The Sibudan is a technocomplex within the cultural stratigraphy of the southern African Middle Stone Age (MSA), first formulated in 2012. The term was introduced as a working concept to organize the spatio-temporal variability in material culture among the archaeological record following the Howiesons Poort during Marine Isotope Stage 3 (MIS 3; ~59–24 ka). In contrast to the more widely used name “post-Howiesons Poort” (“post-HP”)—an umbrella term resting primarily upon temporal aspects—the Sibudan possesses a formal definition based on characteristic elements of its lithic technology. The site of Sibudu, located in the eastern part of southern Africa (KwaZulu-Natal), serves as type locality since it has yielded a rich and high-resolution record of modern human occupations during MIS 3.
The Sibudan type sequence at Sibudu, dated to ~58 ka and encompassing twenty-three layers, features both characteristic traits and diachronic variability. The consistent techno-typological elements include predominantly local raw material procurement, concomitant use of multiple core reduction methods (Levallois, discoid, platform, and bipolar), manufacture of flake and blade assemblages, as well as soft stone hammer percussion for blades. Temporal variability exists in the proportions and morphologies of tools and unifacial points in particular—including Tongati, Ndwedwe, and asymmetric convergent tools—the presence of bifacial points, as well as the frequency of blank types and different core reduction methods.
Comparative studies since 2014 suggest a spatio-temporal extension of the Sibudan in the eastern part of southern Africa during early MIS 3 (~58–50 ka), with marked differences to assemblages of similar ages along the southern coast and Western Cape. The concept is thus not a direct substitute or congruent with the “post-HP” and “Sibudu technocomplex.” On a more interpretive level, the Sibudan has featured in discussions on the trajectory of cultural evolution among early modern humans, the scale and mechanisms of behavioral change during the MSA, and theoretical debate on the relevance of technocomplexes.
Preface: Understanding spatio-temporal variability of water resources and the implications for IWRM in semi-arid eastern and southern Africa