EXCAVATIONS AT SITE C NORTH, KALAMBO FALLS, ZAMBIA: NEW INSIGHTS INTO THE MODE 2/3 TRANSITION IN SOUTH-CENTRAL AFRICA

被引:28
作者
Barham, Lawrence [1 ]
Tooth, Stephen [2 ]
Duller, Geoff A. T. [2 ]
Plater, Andrew J. [3 ]
Turner, Simon [4 ]
机构
[1] Univ Liverpool, Dept Archaeol Class & Egyptol, Liverpool L69 3GS, Merseyside, England
[2] Aberystwyth Univ, Dept Geog & Earth Sci, Aberystwyth SY23 3DB, Dyfed, Wales
[3] Univ Liverpool, Dept Geog & Planning, Liverpool L69 7ZT, Merseyside, England
[4] UCL, Dept Geog, London WC1E 6BT, England
基金
英国艺术与人文研究理事会;
关键词
South-central Africa; Acheulean; Middle Stone Age; luminescence dating; sedimentology; palaeoenvironment; LATE PLEISTOCENE; LAKE TANGANYIKA; RIVER;
D O I
10.3213/2191-5784-10270
中图分类号
K85 [文物考古];
学科分类号
0601 ;
摘要
We report on the results of small-scale excavations at the archaeological site of Kalambo Falls, northern Zambia. The site has long been known for its stratified succession of Stone Age horizons, in particular those representing the late Acheulean (Mode 2) and early Middle Stone Age (Mode 3). Previous efforts to date these horizons have provided, at best, minimum radiometric ages. The absence of a firm chronology for the site has limited its potential contribution to our understanding of the process of technological change in the Middle Pleistocene of south-central Africa. The aim of the excavations was to collect samples for luminescence dating that bracketed archaeological horizons, and to establish the sedimentary and palaeoenvironmental contexts of the deposits. Four sedimentary packages were identified with the oldest containing Mode 2 and Mode 3 horizons. In this paper we consider the implications of the luminescence ages for the archaeological record at Kalambo Falls, and place them in a regional context. The reworking and preservation of the archaeological horizons is interpreted as the result of successive phases of meander migration and aggradation. Limited pollen evidence suggests a persistent floodplain palaeoenvironment with intermittent swamp forest and adjacent valley woodland, while mineral magnetic susceptibility data support an interpretation of river flow variability without any significant change in sediment provenance. The dynamics of the fluvial system cannot as yet be linked directly with regional climate change. The age range of similar to 500-300 ka for the oldest sedimentary package places the Mode 2/3 succession firmly in the Middle Pleistocene, and contributes to an expanding African record of technological innovation before the evolution of Homo sapiens.
引用
收藏
页码:187 / 214
页数:28
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