“Diffusion with modifications”: Nubian assemblages in the central Negev highlands of Israel and their implications for Middle Paleolithic inter-regional interactions
Introduction
Nubian Levallois technology was initially suggested to represent a technological component found within different local lithic industries confined geographically to the Nile Valley and Nubia (Guichard and Guichard, 1965, Marks, 1968a, Van Peer, 1992). These industries were later integrated into a single techno-complex defined as the Nubian Complex (Van Peer, 1998, Van Peer, 2001, Van Peer and Vermeersch, 2000). In Africa discoveries of Nubian cores have been reported from Kenya (Tryon et al., 2012), Ethiopia (e.g., Wendorf and Schild, 1974, Kurashina, 1978), and the Libyan Desert (Foley et al., 2013). The discovery of Nubian cores in surface collected assemblages from Arabia (See Table 1 for a list of assemblages with Nubian cores and Fig. 1 for a map of with their location) led to the revival of the discussion as to their cultural significance (Rose et al., 2011, Crassard and Hilbert, 2013, Usik et al., 2013), using Nubian Levallois technology as a “type fossil” for the dispersal of Homo sapiens out of Africa and into Arabia (Van Peer and Vermeersch, 2007, Usik et al., 2013) or vice versa (Rose et al., 2011, Marks and Rose, 2014). Dated sites with a Nubian component are few (Table 2), including only one dated occurrence in Arabia with Nubian technology – Aybut Al Auwal in Oman dated to a minimum of ∼107 ka (Rose et al., 2011). Other sites in Arabia were assigned to MIS 5 based on paleoclimatic inferences (Crassard et al., 2013, Usik et al., 2013). The same is true for the Nile Valley Nubian assemblages. Excluding Taramsa 1 and Sodmein cave, dated to 68–78 ka and 118 ka respectively, all other sites were assigned a chronological framework based on geographical and paleoclimatic considerations (Mercier et al., 1999, Van Peer, 1998, Vermeersch and Van Peer, 2002, Chiotti et al., 2009, Van Peer et al., 2010: 224, 229; Scerri et al., 2014a).
To date, only sporadic occurrences of Nubian cores have been recorded from Levantine Middle Paleolithic (MP) assemblages (Munday, 1976a, Vermeersch, 2001). The finding of Nubian core technology in the previously unpublished H2 surface collection (N = 686) from the Negev highlands (Fig. 1), and the recognition of Nubian cores in other published MP surface collections from Har Oded (HO) and North Mitzpe Ramon (NMR), situated in the same area (Boutié and Rosen, 1989), rekindles interest in the southern Levant within the context of discussing Late Pleistocene modern human dispersals across vast geographical areas (i.e. northeastern Africa, eastern Africa, the Nile Valley and adjacent deserts, the Levant and Arabia). In addition, several researchers have proposed that the Nubian technology should be viewed as an antecedent for the transitional industry at Boker Tachtit Level 1 (Van Peer, 2004, Belfer-Cohen and Goring-Morris, 2007, Belfer-Cohen and Goring-Morris, 2009, Van Peer et al., 2010: 241–242; Rose and Marks, 2014). In this context, finding Nubian technology in MP assemblages from the central Negev highlands may suggest the presence of a local antecedent for the Boker Tachtit assemblages.
Three common explanations are used to explain the existence of technological similarities in assemblage compositions across the landscape: convergence, dispersal and diffusion (Will et al., 2015, Groucutt et al., 2015). As lithic assemblages are comprised of one or multiple technological traits, identifying the permutations of distinct technological trait sets within assemblages may assist in recognizing past human interactions, diffusion of knowledge and possibly dispersals.
Adapting to a changing environment propagates the search for technological solutions, and such factors may therefore result in convergence, manifesting the same set of solutions even if they emerge from different, unrelated conditions (Shennan, 2000). Convergence has also been suggested for the existence of technological similarities across geographical and temporal discontinuities (Wang et al., 2012, Adler et al., 2014, Will et al., 2015). Another explanation ties convergence to small effective population sizes, geographically restricted social networks, or high extinction rates (Hopkinson et al., 2013).
