Legacy effects of soil moisture on microbial community structure and N2O emissions. (April 2016)

• Record Type: Journal Article
• Authors: Banerjee, Samiran; Helgason, Bobbi; Wang, Lianfeng; Winsley, Tristrom; Ferrari, Belinda C.; Siciliano, Steven D.
• Is Part Of: Soil biology and biochemistry. Volume 95(2016)
• Page Start: 40
• Page End: 50
• Publication Date: 2016-04
• Subjects: Previous soil moisture -- Microbial community composition -- Nitrous oxide -- Transcript abundance -- Pyrosequencing; Soil biochemistry -- Periodicals; Soil biology -- Periodicals; Sols -- Biochimie -- Périodiques; Sols -- Biologie -- Périodiques; Sols -- Microbiologie -- Périodiques; Bodembiologie; Biochemie; 631.46
• DOI: 10.1016/j.soilbio.2015.12.004
• Languages: English
• ISSNs: 0038-0717

Abstract

Abstract: Soil moisture is a strong determinant of microbial activity exerting dominant control over gaseous and liquid diffusion rates and affecting O2 and substrate availability. Often, measures of microbial community structure and soil moisture status fail to inform our understanding of soil processes, particularly those that are governed by complex feedbacks between substrate availability and environmental conditions (e.g. nitrogen transformations). Nitrous oxide (N2 O) emissions, although conceptually regulated by soil moisture, are notoriously difficult to predict based on soil water content and nutrient status. Here, we studied agricultural soils under wetting, drying, and static moisture conditions to assess the impact of current and previous moisture on bacterial 16S rRNA composition; transcription of amoA, hao, norB, and nosZ ; and net N2 O production. Microbial community composition was dependent on previous moisture. As soils dried, bacterial rRNA contained fewer and more evenly distributed genera. We hypothesize that this was linked to the evenness of resource distribution as controlled by differences in substrate diffusion in wetting vs. drying conditions. N2 O flux depended on previous, as well as current, soil moisture status and this legacy effect was greatest at 80% water filled pore space. Overall, we found that previous moisture affected microbial activity, transcription, composition and ultimately, N2 O emissions. Our study demonstrates that, for soil microorganisms and processes, it is not only what soil moisture is, but also what it was that is important. Highlights: Nitrous oxide flux depended on previous, as well as current, soil moisture. Wetting and drying strongly affected nitrifier and denitrifier transcript abundance. Direction of soil moisture change altered bacterial community characteristics. The effect of soil moisture was greatest at 80% WFPS.