North-western Africa experienced significant environmental shifts during Marine Isotope Stage 2, including periods of major aridity and intense cooling (Heinrich events 2 and 1).
In order to understand the relationship between those environmental fluctuations and the technical systems/land-use dynamics of local Late Pleistocene hunter-gatherers, the results of work recently undertaken at the archaeological site of Ifri El Baroud (NE Morocco) are presented.
The site yields a well-stratified sequence of ca. 3 m thickness of LSA deposits (Early and Late Iberomaurusian) very rich in charcoal and archaeological finds. Technological analysis of the lithic assemblages compared with the study of the vertebrate fauna, molluscs and botanical remains reveal a high dynamic interplay between environmental and behavioural changes.
Ifri El Baroud is one of the few sites of the Maghreb with both Early and Late Iberomaurusian layers. For this reason it plays a relevant role in assessing the nature of continuities/discontinuities in human and landscape ecology within the context of the LSA occupation of NW Africa.
Date, Time: 11/07/2016, 14:00 h – 14:45 h