Elsevier

Quaternary International

Volume 526, 20 August 2019, Pages 116-128
Quaternary International

Taphonomic analysis of the level 3b fauna at BK, Olduvai Gorge

https://doi.org/10.1016/j.quaint.2019.06.020Get rights and content

Abstract

The association of stone tools and modified bones at archaeological African Plio-Pleistocene sites is essential to understanding the socio-economics of early hominin behavior. Previous research at BK suggests the site was repeatedly visited by hominins for short time periods. During these occupations, the hominins had a primary role in the exploitation of small, medium, and large size carcasses. The present study analyzes the faunal material recovered from level 3b at BK (BK3b). The results indicate that BK3b operated as a place consciously selected by hominins to carry out specific activities, which resulted in a large accumulation of lithic materials and bone remains. The high frequency of cut-marked specimens, even more than is documented at FLK Zinj, supports the idea that hominins at BK3b butchered and demarrowed the bones from animals of all sizes.

Introduction

The African Plio-Pleistocene witnessed the first stone tool assemblages associated with bones from several animals. Sites such as Ain Boucherit, dated to 2.4 million years ago (Ma) (Sahnouni et al., 2018), Gona dated to 2.5–2.1 Ma (Domínguez-Rodrigo et al., 2005), and Lokalalei 2C (2.34 Ma) (Roche et al., 1999) all show evidence of butchery marks on bones belonging mainly to medium and small carcasses. Nevertheless, all these assemblages are not in primary context or the samples are too small to fully ascertain the socio-economic behavior of early hominins. From 2 Ma onwards several archaeological sites that preserve stone artifacts and cut-marked fossil bones belonging to different taxa from the same level are documented. These sites are referred to as “Type C″ sites (Isaac, 1978, 1984) and are found at several localities, including Koobi Fora (1.95 Ma) (Bunn, 1994), FLK Zinj (1.84 Ma) (Leakey, 1971), El-Kherba (1.78 Ma) (Sahnouni et al., 2013), FLK W (1.7 Ma) (Yravedra et al., 2017b), the ST site complex at Peninj (1.5–1.3 Ma) (Domínguez-Rodrigo et al., 2002), SHK (∼1.5 Ma) (Domínguez-Rodrigo et al., 2014a), and BK (1.35 Ma) (Domínguez-Rodrigo et al., 2009a, 2014b; Organista et al., 2015, 2017). The growing sample of Type C sites now allows us to better characterize their relationship with the behavior of early Homo. At the Bell's Korongo (BK) site in particular there is strong evidence for repeated carcass butchery throughout a deep stratigraphic sequence that spans a significant amount of time, which offers us the opportunity to understand in some detail the socio-economic behavior and evolution of early Homo.

Early access (implying bulk defleshing) by hominins to large carcasses has now been demonstrated at several Early Pleistocene sites such as Kanjera South (e.g., Ferraro et al., 2013), Koobi Fora: FxJj50 (Bunn, 1994) and FwJj20 (Braun et al., 2010), El-Kherba (Sahnouni et al., 2013), Buia (Fiore et al., 2004), and the ST Site Complex (Domínguez-Rodrigo et al., 2002). To date, at Olduvai Gorge, the archaeological record preserves only limited taphonomic evidence for the manipulation by hominins of megafauna during Bed I times at FLK North (Domínguez-Rodrigo et al., 2010) and during lower Bed II times at SHK (Domínguez-Rodrigo et al., 2014a) and FLK West (Yravedra et al., 2017b). This situation changes during middle and upper Bed II times, where hominins' systematic exploitation of megafauna is thoroughly documented throughout the stratigraphic sequence of BK (Domínguez-Rodrigo et al., 2014b; Organista et al., 2015, 2017; Yravedra et al., 2019 accepted). In the current study, we present the taphonomic results of a new archaeological level with evidence for anthropogenic activity, level 3b at BK, which was initially excavated by M. Leakey (1971) and reopened by The Olduvai Paleoanthropology and Paleoecology Project (TOPPP) in 2006.

