Abstract

Naturally produced by microbial processes in soil, nitrous oxide (N2O) is an important greenhouse gas contributing to climate change. Accordingly, there is a need to accurately quantify the capability of forest ecosystems to exchange N2O with the atmosphere. While N2O emissions from soils have been well studied, trees have so far been overlooked in N2O inventories. Here, we show that stems of mature beech trees (Fagus sylvatica) may act as a substantial sink of N2O from the atmosphere under conditions of soils consuming N2O. Consistent consumption of N2O by all stems investigated (ranging between −2.4 and −3.8 µg m−2 h−1) is a novel finding in contrast to current studies presenting trees as N2O emitters. To understand these fluxes, N2O exchange of photoautotrophic organisms associated with beech bark (lichens, mosses and algae) was quantified under laboratory conditions. All these organisms were net N2O sinks at full rehydration and temperature of 25 °C. The consumption rates were comparable to stem consumption rates measured under field conditions. Cryptogamic stem covers could be a relevant sink of N2O in European beech forests.

Highlights

  • Nitrous oxide (N2O) is the dominant substance depleting stratospheric ozone and contributes importantly to global radiative forcing that leads to changes in the Earth’s climate[1]

  • N2O fluxes between forests and the atmosphere have been calculated only based on N2O exchange at the soil–atmosphere interface

  • Trees have widely been overlooked as possible N2O emitters or have been presumed to play only a negligible role in forest ecosystems’ N2O exchange

Read more

Summary

Introduction

Nitrous oxide (N2O) is the dominant substance depleting stratospheric ozone and contributes importantly to global radiative forcing that leads to changes in the Earth’s climate[1]. The difference in N2O and CO2 exchange rates between the sites might be related to soil temperature being lower in Conventwald than in Stitna during the measurement campaigns (at 0.3 m depth, 9.6 °C and 15.2 °C, respectively).

Results
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.