Abstract

To understand how and to what extent single or multiple perturbations can alter the relationships between the abundances of different nitrifier groups and nitrification, soil microcosms were exposed to six disturbance treatments: a heat shock, cold shock, or control conditions applied to undisturbed soils or to soils that had previously been subjected to a first heat shock. We monitored the recovery of the abundances of four main nitrifier groups (ammonia-oxidizing archaea and bacteria, AOA and AOB, respectively, and Nitrobacter and Nitrospira nitrite oxidizers) as well as nitrification activity for 25 days. AOA were sensitive to cold shocks, whereas AOB were not; the latter were sensitive to heat shock. Despite the variations, both groups were resilient to the first disturbance. In contrast, Nitrobacter was affected by both disturbances, whereas Nitrospira was resistant to both shocks. Prior exposure to a heat shock affected each group’s responses as well as the relationships between them. For example, AOB were more vulnerable to heat shock in pre-exposed soils, whereas under the same circumstances, AOA were resilient. Nitrification activity was resistant to the first disturbances, but a legacy effect was observed, and nitrification was highest in Heat-Heat and lowest in Heat-Cold treatments. Overall, our study shows that within soil nitrifiers, temporal patterns and legacy effects interact to result in complex disturbance responses.

Highlights

  • Introduction2 iDiv (German Centre for Integrative Biodiversity Research Halle-Jena-Leipzig), Deutscher pl

  • Nitrification, the oxidation of ammonia to nitrite and nitrate, is an essential ecosystem function, tied to fertility and plantElectronic supplementary material The online version of this article contains supplementary material, which is available to authorized users.2 iDiv (German Centre for Integrative Biodiversity Research Halle-Jena-Leipzig), Deutscher pl. 5E, 04103 Leipzig, GermanyAmmonia oxidation is performed by the bacterial genera Nitrosomonas, Nitrosospira (β-Proteobacteria), and Nitrosococcus (γ- Proteobacteria; Purkhold et al 2000) and by archaea from the phylum Thaumarchaeota (Leininger et al 2006)

  • and/or archaea (AOA) abundance in heat-shocked soils was 27.7% of that found for controls (p = 0.025) and 6.7% of that of controls in coldshocked soils (p < 0.001) on day 11

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Summary

Introduction

2 iDiv (German Centre for Integrative Biodiversity Research Halle-Jena-Leipzig), Deutscher pl. Ammonia oxidation is performed by the bacterial genera Nitrosomonas, Nitrosospira (β-Proteobacteria), and Nitrosococcus (γ- Proteobacteria; Purkhold et al 2000) and by archaea from the phylum Thaumarchaeota (Leininger et al 2006). Both AOB and AOA harbor the ammonia. Biol Fertil Soils monooxygenase gene (amoA), which serves as a functional gene marker for the identification of ammonia oxidizers in environmental samples (Leininger et al 2006). AOB are favored under high soil N availability (Di et al 2009; Sterngren et al 2015; Ma et al 2016)

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