Abstract
Using an empirical approach, we report that the slope of the short-term log-transformed leaf respiration (R)- temperature (T) curves declines with increasing leaf T in a manner that is uniform across biomes (1); the results have utility for modeling carbon fluxes in terrestrial biosphere models (TBMs). The use of an empirical approach reflects the fact that, despite advances in understanding of factors regulating R (2-4) and its T-response (5), basic information on key determinants of R remains lacking, hindering development of a process-based model with utility for TBMs.
| Original language | English |
|---|---|
| Pages (from-to) | E5996-E5997 |
| Number of pages | 2 |
| Journal | Proceedings of the National Academy of Sciences of the United States of America |
| Volume | 113 |
| Issue number | 41 |
| DOIs | |
| Publication status | Published - 11 Oct 2016 |
Keywords
- climatic changes
- ecosystems
- leaf respiration
- leaves
- temperature
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