Abstract
Our aim in this paper is to create a palaeoenvironmental and spatio-temporal framework for interpreting human land use and exploitation of large mammals in the Central Kenya Rift over the past 2 million years, with particular reference to the Nakuru-Elmenteita-Naivasha basin and its adjacent rift flanks on the Kinangop Plateau and Mau escarpment. We pay particular attention to the tectonic and volcanic history of the region, and to the system of lakes that have undergone periodic expansion and contraction during the Pleistocene in response to climatic and tectonic controls. We use this information to reconstruct topographic features as they would have existed at different periods of the past and their likely influence on patterns of large-mammal movements. In addition we present a systematic mapping of variations in the mineral nutrients of soils – soil edaphics – based on 150 analyses of trace elements in modern soil and vegetation samples. Soil edaphics play an important role in animal and human health today, with serious deficiencies in some areas, and would have exerted an important constraint on animal distributions and movements in the past. We show how soil-edaphic properties vary across the region and demonstrate a close relationship between them and the underlying geology and sediments, which allows us to project patterns back into the past and extrapolate them over larger areas. Using this combination of variables, we construct maps that help to place archaeological sites into their wider regional setting. We focus in particular on the Acheulean site of Kariandusi and show that it occupied a unique window of opportunity in place and time for trapping mammals constrained to move through a narrowly defined topographic bottleneck between edaphically-rich areas. We infer that the site was used for a simple form of ambush hunting and briefly explore the implications for differential site use, formation, preservation and visibility.
Highlights
The Kenya Rift is regarded as one of the most important regions for the study of Pleistocene mammals in Africa and the evolution of early hominins, with a notable concentration of fossil and archaeological sites (Figure 1)
We describe our approach as landscape research, but emphasise that it differs in significant ways from the wellestablished tradition of landscape analysis commonly applied in the study of Plio-Pleistocene deposits in the African Rift (e.g., Isaac, 1977; Isaac & Harris, 1978; Bunn et al, 1980; Kroll, 1994; Stern, 1994; Blumenschine & Peters, 1998; Potts, Behrensmeyer & Ditchfield, 1999; Kingston, 2007; Blumenschine et al, 2012)
The Kinangop Plateau is an extensive area of smoother terrain confined to east and west by these fault scarps; its north-western border is dissected by deeply incised rivers, and its southeastern border comprises complex faulting and rough topography, making the plateau an enclosed area with very limited points of easy access, the easiest route to and from the rift floor being via the Kariandusi River (Figure 5)
Summary
The Kenya Rift is regarded as one of the most important regions for the study of Pleistocene mammals in Africa and the evolution of early hominins, with a notable concentration of fossil and archaeological sites (Figure 1). Establishing robust correlations between environmental variables, especially features of the physical landscape, and distributions of
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