Mid-Holocene climate variations revealed by high-resolution speleothem records from Soreq Cave, Israel and their correlation with cultural changes

@article{BarMatthews2011MidHoloceneCV,
  title={Mid-Holocene climate variations revealed by high-resolution speleothem records from Soreq Cave, Israel and their correlation with cultural changes},
  author={Miryam Bar-Matthews and Avner Ayalon},
  journal={The Holocene},
  year={2011},
  volume={21},
  pages={163 - 171}
}
Mid-Holocene (7000—4000 yr BP) paleoclimate conditions were reconstructed for the eastern Mediterranean region through a high-resolution (3—20 yr) oxygen and carbon isotopic record in a speleothem from Soreq Cave, Israel. Mid-Holocene climate change is characterized by sinusoidal cycles lasting ~1500 years, that represent changes of ~400 mm (between ~700 and ~300 mm) in annual rainfall, coincident with major cultural changes. Two major cultural changes occurred during wet events at 6550—6450 yr… 

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