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Landscape evolution and hydrology at the Late Pleistocene archaeological site of Narabeb in the Namib Sand Sea, Namibia

Landscape evolution and hydrology at the Late Pleistocene archaeological site of Narabeb in the Namib Sand Sea, Namibia
Landscape evolution and hydrology at the Late Pleistocene archaeological site of Narabeb in the Namib Sand Sea, Namibia
The Namib Sand Sea (NSS) in Namibia is known to preserve a wide variety of Pleistocene-age archaeological sites. However, few Middle Stone Age (MSA) sites in this region have been systematically investigated and basic questions around chronology and technological organization remain open. Here we examine Narabeb, an open air MSA surface site exposed in an interdune pan, ∼30 km into the northern NSS. Narabeb was first documented in the 1970s, and then re-examined in 2021 and 2022 by members of this team. Lithic technological analysis combined with a geomorphological description of the site, palaeoenvironmental interpretation of fine-grain water-lain sediments, and luminescence ages from northern and southern locations on the Narabeb pan provide some of the first understanding of human-environmental interactions and estimates of chronology from the later-Middle and Late Pleistocene in the NSS. In addition, we apply a quantitative approach to aeolian linear dune accumulation and extension to explore possible scenarios for landscape development at this site, in order to better understand the former water course(s) affecting the area. The new chronology suggests this site contained standing water at, or just after, the MIS 7/6 transition, and again at, or just after, the end of MIS 6 into early MIS 5. The timing of greater phases of water availability have some overlap with the speleothem growth record at Rössing Cave, situated ∼90 km north of the NSS (and ∼135 km north of Narabeb). Our results provide the foundation for larger, regional-scale analyses of early human adaptive strategies in this unique environment within Southern Africa.
Stone, Abi
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Leader, George
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Marks, Theodore
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Stratford, Dominic
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Efraim, Kaarina
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Bynoe, Rachel
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Smedley, Rachel
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Gunn, Andrew
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Marais, Eugene
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Stone, Abi
2ce54bc8-e380-48cd-91fe-f6c0fc8a34fd
Leader, George
be5bc690-00fe-4174-bcc6-0b5b5464a097
Marks, Theodore
74224369-ab2d-4c6d-ba0d-d090edb20a38
Stratford, Dominic
b794183c-2c18-49a2-9f99-18b09a43fd13
Efraim, Kaarina
c8a61462-bf5a-409e-bb26-8a41c869fb31
Bynoe, Rachel
21c246e1-0fa1-48ba-acdc-d29cac364027
Smedley, Rachel
d55e54b8-fd1c-4bf5-a417-b021762ce045
Gunn, Andrew
35b06362-b771-4df0-88a1-6cd0a6b049a1
Marais, Eugene
2a2a0845-a728-4331-9390-b92bc96b966a

Stone, Abi, Leader, George, Marks, Theodore, Stratford, Dominic, Efraim, Kaarina, Bynoe, Rachel, Smedley, Rachel, Gunn, Andrew and Marais, Eugene (2024) Landscape evolution and hydrology at the Late Pleistocene archaeological site of Narabeb in the Namib Sand Sea, Namibia. Quaternary Science Advances, 14, [100190]. (doi:10.1016/j.qsa.2024.100190).

Record type: Article

Abstract

The Namib Sand Sea (NSS) in Namibia is known to preserve a wide variety of Pleistocene-age archaeological sites. However, few Middle Stone Age (MSA) sites in this region have been systematically investigated and basic questions around chronology and technological organization remain open. Here we examine Narabeb, an open air MSA surface site exposed in an interdune pan, ∼30 km into the northern NSS. Narabeb was first documented in the 1970s, and then re-examined in 2021 and 2022 by members of this team. Lithic technological analysis combined with a geomorphological description of the site, palaeoenvironmental interpretation of fine-grain water-lain sediments, and luminescence ages from northern and southern locations on the Narabeb pan provide some of the first understanding of human-environmental interactions and estimates of chronology from the later-Middle and Late Pleistocene in the NSS. In addition, we apply a quantitative approach to aeolian linear dune accumulation and extension to explore possible scenarios for landscape development at this site, in order to better understand the former water course(s) affecting the area. The new chronology suggests this site contained standing water at, or just after, the MIS 7/6 transition, and again at, or just after, the end of MIS 6 into early MIS 5. The timing of greater phases of water availability have some overlap with the speleothem growth record at Rössing Cave, situated ∼90 km north of the NSS (and ∼135 km north of Narabeb). Our results provide the foundation for larger, regional-scale analyses of early human adaptive strategies in this unique environment within Southern Africa.

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Accepted/In Press date: 17 April 2024
e-pub ahead of print date: 28 April 2024
Published date: 6 May 2024

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Local EPrints ID: 498321
URI: http://eprints.soton.ac.uk/id/eprint/498321
PURE UUID: 9f1c0b27-e116-4620-ae11-1088cb29a9f0

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Date deposited: 14 Feb 2025 17:52
Last modified: 21 Aug 2025 03:31

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Contributors

Author: Abi Stone
Author: George Leader
Author: Theodore Marks
Author: Dominic Stratford
Author: Kaarina Efraim
Author: Rachel Bynoe
Author: Rachel Smedley
Author: Andrew Gunn
Author: Eugene Marais

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