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Les Changements dans l'environnement au Moyen-Orient de 20 000 BP à 6 000 BP.
Abstract
Supported by the diffèrent papers of this thematic issue on the paleoenvironments of the Middle East between 20 Kys and 6 Kys, the author attempts to demonstrate that the evolution was rather synchronous everywhere from Anatolia to Egypt and South Arabia : the Last Glacial Maximum on the whole dry and cold, precipitation and temperature increase and forest expansion during the Late Glacial, sudden coming-back of cold and dryness during the Younger Dryas, lastly Holocene Climatic Optimum up to 6/5 Kys. Every proxy data has to be taken into consideration but data value varies much from one area to another and we must try hard to know and date the evolutions and to determine the regional particularities. So it is absolutely necessary to work out two different chronologies : one for the environment, one for archaeology. The Man-environment interrelations testify to the primacy of Culture but frequent and rapid climatic and environmental changes probably greatly oriented choices and accelerated the evolution.
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No major climate change has been demonstrated for the last 5,000 to 4,500 years.
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From Building a model to reconstruct the hellenistic and roman road networks of the eastern desert of Egypt, a semi-empirical approach based on modern travelers’ itineraries (2021) · cites this paper as Sanlaville 1997
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Manière, L., Crépy, M., & Redon, B. (2021) · Journal of Computer Applications in Archaeology · doi:10.5334/jcaa.67 · Cited by 28
Metadata
- Authors
- Sanlaville, P.
- Venue
- Paléorient
- Publisher
- PERSEE Program
- Published
- 1997
- Volume
- 23
- Issue
- 2
- Pages
- 249-262
- ISSN
- 0153-9345
- Cited by
- 39
- References
- 0
- Language
- fr
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