Abstract

Biological nitrogen (N) fixation is an important process supporting primary production in ecosystems, especially in those where N availability is limiting growth, such as peatlands and boreal forests. In many peatlands, peat mosses (genus Sphagnum) are the prime ecosystem engineers, and like feather mosses in boreal forests, they are associated with a diverse community of diazotrophs (N2-fixing microorganisms) that live in and on their tissue. The large variation in N2 fixation rates reported in literature remains, however, to be explained. To assess the potential roles of habitat (including nutrient concentration) and species traits (in particular litter decomposability and photosynthetic capacity) on the variability in N2 fixation rates, we compared rates associated with various Sphagnum moss species in a bog, the surrounding forest and a fen in Sweden. We found appreciable variation in N2 fixation rates among moss species and habitats, and showed that both species and habitat conditions strongly influenced N2 fixation. We here show that higher decomposition rates, as explained by lower levels of decomposition-inhibiting compounds, and higher phosphorous (P) levels, are related with higher diazotrophic activity. Combining our findings with those of other studies, we propose a conceptual model in which both species-specific traits of mosses (as related to the trade-off between rapid photosynthesis and resistance to decomposition) and P availability, explain N2 fixation rates. This is expected to result in a tight coupling between P and N cycling in peatlands.

Highlights

  • Nitrogen (N) fixation is the only biological pathway in which atmospheric dinitrogen (N2) is converted to a reduced form (NHx) accessible to plants

  • N2 fixation rates were the highest for S. fallax samples, but the rates of these samples could only be statistically distinguished from S. fuscum (OB), S. magellanicum (OB) and from the feather moss Hylocomium splendens

  • For S. magellanicum, we saw a strong effect of habitat (Fig 1) with N2 fixation averages being more than 20 times higher in the pine bog (PB) and spruce forest (SF), than in the open bog (OB)

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Summary

Introduction

Nitrogen (N) fixation is the only biological pathway in which atmospheric dinitrogen (N2) is converted to a reduced form (NHx) accessible to plants In this way N2-fixing microorganisms (diazotrophs) significantly contribute to the N pools of ecosystems, and thereby affect primary production of plants, given that N availability is often limiting plant biomass production [1]. Human interference through the development of techniques to artificially fix N2 for agricultural production has led to extensive eutrophication, disrupting the global N cycle [4, 5] As this disturbance of the natural N input into ecosystems affects carbon (C) cycling through its effects on primary production and decomposition [6, 7], knowledge about the drivers of N2 fixation becomes even more important

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