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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Published in | Quaternary international Vol. 196; no. 1; pp. 71 - 85 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.03.2009
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Subjects | |
Online Access | Get full text |
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