Abstract

Freeze-thaw (FT) events can influence soil functions. However, the overall impact of FTs on soil bacterial communities, especially in temperate regions, remains unclear. In this study, soil samples were collected from a midtemperate region in the northeast of China, and three incubation tests were then designed with varied FT amplitudes (i.e., at a freezing temperature of −15, −9, and −3°C, respectively), frequencies of FT cycles (i.e., under one, six, and 15 FT cycles, respectively) and soil water content (SWC) values (i.e., at 10 and 30% SWC, respectively). High-throughput sequencing of 16S rRNA gene amplicons was performed and the functional profile was further predicted based on these data, in addition to examinations of bulk microbial properties. Data analyses suggested that, first of all, the FT amplitude significantly influenced the bulk microbial properties and bacterial community (composition and function); certain taxa showed a nonlinear response to the three amplitudes. Next, compared to a single FTC, multiple FT cycles had only minor effects on the bacterial functional capabilities, although the bulk microbial properties changed significantly after multiple FT cycles. In addition, the bacterial response to FTs was influenced by the SWC, characterized by the significantly different bacterial community structures (composition and function) and the opposite trends of enzyme activities. Finally, RDA plots and a correlation network assembled data from all soil samples across the three tests and suggested that bacterial response trajectories changed because some species were influenced mainly by other species (i.e., biotic environment) during FT processes.

Highlights

  • In temperate regions, freeze-thaw (FT) events are common during spring and fall as well as mild winters and could significantly influence soil functions, such as microbial responses that play a vital role in soil nutrients [1, 2]

  • In the Amplitude test, the Microbial Biomass Nitrogen (MBN) decreased significantly with increasing amplitude, while a significant increase in the Protease activity (PA) was only detected in 9F (P < 0.05, Table 1)

  • Significant differences in either the MBN or PA were only detected between soil water content (SWC) of 10% and 30% (P < 0.05) and not between an FT and the control in the SWC test (Table 1)

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Summary

Introduction

Freeze-thaw (FT) events are common during spring and fall as well as mild winters and could significantly influence soil functions, such as microbial responses that play a vital role in soil nutrients [1, 2]. Studies using distinct soils and methods have always reported inconsistent effects of FT events on microorganisms [3]. In contrast to the decreased microbial biomass detected after FT processes in some systems [5, 6], insignificant effects were reported on microbial biomass [7, 8]. A significant increase in microbial activity was reported in some cases [6, 9], whereas others reported insignificant or significant decrease effects [10, 11]. The results of many investigations within one study should be compiled to help elucidate the impact of FT on soil microorganisms

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