Climate of the last 53,000 years in the eastern Mediterranean, based on soil-sequence stratigraphy in the coastal plain of Israel

Keyphrases

• Israel 100%
• Speleothem 100%
• Coastal Plain 100%
• Eastern Mediterranean 100%
• Coastal Belt 100%
• Soil Sequence 100%
• Sequence Stratigraphy 100%
• Sahara Desert 66%
• Lake Level 66%
• Climatic Events 66%
• Climatic Fluctuations 66%
• Lake Lisan 66%
• Hamra 66%
• Human History 33%
• Magnetic Susceptibility 33%
• Archaeological Record 33%
• Dead Sea 33%
• Paleosol 33%
• Luminescence 33%
• Soil Type 33%
• Desertification 33%
• Karstic Cave 33%
• Carbon Isotopes 33%
• Particle Size Distribution 33%
• Soil Micromorphology 33%
• Soil Parent Material 33%
• Wet Environment 33%
• Red Mediterranean Soils 33%
• Warm Environment 33%
• Freshwater Lake 33%
• Oxygen Isotopes 33%
• Late Holocene 33%
• Younger Dryas 33%
• Sapropel 33%
• Highstand 33%
• Arabian Desert 33%
• Early Holocene 33%
• Widespread Distribution 33%
• Dune Sand 33%
• Clay Soil 33%
• Aeolianite 33%
• Atmospheric Dust 33%
• Thick Bed 33%
• Clay Mineralogy 33%
• Loess Material 33%
• Paleosol Sequence 33%
• Last Glacial Stage 33%
• Human Prosperity 33%

Earth and Planetary Sciences

• Israel 100%
• Speleothem 100%
• Coastal Plain 100%
• Sequence Stratigraphy 100%
• Paleosol 66%
• Lake Level 66%
• Holocene 33%
• Atmospherics 33%
• Sea Level 33%
• Mediterranean Soil 33%
• Magnetic Permeability 33%
• Carbon 14 33%
• Sapropel 33%
• Soil Micromorphology 33%
• Mineralogy 33%
• Parent Material 33%
• Particle Size Distribution 33%
• Younger Dryas 33%
• Last Glacial 33%
• Early Holocene 33%
• Soil Type 33%