Section snippets

Site context

Bell's Korongo (BK) is located on the south bank of the Side Gorge, ∼3 km upstream from the junction of the main and side branches. The site was first recorded in 1935 at the top of Bed II in lateral connection with Tuff IID (Leakey, 1971; Hay, 1976). In the 1950s and 1960s, the Leakeys excavated a total of 10 trenches at BK, which revealed a rich fossiliferous assemblage (Leakey, 1971). Since 2006 TOPPP has excavated a 55 m2 surface through five archaeological levels, each of which represent

Site integrity

Due to the fluvial depositional context of BK, level 3b (BK3b) has been analyzed for potential fluvial distortion. Since flowing water may modify the spatial position of archaeological materials and generate preferential orientation of specimens, compasses and clinometers were used to measure the horizontal and vertical orientations of each specimen with a longitudinal axis at least twice as long as its width (Voorhies, 1969; Fiorillo, 1991; Alcalá, 1994; Howard, 2007). Measurements were taken

The integrity of the assemblage

The orientation of archaeological items (bones and lithics) shows a horizontal trend (Fig. 3a). The mean direction is about 50° east - 230° west as shown by the 95% confidence interval of the stereogram but, as the rose diagram shows (Fig. 3b left), the azimuth confidence interval shows clearly identifiable anisotropic orientations. The Woodcock diagram shows an isotropic fabric for the assemblage with a von Mises distribution k concentration value lower than 0.2 (Fig. 3c). The Rayleigh test

Discussion

To date, five archaeological levels have been excavated at BK, all of them preserved in a fluvial deposit of low to moderate energy. The anisotropy documented is probably the result of a local reorganization of the materials rather than sustained water flow. The lower frequency of small specimens suggests that the spatial properties of the assemblage probably have been lost due to rearrangement by water. However, the presence of shaft fragments with good preservation corresponding to all

Conclusion

The taphonomic study of Level 3b at BK provides convincing evidence for the systematic accumulation and exploitation of animals of different sizes and taxa by hominins. The frequency and distribution of cut and percussion marks on specimens corresponding to large animals suggest that hominins had early access to large quantities of meat and marrow. This exploitation of megafauna underscores the importance of meat to the diets of our ancestors -possibly because groups were larger and, thus, had

Acknowledgments

We thank the Tanzanian Commission for Science and Technology (COSTECH), the Department of Antiquities, the Ngorongoro Conservation Area Authority in the Ministry of Natural Resources and Tourism and the National Museums of Tanzania for permission to conduct research at Olduvai Gorge and at the National Museum in Dar es Salaam. We also thank the Spanish Ministry of Economy and Competitiveness for funding this research (HAR2017-82463-C4-1-P) and the Ministry of Culture for funding our research

References (92)

  • M. Domínguez-Rodrigo et al.

    A new protocol to differentiate trampling marks from butchery cut marks

    J. Archaeol. Sci.

    (2009)
  • M. Domínguez-Rodrigo et al.

    Disentangling hominin and carnivore activities near a spring at FLK North (Olduvai Gorge, Tanzania)

    Quat. Res.

    (2010)
  • M. Domínguez-Rodrigo et al.

    Study of the SHK Main Site faunal assemblage, Olduvai Gorge, Tanzania: implications for Bed II taphonomy, paleoecology, and hominin utilization of megafauna

    Quat. Int.

    (2014)
  • M. Domínguez-Rodrigo et al.

    On meat eating and human evolution: a taphonomic analysis of BK4b (upper bed II, Olduvai Gorge, Tanzania), and its bearing on hominin megafaunal consumption

    Quat. Int.

    (2014)
  • M. Domínguez-Rodrigo et al.

    Autochthonous anisotropy of archaeological materials by the action of water: experimental and archaeological reassessment of the orientation patterns at the Olduvai sites

    J. Archaeol. Sci.

    (2014)
  • M. Domínguez-Rodrigo et al.

    The meta-group social network of early humans: a temporal–spatial assessment of group size at FLK Zinj (Olduvai Gorge, Tanzania)

    J. Hum. Evol.

    (2019)
  • M. Domı́nguez-Rodrigo et al.

    The ST site complex at Peninj, West Lake Natron, Tanzania: implications for early hominid behavioural models

    J. Archaeol. Sci.

    (2002)
  • C.P. Egeland et al.

    Taphonomic perspectives on hominid site use and foraging strategies during bed II times at Olduvai Gorge, Tanzania

    J. Hum. Evol.

    (2008)
  • J.T. Faith et al.

    Skeletal element abundances in archaeofaunal assemblages: economic utility, sample size, and assessment of carcass transport strategies

    J. Archaeol. Sci.

    (2007)
  • Y. Fernández-Jalvo et al.

    Small mammal taphonomy of gran dolina, Atapuerca (Burgos), Spain

    J. Archaeol. Sci.

    (1992)
  • A.R. Fiorillo

    Taphonomy and depositional setting of Careless Creek Quarry (Judith River formation), Wheatland County, Montana, U.S.A. Palaeogeography, Palaeoclimatology,

    Palaeoecology

    (1991)
  • A.O. Gidna et al.

    An ecological neo-taphonomic study of carcass consumption by lions in Tarangire National Park (Tanzania) and its relevance for human evolutionary biology

    Quat. Int.

