A 60,000-year record of hydrologic variability in the Central Andes from the hydrogen isotopic composition of leaf waxes in Lake Titicaca sediments

Keyphrases

• Last Glacial Period 100%
• Hydrogen Isotopes 100%
• South American Summer Monsoon 100%
• Hydrological Variability 100%
• Lake Titicaca 100%
• Central Andes 100%
• Leaf Wax 100%
• High Latitude 66%
• Wet Condition 66%
• North Atlantic 33%
• Centralized Control 33%
• Sediment Core 33%
• Younger Dryas 33%
• Last Deglaciation 33%
• Ice Core 33%
• Evapotranspiration 33%
• Late Holocene 33%
• Early Holocene 33%
• Primary Control 33%
• Summer Insolation 33%
• Drying Conditions 33%
• Precipitation Variability 33%
• Late Glacial 33%
• Monsoon Precipitation 33%
• Monsoon Variability 33%
• Dominant Controls 33%
• Summer Monsoon Rainfall 33%
• Holocene Epoch 33%
• Millennial-scale Events 33%
• Insolation Forcing 33%
• Titicaca 33%
• Tropical Forcing 33%

Earth and Planetary Sciences

• Isotopic Composition 100%
• Andes 100%
• Last Glacial 100%
• Holocene 66%
• North Atlantic 33%
• Sediment Core 33%
• Younger Dryas 33%
• Last Deglaciation 33%
• Early Holocene 33%
• Ice Core 33%
• Late Glacial 33%
• Evapotranspiration 33%