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Microbial activity and soil respiration under nitrogen addition in Alaskan boreal forest
| Content Provider | CiteSeerX |
|---|---|
| Abstract | Climate warming could increase rates of soil organic matter turnover and nutrient mineralization, particularly in northern high-latitude ecosystems. However, the effects of increasing nutrient availability on microbial processes in these ecosystems are poorly understood. To determine how soil microbes respond to nutrient enrichment, we measured microbial biomass, extracellular enzyme activities, soil respiration, and the community composition of active fungi in nitrogen (N) fertilized soils of a boreal forest in central Alaska. We predicted that N addition would suppress fungal activity relative to bacteria, but stimulate carbon (C)-degrading enzyme activities and soil respiration. Instead, we found no evidence for a suppression of fungal activity, although fungal sporocarp production declined significantly, and the relative abundance of two fungal taxa changed dramatically with N fertilization. Microbial biomass as measured by chloroform fumigation did not respond to fertilization, nor did the ratio of fungi: bacter-ia as measured by quantitative polymerase chain reaction. However, microbial biomass C:N ratios narrowed significantly from 16.0 1.4 to 5.2 0.3 with fertilization. N |
| File Format | |
| Access Restriction | Open |
| Subject Keyword | Soil Respiration Microbial Activity Nitrogen Addition Alaskan Boreal Forest Microbial Biomass Fungal Activity Stimulate Carbon Northern High-latitude Ecosystem Extracellular Enzyme Activity Microbial Process Relative Abundance Soil Organic Matter Turnover Climate Warming Boreal Forest Nutrient Mineralization Central Alaska Community Composition Chloroform Fumigation Enzyme Activity Quantitative Polymerase Chain Reaction Soil Microbe Respond Nutrient Availability Active Fungi Nutrient Enrichment Fungal Taxon Fungal Sporocarp Production |
| Content Type | Text |