Thermal acclimation of leaf respiration of tropical trees and lianas: Response to experimental canopy warming, and consequences for tropical forest carbon balance

Climate warming is expected to increase respiration rates of tropical forest trees and lianas, which may negatively affect the carbon balance of tropical forests. Thermal acclimation could mitigate the expected respiration increase, but the thermal acclimation potential of tropical forests remains l...

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Autores:
Tipo de recurso:
Fecha de publicación:
2014
Institución:
Universidad del Rosario
Repositorio:
Repositorio EdocUR - U. Rosario
Idioma:
eng
OAI Identifier:
oai:repository.urosario.edu.co:10336/24157
Acceso en línea:
https://doi.org/10.1111/gcb.12563
https://repository.urosario.edu.co/handle/10336/24157
Palabra clave:
Acclimation
Carbon balance
Carbon cycle
Carbon flux
Climate effect
Forest canopy
Global warming
Leaf
Primary production
Respiration
Temperature effect
Tropical forest
Panama [central america]
Acclimatization
Biological model
Carbon cycle
Forest
Heat
Oxygen consumption
Panama
Physiology
Plant leaf
Tree
Tropic climate
Acclimatization
Carbon cycle
Forests
Hot temperature
Oxygen consumption
Panama
Plant leaves
Trees
Tropical climate
Carbon flux
Climate change
Dgvm
Experimental leaf warming
Global warming
Npp
Panama
Respiration
Tropical forest
biological
Models
Rights
License
Abierto (Texto Completo)
Description
Summary:Climate warming is expected to increase respiration rates of tropical forest trees and lianas, which may negatively affect the carbon balance of tropical forests. Thermal acclimation could mitigate the expected respiration increase, but the thermal acclimation potential of tropical forests remains largely unknown. In a tropical forest in Panama, we experimentally increased nighttime temperatures of upper canopy leaves of three tree and two liana species by on average 3 °C for 1 week, and quantified temperature responses of leaf dark respiration. Respiration at 25 °C (R25) decreased with increasing leaf temperature, but acclimation did not result in perfect homeostasis of respiration across temperatures. In contrast, Q10 of treatment and control leaves exhibited similarly high values (range 2.5-3.0) without evidence of acclimation. The decrease in R25 was not caused by respiratory substrate depletion, as warming did not reduce leaf carbohydrate concentration. To evaluate the wider implications of our experimental results, we simulated the carbon cycle of tropical latitudes (24°S-24°N) from 2000 to 2100 using a dynamic global vegetation model (LM3VN) modified to account for acclimation. Acclimation reduced the degree to which respiration increases with climate warming in the model relative to a no-acclimation scenario, leading to 21% greater increase in net primary productivity and 18% greater increase in biomass carbon storage over the 21st century. We conclude that leaf respiration of tropical forest plants can acclimate to nighttime warming, thereby reducing the magnitude of the positive feedback between climate change and the carbon cycle. © 2014 John Wiley and amp; Sons Ltd.