The Role of Different Raw Materials in Lithic Technology and Settlement Patterns During the Middle Stone Age of Southern Africa
Afr Archaeol Rev
https://doi.org/10.1007/s10437-021-09446-6
ORIGINAL ARTICLE
The Role of Different Raw Materials in Lithic Technology
and Settlement Patterns During the Middle Stone Age
of Southern Africa
Manuel Will
Accepted: 6 June 2021
© The Author(s) 2021
Abstract The study of raw materials is an essential
step in lithic analysis, regardless of the age, provenance, and technology of the assemblages. As in
many other contexts of the Paleolithic, researchers of
the Middle Stone Age (MSA) in southern Africa have
often focused their attention on fine-grained, nonlocal rock types, such as silcrete. Here, I spotlight
raw materials considered to be of lower suitability for
knapping and frequently acquired from local sources.
Due to their coarse-grained nature, artifacts from rock
types such as calcrete, sandstone, and quartzite might
show attributes that are different from finer-grained
materials. Some of these knapped stones even constitute the substrate of the sites they are from, at times
resulting in their neglect or not being recognized as
anthropogenic artifacts. Knapped vein quartz features sharp and durable edges, but its complicated
fracture mechanics hamper comparative analysis and
provide methodological challenges. In this study, raw
materials from different transport distances and with
Archaeological time period: Middle Stone Age/Stone
Age
Country and region discussed: South Africa, KwaZuluNatal/Western Cape
M. Will (*)
Department of Early Prehistory and Quaternary Ecology,
University of Tübingen, Schloss Hohentübingen,
72070 Tübingen, Germany
e-mail:
different presumed qualities are compared in terms
of their roles in MSA lithic technology and settlement patterns. In the first step, the article focuses on
the open-air special-purpose camp of Hoedjiespunt 1
(HDP1, Western Cape) and the rockshelter residential
site of Sibudu (KwaZulu-Natal), especially on assemblages dated between ~ 130–100 and ~ 58 ka. Subsequently, I review relevant materials for the southern
African MSA. At HDP1 and Sibudu, local raw materials of lower knapping suitability assume several
roles, from the “staple” material for all manufacturing
stages to special-purpose and “add-on” functions. In
the broader southern African region, MSA knappers
also used these rock types in a flexible manner with
gradual differences but also similarities to their use of
finer-grained raw material. These differences depend
on a complex interaction of raw material availability,
differential site use, and the position of the localities
in the settlement system.
Resúmé L’étude des matières premières est une
étape essentielle de l’analyse lithique, quels que soient
l’âge, la provenance et la technologie des assemblages
concernés. Comme dans de nombreux autres contextes du Paléolithique, les chercheurs du Middle Stone
Age (MSA) en Afrique australe ont souvent concentré leur attention sur des types de roches non locales
à grain fin, comme le silcrete. Ici, je mets en lumière les matières premières considérées comme moins
aptes au taillage qui étaient fréquemment acquises
auprès de sources locales. En raison de leur nature à
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Afr Archaeol Rev
gros grains, les artefacts provenant de types de roches comme le calcaire, le grès et le quartzite peuvent
montrer différentes expressions des attributs des matériaux à grains plus fins. Certaines de ces pierres
taillées constituent même le substrat des sites d’où
elles proviennent, ce qui entraîne parfois leur négligence ou leur non-reconnaissance comme des artefacts anthropiques. Le quartz veiné taillé présente des
arêtes vives et durables, mais sa mécanique de rupture
compliquée entrave les analyses comparatives et pose
des défis méthodologiques. Dans cette étude, les matières premières de différentes distances de transport et
de qualité présumée sont comparées en termes de leur
rôle pour la technologie lithique MSA et les modèles
de mobilité. D’abord, l’étude porte sur le campement
à ciel ouvert de Hoedjiespunt 1 (Cap-Occidental) et le
site résidentiel abri sous roche de Sibudu (KwaZuluNatal), sur des assemblages datés entre ~ 130–100 ka
et ~ 58 ka. Par la suite, je passe en revue les documents
pertinents pour la MSA d’Afrique australe. Chez
HDP1 et Sibudu, les matières premières locales moins
aptes à la taille jouent plusieurs rôles, du matériau
« de base» pour toutes les étapes de fabrication aux
fonctions spéciales et « complémentaires». Au niveau
de l’Afrique australe, les tailleurs de MSA ont utilisé
ces types de roches de manière flexible avec des différences et similitudes avec l’utilisation de matières
premières plus fines. Ces différences dépendent d’une
interaction complexe entre la disponibilité des matières premières, l’utilisation différentielle des sites et
la position des localités dans le système de mobilité.
Introduction
Lithic raw material constitutes the physical source
for stone tool technology. Therefore, the study of raw
materials is an essential step in lithic analyses, regardless of the provenance, age, and technology of specific assemblages. Analyses of the natural distribution, accessibility, knapping quality, and package size
of different rock types, as well as their consequent
procurement, transport, use, and discard, provide
manifold insights into past behaviors (e.g., Andrefsky,
1994; Bamforth, 1986; Binford, 1979, 1980; FéblotAugustins, 1997; Gould, 1980; Kelly, 1983; Kuhn,
1992, 1994; Nelson, 1991; Riel-Salvatore & Barton,
2004; Terradillos-Bernal & Rodríguez-Álvarez, 2017;
Tomasso & Porraz, 2016).
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In many spatial and temporal contexts of the
Paleolithic, archaeologists have focused their attention on the role of fine-grained, “high-quality” rock
types. In the European Paleolithic, this phenomenon
is called “flint thinking” (Knutsson, 1998, 2014).
This term refers to an underappreciation of nonflint materials, both in archaeological assemblages
and from a methodological point of view. For over
a century, scholars in Paleolithic Europe based their
technological and typological classifications predominantly on flint assemblages and then imposed
them on raw materials with different flaking properties. Knutsson (1998, 2014) explicates these problems
for quartz assemblages, which have been frequently
interpreted as “archaic” or “amorphous” due to their
different appearances. Researchers in the Middle
Stone Age (MSA) of southern Africa, a period dating
between ~ 300 and 30 ka and associated with the early
evolution of Homo sapiens, have not been exempt
from this bias for fine-grained rocks.
In southern Africa, numerous diverse raw materials appear in MSA assemblages, but none corresponds
to the classic “flint” category of Europe. Yet, a similar
focus on the role of “fine-grained” and often non-local
raw materials (silcrete, in particular) can be observed
in the past decades, mirroring some of the observations
from Europe. The procurement and the use of silcrete
have been associated with specific techno-complexes, (...truncated)