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Published July 15, 2014 | public
Journal Article

Pliocene–Pleistocene climate change, sea level and uplift history recorded by the Horingbaai fan-delta, NW Namibia

Abstract

Its location on a tectonically relatively stable passive margin and its degree of interaction with the sea make the Horingbaai fan-delta, NW Namibia, an exceptional record of coastal activity, providing insights into the response of ephemeral fluvial systems to changes in climate, sea level and continent-scale uplift. The fan comprises upper, middle and lower segments. The upper fan and middle fan are dominated by a braided river system; only in the upper fan are fluvial sediments interleaved with hyperconcentrated flow deposits. Plio–Pleistocene sea level highstands have left marine terraces on the fan surface which enable correlation with the offshore marine record and provide timelines to constrain fan growth. The bulk of fan-delta progradation took place at ∼ 2.7–2.4 Ma, between the formation of a widespread erosional surface incising the middle Pliocene Karpfenkliff and Kamberg Formations, but prior to the emplacement of the warm-water fauna-bearing late Pliocene "Oyster Terrace" (∼ 2.4–2.2 Ma), an equivalent of the + 30 mP (marine terrace package) in coastal southwestern Africa. Major fan progradation is contemporaneous with widespread regional uplift (~ 12 ± 5 m/Ma) and climate change in southwestern Africa, the latter associated with intensification of northern hemisphere glaciations. Younger fan growth phases are weaker and constrained by < 10 m asl marine terrace bodies that yield mostly cold-water fauna, corresponding to the onset of strong glacial/interglacial climatic fluctuations superimposed on a general aridification trend and the introduction of colder sea-surface temperatures after 2.2 Ma.

Additional Information

© 2014 Elsevier B.V. Received 2 February 2014, Revised 23 May 2014, Accepted 24 May 2014, Available online 2 June 2014. This study was funded by the German Science Foundation (DFG grant STO 275/7-1) and the German Academic Exchange Service (DAAD) which is gratefully acknowledged. Special thanks are due to the Namibian Geological Survey, in particular its Director Dr. Gabi Schneider, for generous help with logistics, to the Ministry of Mines and Energy and to the Ministry of Environment and Tourism as well as the game wardens of the Skeleton Coast Park for their permission and support to work in the area. The paper benefited greatly from on-site discussions with John Pether and Frank Preusser. Christoph Krämer, Benjamin Hagedorn, Anna Uffmann, Henning Schulz and Bastian Wirth are acknowledged for field assistance during surveys of fan and marine terrace profiles. The manuscript was greatly improved by comments from David Bridgland and an anonymous reviewer and the work of Jasper Knight, the editor.

Additional details

Created:
August 22, 2023
Modified:
October 17, 2023