Rewetted peatlands are reestablished hot spots for CH4 emissions, which are subject to increased drought events
in the
course of climate change. However, the dynamics of soil methane-cycling
microbiomes in rewetted peatlands during summer drought are still
poorly characterized. Using a quantitative metatranscriptomic approach,
we investigated the changes in the transcript abundances of methanogen
and methanotroph rRNA, as well as mcrA and pmoA mRNA before, during, and after the 2018 summer drought
in a coastal and a percolation fen in northern Germany. Drought changed
the community structure of methane-cycling microbiomes and decreased
the CH4 fluxes as well as the rRNA and mRNA transcript
abundances of methanogens and methanotrophs, but they showed no recovery
or increase after the drought ended. The rRNA transcript abundance
of methanogens was not correlated with CH4 fluxes in both
fens. In the percolation fen, however, the mcrA transcript
abundance showed a positive and significant correlation with CH4 fluxes. Importantly, when integrating pmoA abundance, a stronger correlation was observed between CH4 fluxes and mcrA/pmoA, suggesting
that relationships between methanogens and methanotrophs are the key
determinant of CH4 turnover. Our study provides a comprehensive
understanding of the methane-cycling microbiome feedbacks to drought
events in rewetted peatlands.