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Published on: July 3, 2016
Soil microbial legacies differ following drying-rewetting and freezing-thawing cycles
Annelein Meisner1,2,3,4, Basten L Snoek5, Joseph Nesme6
1Microbial Ecology, Department of Biology, Lund University, Ecology Building, SE-223 62, Lund, Sweden. AnneleinMeisner@gmail.com.
Soil drying-rewetting cycles significantly impact soil microbes and CO2 emissions more than freezing-thawing cycles. The legacy of drying-rewetting alters microbial responses to subsequent freezing-thawing events.
Area of Science:
- Soil science
- Microbiology
- Climate change impacts
Background:
- Climate change is altering soil moisture dynamics through altered drying-rewetting and freezing-thawing cycles.
- Soil water availability is a key factor influencing soil microbial activity and community structure.
- The long-term effects of these cycles on soil microbiome resilience and function remain under investigation.
Purpose of the Study:
- To investigate the legacy effects of drying-rewetting and freezing-thawing cycles on soil microbial communities.
- To compare the impact of these two distinct climate-driven soil moisture fluctuations on soil respiration and microbiome structure.
- To test the hypothesis that freezing-thawing and drying-rewetting cycles have similar effects on the soil microbiome.
Main Methods:
- Microcosm experiments were designed with a two-phase approach to establish legacy effects.
- Phase 1 involved exposing soil samples to either a drying-rewetting or freezing-thawing cycle.
- Phase 2 subjected these previously treated soils to the alternative cycle, measuring soil respiration and analyzing microbiome structure.
Main Results:
- Rewetting events following drying caused larger carbon dioxide (CO2) pulses and greater shifts in microbiome structure compared to thawing events.
- A prior drying-rewetting cycle (legacy) significantly influenced the soil microbiome's response and CO2 emissions during a subsequent freezing-thawing cycle.
- Conversely, a freezing-thawing legacy did not substantially alter the microbial response to a subsequent drying-rewetting cycle.
Conclusions:
- Drying-rewetting cycles exert a stronger influence on soil microbial communities and associated CO2 production than freezing-thawing cycles.
- The observed differences are attributed to sustained alterations in soil microbiome structure induced by drying-rewetting events.
- Understanding these differential impacts is crucial for predicting soil ecosystem responses to climate change.
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