TY - JOUR
T1 - Global convergence in the temperature sensitivity of respiration at ecosystem level
AU - Mahecha, Miguel D.
AU - Reichstein, Markus
AU - Carvalhais, Nuno
AU - Lasslop, Gitta
AU - Lange, Holger
AU - Seneviratne, Sonia I.
AU - Vargas, Rodrigo
AU - Ammann, Christof
AU - Arain, M. Altaf
AU - Cescatti, Alessandro
AU - Janssens, Ivan A.
AU - Migliavacca, Mirco
AU - Montagnani, Leonardo
AU - Richardson, Andrew D.
PY - 2010/8/13
Y1 - 2010/8/13
N2 - The respiratory release of carbon dioxide (CO2) from the land surface is a major flux in the global carbon cycle, antipodal to photosynthetic CO2 uptake. Understanding the sensitivity of respiratory processes to temperature is central for quantifying the climate-carbon cycle feedback. We approximated the sensitivity of terrestrial ecosystem respiration to air temperature (Q10) across 60 FLUXNET sites with the use of a methodology that circumvents confounding effects. Contrary to previous findings, our results suggest that Q10 is independent of mean annual temperature, does not differ among biomes, and is confined to values around 1.4 ± 0.1. The strong relation between photosynthesis and respiration, by contrast, is highly variable among sites. The results may partly explain a less pronounced climate-carbon cycle feedback than suggested by current carbon cycle climate models.
AB - The respiratory release of carbon dioxide (CO2) from the land surface is a major flux in the global carbon cycle, antipodal to photosynthetic CO2 uptake. Understanding the sensitivity of respiratory processes to temperature is central for quantifying the climate-carbon cycle feedback. We approximated the sensitivity of terrestrial ecosystem respiration to air temperature (Q10) across 60 FLUXNET sites with the use of a methodology that circumvents confounding effects. Contrary to previous findings, our results suggest that Q10 is independent of mean annual temperature, does not differ among biomes, and is confined to values around 1.4 ± 0.1. The strong relation between photosynthesis and respiration, by contrast, is highly variable among sites. The results may partly explain a less pronounced climate-carbon cycle feedback than suggested by current carbon cycle climate models.
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U2 - 10.1126/science.1189587
DO - 10.1126/science.1189587
M3 - Article
C2 - 20603495
AN - SCOPUS:77955605650
SN - 0036-8075
VL - 329
SP - 838
EP - 840
JO - Science
JF - Science
IS - 5993
ER -