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What makes decomposition faster under conspecific trees? The factors controlling the magnitude of home-field advantage

Daumal, Maya1; Oguro, Michio2; Ueda, Miki3; Takayanagi, Sakino4; Nakashizuka, Tohru2; Kurokawa, Hiroko5

Published Jun 14, 2024 on Dryad. https://doi.org/10.5061/dryad.8pk0p2nrs

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Jun 14, 2024 version files 8.74 GB

Abstract

The “home-field advantage (HFA)” for decomposition means that leaf litter decomposes faster on soils under the conspecific species (i.e., the home field) than on soils under different species (i.e., “away”). Many previous studies have demonstrated the HFA, but the underlying mechanisms remain unclear. We conducted a reciprocal litter-decomposition experiment using two species with different leaf traits: Abies mariesii, an evergreen conifer, and Fagus crenata, a deciduous broad-leaved tree. The dominance of these species shifts along an elevation gradient with a transition zone where both species coexist. In mixed forests of the transition zone along the elevation gradient, we explored how the magnitude of HFA between these two species was influenced by temperature, soil properties, or leaf litter traits which could directly affect the decomposition rate. The magnitude of HFA observed between the two species varied widely from -3.89% to 28.3%. Our modeling showed that the magnitude of HFA increased with decreasing soil pH and leaf litter N, i.e., in more acidic soil and for less decomposable litter. Soil pH affected leaf litter decomposition in the home plots of each species, whereas leaf litter N did not. The magnitude of the HFA increased as the difference in soil pH between the F. crenata and A. mariesii plots at the same elevation became greater, but decreased as the difference in soil C became greater. Thus, the response of leaf litter decomposition to environmental changes might vary not only through direct effects of vegetation traits but also through indirect effects of the HFA. This highlights the importance of considering HFA for accurately predicting the response of local carbon and nutrient cycles to climate change, particularly in communities where a replacement of dominant species by others is expected due to climate change.