Contribution of the δ13c isotopic signal on archaeological charcoal to infer pleistocene climate change: methods and first applications on paleolithic settlements
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8 janvier 2019
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- handle: 10670/1.g5cboa
- hal: hal-02383578
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Instruction and study--Methods Prehistoric antiquities Prehistory Prehistoric archaeology Social science Sciences, Social Human sciences Social studies Behavioral sciences Natural science Sciences Science of science Early man Prehistoric human beings Cavemen (Prehistoric peoples) Prehistoric humans Man, Prehistoric Prehistory Prehistoric archaeology Climatic changes--Environmental aspects Global climate changes Climate change Climatic change Climate variations Climate changes Global climatic changes Changes, Climatic Climatic variations Climatic fluctuations Instruction and study--Methods Paleolithic Age de la pierre Age de pierre ép paléolithiqueCiter ce document
Benjamin Audiard et al., « Contribution of the δ13c isotopic signal on archaeological charcoal to infer pleistocene climate change: methods and first applications on paleolithic settlements », HAL-SHS : archéologie, ID : 10670/1.g5cboa
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