- The George Washington University, Center for Advanced Study of Hominid Paleobiology, Graduate StudentHarvard University, Anthropology, Post-Docadd
- Paleolithic Archaeology, African Archaeology, Experimental Archaeology, Middle Stone Age (Archaeology), Geometric Morphometrics, 3d Modeling, and 12 moreLithic Technology, Archaeology, Paleoanthropology, 3D Modelling (Architecture), Photogrammetry, Tanzania, Levallois, Middle Paleolithic, Variability, Anthropology, Prehistoric Archaeology, and Landscape Archaeologyedit
- I am an anthropologist and archaeologist interested in the relationship of human cultural transmission and technology... moreI am an anthropologist and archaeologist interested in the relationship of human cultural transmission and technology throughout the African later Quaternary. My primary research area is eastern Africa, particularly Tanzania and Kenya, where I have led research projects since 2008.
Currently I am leading a community archaeology project at Kisese II rockshelter in Kondoa, central Tanzania (a UNESCO World Heritage Centre).edit
Levallois technology is a hallmark of many Middle and Late Pleistocene stone artifact assemblages, but its definition has been much debated. Here we use three-dimensional photogrammetry to investigate the geometric variation among... more
Levallois technology is a hallmark of many Middle and Late Pleistocene stone artifact assemblages, but its definition has been much debated. Here we use three-dimensional photogrammetry to investigate the geometric variation among Levallois and discoidal core technologies. We created models of experimental and archaeological stone artifact assemblages to quantitatively investigate the morphologies of Levallois and discoidal core technologies. Our results demonstrate that technological characteristics of Levallois technology can be distinguished from discoidal variants by analyzing the relative volumes and angles of the two flaking surfaces. We apply these methods to a random subset of Middle Paleolithic cores from Skhūl (Israel) and show that, overall, the Skhūl archaeological sample falls in range with the experimental Levallois sample. This study advocates the investigation of core technology on a spectrum to elucidate particular reduction trajectories while maintaining visible outliers and dispersion within an assemblage. Our quantified approach to studying centripetal core technology broadly is particularly applicable in studies related to forager mobility strategy and raw material use. Ultimately, the methods developed here can be used across temporal and geographic boundaries and facilitate attribute-based inter-site comparisons.
Research Interests:
Late Pleistocene and Holocene evidence from multiple rockshelters in north-central Tanzania suggests a regional pattern of changing technological behaviors through time. We use independent chronological evidence to test if the proposed... more
Late Pleistocene and Holocene evidence from multiple rockshelters in north-central Tanzania suggests a regional pattern of changing technological behaviors through time. We use independent chronological evidence to test if the proposed technological patterns across space were also temporally equivalent. We applied AMS radiocarbon dating methods to the carbonate fraction of five ostrich eggshell fragments from Mehlman’s 1975-1976 excavations at Nasera rockshelter and compared our results to recent re-dating efforts of Mumba rockshelter. We document radiocarbon results >46 ka at Nasera in Level 5, indicating that associated and underlying technologies (including what Mehlman termed the ‘Nasera Industry’) are older than previously documented. Backed pieces first appear >46 ka at Nasera, which is in accordance with recent evidence from nearby rockshelters like Enkapune ya Muto, Panga ya Saidi, and potentially Kisese II. We also provide an age of 11,260-11,710 calBP for the ‘Silale Industry’ of Level 3B. Overall, the shifts in lithic technology previously considered to be shared between Mumba and Nasera rockshelters are not temporally aligned, emphasizing the possibility that intra-site variability was the norm throughout the Late Pleistocene in eastern Africa.
