Title: Earthworms and warming alter methane uptake and methane-cycling microbial community in meadow soil
https://doi.org/10.1007/s42832-024-0255-1
The function and service of biologically driven ecosystems are undergoing significant changes due to climate warming. Earthworms play a crucial role as soil engineer by modulating the effects of climate change on soil nutrient cycle through alterations to biotic and abiotic soil conditions. However, there is currently a scarcity of information regarding the impacts of earthworms and warming on soil CH4 uptake and their associated microbial mechanisms. This study conducted a 61-day microcosm experiment to investigate the impact of warming (temperature rise from 14.2 °C to 17.2 °C) and the presence of earthworms (Eisenia fetida and Moniligaster japonicus) on soil CH4 uptake. We employed gas chromatography and high-throughput sequencing to investigate the fluctuations in soil CH4 uptake and the microbial communities involved in methane cycling. Compared to low temperature conditions (14.2 °C), we observed that warming significantly increased soil CH4 uptake in all treatments (non-earthworm: 51.85%; Eisenia fetida: 50.88%; Moniligaster japonicus: 71.78%). Both Eisenia fetida and Moniligaster japonicus significantly reduced soil CH4 uptake at two temperatures compared to the non-earthworm treatment. Nevertheless, no significant impacts were found on soil CH4 uptake due to the interactions between earthworms and warming. The methanotroph communities exhibited notable variations among earthworm treatments, whereas the methanogenic communities displayed significant differences among temperature treatments. The interaction between earthworm and warming also resulted in noticeable variations in both methanogenic and methanotrophic communities. The FAPROTAX analysis revealed that earthworms and warming altered relative abundance of methanogens and methanotroph associated with CH4 cycle functions. Soil properties exhibited a negative impact on CH4 uptake, with DOC identified as the most crucial variable in predicting soil CH4 uptake, while the α-diversity of methanotrophs was associated with enhanced CH4 uptake. This study emphasized the crucial role of soil fauna in adjusting soil greenhouse gas emissions under the context of global warming.
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