Environment and settlements in the Mid-Holocene palaeo-oasis of Wadi Tanezzuft (Libyan Sahara)

被引:19
|
作者
Cremaschi, M [1 ]
Di Lernia, S
机构
[1] Univ Milan, CIRSA CNR CGAQ, I-20133 Milan, Italy
[2] Univ Roma La Sapienza, I-00185 Rome, Italy
关键词
Holocene; palaeo-oasis; geoarchaeology; Libyan Sahara;
D O I
10.1017/S0003598X00089390
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
During the wet middle Holocene (7th-6th millennia BP), not only the ergs, but almost all the landscape units of the Wadi Tanezzuft were rich in water, which was provided by a rainy season connected to the northward movement of the central African monsoon. The whole desert around the Wadi Tanezzuft was suitable for intensive human occupation, constituted by semi-nomadic pastoral groups. The subsequent withdrawal of the monsoon to a more southerly position affected in different ways each of the landscape units in the area. At about 5000 BP, probably as a direct result of the monsoon shift, the most hydrologically fragile segments of the area (pediment, playas and dune field lakes) dried out, while the depletion of soil water reserves had been completed, at least locally, by about 3500 BP. Even so, fluvial activity along the course of Wadi Tanezzuft, notwithstanding the inactivation of the western branches, survived at least to 2700 BP. The reason for this seems to have been due to the immense amount of water stored in the catchment basin of the Tanezzuft during the wet Holocene. Three main phases of cultural adaptation to the changing landscape can be distinguished. An initial Middle Holocene phase, probably commencing around 6000 BP, with an 'anomalous' Middle Pastoral occupation, characterized by large settlements in the Titersin area, in the playa and along the dune fields, exploiting riverine resources, and with a specific socioeconomic organization. A second phase, roughly datable to the beginning of the Late Pastoral, associated with the first contraction and shift of the Tanezzuft system, which led to increasing site density in the region between Kaf Jinun and Tahala oasis. This region became the focal area for human communities, but dramatic site density, decreasing resources, and overexploitation of the landscape probably led to the emergence of social stratification, as suggested by the funerary rituals associated with this phase (di Lernia et al. 2001). Specifically, around this period cemeteries increase in size, with the co-existence of single and multiple burials, and there is much greater differentiation of grave goods, particularly along gender lines. Ovicaprine herding and soil management for plant exploitation appear to have provided the subsistence base. Ceramic containers underwent significant modifications in manufacture, shape, and decoration, highlighting a level of regional fragmentation and discontinuity with the surrounding areas, mostly the Acacus.
引用
收藏
页码:815 / 825
页数:11
相关论文
共 39 条
  • [1] Dynamic Vegetation Simulations of the Mid-Holocene Green Sahara
    Lu, Zhengyao
    Miller, Paul A.
    Zhang, Qiong
    Zhang, Qiang
    Warlind, David
    Nieradzik, Lars
    Sjolte, Jesper
    Smith, Benjamin
    GEOPHYSICAL RESEARCH LETTERS, 2018, 45 (16) : 8294 - 8303
  • [2] Remote Vegetation Feedbacks and the Mid-Holocene Green Sahara
    Swann, Abigail L. S.
    Fung, Inez Y.
    Liu, Yuwei
    Chiang, John C. H.
    JOURNAL OF CLIMATE, 2014, 27 (13) : 4857 - 4870
  • [3] Greening of the Sahara suppressed ENSO activity during the mid-Holocene
    Francesco S. R. Pausata
    Qiong Zhang
    Francesco Muschitiello
    Zhengyao Lu
    Léon Chafik
    Eva M. Niedermeyer
    J. Curt Stager
    Kim M. Cobb
    Zhengyu Liu
    Nature Communications, 8
  • [4] Habitat fragmentation and the sporadic spread of pastoralism in the mid-Holocene Sahara
    Manning, Katie
    Breeze, Paul S.
    Drake, Nick
    Dunne, Julie
    Casanova, Emmanuelle
    Evershed, Richard P.
    QUATERNARY SCIENCE REVIEWS, 2023, 309
  • [5] Contribution of lakes in sustaining the Sahara greening during the mid-Holocene
    Li, Yuheng
    Kino, Kanon
    Cauquoin, Alexandre
    Oki, Taikan
    CLIMATE OF THE PAST, 2023, 19 (10) : 1891 - 1904
  • [6] Greening of the Sahara suppressed ENSO activity during the mid-Holocene
    Pausata, Francesco S. R.
    Zhang, Qiong
    Muschitiello, Francesco
    Lu, Zhengyao
    Chafik, Leon
    Niedermeyer, Eva M.
    Stager, J. Curt
    Cobb, Kim M.
    Liu, Zhengyu
    NATURE COMMUNICATIONS, 2017, 8
  • [7] Sand, stone, and bones: the archaeology of death in the Wadi Tanezzuft Valley (5000-2000 BP). The archaeology of the Libyan Sahara, vol 1.
    Smith, AB
    SOUTH AFRICAN ARCHAEOLOGICAL BULLETIN, 2003, 58 (178): : 94 - 95
  • [8] Mid-Holocene climatic change and man in the present-day Sahara Desert
    Petit-Maire, N
    Guo, ZT
    QUATERNARY DESERTS AND CLIMATIC CHANGE, 1998, : 351 - 356
  • [9] SEDIMENT AND POLLEN EVIDENCE FOR AN EARLY TO MID-HOLOCENE HUMID PERIOD IN THE EASTERN SAHARA
    RITCHIE, JC
    EYLES, CH
    HAYNES, CV
    NATURE, 1985, 314 (6009) : 352 - 355
  • [10] AMOC and Climate Responses to Dust Reduction and Greening of the Sahara during the Mid-Holocene
    Zhang, Ming
    Liu, Yonggang
    Zhang, Jian
    Wen, Qin
    JOURNAL OF CLIMATE, 2021, 34 (12) : 4893 - 4912