4.7 Article

Neolithic water management and flooding in the Lesser Caucasus (Georgia)

Journal

QUATERNARY SCIENCE REVIEWS
Volume 197, Issue -, Pages 267-287

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quascirev.2018.08.016

Keywords

Holocene; Early water management; Neolithic; Lesser Caucasus; Flood; Geomorphology; Palaeoclimatology; Radiogenic isotopes; Stable isotopes; Plant macrofossils

Funding

  1. ANR ORIMIL [ANR-12-JSH3-0003]
  2. ANR-DFG KURA IN MOTION! [ANR-12-FRAL-0011]
  3. CNRS (LIA GATES)
  4. French-Armenian LIA NHASA (Natural Hazards and Adaptation Strategies in Armenia from 10 000 BC onwards)
  5. Labex OT MED program GEOART
  6. AMIDEX Water Traces program
  7. Agence Nationale de la Recherche (ANR) [ANR-12-FRAL-0011] Funding Source: Agence Nationale de la Recherche (ANR)

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River management is generally thought to have started at 5500 cal. BC within the development of eastern Neolithic societies. In the Lesser Caucasus, evidence of early river management has been discovered around the famous Neolithic sites of Shulaveri, Gadachrili Gora, and Imiris Gora in Georgia. Here we report a preliminary data set indicating that river management was set up at 5900 cal. BC leading to the flooding, destruction, and local abandonment of the hydraulic infrastructures of the Gadachrili village between 5750 and 5430 cal. BC. The hydraulic infrastructures were developed during a more humid period encompassing the 8200 cal. BP (6200 cal. BC) climatic event, probably to optimize agricultural yield. It potentially led to the first prehistoric engineering accident for which there is evidence, which may have been followed by the reorganisation of the occupation and/or to architectural modifications. (C) 2018 Elsevier Ltd. All rights reserved.

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