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Drought Impacts on Plant-Soil Carbon Allocation-Integrating Future Mean Climatic Conditions
Vinzent Leyrer1, Juliette Blum1, Sven Marhan1
1Department of Soil Biology, Institute of Soil Science and Land Evaluation, University of Hohenheim, Stuttgart, Germany.
Drought impacts soil microbes and carbon allocation, but warming is the main driver of agroecosystem response. Prior reduced precipitation legacies affect carbon flow to microbial biomass during drought.
Area of Science:
- Soil Science
- Microbiology
- Climate Change Ecology
Background:
- Droughts significantly alter soil microbial communities and plant-soil carbon dynamics.
- Previous climate conditions can modify drought impacts on soil microbiomes.
- Future climate projections indicate warmer and drier conditions, necessitating studies under simulated future climates.
Purpose of the Study:
- To investigate the effects of simulated drought on an agroecosystem pre-conditioned to warmer and drier conditions.
- To trace the allocation of recently assimilated carbon from plants to soil microbes under drought and rewetting.
- To assess the legacy effects of reduced mean precipitation and continuous warming on carbon cycling.
Main Methods:
- Utilized the 'Hohenheim Climate Change' field experiment with 12 years of simulated climate change.
- Applied an 8-week drought followed by rewetting to an arable agroecosystem.
- Used in situ 13CO2 pulse labeling of winter wheat to track carbon allocation dynamics before, during, and after drought.
Main Results:
- Severe drought reduced soil respiration and gram-positive bacteria abundance but did not affect other microbial groups or total microbial biomass carbon.
- Pre-exposure to reduced mean precipitation had a legacy effect, decreasing carbon allocation to microbial biomass by 50%.
- Continuous soil warming increased plant biomass, labile carbon, respiration, and shifted microbial carbon sources towards soil organic matter.
Conclusions:
- Moderate shifts in precipitation patterns can create legacies affecting plant-derived carbon allocation in microbial biomass during drought.
- Soil warming is a dominant factor influencing temperate agroecosystem responses to drought, primarily by increasing temperature.
- Future drought impacts on agroecosystems will likely be dominated by rising temperatures rather than precipitation changes alone.
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