ausblenden:
Schlagwörter:
C-14
litter decomposition
radiocarbon
root respiration
soil
respiration sources
carbon-dioxide
european forests
beech forest
respiration
efflux
root
temperature
exchange
patterns
rates
Zusammenfassung:
Soil respiration is derived from heterotrophic (decomposition of soil organic matter) and autotrophic (root/rhizosphere respiration) sources, but there is considerable uncertainty about what factors control variations in their relative contributions in space and time. We took advantage of a unique whole-ecosystem radiocarbon label in a temperate forest to partition soil respiration into three sources: (1) recently photosynthesized carbon (C), which dominates root and rhizosphere respiration; (2) leaf litter decomposition and (3) decomposition of root litter and soil organic matter > 1-2 years old. Heterotrophic sources and specifically leaf litter decomposition were large contributors to total soil respiration during the growing season. Relative contributions from leaf litter decomposition ranged from a low of similar to 1 +/- 3% of total soil respiration (6 +/- 3 mg C m(-2) h(-1)) when leaf litter was extremely dry, to a high of 42 +/- 16% (96 +/- 38 mg C m(-2) h(-1)). Total soil respiration fluxes varied with the strength of the leaf litter decomposition source, indicating that moisture-dependent changes in litter decomposition drive variability in total soil respiration fluxes. In the surface mineral soil layer, decomposition of C fixed in the original labeling event (3-5 years earlier) dominated the isotopic signature of heterotrophic respiration. Root/rhizosphere respiration accounted for 16 +/- 10% to 64 +/- 22% of total soil respiration, with highest relative contributions coinciding with low overall soil respiration fluxes. In contrast to leaf litter decomposition, root respiration fluxes did not exhibit marked temporal variation ranging from 34 +/- 14 to 40 +/- 16 mg C m(-2) h(-1) at different times in the growing season with a single exception (88 +/- 35 mg C m(-2) h(-1)). Radiocarbon signatures of root respired CO2 changed markedly between early and late spring (March vs. May), suggesting a switch from stored nonstructural carbohydrate sources to more recent photosynthetic products.
