A Canopy Shift in Interior Alaskan Boreal Forests: Consequences for Above- and Belowground Carbon and Nitrogen Pools during Post-fire Succession

Keyphrases

• Aboveground Carbon 100%
• Aboveground Net Primary Productivity 25%
• Accumulation Pattern 25%
• Aging Trajectories 25%
• Alaska Paper Birch 25%
• Belowground Carbon 100%
• Betula Neoalaskana 25%
• Black Spruce 100%
• Boreal Forest 100%
• C Accumulation 50%
• C Pools 50%
• Carbon C 25%
• Carbon Pools 100%
• Change Model 25%
• Climate Feedback 25%
• Climate Warming 25%
• CO2 Emissions 25%
• Deciduous Species 25%
• Decomposition Rate 25%
• Drying Conditions 25%
• Fast Rates 25%
• Fire Behavior 25%
• Fire Climate 25%
• Fire Severity 25%
• Flammability 25%
• Forest Carbon 25%
• Forest Regrowth 25%
• Fungal Decomposers 25%
• Global Change 25%
• High Latitude 25%
• Interior Alaska 25%
• Mannan-oligosaccharide 25%
• N Accumulation 25%
• N Availability 25%
• N Pool 50%
• Negative Feedback 25%
• Nitrogen N 25%
• Nitrogen Pools 100%
• Picea Mariana 25%
• Pool Size 25%
• Populus Tremuloides 25%
• Positive Feedback 25%
• Post-fire Succession 100%
• Reduced Exposure 25%
• Self-replication 25%
• Soil Organic Layer 50%
• Species Replacement 25%
• Spruce Stands 25%
• Stem Wood 75%
• Successional Trajectory 75%
• Thick Layer 25%
• Trembling Aspen 25%

Agricultural and Biological Sciences

• Betula 16%
• Betula papyrifera 16%
• Boreal Forest 100%
• Deciduous 100%
• Fire Severity 16%
• Global Change 16%
• Organic Soil 33%
• Picea mariana 83%
• Populus 16%
• Populus tremuloides 16%
• Primary Productivity 16%
• Regrowth 16%
• Stemwood 50%