Climate change and agropastoralist settlement in the Shashe-Limpopo River Basin, Southern Africa: AD 880 to 1700

被引:53
|
作者
Smith, Jeannette [1 ]
Lee-Thorp, Julia [2 ]
Hall, Simon [3 ]
机构
[1] Univ Witwatersrand, Sch Geog Archaeol & Environm Studies, ZA-2050 Johannesburg, South Africa
[2] Univ Bradford, Div Archaeol Goeg & Environm Studies, Bradford BD7 1DP, W Yorkshire, England
[3] Univ Cape Town, Dept Archaeol, ZA-7701 Cape Town, South Africa
来源
SOUTH AFRICAN ARCHAEOLOGICAL BULLETIN | 2007年 / 62卷 / 186期
关键词
Iron Age; Shashe-Limpopo River Basin; South Africa; climate; farming; stable nitrogen isotopes;
D O I
10.2307/20474967
中图分类号
K85 [文物考古];
学科分类号
0601 ;
摘要
The expansion and decline of complex socio-political farming systems in the Shashe-Limpopo River Basin, southern Africa, has been linked to large-scale climate shifts in which increased rainfall favoured intensified agropastoral production and expanded settlement, while the onset of and conditions led to collapse and abandonment of the area. This study uses stable nitrogen isotope ratios ((NN)-N-15-N-14) from modern and archaeological fauna to construct a proxy-rainfiall sequence for the region from AD 880 onwards. The resulting sequence provides a revised climatic context for agropastoral settlement of the river basin and evidence of greater climatic variation than previously documented. Stable nitrogen isotope data from the bone collagen of archaeological fauna show that settlement by Zhizo agropastoralists between AD 880 and 1010 took place under semi-arid conditions, with average annual rainfall of <500 mm. Results for sites dating between AD 1010 to 1290 are consistent with previous interpretations that the Leopard's Kopje A and B cultural period 'capitals' of K2 and Mapungubwe, respectively, rose to prominence under a trend towards increased average annual rainfall that was :500 mm. The data indicate also that the phase of increased moisture extended beyond the abandonment of Mapungubwe at AD 1290 and continued to be evident in fauna dating to the Moloko/Icon cultural period between AD 1310 and 1415. Data from the Moloko/Khami cultural period sites suggest that markedly drier conditions were not evident in the area until after AD 1450. Based on the isotope data, increased rainfall appears to have coincided with the expansion and intensification of settlement in the Shashe-Limpopo River Basin. Reconsideration, however, needs to be given to the correlation between the abandonment of Mapungubwe with the onset of and conditions unfavourable for agropastoralism; other explanations, encompassing socio-economic and political choices, also must be sought.
引用
收藏
页码:115 / 125
页数:11
相关论文
共 50 条
  • [31] Identification and simulation of space-time variability of past hydrological drought events in the Limpopo River basin, southern Africa
    Trambauer, P.
    Maskey, S.
    Werner, M.
    Pappenberger, F.
    van Beek, L. P. H.
    Uhlenbrook, S.
    HYDROLOGY AND EARTH SYSTEM SCIENCES, 2014, 18 (08) : 2925 - 2942
  • [32] Impacts of climate variability and change on drought characteristics in the Niger River Basin, West Africa
    Philip G. Oguntunde
    Gunnar Lischeid
    Babatunde J. Abiodun
    Stochastic Environmental Research and Risk Assessment, 2018, 32 : 1017 - 1034
  • [33] Impacts of climate variability and change on drought characteristics in the Niger River Basin, West Africa
    Oguntunde, Philip G.
    Lischeid, Gunnar
    Abiodun, Babatunde J.
    STOCHASTIC ENVIRONMENTAL RESEARCH AND RISK ASSESSMENT, 2018, 32 (04) : 1017 - 1034
  • [34] Tropical systems from the southwest Indian Ocean making landfall over the Limpopo River Basin, southern Africa: a historical perspective
    Malherbe, J.
    Engelbrecht, F. A.
    Landman, W. A.
    Engelbrecht, C. J.
    INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2012, 32 (07) : 1018 - 1032
  • [35] Linkages between local knowledge drought forecasting indicators and scientific drought forecasting parameters in the Limpopo River Basin in Southern Africa
    Chisadza, Bright
    Tumbare, Michael J.
    Nyabeze, Washington R.
    Nhapi, Innocent
    INTERNATIONAL JOURNAL OF DISASTER RISK REDUCTION, 2015, 12 : 226 - 233
  • [36] Climate Change Signals Over Senegal River Basin Using Regional Climate Models of the CORDEX Africa Simulations
    Mbaye, Mamadou Lamine
    Diatta, Samo
    Gaye, Amadou Thierno
    INNOVATIONS AND INTERDISCIPLINARY SOLUTIONS FOR UNDERSERVED AREAS, INTERSOL 2018, 2018, 249 : 123 - 132
  • [37] Using multiple climate projections for assessing hydrological response to climate change in the Thukela River Basin, South Africa
    Graham, L. Phil
    Andersson, Lotta
    Horan, Mark
    Kunz, Richard
    Lumsden, Trevor
    Schulze, Roland
    Warburton, Michele
    Wilk, Julie
    Yang, Wei
    PHYSICS AND CHEMISTRY OF THE EARTH, 2011, 36 (14-15) : 727 - 735
  • [38] The Impact of Climate Change on Crop Production in West Africa: An Assessment for the Oueme River Basin in Benin
    Sonneveld, B. G. J. S.
    Keyzer, M. A.
    Adegbola, P.
    Pande, S.
    WATER RESOURCES MANAGEMENT, 2012, 26 (02) : 553 - 579
  • [39] Effect of Climate Change and Anthropogenic Activities on Streamflow Indicators in a Tropical River Basin in Southern China
    Xu, Fei
    Zhao, Lingling
    Niu, Cunwen
    Qiu, Yaqin
    WATER, 2022, 14 (03)
  • [40] The Impact of Climate Change on Crop Production in West Africa: An Assessment for the Oueme River Basin in Benin
    B. G. J. S. Sonneveld
    M. A. Keyzer
    P. Adegbola
    S. Pande
    Water Resources Management, 2012, 26 : 553 - 579