The term “dispersal” refers to the movement of groups across the landscape with no preferred direction, in search for resources. The term “demic diffusion” in the sense of Ammerman and Cavalli-Sforza (1984) is used to describe the spread of populations and their associated cultural behaviors, in this case lithic technology, into and across areas previously uninhabited by the dispersing groups. Should this area be inhabited by other groups, the process of demic diffusion can lead to displacement, replacement or intermixing with a pre-existing population. Demic diffusions were suggested as the cause of changes in material culture during the European colonization by modern humans and the appearance of agriculture during the Neolithic (Ammerman and Cavalli-Sforza, 1984, Fort, 2012). Finally, “cultural diffusion” consists of the transfer of ideas and knowledge. This process of transmission can occur along several trajectories, the two main ones being “vertical” transmission, which occurs within the social group usually from parent to offspring, and “horizontal” transmission, often originating from outside the social group (Guglielmino et al., 1995, Shennan, 2000). While vertical transmission adds to the stability of cultural traits along time (Guglielmino et al., 1995), horizontal transmission is the main driver of the diffusion of innovations and new technologies (Shennan, 2000, Henrich, 2001, Fort, 2012). In the context of this article, we refer to situations where dispersals of human groups do not result in the total replacement of one culture by another as “diffusion with modifications”. In such cases, dispersals result in cultural diffusion of technological traits and ideas which are then integrated into the locally-used technology.
A special variant of the Levallois “tortoise” cores in the Egyptian Nile Valley was first described by Seligman (1921), although the name Nubian was given to these cores by Guichard and Guichard (1965) who defined two types of Nubian cores. These initial definitions have since been refined and expanded by many researchers, at times widening it by adding intermediate types (Chiotti et al., 2009, Crassard and Thiébaut, 2011, Rose et al., 2011, Usik et al., 2013). Although the terminology that defines the Nubian core technology alludes to shape (i.e., typology), it encapsulates a number of technological processes that must be carried out to obtain the shape, which distinguishes it from other Levallois reduction sequences. For the Nubian technology to be used as a marker for hominin movements, its definition must rest on a set of technological criteria that can be associated with a repeatedly-occurring set of technological traits, referred to here as a “lithic technological package”. In the case of the Nubian cores, current evidence suggests that their geographic distribution does not extend into the northern Levant or Europe, which indicates that their presence is not merely a by-product of Levallois production (see below). Thus when repeatedly associated with a technological package, even low frequencies of Nubian cores may justify their use as markers for hominin movements and interactions.
This paper discusses the technological characteristics of Nubian flaking technology at site H2 and other Negev highland sites in the southern Levant. From this specific case study we go on to argue that the existence of extensive technological variability amongst MP populations in the southern Levant during MIS 5 may be linked to events of population dispersals, as predicted by the range expansion model of modern human dispersals along ecological corridors (Lahr and Foley, 1994, Lahr and Foley, 1998, Foley and Lahr, 1997, Foley et al., 2013). We then discuss the relevance of Nubian technology as a means to track hominin dispersals and technological diffusion through inter-group contacts.
