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Updated: Mar 1, 2026

Technique for Studying Arthropod and Microbial Communities within Tree Tissues
Published on: November 16, 2014
Microbial community composition and function beneath temperate trees exposed to elevated atmospheric carbon dioxide
Rebecca L Phillips1, Donald R Zak2, William E Holmes2
1School of Natural Resources and Environment, University of Michigan, 430 E. University Avenue, Ann Arbor, MI, 48109-1115, USA. rebecca@aero.und.edu.
Elevated atmospheric carbon dioxide (CO2) increased carbon flow in soil food webs, particularly affecting microbial respiration and fungal activity. These effects varied by tree species, with early-successional species showing greater responses to CO2 and ozone (O3) enrichment.
Area of Science:
- Soil Science
- Microbial Ecology
- Plant Ecology
Background:
- Atmospheric CO2 and O3 enrichment can alter plant growth and carbon allocation.
- Soil food webs play a crucial role in nutrient cycling and carbon sequestration.
- Understanding how these atmospheric changes impact soil microbial communities is vital for predicting ecosystem responses.
Purpose of the Study:
- To investigate the impact of elevated atmospheric CO2 and O3 on carbon flow through soil food webs.
- To determine if these effects vary among different temperate tree species.
- To assess the role of microbial metabolism in response to altered atmospheric conditions.
Main Methods:
- Utilized soils from a free-air CO2 and O3 enrichment site.
- Applied 13C-labeled cellobiose or N-acetylglucosamine to soils under factorial CO2 and O3 treatments.
- Analyzed 13C recovery in microbial respiration and phospholipid fatty acids (PLFAs).
Main Results:
- Elevated CO2 increased microbial respiration of 13C by 29% compared to ambient conditions; elevated O3 negated this effect.
- Soils under aspen and aspen-birch showed greater 13C-CO2 production than those under aspen-maple.
- Elevated CO2 enhanced microbial metabolism of 13C-cellobiose, with increased fungal activity indicated by 13C-PLFAs.
- N-acetylglucosamine amendment resulted in an order of magnitude greater 13C recovery in PLFAs than cellobiose.
Conclusions:
- Elevated CO2 significantly alters carbon flow in soil food webs, primarily by increasing microbial respiration and fungal activity.
- The impact of CO2 and O3 enrichment on soil microbial processes is species-specific, with early-successional trees (aspen, birch) exhibiting stronger responses than late-successional species (maple).
- Substrate availability (cellobiose vs. N-acetylglucosamine) influences the extent of microbial metabolism and soil carbon cycling under altered atmospheric conditions.
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