GRADCATCH - Using natural environmental GRADients to decipher the adaptation of soil microbial Communities to climATe CHange

Climate change has large effects on most biomes on Earth. This includes effects on soil microorganisms and their activity, which in turn may affect the release of greenhouse gases and the turnover of nutrients important to plants. Despite their importance, these effects are poorly understood by the scientific community. The overall aim of GRADCATCH is to unravel the effects of climate change at regional and global scales on soil microorganisms and their feedbacks on climate. To accomplish this, GRADCATCH will study trans-continental natural gradients in aridity, latitude and altitude.

 

 

The GRADCATCH project investigated the short- and long-term effects of climate on soil microorganisms across six major climate gradients. This included three temperature gradients (from N to S Greenland, from N to S Europe, and from mountain top to valley in the Alps) and three aridity gradients (from moist N Spain to dry SE Spain and two gradients in South Africa from moist mountains to hot deserts).

GRADCATCH made significant strides in understanding the links between soil microbial diversity and key ecosystems functions performed by microorganisms, such as nutrient cycling and emission of greenhouse gases. GRADCATCH showed how soil microbial communities respond to climate change, with several key findings that have important implications for science and environmental management.

Across the European gradient, we demonstrated the importance of fungal diversity in sustaining functionality related to soil carbon, nitrogen and phosphorous cycling. This highlights the importance of fungal diversity in maintaining soil health and regulating ecosystem functions, particularly in temperate forests.

The Alpine elevational gradient revealed how soil organic matter influences microbial activity and greenhouse gas emissions in mountains. 

In Spain, we found that increasing aridity changes microbial community structures, but key soil functions remained stable due to functional redundancy, i.e. different soil microorganisms perform similar functions in different environments across the strong gradient from moist forests to drylands. This means that even if some microbes are lost due to increased aridity, others can take over their roles, helping to maintain soil health. 

In contrast to the Spanish soils, microbial activity in a Greenlandic soil peaked at moderate drought levels but declined sharply under severe drought, indicating a tipping point in drought response. Also, High Arctic soils from North Greenland showed lower resistance compared to southern soils indicating higher sensitivity to drought events. Across the Greenlandic gradient, soil organic matter content was found to be crucial for microbial activity during droughts. 

A marker gene-based workflow developed during GRADCATCH allowed us to link soil bacterial traits to environmental factors, showing how changes in climate and vegetation affect bacterial communities. This novel approach can complement metagenomic studies and improve trait-based biogeochemical models, leading to better predictions of e.g. how ecosystems will respond to climate change.

Overall, GRADCATCH provided valuable insights into the complex interactions between climate, soil properties, and microbial communities. These findings are crucial for predicting ecosystem responses to climate change and guiding soil management practices to maintain healthy and productive soils.

 

 

 

  • Donhauser, Doménech-Pascual, Han X., Jordaan K., Ramond J.-B., Frossard A., Romaní A.M., and Priemé A. (2024) Modelling soil prokaryotic traits across environments with the trait sequence database ampliconTraits and the R package MicEnvMod. Biological Informatics 83, article 102817. https://doi.org/10.1016/j.ecoinf.2024.102817

  • Han, X., Beck. K., Bürgmann H., Frey, B., Stierli, B., Frossard, A. (2023). Synthetic oligonucleotides as quantitative PCR standards for quantifying microbial genes. Frontiers in Microbiology 14:1279041. https://doi.org/10.3389/fmicb.2023.1279041

  • Han X., Doménech-Pascual A., Casas-Ruiz J.P., Donhauser J., Jordaan K., Ramond J.-B., Priemé A., Romaní A.M., and Frossard A. (2024) Soil organic matter properties drive microbial enzyme activity and greenhouse gas fluxes along an elevational Geoderma, 449, article 116993. https://doi.org/10.1016/j.geoderma.2024.116993

  • Doménech-Pascual Rodriguez L.C., Han X., Casas-Ruiz J.P., Ferriol-Ciurana J., Donhauser J., Jordaan K., Allison S.D., Frossard A., Priemé A., Ramond J.B., and Romaní A.M. Soil functions are shaped by aridity through soil properties and the microbial community structure. Accepted for publication in Applied Soil Ecology, APSOIL-D-25-00261R1.

 

 

 

 

 

Staff

Name Title
Aline Frossard Tenure-track research scientist
Anders Priemé Professor
Anna Doménech Laboratory assistant
Anna M. Rómani Professor
Han Xingguo Post doc
Jean-Baptiste Ramond Assistant professor
Joan Pere Casas-Ruiz Post doc
Luis Bañeras Vives Associate professor
Steven Allison Professor

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