Section snippets
The Levallois flaking system
The Levallois reduction system is recognized as a dominant technological feature in the MP of the Old World (see a recent discussion in Hovers, 2009:20), resulting in three main morphotypes as end products: flakes, points and blades (Van Peer, 1992). The end products are determined by the organization of core geometry and surface topography, reflected by the patterns of scars and ridges on the cores flaking surface. This technology has been used at sites in varying environmental settings
Assemblage composition
The H2 assemblage is an unpublished surface collection from an area of 60 m2, just north of the town of Mitzpe Ramon (Fig. 1). The site was discovered in 1972 by Mitzpe Ramon resident Justus Cohen and reported to Anthony Marks and the Department of Antiquities of Israel. Marks reported in 1972 that:
“The site suffered from slope wash as it now covers about 1700 m2 with a low density of artifacts. The artifactual material is clearly Mousterian of Levallois facies but the percentage distribution
Site H2 in the context of the Middle Paleolithic in the Negev
Three MP surface collections (NMR, MR I and MR II) have been reported from the Mitzpe Ramon area and one from Har Oded (HO), just south of the Ramon Crater (Boutié and Rosen, 1989). Two other major MP site clusters are found in the central Negev, one in the Avdat/Aqev area and a smaller cluster in the area of Givat Barnea (Marks, 1976, Marks, 1977). Like H2, the other Mitzpe Ramon sites and HO are situated on surfaces rich in flint blocks and were probably workshops. This suggestion is
Middle Paleolithic lithic diversity in the Levant
Conforming to a general classification as “Levantine Mousterian” (Bar-Yosef, 2006), MP assemblages north of the Negev are dominated by Levallois as the major (but never exclusive) formal flaking system. Intra-site and inter-site variability is mostly based on quantitative differences in the Levallois modes used, the morphotypes produced and the end-products (Goren-Inbar and Belfer-Cohen, 1998, Hovers and Belfer-Cohen, 2013). Already Crew (1975) has commented on the special character of the
Nubian technology in the Nile Valley, Nubia and adjacent deserts
MP assemblages in Nubia, the Upper Nile Valley and adjacent deserts are associated with assemblages displaying a wide range of techno-typological diversity. These have been variably classified as Nubian Middle Paleolithic, Denticulate Mousterian, Nubian Mousterian, Nubian Complex, Khormusan, K-group, N-group, and Aterian (Guichard and Guichard, 1965, Guichard and Guichard, 1968, Marks, 1968a, Marks, 1968b, Wendorf et al., 1993, Van Peer, 1998, Vermeersch, 2001). Within the Nubian Complex as
Nubian technology in Arabia
Nubian assemblages in Arabia are spread across vast distances. As is the case in the Nile Valley, eastern Africa and the Levant, more than one industry is associated with the MP in Arabia (Groucutt and Petraglia, 2012). The paucity of chronometric data precludes determining the sequential relations between these industries (Marks, 2009, Armitage et al., 2011, Petraglia et al., 2011, Rose et al., 2011, Delagnes et al., 2012, Delagnes et al., 2013). The attribution of the Arabian Nubian
The Negev Nubian assemblages in a broader inter-regional context
The Negev highland assemblages represent a technological package with similarities to the Nubian Complex sites from the Nile Valley and the Abydos high desert. Specifically, assemblages from both regions share the association of Nubian and centripetal Levallois modes of production, though the ratio between Nubian and other Levallois cores differs in each assemblage. Retouched tools are very few in all assemblages and formal Levallois points are nearly absent. It is these characteristics that
Discussion
To this day, the Levant is the only region in western Asia and in Europe where diagnostic remains of pre-Upper Paleolithic (UP) modern humans are found (McCown and Keith, 1939, Vandermeersch, 1981, Schwarcz et al., 1988, Valladas et al., 1988, Stringer et al., 1989, Mercier et al., 1993). The association of these remains with MP lithic artifacts, coupled with the presence of Neanderthal populations in the southern Levant during late MIS 4 and MIS 3, has led to many, often conflicting,
Acknowledgments
Photographs were taken by V. Naikhin and Y.Yolovitch, the Israel Antiquities Authority, and by M. G-G. The drawings were done by N.G. We thank Steve Rosen for granting us permission to use the figures from Boutié and Rosen (1989). We would also like to thank Naama Goren-Inbar, Nigel Goring-Morris, Ariel Malinsky-Buller and Huw Grocutt, as well as three anonymous reviewers, for their helpful comments on earlier drafts of this paper.
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