Research Interests:
Decades of MSA research has focused on the timing of the appearance of archaeological signatures deemed “behaviorally modern”. However an often-overlooked aspect of the MSA is that it is marked by systematic long-term habitation of rock... more
Decades of MSA research has focused on the timing of the appearance of archaeological signatures deemed “behaviorally modern”. However an often-overlooked aspect of the MSA is that it is marked by systematic long-term habitation of rock shelters (e.g. Klasies River, Pinnacle Point, Mumba, Nasera, Lukenya Hill). The presence of these high-density artifact clusters within shelters suggests the differentiation of behaviors across a landscape in the MSA, and therefore questions regarding human behavior in this time period require a landscape scale approach (Isaac and Harris 1980). In this paper I first provide an overview of landscape approaches to the MSA, including the central questions that can be asked with these methods. Additionally, I highlight an example of landscape methods in this time period using the MSA occurrences at Koobi Fora, excavated by Harris and Kelly. I analysed core reduction strategies across three different areas of MSA occurrences at Koobi Fora: the Ileret localities near the modern lake shore (FwJi 2/3), the Karari escarpment near the basin margin (FxJj 61/66), and GaJj17, located on a lacustrine paleo-beach. Building on Kelly’s 1995 analysis, I analysed cores according to reduction intensity (Clarkson 2013) and core reduction strategy (Inizan et al 1999), taking into account raw material. Differential raw material abundances across these areas (Kelly 1995) enable us to investigate the extent to which core reduction strategies were conserved across environments (as demonstrated by Thompson et al 2014) and/or constrained by raw material. This study provides an important starting point for testing landscape scale hypotheses regarding human behavior in the Late Pleistocene.
Research Interests:
The potential to detect signatures of cultural transmission in stone tool technology is quickly gaining traction in Paleolithic archaeology (e.g. Tostevin 2012). These methods, rooted in middle range theory, remain to be tested through... more
The potential to detect signatures of cultural transmission in stone tool technology is quickly gaining traction in Paleolithic archaeology (e.g. Tostevin 2012). These methods, rooted in middle range theory, remain to be tested through controlled experiment. This project uses experimental flint knapping and a social learning framework to test the hypothesis that signatures of direct cultural transmission can be detected in core reduction strategies. The participant pool included experienced North American flint knappers. The experiment consisted of three isolated sessions simulating different degrees of information transfer ranging from Baseline (low fidelity) to Imitation (high fidelity). Preliminary results suggest that variation in core form is driven primarily by shape of the original cobble and skill level. Skill was determined by both post-experiment questionnaire and by pre-experiment observation. Variation in flake morphology was correlated to different stages of reduction intensity. This study attempted to empirically elucidate signatures of cultural transmission and demonstrates the importance of analyzing these markers across the reduction sequence. The lithic variables measured in this study can be applied to various spatial and temporal contexts.
Research Interests:
The Levallois reduction strategy is often considered a key component of Middle and Later Pleistocene industries. It has been linked to derived degrees of planning and forethought associated with “prepared core” techniques. However,... more
The Levallois reduction strategy is often considered a key component of Middle and Later Pleistocene industries. It has been linked to derived degrees of planning and forethought associated with “prepared core” techniques. However, unambiguous quantitative methods for identifying Levallois reduction in the archaeological record are problematic. The debitage products of Levallois reduction are often employed to identify Levallois technology but these flakes may be obtained by other knapping strategies. Levallois cores are likely to preserve a better understanding of the reduction strategy, especially if refitting is possible. Boëda defined diagnostic criteria of Levallois reduction, yet identifying these criteria remains subjective. Here we develop a quantitative technique for identifying Levallois reduction guided by principles in Boëda’s definition, namely the presence of two asymmetric, hierarchical faces with opposing convexities. To test the validity of these criteria we employ photogrammetric methods to capture three-dimensional form of cores from various archaeological sites across Southwest Asia, Europe, and Africa. Core forms were captured as high-resolution 3D models. This enabled the visualization and shape quantification of portions of cores (e.g. hemispheres) that would otherwise be unattainable with conventional measurements. This research lends new perspectives on the quantitative identification of Levallois technology in the archaeological record.
