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Divergent apparent temperature sensitivity of forest-floor respiration across a managed boreal forest landscape.

Authors :
Guo Z
Martínez-García E
Chi J
Nilsson MB
Jia X
Peichl M
Source :
The Science of the total environment [Sci Total Environ] 2024 Dec 10; Vol. 955, pp. 176950. Date of Electronic Publication: 2024 Oct 23.
Publication Year :
2024

Abstract

Understanding the apparent temperature sensitivity (Q10) of forest floor respiration (Q10R <subscript>ff</subscript> ) and its plant autotrophic (Q10R <subscript>a</subscript> ) and soil heterotrophic (Q10R <subscript>h</subscript> ) components is critical for determining the strength and direction of forest carbon cycle-climate feedbacks. However, the spatial variability of Q10R <subscript>ff</subscript> and its controlling factors across the spatially heterogeneous boreal forest landscape remains poorly understood. In this study, we used chamber-based respiration measurements conducted on paired natural and trenching plots over three growing seasons (2016-2018) to determine Q10R <subscript>ff</subscript> , Q10R <subscript>h</subscript> and Q10R <subscript>a</subscript> to soil temperature across 50 diverse forest stands (ranging 5-211 years old) in a managed landscape in northern Sweden. Additionally, we estimated ecosystem- and landscape-scale Q10 based on conventional and tall tower eddy covariance measurements, respectively, conducted over the same landscape. Our results suggest manifold variations (i.e., 10th to 90th percentiles) of Q10R <subscript>ff</subscript> (1.7 to 6.6), with Q10R <subscript>a</subscript> (0.9 to 7.4) showing a greater range than Q10R <subscript>h</subscript> (1.6 to 5.3). Forest-floor understory biomass was the main control of variations in Q10R <subscript>a</subscript> , whereas soil properties explained best those of Q10R <subscript>h</subscript> . Furthermore, a seasonal hysteresis of Q10R <subscript>ff</subscript> was observed, with higher values mostly occurring during the late growing season. The magnitude of this hysteresis scaled with stand age in response to concurrent changes in net primary production. The Q10R <subscript>ff</subscript> to air temperature declined with increasing stand age, which was attributed to the increased decoupling of air and soil temperatures with canopy development. Despite the considerable stand-level variations, when averaged over the 50 forest stands, Q10R <subscript>ff</subscript> to air temperature converged with that of both ecosystem- and landscape-scale respiration. In conclusion, our study highlights the complexity of Q10R <subscript>ff</subscript> , which needs to be considered in predictions of the interactions of climate change and management with the carbon cycle of managed boreal forests.<br />Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.<br /> (Copyright © 2024 Elsevier B.V. All rights reserved.)

Details

Language :
English
ISSN :
1879-1026
Volume :
955
Database :
MEDLINE
Journal :
The Science of the total environment
Publication Type :
Academic Journal
Accession number :
39454781
Full Text :
https://doi.org/10.1016/j.scitotenv.2024.176950