Warming induces unexpectedly high soil respiration in a wet tropical forest

Tropical forests are a dominant regulator of the global carbon cycle, exchanging more carbon dioxide with the atmosphere than any other terrestrial biome. Climate models predict unprecedented climatic warming in tropical regions in the coming decades; however, in situ field warming studies are severely lacking in tropical forests. Here we present results from an in situ warming experiment in Puerto Rico, where soil respiration responses to <sup>+</sup>4 <sup>o</sup>C warming were assessed half-hourly for a year. Soil respiration rates were 42-204% higher in warmed relative to ambient plots, representing some of the highest soil respiration rates reported for any terrestrial ecosystem. While respiration rates were significantly higher in the warmed plots, the temperature sensitivity (Q<sub>10</sub>) was 71.7% lower, pointing to a mechanistic shift. Even with reduced Q<sub>10</sub>, if observed soil respiration rates persist in a warmer world, the feedback to future climate could be considerably greater than previously predicted or observed.

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Publication Details

Journal
Nature Communications
Published
2025-09-16
DOI
https://doi.org/10.1038/s41467-025-62065-6
Citations
2
Primary Topic
Plant Water Relations and Carbon Dynamics
Type
article
Field-Weighted Citation Impact
2.21

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article

Warming induces unexpectedly high soil respiration in a wet tropical forest

Aura M. Alonso‐Rodríguez, Iana F. Grullón‐Penkova, Molly A. Cavaleri, Sasha C. Reed et al.
2 citations
Nature Communications
Plant Water Relations and Carbon Dynamics
2.21
article

Warming induces unexpectedly high soil respiration in a wet tropical forest

Aura M. Alonso‐Rodríguez, Iana F. Grullón‐Penkova, Molly A. Cavaleri, Sasha C. Reed, Colin Tucker, Christine S. O’Connell, Tana E. Wood, M. Isabel Loza
article en
2 citations

Abstract

Tropical forests are a dominant regulator of the global carbon cycle, exchanging more carbon dioxide with the atmosphere than any other terrestrial biome. Climate models predict unprecedented climatic warming in tropical regions in the coming decades; however, in situ field warming studies are severely lacking in tropical forests. Here we present results from an in situ warming experiment in Puerto Rico, where soil respiration responses to <sup>+</sup>4 <sup>o</sup>C warming were assessed half-hourly for a year. Soil respiration rates were 42-204% higher in warmed relative to ambient plots, representing some of the highest soil respiration rates reported for any terrestrial ecosystem. While respiration rates were significantly higher in the warmed plots, the temperature sensitivity (Q<sub>10</sub>) was 71.7% lower, pointing to a mechanistic shift. Even with reduced Q<sub>10</sub>, if observed soil respiration rates persist in a warmer world, the feedback to future climate could be considerably greater than previously predicted or observed.

Nature CommunicationsVol. 16(1)
University of Vermont (US), Michigan Technological University (US), United States Geological Survey (US), Chapman University (US), Morton Arboretum (US), Northern Research Station (US), International Institute of Tropical Forestry (PR), Southwest Biological Science Center, Macalester College (US)
National Science Foundation, U.S. Department of Energy, U.S. Department of Agriculture, Office of Science, U.S. Forest Service, Biological and Environmental Research, International Institute of Tropical Forestry
Openalex Percentile: Top 11%
Plant Water Relations and Carbon Dynamics
2.21
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