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Warming-related increases in soil CO2 efflux are explained by increased below-ground carbon flux
|Title:||Warming-related increases in soil CO2 efflux are explained by increased below-ground carbon flux|
|Other Titles:||Accelerated soil carbon loss does not explain warming related increases in soil CO2 efflux|
|Authors:||Giardina, Christian P.|
Litton, Creighton M.
Crow, Susan E.
Asner, Gregory P.
|Issue Date:||20 Jul 2014|
|Publisher:||Nature Climate Change|
|Citation:||Giardina CP, Litton CM, Crow SE, Asner GP. Warming-related increases in soil CO2 efflux are explained by increased below-ground carbon flux. Nat. Climate Change 2014;4:822-827.|
|Abstract:||The universally observed exponential increase in soil-surface CO2 efflux (‘soil respiration’; FS) with increasing temperature has led to speculation that global warming will accelerate soil-organic-carbon (SOC) decomposition, reduce SOC storage, and drive a positive feedback to future warming. However, interpreting temperature–FS relationships, and so modelling terrestrial carbon balance in a warmer world, is complicated by the many sources of respired carbon that contribute to FS (ref. 3) and a poor understanding of how temperature influences SOC decomposition rates. Here we quantified FS, litterfall, bulk SOC and SOC fraction size and turnover, and total below-ground carbon flux (TBCF) across a highly constrained 5.2 °C mean annual temperature (MAT) gradient in tropical montane wet forest. From these, we determined that: increases in TBCF and litterfall explain >90% of the increase in FS with MAT; bulk SOC and SOC fraction size and turnover rate do not vary with MAT; and increases in TBCF and litterfall do not influence SOC storage or turnover on century to millennial timescales. This gradient study shows that for tropical montane wet forest, long-term and whole-ecosystem warming accelerates below-ground carbon processes with no apparent impact on SOC storage.|
|Appears in Collections:||CTAHR Faculty & Researcher Works|
Litton, Creighton M.
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