Abstract
Background
Soil is an important organic carbon (C) pool in terrestrial ecosystems, but knowledge on soil organic carbon (SOC) decomposition rate and influencing factors remains limited, particularly in arid and semi-arid grasslands. Models show that global semi-arid regions are experiencing more extreme climate events, which may trigger more C loss from soils.
Methods
We used the stable carbon isotope (δ13C) of plant and soil depth profile to examine decomposition rates of SOC along a 2200 km semi-arid grassland transect in northern China. Beta (β) was calculated from the relationship between δ13C and C concentrations of plant and soil profile (0–100 cm). Partial correlation analysis and structure equation models were used to analyze correlations between beta and climatic and edaphic variables.
Results
We found that the δ13C values increased from plant tissues to surface soil and then deep soil at all sites, while the SOC concentration decreased. The β values ranged from −0.33 to −2.27, with an average value at −1.37. There was a positive correlation between β value and SOC decomposition rate constant (k), supporting the hypothesis that enrichment of δ13C along soil depth profile was mainly due to isotopic fractionation during microbial SOC decomposition. The correlation between β value and aridity index was mainly due to the variations of edaphic properties such as soil C/N ratio with aridity index, pointing to the more important role of edaphic properties in β value than climatic factors.
Conclusions
Despite uncertainties associated with the interpretation of soil δ13C along its depth profile, our results demonstrated that soil δ13C could provide an independent benchmark for examining model-based predictions of SOC decomposition in semi-arid grasslands. Incorporation of both climatic and edaphic variables into models may enhance the predictions for SOC dynamics under global climate changes.
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Abbreviations
- N:
-
Nitrogen
- C:
-
Carbon
- SOC:
-
Soil organic carbon
- SOM:
-
Soil organic matter
- MAP:
-
Mean annual precipitation
- MAT:
-
Mean annual temperature
- AI:
-
Aridity index
- PET:
-
Potential evaportranspiration
- SEMs:
-
Structure equation models
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Acknowledgements
We thank two anonymous reviewers for useful comments on an earlier version of the manuscript. This work was financially supported by Major State Basic Research Development Program of China (973 Program, 2014CB954400), the National Natural Science Foundation of China (31522010 and 41601255), and Key Research Program of Frontier Sciences, CAS (QYZDB-SSWDQC006). We gratefully acknowledge all members of the Shenyang Sampling Campaign Team from the Institute of Applied Ecology, Chinese Academy of Sciences for their assistance during field sampling.
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Wang, C., Wei, H., Liu, D. et al. Depth profiles of soil carbon isotopes along a semi-arid grassland transect in northern China. Plant Soil 417, 43–52 (2017). https://doi.org/10.1007/s11104-017-3233-x
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DOI: https://doi.org/10.1007/s11104-017-3233-x