Abstract

In pristine ombrotrophic Sphagnum-dominated peatland ecosystems nitrogen (N) is often a limiting nutrient, which is replenished by biological N2 fixation and atmospheric N deposition. It is, however, unclear which impact long-term N deposition has on microbial N2 fixing activity and diazotrophic diversity, and whether phosphorus (P) modulates the response. Therefore, we studied the impact of increased N deposition and N depletion on microbial N2 fixation and diazotrophic diversity associated with the peat moss Sphagnum magellanicum, and their interaction with P availability. Nitrogenase activities of S. magellanicum-associated microorganisms were determined by acetylene reduction assays (ARA) and 15N2 tracer methods on mosses from two geographically distinct locations with different N deposition histories, high or low N deposition, and in samples depleted in N (grown 3 years in the greenhouse) versus recent field samples. The short-term response to increased N deposition was tested for mosses differing in N and P fertilization histories. In addition, diversity of diazotrophic microorganisms was assessed by nifH gene amplicon sequencing of N-depleted mosses. We showed distinct and persistent differences in diazotrophic communities and their activities associated with S. magellanicum from sites with high versus low N deposition. Initially, diazotrophic activity was six times higher for the low N site. During incubation and repeated ARA, however, this activity strongly decreased, while it remained stable for the high N site. Activity for the high N site could not be increased by long-term experimental N deprivation. Short-term, experimental N application had an inhibitory effect on N2 fixation for both sites, which was not observed in mosses with high indirect P availability. We conclude that although N deposition negatively affects N2 fixation as also shown in previous studies, long-term effects of N deprivation on the diazotrophic activity and community are more complex. Furthermore, our results indicated that P availability might be an important factor in modulating the response of Sphagnum-associated diazotrophs to N deposition.

Highlights

  • Nitrogen (N) in the form of dinitrogen gas (N2) is the most abundant element in the Earth’s atmosphere, low availability of this essential element for plants is often limiting primary production in pristine ecosystems (Canfield et al 2010)

  • Nitrogenase activities of S. magellanicumassociated microorganisms were determined by acetylene reduction assays (ARA) and 15N2 tracer methods on mosses from two geographically distinct locations with different N deposition histories, high or low N deposition, and in samples depleted in N versus recent field samples

  • We showed distinct and persistent differences in diazotrophic communities and their activities associated with S. magellanicum from sites with high versus low N deposition

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Summary

Introduction

Nitrogen (N) in the form of dinitrogen gas (N2) is the most abundant element in the Earth’s atmosphere, low availability of this essential element for plants is often limiting primary production in pristine ecosystems (Canfield et al 2010). Biological N2 fixation is estimated to contribute about 200–250 Tg N year−1 (Tg = 1012 g) to the biosphere, including N2 fixation associated with agricultural crops (Gruber and Galloway 2008; Fowler et al 2013), while anthropogenic input from fertilizers and increased atmospheric deposition of reactive nitrogen (NHx, NOy) nearly matches this value (up to 195 Tg N year−1; Gruber and Galloway 2008) This has massively disturbed the N balance in many (pristine) ecosystems, and is expected to possibly change even N-limited sites to sites with excess N availability (Bobbink et al 1998; Granath et al 2014).

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