Century-scale time since permafrost thaw affects temperature sensitivity of net methane production in thermokarst-lake and talik sediments

Keyphrases

• Soil Organic Carbon 100%
• Temperature Sensitivity 100%
• Methane Production 100%
• Permafrost Thaw 100%
• Thermokarst Lakes 100%
• Talik 100%
• Microbial Community 66%
• Anaerobic Conditions 66%
• Incubation Temperature 66%
• Temperature Control 33%
• Methane 33%
• Climate Warming 33%
• In Situ 33%
• Microbial Community Structure 33%
• Lake Sediment Core 33%
• Functional Microbial Community 33%
• Greenhouse Gas 33%
• Carbon Dioxide CO2 33%
• Microbial Degradation 33%
• Positive Feedback 33%
• Temperature Variation 33%
• Chronosequence 33%
• Frozen Soil 33%
• Low Abundant 33%
• Sensitivity to Change 33%
• C Mineralization 33%
• Difference in Temperature 33%
• CH4 Production 33%
• Permafrost Soils 33%
• Methanogenic Community 33%
• Permafrost Carbon Feedback 33%
• CH4 Production Potential 33%
• SOM Quality 33%
• Community Sensitisation 33%

Earth and Planetary Sciences

• Methane 100%
• Thermokarst 100%
• Talik 100%
• Timescale 100%
• Microbial Community 60%
• Soil Organic Carbon 60%
• Carbon Dioxide 40%
• Temperature Control 20%
• Sediment Core 20%
• Lacustrine Deposit 20%
• Positive Feedback 20%
• Community Composition 20%
• Frozen Soil 20%
• Emissions 20%
• Greenhouse Gas 20%
• Chronosequence 20%

Immunology and Microbiology

• Temperature Sensitivity 100%
• Mineralization 66%
• Incubation Temperature 66%
• Microbial Degradation 33%
• Positive Feedback 33%
• Chronosequence 33%