Abstract

Both plant invasion and nitrogen (N) enrichment should have significant impact on mangrove ecosystems in coastal regions around the world. However, how N2O efflux in mangrove wetlands responds to these environmental changes has not been well studied. Here, we conducted a mesocosm experiment with native mangrove species Kandelia obovata, invasive salt marsh species Spartina alterniflora, and their mixture in a simulated tide rotation system with or without nitrogen addition. In the treatments without N addition, the N2O effluxes were relatively low and there were no significant variations among the three vegetation types. A pulse loading of exogenous ammonium nitrogen increased N2O effluxes from soils but the stimulatory effect gradually diminished over time, suggesting that frequent measurements are necessary to accurately understand the behavior of N-induced response of N2O emissions. With the N addition, the N2O effluxes from the invasive S. alterniflora were lower than that from native K. obovata mesocosms. This result may be attributed to higher growth of S. alterniflora consuming most of the available nitrogen in soils, and thus inhibiting N2O production. We concluded that N loading significantly increased N2O effluxes, while the invasion of S. alterniflora reduced N2O effluxes response to N loading in this simulated mangrove ecosystem. Thus, both plant invasion and excessive N loading can co-regulate soil N2O emissions from mangrove wetlands, which should be considered when projecting future N2O effluxes from this type of coastal wetland.

Highlights

  • Nitrous oxide (N2O) contributes only 5% to estimated global warming potentials [1], its global warming strength is 265 times more powerful than CO2 over a 100-year time frame [2]

  • With N addition, after the refreshment of tidal water, the rate of NH4+-N loading in the mesocosms decreased with time from 1.54 to 0.002 g m-2, the rate of NO3--N loading in the mesocosms increased to a peak by the day 8 (0.21 mg m-2), and decreased gradually to

  • Compared to the treatment with N addition, we found that the N2O effluxes were relatively low (

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Summary

Introduction

Nitrous oxide (N2O) contributes only 5% to estimated global warming potentials [1], its global warming strength is 265 times more powerful than CO2 over a 100-year time frame [2]. The rapid increase in atmospheric N2O concentrations has gained much attention in quantifying N2O effluxes from various sources. N2O effluxes from wetlands are related to several biological processes, mainly including nitrification (ammonium oxidation and nitrifier denitrification) [6], denitrification and nitrate-ammonification [7]. These processes can be affected by many abiotic and biotic factors, such as soil temperature, oxygen level, and substrate availability (bioavailable carbon, ammonium and nitrate) in the soil [8, 9]. The change in vegetation type, such as plant invasion, may have a potential effect on N2O effluxes

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