Fire, vegetation, and Holocene climate in a southeastern Tibetan lake: A multi-biomarker reconstruction from Paru Co

Keyphrases

• Holocene Climate 100%
• Polycyclic Aromatic Hydrocarbons 100%
• Vegetation Change 100%
• Fire Climate 100%
• Indian Summer Monsoon 100%
• Multi-biomarker 100%
• Tibetan Lakes 100%
• Fire History 66%
• Combustion 66%
• Late Holocene 66%
• N-alkanes 66%
• Levoglucosan 66%
• Vegetation Fires 66%
• Fecal Sterols 66%
• Fecal Stanols 66%
• Climate Change 33%
• Millennial-scale 33%
• Molecular Biomarkers 33%
• Tibetan Plateau 33%
• Grass 33%
• High Temperature 33%
• Shallow Lakes 33%
• Grassland 33%
• Anthropogenic Influence 33%
• Core Sediments 33%
• Oscillation 33%
• Ice Core 33%
• Human Animals 33%
• Early Holocene 33%
• Insolation 33%
• Civilization 33%
• Sediment Samples 33%
• Specific Marker 33%
• Sedimentary Core 33%
• Method Detection Limit 33%
• Forest Cover 33%
• Net Increase 33%
• Grazing Animals 33%
• Burning Process 33%
• Multiple Biomarkers 33%
• Distribution Type 33%
• Continuous Record 33%
• Peak Temperature 33%
• Vegetation Distribution 33%
• Multi-proxy Approach 33%
• Fire Events 33%
• Organic Molecular 33%
• Fire Type 33%
• Southeastern Tibetan Plateau 33%
• High Molecular Weight Polycyclic Aromatic Hydrocarbons 33%
• Mannosan 33%
• Monosaccharide Anhydrides 33%
• Nyainqentanglha 33%
• Smoldering Fire 33%
• Millennial Timescale 33%
• Human Fecal Sample 33%
• Small Lakes 33%
• Holocene Fires 33%
• Local Environmental Changes 33%

Earth and Planetary Sciences

• Holocene 100%
• Polycyclic Aromatic Hydrocarbon 57%
• Indian Summer Monsoon 42%
• Fire History 28%
• Tibetan Plateau 28%
• Alkane 28%
• Climate Change 14%
• Environmental Change 14%
• Forest Cover 14%
• Sediment Core 14%
• Early Holocene 14%
• Ice Core 14%
• Detection Method 14%
• Molecular Weight 14%
• Grassland 14%
• Peak Temperature 14%