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The East African Early Acheulean of Peninj (Lake Natron, Tanzania)

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The Emergence of the Acheulean in East Africa and Beyond

Part of the book series: Vertebrate Paleobiology and Paleoanthropology ((VERT))

Abstract

The Pleistocene record of Peninj , dated to 1.5–1.4 Ma and located on the Western shore of Lake Natron (Tanzania), is one of the classic archaeo-paleontological sources for the study of the early Acheulean in Africa. Beginning with the seminal project led by Glynn Isaac in the decades of 1960s and 1980s, other research programs have been carried out in Peninj since then, particularly the landscape archaeology approach undertaken by M. Domínguez-Rodrigo between 1995 and 2005. In 2007, fieldwork was resumed in the area and a new project is currently in progress. As a result of this long-lasting scientific effort, the variety of geological, contextual, technological, and spatial information gathered so far can shed light on a number of aspects related to the early Acheulean record identified in the three different archaeological areas of Peninj (the Type Section, the North and the South Escarpments ). This paper presents a synthesis of the history of research in Lake Natron and the geology of the Peninj Group. It also reviews some of the main discussions related to the Type Section technology, the bifacial hierarchical centripetal method hypothesis, and the Oldowan–Acheulean dichotomy for the attribution of the lithic samples in the framework of the archaeological record of Peninj . The paper includes a synthesis of the new data gathered in the Acheulean sites of the Escarpments in the course of the present research project and, finally, a regional interpretation of the early Acheulean of the Lake Natron .

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Notes

  1. 1.

    1901: Mitteilungen über meine Reise nach Äquatorial-Ostafrika und Uganda 1896–1897. [A report of my journey in Eastern Equatorial Africa and Uganda between 1896 and 1897].

  2. 2.

    The USC member has a thickness that varies between 4 and 20 m. It consists of alluvial facies constituted by clays, silts, sands, and dolomitic carbonates. These alluvial materials are interbedded with five volcanic tuffs (from bottom to top, T1 to T5) (Luque et al. 2009b) (Fig. 7.3)

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Authors and Affiliations

  1. Department of Prehistory and Archaeology, University of Valladolid, Plaza del Campus s/n, 47011, Valladolid, Spain

    Fernando Diez-Martín & Policarpo Sánchez-Yustos

  2. Fundación Conjunto Paleontológico de Teruel-Dinópolis, Avenida de Sagunto s/n, 44002, Teruel, Spain

    Luis de Luque

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  1. Fernando Diez-Martín
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  2. Policarpo Sánchez-Yustos
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  3. Luis de Luque
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Correspondence to Fernando Diez-Martín .

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  1. Dipartimento di Scienze dell’Antichità, Sapienza Università di Roma, Rome, Italy

    Rosalia Gallotti

  2. Dipartimento di Scienze dell’Antichità, Sapienza Università di Roma, Rome, Italy

    Margherita Mussi

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Diez-Martín, F., Sánchez-Yustos, P., de Luque, L. (2018). The East African Early Acheulean of Peninj (Lake Natron, Tanzania). In: Gallotti, R., Mussi, M. (eds) The Emergence of the Acheulean in East Africa and Beyond. Vertebrate Paleobiology and Paleoanthropology. Springer, Cham. https://doi.org/10.1007/978-3-319-75985-2_7

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