Large seasonal variation of soil respiration in a secondary tropical moist forest in Puerto Rico

Abstract Tropical forests are the largest contributors to global emissions of carbon dioxide (CO2) to the atmosphere via soil respiration (Rs). As such, identifying the main controls on Rs in tropical forests is essential for accurately projecting the consequences of ongoing and future global enviro...

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Main Authors: Omar Gutiérrez del Arroyo, Tana E. Wood
Format: Article
Language:English
Published: Wiley 2021-01-01
Series:Ecology and Evolution
Subjects:
Online Access:https://doi.org/10.1002/ece3.7021
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author Omar Gutiérrez del Arroyo
Tana E. Wood
author_facet Omar Gutiérrez del Arroyo
Tana E. Wood
author_sort Omar Gutiérrez del Arroyo
collection DOAJ
description Abstract Tropical forests are the largest contributors to global emissions of carbon dioxide (CO2) to the atmosphere via soil respiration (Rs). As such, identifying the main controls on Rs in tropical forests is essential for accurately projecting the consequences of ongoing and future global environmental changes to the global C cycle. We measured hourly Rs in a secondary tropical moist forest in Puerto Rico over a 3‐year period to (a) quantify the magnitude of Rs and (b) identify the role of climatic, substrate, and nutrient controls on the seasonality of Rs. Across 3 years of measurements, mean Rs was 7.16 ± 0.02 μmol CO2 m‐2 s‐1 (or 2,710 g C m‐2 year‐1) and showed significant seasonal variation. Despite small month‐to‐month variation in temperature (~4°C), we found significant positive relationships between daily and monthly Rs with both air and soil temperature, highlighting the importance of temperature as a driver of Rs even in warm ecosystems, such as tropical forests. We also found a significant parabolic relationship between mean daily volumetric soil moisture and mean daily Rs, with an optimal moisture value of 0.34 m3 m‐3. Given the relatively consistent climate at this site, the large range in mean monthly Rs (~7 μmol CO2 m‐2 s‐1) was surprising and suggests that even small changes in climate can have large implications for ecosystem respiration. The strong positive relationship of Rs with temperature at monthly timescales particularly stands out, as moisture is usually considered a stronger control of Rs in tropical forests that already experience warm temperatures year‐round. Moreover, our results revealed the strong seasonality of Rs in tropical moist forests, which given its high magnitude, can represent a significant contribution to the seasonal patterns of atmospheric (CO2) globally.
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spelling doaj.art-757d99d9c86f4eba927914b6635f88c32022-12-21T21:28:37ZengWileyEcology and Evolution2045-77582021-01-0111126327210.1002/ece3.7021Large seasonal variation of soil respiration in a secondary tropical moist forest in Puerto RicoOmar Gutiérrez del Arroyo0Tana E. Wood1Department of Biology University of Puerto Rico Río Piedras Puerto RicoUSDA Forest Service International Institute of Tropical Forestry Rio Piedras Puerto RicoAbstract Tropical forests are the largest contributors to global emissions of carbon dioxide (CO2) to the atmosphere via soil respiration (Rs). As such, identifying the main controls on Rs in tropical forests is essential for accurately projecting the consequences of ongoing and future global environmental changes to the global C cycle. We measured hourly Rs in a secondary tropical moist forest in Puerto Rico over a 3‐year period to (a) quantify the magnitude of Rs and (b) identify the role of climatic, substrate, and nutrient controls on the seasonality of Rs. Across 3 years of measurements, mean Rs was 7.16 ± 0.02 μmol CO2 m‐2 s‐1 (or 2,710 g C m‐2 year‐1) and showed significant seasonal variation. Despite small month‐to‐month variation in temperature (~4°C), we found significant positive relationships between daily and monthly Rs with both air and soil temperature, highlighting the importance of temperature as a driver of Rs even in warm ecosystems, such as tropical forests. We also found a significant parabolic relationship between mean daily volumetric soil moisture and mean daily Rs, with an optimal moisture value of 0.34 m3 m‐3. Given the relatively consistent climate at this site, the large range in mean monthly Rs (~7 μmol CO2 m‐2 s‐1) was surprising and suggests that even small changes in climate can have large implications for ecosystem respiration. The strong positive relationship of Rs with temperature at monthly timescales particularly stands out, as moisture is usually considered a stronger control of Rs in tropical forests that already experience warm temperatures year‐round. Moreover, our results revealed the strong seasonality of Rs in tropical moist forests, which given its high magnitude, can represent a significant contribution to the seasonal patterns of atmospheric (CO2) globally.https://doi.org/10.1002/ece3.7021litterfallmoisturenutrientsseasonalitysoil respirationtemperature
spellingShingle Omar Gutiérrez del Arroyo
Tana E. Wood
Large seasonal variation of soil respiration in a secondary tropical moist forest in Puerto Rico
Ecology and Evolution
litterfall
moisture
nutrients
seasonality
soil respiration
temperature
title Large seasonal variation of soil respiration in a secondary tropical moist forest in Puerto Rico
title_full Large seasonal variation of soil respiration in a secondary tropical moist forest in Puerto Rico
title_fullStr Large seasonal variation of soil respiration in a secondary tropical moist forest in Puerto Rico
title_full_unstemmed Large seasonal variation of soil respiration in a secondary tropical moist forest in Puerto Rico
title_short Large seasonal variation of soil respiration in a secondary tropical moist forest in Puerto Rico
title_sort large seasonal variation of soil respiration in a secondary tropical moist forest in puerto rico
topic litterfall
moisture
nutrients
seasonality
soil respiration
temperature
url https://doi.org/10.1002/ece3.7021
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