Impact of Multiple Ecological Stressors on a Sub-Arctic Ecosystem: No Interaction Between Extreme Winter Warming Events, Nitrogen Addition and Grazing

Climate change is one of many ongoing human-induced environmental changes, but few studies consider interactive effects between multiple anthropogenic disturbances. In coastal sub-arctic heathland, we quantified the impact of a factorial design simulating extreme winter warming (WW) events (7 days a...

Full description

Saved in:
Bibliographic Details
Published inFrontiers in plant science Vol. 9; p. 1787
Main Authors Bokhorst, Stef, Berg, Matty P, Edvinsen, Guro K, Ellers, Jacintha, Heitman, Amber, Jaakola, Laura, Mæhre, Hanne K, Phoenix, Gareth K, Tømmervik, Hans, Bjerke, Jarle W
Format Journal Article
LanguageEnglish
Published Switzerland Frontiers Media 2018
Frontiers Media S.A
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Climate change is one of many ongoing human-induced environmental changes, but few studies consider interactive effects between multiple anthropogenic disturbances. In coastal sub-arctic heathland, we quantified the impact of a factorial design simulating extreme winter warming (WW) events (7 days at 6-7°C) combined with episodic summer nitrogen (+N) depositions (5 kg N ha ) on plant winter physiology, plant community composition and ecosystem CO fluxes of an dominated heathland during 3 consecutive years in northern Norway. We expected that the +N would exacerbate any stress effects caused by the WW treatment. During WW events, ecosystem respiration doubled, leaf respiration declined (-58%), efficiency of Photosystem II (Fv/Fm) increased (between 26 and 88%), while cell membrane fatty acids showed strong compositional changes as a result of the warming and freezing. In particular, longer fatty acid chains increased as a result of WW events, and eicosadienoic acid (C20:2) was lower when plants were exposed to the combination of WW and +N. A larval outbreak of geometrid moths ( and ) following the first WW led to a near-complete leaf defoliation of the dominant dwarf shrubs (-87%) and (-81%) across all experimental plots. Leaf emergence timing, plant biomass or composition, NDVI and growing season ecosystem CO fluxes were unresponsive to the WW and +N treatments. The limited plant community response reflected the relative mild winter freezing temperatures (-6.6°C to -11.8°C) recorded after the WW events, and that the grazing pressure probably overshadowed any potential treatment effects. The grazing pressure and WW both induce damage to the evergreen shrubs and their combination should therefore be even stronger. In addition, +N could have exacerbated the impact of both extreme events, but the ecosystem responses did not support this. Therefore, our results indicate that these sub-arctic -dominated ecosystems are highly resilient and that their responses may be limited to the event with the strongest impact.
Bibliography:Frontiers in Plant Science
Reviewed by: Raquel Esteban, Universidad del País Vasco, Spain; Juergen Kreyling, University of Greifswald, Germany
Edited by: Hans J. De Boeck, University of Antwerp, Belgium
This article was submitted to Functional Plant Ecology, a section of the journal Frontiers in Plant Science
ISSN:1664-462X
1664-462X
DOI:10.3389/fpls.2018.01787