EGU2020-13985, updated on 12 Jun 2020
https://doi.org/10.5194/egusphere-egu2020-13985
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Soil warming leads to an up-regulation of genes involved in the decomposition of organic N in a subarctic grassland

Joana Séneca1, Andrea Söllinger2, Alexander Tveit2, Petra Pjevac1,3, Craig Herbold1, Tim Urich4, Josep Peñuelas5,6, Ivan Janssens7, Michael Wagner1, Bjarni Sigurdsson8, and Andreas Richter1
Joana Séneca et al.
  • 1Centre for Microbiology and Environmental Systems Science, University of Vienna, Althanstrasse 14, 1090 Vienna, Austria
  • 2Department of Arctic and Marine Biology, UiT The Arctic University of Norway, Framstredet 39, 9037, Tromsø,Norway
  • 3Joint Microbiome Facility of the Medical University of Vienna and the University of Vienna, Vienna, Austria
  • 4Institute of Microbiology, Center for Functional Genomics of Microbes, University of Greifswald, Felix-Hausdorff-Str. 8 17487 Greifswald, Germany
  • 5CSIC, Global Ecology Unit CREAF-CSIC-UAB, Barcelona, Spain
  • 6CREAF, Cerdanyola del Vallès, 08193, Catalonia, Spain
  • 7Department of Biology, University of Antwerp, Universiteitsplein 1, Wilrijk 2610, Belgium
  • 8Faculty of Natural Resources and Environmental Sciences, Agricultural University of Iceland, Hvanneyri, IS-311, Borgarnes, Iceland

Soil microorganisms control the breakdown (depolymerization) of high molecular weight organic matter in soil and its mineralization and release as CO2 to the atmosphere. The enzymatic reactions involved in these steps are known to be temperature sensitive. Therefore, increasing global temperatures are expected to accelerate microbial activity and ecosystem processes and stimulate further CO2 emissions, potentially causing a positive feedback to climate change. On the other hand, higher turnover rates demand an increased amount of energy allocated for growth, enzyme production and maintenance, which can progressively deplete soils from substrate, forcing a reduction of microbial biomass and/or activity and a higher metabolic investment in resource acquisition.

The response of ecosystems to warming has been shown to be related with its duration and magnitude. In this study, we analyzed soils from long-term (>50 years) and short-term (8 years) warmed plots at the natural geothermal warming experiment ForHot (https://forhot.is), located in a sub-arctic grassland in Iceland. Previous studies at this warming experiment have shown an accelerated C cycle in response to warming, with decreased soil carbon stocks, and higher rates of decomposition of labile and recalcitrant organic matter, regardless of the warming duration. In addition to carbon losses, increased N losses from soils were found, but no change in the N content of the vegetation along the temperature gradient. Additionally, both ammonification and nitrification rates were shown to increase under warming, pointing to higher N losses from warmed soils.

In this study, we tested the hypothesis that under warming microorganisms become progressively limited in organic substrates, leading to a higher microbial investment in organic N decomposing enzymes to mine the existing organic N sources present in their surroundings. This hypothesis is based on previous data, that showed that microbial turnover was increased in the warmed plots. Under this assumption, we expected to observe higher expression levels of genes coding for organic N mining extracellular enzymes in warmed plots.

We analyzed the metatranscriptome from a total of 16 soil samples representative of ambient (n=4) and +6°C warmed (n=4) soils, for both grassland types. Additionally, we sequenced the metagenomes of 4 soil samples, representative of each condition, to allow for transcript mapping and differential gene expression analysis.

We used Hidden Markov models to screen the assembled metatranscriptomes for genes involved in the degradation of chitin, proteinaceous compounds, nucleic acids and microbial cell walls. The subcellular location and presence/absence of signal peptides was assessed with Psort and SignalP to discriminate transcripts involved in internal recycling from those targeted for secretion. First results show a general up-regulation of all transcripts involved in organic N degradation in the grassland subjected to long-term warming, whereas this trend is less clear in the short-term warmed grassland. Further work includes cross-referencing gene expression patterns with potential changes in active community composition.

We conclude that an acceleration in microbial turnover rates in response to warming is coupled to a higher investment in N acquisition enzymes, as indicated by an up-regulation of genes involved in upstream processes of organic N degradation.

How to cite: Séneca, J., Söllinger, A., Tveit, A., Pjevac, P., Herbold, C., Urich, T., Peñuelas, J., Janssens, I., Wagner, M., Sigurdsson, B., and Richter, A.: Soil warming leads to an up-regulation of genes involved in the decomposition of organic N in a subarctic grassland, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13985, https://doi.org/10.5194/egusphere-egu2020-13985, 2020