    (2014)
  • L.A. Kreutzer

    Bison and deer bone mineral densities: comparisons and implications for the interpretation of archaeological faunas

    J. Archaeol. Sci.

    (1992)
  • C.W. Marean et al.

    Impact of carnivore ravaging of bone in archaeological assemblages

    J. Archaeol. Sci.

    (1991)
  • C.W. Marean et al.

    Captive hyaena bone choice and destruction, the schlepp effect and Olduvai archaeofaunas

    J. Archaeol. Sci.

    (1992)
  • C.M. Monahan

    New zooarchaeological data from Bed II, Olduvai Gorge, Tanzania: implications for hominid behavior in the Early Pleistocene

    J. Hum. Evol.

    (1996)
  • E. Organista et al.

    An experimental lion-to-hammerstone model and its relevance to understand hominin-carnivore interactions in the archeological record

    J. Archaeol. Sci.

    (2016)
  • E. Organista et al.

    Biotic and Abiotic Processes affecting the Formation of BK Level 4c (Bed II, Olduvai Gorge) and their Bearing on Hominin Behaviour at the Site

    Palaeogeogr. Palaeoclimatol. Palaeoecol.

    (2017)
  • A. Outram et al.

    Meat and marrow utility indices for horse (Equus)

    J. Archaeol. Sci.

    (1998)
  • M.C. Pante et al.

    Fluvial transport of bovid long bones fragmented by the feeding activities of hominins and carnivores

    J. Archaeol. Sci.

    (2010)
  • M.C. Pante et al.

    Validation of bone surface modification models for inferring fossil hominin and carnivore feeding interactions, with reapplication to FLK 22, Olduvai Gorge, Tanzania

    J. Hum. Evol.

    (2012)
  • J.A. Parkinson

    Revisiting the hunting-versus-scavenging debate at FLK Zinj: A GIS spatial analysis of bone surface modifications produced by hominins and carnivores in the FLK 22 assemblage, Olduvai Gorge, Tanzania

    Palaeogeogr. Palaeoclimatol. Palaeoecol.

    (2018)
  • T.R. Pickering et al.

    Experimental patterns of hammerstone percussion damage on bones: implications for inferences of carcass processing by humans

    J. Archaeol. Sci.

    (2006)
  • T.R. Pickering et al.

    Bone modifications resulting from captive chimpanzee mastication: implications for the interpretation of Pliocene archaeological faunas

    J. Archaeol. Sci.

    (1997)
  • T.R. Pickering et al.

    Importance of limb bone shaft fragments in zooarchaeology: a response to “On in situ attrition and vertebrate body part profiles” (2002), by MC Stiner

    J. Archaeol. Sci.

    (2003)
  • T.R. Pickering et al.

    Testing the “shift in the balance of power” hypothesis at Swartkrans, South Africa: hominid cave use and subsistence behavior in the Early Pleistocene

    J. Anthropol. Archaeol.

    (2008)
  • M. Sahnouni et al.

    The first evidence of cut marks and usewear traces from the Plio-Pleistocene locality of El-Kherba (Ain Hanech), Algeria: implications for early hominin subsistence activities circa 1.8 Ma

    J. Hum. Evol.

    (2013)
  • M.C. Stiner

    Food procurement and transport by human and non-human predators

    J. Archaeol. Sci.

    (1991)
  • C.E. Thompson et al.

    The abrasion of modern and archaeological bones by mobile sediments: the importance of transport modes

    Journal of Archaeological Science

    (2011)
  • L. Alcalá

    Macromamíferos neógenos de la fosa Alfambra-Teruel

    (1994)
  • H. Arráiz-Rodríguez et al.

    Paleovegetation changes accompanying the evolution of a riverine system at the BK paleoanthropological site (Upper Bed II, Olduvai Gorge, Tanzania)

    Palaeogeogr. Palaeoclimatol. Palaeoecol.

    (2017)
  • C.A.M. Attwell

    Age determination of the blue wildebeest Connochaetes taurinus in Zululand

    S. Afr. J. Zool.

    (1980)
  • C. Badgley

    Counting individuals in mammalian fossil assemblages from fluvial environments

    Palaios

    (1986)
  • C. Badgley

    Taphonomy of mammalian fossils remains from Siwalik rocks of Pakistan

    Paleobiology

    (1986)
  • R. Barba et al.

    Nueva aproximación al estudio de las marcas de corte: definición de “zonas calientes” como indicador de un consumo inicial de las carcasas por parte de los homínidos. Aplicación al conjunto de FLK Zinj (Olduvai)

    Complutum

    (2008)
  • A.K. Behrensmeyer

    Taphonomic and ecological information from bone weathering

    Paleobiology

    (1978)
  • View full text