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

Earth and Planetary Sciences

• Record 100%
• Oxygen Isotope 60%
• Structural Basin 60%
• Lake 60%
• Peninsula 40%
• Drying 40%
• Open Water 40%
• Lake Level 40%
• Climate Variation 40%
• Lacustrine Deposit 40%
• Ostracod 40%
• Datum 40%
• Document 40%
• Core 40%
• Deposit 40%
• Holocene 40%
• Organic Matter 20%
• Rainfall 20%
• Sedimentation 20%
• Trace Element 20%
• Inference 20%
• Aragonite 20%
• Covariance 20%
• Wetland 20%
• Green Alga 20%
• Paleoclimate 20%
• Isotopic Composition 20%
• Reconstruction 20%
• Basin Hydrology 20%
• Bronze Age 20%
• Sinkhole 20%
• Information 20%
• Mediterranean Region 20%
• Temperature 20%
• Culture 20%
• History 20%
• Vegetation 20%
• Condition 20%
• Support 20%
• Plant 20%
• Bicarbonate 20%
• Filling 20%
• Isotope 20%
• Expansion 20%
• Calcite 20%
• Peat 20%
• Western Asia 20%