Extended Data Fig. 8: Results of the van’t Hoff model and macromolecular rate theory (MMRT) in fitting temperature‒respiration relationships across 1362 site-years.
From: Thermal adaptation of respiration in terrestrial ecosystems alleviates carbon loss
a Frequency distribution of ΔC‡P from the MMRT model, with a positive ΔC‡P at 493 site-years. b The optimum temperature (Topt) of MMRT for 582 site-years is higher than the recorded maximum temperature (Tmax). c A total of 276 site-years are better fitted by the MMRT model than by the van’t Hoff model according to a comparison of their Akaike information criterion (AIC) values (ΔAIC > 2).
