Historical climate important for soil responses to future climate change
According to the study, microorganisms that have been subjected to long-term drought find it easier than other microbes to recover when moisture in the soil increases again.
“Our results show that the historical climate will affect how microorganisms respond and contribute to climate change in the future. Bacteria adapted to drought could slow the rate of carbon loss from soils”, explains Lettice Hicks, biologist at Lund University.
In the study, she and her colleagues examined soil that had been subjected to long-term drought – in this case 18 years of experimental summer drought. The aim was to study how the microorganisms cope and how they recover.
When the soil is moist, the bacteria are active, breaking down organic material. This process provides essential nutrients for plants, and, while a proportion of the carbon from organic matter is stored in the soil as bacterial tissue, some is released into the air as carbon dioxide.
During drought, however, the bacteria stop growing and no longer perform their important task in the ecosystem. When rain eventually falls and the soil regains moisture, the bacteria begin to work again. The result is an immediate increase in emissions of carbon dioxide into the air, but as the bacteria recover very quickly, the fraction of carbon released from the soil decreases.
“The carbon balance is affected, as the growth of bacteria keeps carbon in the soil. These findings suggest that microbial communities can adapt to changing climatic conditions, and this might slow the rate of carbon loss from soils”, concludes Lettice Hicks.
Publication: Soil microbial moisture dependences and responses to drying‐rewetting: the legacy of 18 years drought
Lettice Hicks, researcher
Department of Biology, Lund University
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