Abstract

Drought represents a significant stress to microorganisms and is known to reduce microbial activity and organic matter decomposition in Mediterranean ecosystems. However, we lack a detailed understanding of the drought stress response of microbial decomposers. Here we present metatranscriptomic and metabolomic data on the physiological response of in situ microbial communities on plant litter to long-term drought in Californian grass and shrub ecosystems. We hypothesised that drought causes greater microbial allocation to stress tolerance relative to growth pathways. In grass litter, communities from the decade-long ambient and reduced precipitation treatments had distinct taxonomic and functional profiles. The most discernable physiological signatures of drought were production or uptake of compatible solutes to maintain cellular osmotic balance, and synthesis of capsular and extracellular polymeric substances as a mechanism to retain water. The results show a clear functional response to drought in grass litter communities with greater allocation to survival relative to growth that could affect decomposition under drought. In contrast, communities on chemically more diverse and complex shrub litter had smaller physiological differences in response to long-term drought but higher investment in resource acquisition traits across precipitation treatments, suggesting that the functional response to drought is constrained by substrate quality. Our findings suggest, for the first time in a field setting, a trade off between microbial drought stress tolerance, resource acquisition and growth traits in plant litter microbial communities.

Highlights

  • Supplementary information The online version of this article contains supplementary material, which is available to authorized users.Drought is common in terrestrial ecosystems, and climate change is making drought more frequent and severe [1, 2]

  • We found distinctive physiological signatures of microbial communities growing on plant leaf litter in response to simulated decade-long drought

  • Given that natural rainfall was not observed or manipulated during our 2.5-month experiment, the differing gene expression and metabolite patterns across long-term precipitation treatments likely arose due to indirect legacy effects on microbial communities or litter chemistry driven by changes in plant communities [7, 12]

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Summary

Introduction

Drought affects biogeochemical processes through mechanisms including limitations to resource diffusion and transport as well as organismal physiological responses to water stress [4,5,6,7] Both mechanisms may cause a decline in growth and activity of microbial decomposers [6, 8]. Water limitation affects microbial growth and survival indirectly by altering substrate transport and cellular motility [6] Selection based on these physiological adaptations influences microbial community composition through changes in taxa abundance and genetic variation [6, 11, 12]. We do not have a thorough understanding of the key physiological adaptations of in situ microbes to long-term drought This knowledge gap introduces uncertainty in predictions of ecosystem processes under environmental change

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