'Adaptive cycles' and climate fluctuations: a case study from Linear Pottery Culture in western Central Europe

被引:51
|
作者
Gronenborn, Detlef [1 ]
Strien, Hans-Christoph [2 ]
Dietrich, Stephan [3 ]
Sirocko, Frank [4 ]
机构
[1] Romisch German Zent Museum, D-55116 Mainz, Germany
[2] Johannes Gutenberg Univ Mainz, Inst Vor & Fruhgeschichte, D-55116 Mainz, Germany
[3] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany
[4] Johannes Gutenberg Univ Mainz, Inst Geosci Climate & Sediments, D-55099 Mainz, Germany
关键词
Linear Pottery Culture; Climate fluctuations; Adaptive cycles; West-central Europe; Expansion; Social dynamics; HOLOCENE CLIMATE; RESILIENCE THEORY; SOCIETIES; ATLANTIC; IMPACT; VARIABILITY; COLLAPSE; OAKS;
D O I
10.1016/j.jas.2013.03.015
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
By applying cycle-based resilience theory the dynamics of the Early Neolithic west-central European Linear Pottery Culture (LBK) are investigated. These are interpreted as resulting from a combination of internal socio-economic processes as well as external environmental parameters. Resilience theory is helpful in understanding periods of increased vulnerability and inherent trends to social complexity. Cycles and threshold levels also help to understand why societies experience periods of increasing fragility and subsequent decline. Results are based on the correlation of a typology and dendrochronology-based archaeological chronology for western LBK and various palaeoclimatic proxy-data. The C-14-production curve is taken as an indicator for solar activity fluctuations, and an age model for laminated sediments as an indicator for rainfall fluctuations. We currently consider this correlation as agreeably robust; however future fine-dating may result in slight shifts within the archaeological chronology. According to the applied age model, the simple farming societies of the LBK (5600-4900 cal BC) in west-central Europe were not immediately and devastatingly affected by most climate fluctuations. Yet, they might have been one destabilising component within broader processes. However, periods of decreased or irregularly spaced rainfall are contemporaneous to periods of population decline, while periods of increased rainfall may have favoured population growth. Towards the end of the 6th millennium cal BC, the final years of LBK in western Central Europe are contemporaneous to a general trend to less rainfall punctuated by short-term increases in precipitation. During this climatically highly volatile period LBK reaches its highest population rates and at the same time experiences a period of warfare. Thereafter population rates decline and LBK gradually vanishes from the archaeological record, being replaced by Middle Neolithic societies. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:73 / 83
页数:11
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