Research Interests:
Kathryn Ranhorn, The George Washington University Alison Brooks, The George Washington University/ Smithsonian Institution Fidelis Masao, University of Dar es Salaam John Yellen, National Science Foundation/ Smithsonian Institution... more
Kathryn Ranhorn, The George Washington University
Alison Brooks, The George Washington University/ Smithsonian Institution
Fidelis Masao, University of Dar es Salaam
John Yellen, National Science Foundation/ Smithsonian Institution
The origin and routes by which modern humans spread within Africa remain ambiguous, particularly in the intermediate regions between the better-known sites of South Africa and those of Kenya and Ethiopia. Current archaeological evidence indicates Middle Stone Age occupations in northern and central Tanzania at Magubike, Mumba, Nasera and other rock shelters, and the Ndutu Beds at Olduvai Gorge, as well as at Karonga, Malawi and in the Lake Niassa region of northern Mozambique. Southeastern Tanzania, with woodland environments closer to those of central/southern Africa than to the Rift Valley and highland regions further north, remains relatively unexplored. Archaeological survey during the 2012 field season recorded 10 Middle Stone Age sites in the Mtwara, Lindi, and Ruvuma Districts of Tanzania near the border of Mozambique, including 9 open air sites and one rock shelter. The predominantly flake-based assemblages include single- and multi-platform cores including classic Levallois cores, a micro-blade core, flake blades, and scrapers, mostly of quartzite and chert. MSA materials were commonly found in association with quartzite outcrops or near channel margins. Acheulian large cutting tools were absent and Later Stone Age artifacts were extremely rare, suggesting that the largest Pleistocene populations lived during the MSA.
Alison Brooks, The George Washington University/ Smithsonian Institution
Fidelis Masao, University of Dar es Salaam
John Yellen, National Science Foundation/ Smithsonian Institution
The origin and routes by which modern humans spread within Africa remain ambiguous, particularly in the intermediate regions between the better-known sites of South Africa and those of Kenya and Ethiopia. Current archaeological evidence indicates Middle Stone Age occupations in northern and central Tanzania at Magubike, Mumba, Nasera and other rock shelters, and the Ndutu Beds at Olduvai Gorge, as well as at Karonga, Malawi and in the Lake Niassa region of northern Mozambique. Southeastern Tanzania, with woodland environments closer to those of central/southern Africa than to the Rift Valley and highland regions further north, remains relatively unexplored. Archaeological survey during the 2012 field season recorded 10 Middle Stone Age sites in the Mtwara, Lindi, and Ruvuma Districts of Tanzania near the border of Mozambique, including 9 open air sites and one rock shelter. The predominantly flake-based assemblages include single- and multi-platform cores including classic Levallois cores, a micro-blade core, flake blades, and scrapers, mostly of quartzite and chert. MSA materials were commonly found in association with quartzite outcrops or near channel margins. Acheulian large cutting tools were absent and Later Stone Age artifacts were extremely rare, suggesting that the largest Pleistocene populations lived during the MSA.
"The Middle Stone Age of Southeastern Tanzania Kathryn Ranhorn, The George Washington University Alison Brooks, The George Washington University/ Smithsonian Institution Fidelis Masao, University of Dar es Salaam John Yellen, National... more
"The Middle Stone Age of Southeastern Tanzania
Kathryn Ranhorn, The George Washington University
Alison Brooks, The George Washington University/ Smithsonian Institution
Fidelis Masao, University of Dar es Salaam
John Yellen, National Science Foundation/ Smithsonian Institution
The origin and spread of modern humans in Africa remains a central question in paleoanthropology today. The Middle Stone Age (MSA), during which modern human behavior emerged, is well documented in South Africa as well as in Kenya, Ethiopia, and parts of northern Tanzania. The intermediate region between southern and eastern Africa, however, remains largely unexplored. Current MSA sites are recorded at Magubike, Mumba, Nasera and other rock shelters in Tanzania, the Ndutu Beds at Olduvai Gorge, as well as Karonga, Malawi and in the Lake Niassa region of northern Mozambique. Southeastern Tanzania however, containing woodland environments paralleling those of central/southern Africa rather than the Rift Valley and highland regions further north, is lacking in published MSA sites. Archaeological survey conducted during the 2012 field season recorded 10 MSA sites in the Mtwara, Lindi, and Ruvuma districts of Tanzania near the border with Mozambique, including nine open air sites and one rock shelter. The sites discussed here mainly cluster approximately 100km inland; however, a new area further west near Tunduru was also explored. The predominantly flake-based assemblages include single- and multi-platform cores including classic Levallois cores, a micro-blade core, flake blades, and scrapers, mostly of quartzite and chert. MSA materials were commonly found in association with quartzite outcrops or near channel margins. Acheulian large cutting tools were absent and Later Stone Age artifacts were extremely rare, suggesting that the largest Pleistocene populations lived during the MSA."
