Pollen and macrofossil evidence of Late Pleistocene and Holocene treeline fluctuations from an alpine lake in Colorado, USA

Keyphrases

• Abies 50%
• Alpine Lake Sediments 50%
• Alpine Lakes 100%
• Artemisia Annua 100%
• Bristlecone pine 50%
• Central Colorado 50%
• Chron 50%
• Climate Cooling 50%
• Climatic Trends 50%
• Colorado 100%
• Early Holocene 100%
• High-resolution 50%
• Kite 50%
• Lake Sediment Core 50%
• Late Holocene 100%
• Late Pleistocene 100%
• Lodgepole pine 50%
• Macrofossils 100%
• Magnetic Susceptibility 50%
• P. Edulis 50%
• Parkland 50%
• Picea 100%
• Pinus 50%
• Pinus Aristata 50%
• Pion 50%
• Plant Macrofossils 50%
• Pollen Plants 50%
• Steppe 50%
• Subalpine 50%
• Summer Insolation 50%
• Treeline 100%
• Tundra 50%
• Vegetation Change 50%
• Warm Conditions 50%
• Warm Period 50%
• Winter Precipitation 50%
• Younger Dryas 50%

Earth and Planetary Sciences

• Colorado 100%
• Early Holocene 66%
• Holocene 100%
• Lacustrine Deposit 33%
• Late Pleistocene 100%
• Magnetic Permeability 33%
• Sediment Core 33%
• Timberline 100%
• United States of America 100%
• Vegetation 33%
• Younger Dryas 33%