Reconstruction of Holocene climate variability within the Central Mediterranean using lake sediments from the Akrotiri Peninsula, Crete

Earth and Planetary Sciences

• Climate Variation 100%
• Lacustrine Deposit 100%
• Holocene 100%
• Oxygen 18 100%
• Open Water 66%
• Lake Level 66%
• Ostracod 66%
• Drying 33%
• Trace Element 33%
• Aragonite 33%
• Covariance 33%
• Green Alga 33%
• Paleoclimate 33%
• Isotopic Composition 33%
• Basin Hydrology 33%
• Bronze Age 33%
• Sinkhole 33%
• Mediterranean Region 33%
• Vegetation 33%
• Calcite 33%
• Western Asia 33%
• Organic Matter 33%

INIS

• sediments 100%
• climates 100%
• lakes 100%
• oxygen isotopes 50%
• deposits 50%
• carbon 14 50%
• data 33%
• levels 33%
• concentration 33%
• water 33%
• shells 33%
• geochemistry 33%
• oxygen 18 33%
• information 16%
• control 16%
• algae 16%
• layers 16%
• drying 16%
• expansion 16%
• calcite 16%
• aragonite 16%
• vegetation 16%
• carbonates 16%
• sedimentation 16%
• isotopes 16%
• peat 16%
• asia 16%
• hydrology 16%
• trace elements 16%
• organic matter 16%
• isotope ratio 16%
• wetlands 16%
• bronze 16%