Abstract

Two patterns of bacterial growth response upon drying and rewetting (DRW) of soils have previously been identified. Bacterial growth can either start increasing immediately after rewetting in a linear fashion (“type 1” response) or start increasing exponentially after a lag period (“type 2” response). The effect of repeated DRW cycles was studied in three soils with different response patterns after a single DRW cycle (“type 1”, “type 2” with a short lag period and “type 2” with a long lag period). The soils were exposed to seven DRW cycles, and respiration and bacterial growth were monitored after 1, 2, 3, 5, and 7 cycles. Exposure to repeated DRW shifted the bacterial growth response from a “type 2” to a “type 1” pattern, resulting in an accelerated growth recovery to a pre-disturbance growth rate. Bacterial growth in soils that initially had a “type 1” response also tended to recover faster after each subsequent DRW cycle. The respiration patterns after DRW also indicated the same transition from a “type 2” to a “type 1” pattern. Our results show that exposure to repeated DRW cycles will shape the bacterial response to future DRW cycles, which might be mediated by a shift in species composition, a physiological adjustment, evolutionary changes, or a combination of the three.

Highlights

  • Soil moisture is one of the canonical factors regulating soil microbial community composition and activity (Waksman and Gerretsen 1931; Kirchman 2018)

  • Soil S exhibited a “type 1” response where the bacterial growth rate started increasing in a linear fashion immediately after rewetting

  • The “type 1” soil exhibited a faster recovery to bacterial growth levels in a continuously moist soil compared to the “type 2” soils, with recovery times of 8.5 h, 25.0 h, and 32.7 h, in soils S, W, and G, respectively

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Summary

Introduction

Soil moisture is one of the canonical factors regulating soil microbial community composition and activity (Waksman and Gerretsen 1931; Kirchman 2018). Drastic changes in soil moisture, like drying and rewetting (DRW) cycles, lead to one of the most dynamic events in soil microbial ecology (Schimel 2018). Soil microbial communities are generally exposed to DRW events. During those events, changes in microbial growth and biomass (Bottner 1985; Kieft et al 1987; Iovieno and Bååth 2008), as well as in nutrient mineralization and availability, take place (Birch 1958; Fierer and Schimel 2002). C mineralization has been found to generally decrease with increasing number of DRW cycles, which has been linked to the depletion of available C (Fierer and Schimel 2002; Mikha et al 2005). It has been suggested that soil microbial communities that have been exposed to repeated DRW cycles may become more resistant to an additional DRW cycle

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