Kathryn Ranhorn, The George Washington University
Alison Brooks, The George Washington University/ Smithsonian Institution
Fidelis Masao, University of Dar es Salaam
John Yellen, National Science Foundation/ Smithsonian Institution
The origin and spread of modern humans in Africa remains a central question in paleoanthropology today. The Middle Stone Age (MSA), during which modern human behavior emerged, is well documented in South Africa as well as in Kenya, Ethiopia, and parts of northern Tanzania. The intermediate region between southern and eastern Africa, however, remains largely unexplored. Current MSA sites are recorded at Magubike, Mumba, Nasera and other rock shelters in Tanzania, the Ndutu Beds at Olduvai Gorge, as well as Karonga, Malawi and in the Lake Niassa region of northern Mozambique. Southeastern Tanzania however, containing woodland environments paralleling those of central/southern Africa rather than the Rift Valley and highland regions further north, is lacking in published MSA sites. Archaeological survey conducted during the 2012 field season recorded 10 MSA sites in the Mtwara, Lindi, and Ruvuma districts of Tanzania near the border with Mozambique, including nine open air sites and one rock shelter. The sites discussed here mainly cluster approximately 100km inland; however, a new area further west near Tunduru was also explored. The predominantly flake-based assemblages include single- and multi-platform cores including classic Levallois cores, a micro-blade core, flake blades, and scrapers, mostly of quartzite and chert. MSA materials were commonly found in association with quartzite outcrops or near channel margins. Acheulian large cutting tools were absent and Later Stone Age artifacts were extremely rare, suggesting that the largest Pleistocene populations lived during the MSA."
Research Interests:
Formal stone tools in standardized stages is seen by some as a marker for the emergence of behavioral modernity (Mellars, 1989). One variable in particular, symmetry, is argued to play a role both in the formal variation of stone tools... more
Formal stone tools in standardized stages is seen by some as a marker for the emergence of behavioral modernity (Mellars, 1989). One variable in particular, symmetry, is argued to play a role both in the formal variation of stone tools and the aerodynamic quality of projectile points. Several studies using digital morphometric methods analyzed symmetry, particularly of Acheulean bifaces (Lycett, 2008) and paleoindian projectile points (Buchanan, 2005). Here we used digital imaging and statistical software to analyze the symmetry of Middle Stone Age (MSA) projectile points from ≠Gi, Northwest District, Botswana. Projectile points were digitized using a Nikon D70 and Adobe PhotoShop CS5. We analyzed points using FlipTest, a statistical program which examines the digital image and outputs an Index of Asymmetry (IA). The IA first calculates the pixel area of an artifact and then superimposes the left half of the image onto the right side. The area of overlap is divided by the overall area to produce the IA value. Thus, more symmetrical artifacts exhibit an IA value closer to zero. To test whether the hafted portion was contributing disproportionally to the IA, we analyzed both whole point and distal portions only. Finally, we compared IA values with metric measurements in which we determined the distance of each half perpendicular to the bisecting line. Preliminary results reveal that by the MSA symmetry played a significant role in projectile point manufacture, especially of unhafted portions. Future analyses of this pilot study include comparing projectile point symmetry of other MSA sites, such as those from Aduma, Ethiopia, and measuring weights of both halves to test the potential aerodynamic function of symmetry.
