

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Bibliographic Details
Published inQuaternary international Vol. 196; no. 1; pp. 71 - 85
Main Authors Brunotte, E., Maurer, B., Fischer, P., Lomax, J., Sander, H.
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.03.2009
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