Decadal forest soil respiration following stem girdling View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2022-08-27

AUTHORS

Elizabeth A. Clippard, Samuel I. Haruna, Peter S. Curtis, Cameron Clay, Ben Bond-Lamberty, Kayla Mathes, Christoph S. Vogel, Christopher M. Gough

ABSTRACT

Key messageLarge-scale stem-girdling experiment reduced soil respiration for five consecutive years. Timing and magnitude of soil respiration declines are better explained by changes in leaf area rather than in soil microclimate.AbstractSoil respiration (Rs) represents the largest flux of carbon (C) from forests to the atmosphere, but the long-term influence of phloem-disrupting disturbance on Rs is poorly understood, limiting robust forecasts of ecosystem C balance. Using a decade of observations from the Forest accelerated succession experiment (FASET), we examined relationships among Rs, soil temperature, soil moisture, and leaf area index (LAI) following the stem girdling-induced mortality of 40% of all canopy trees within a 39-ha area. Mean annual Rs declined by about 20% relative to the control two years after disturbance, but recovered to near pre-disturbance values within five years; this reduction correlated with LAI losses and lower Rs temperature sensitivity (i.e., Q10), with the latter counteracting soil warming caused by partial canopy defoliation. These observations are consistent with progressive reductions in belowground labile C causing reductions in Rs. We conclude that the effects of stem girdling on Rs (1) were not immediate, occurring two years after the treatment, (2) were primarily influenced by biotic rather than soil microclimate changes, and (3) persisted for nearly a decade but were temporally dynamic, underscoring the value of long-term experiments. More... »

PAGES

1-7

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/s00468-022-02340-x

DOI

http://dx.doi.org/10.1007/s00468-022-02340-x

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https://app.dimensions.ai/details/publication/pub.1150553597


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