Skip to main content

Advertisement

Log in

Priming effects of surface soil organic carbon decreased with warming: a global meta-analysis

  • Research Article
  • Published:
Plant and Soil Aims and scope Submit manuscript

Abstract

Aims

Climate warming can potentially cause more plant-derived organic substrates into the surface soil. The newly produced carbon may accelerate or restrict native soil organic carbon (SOC) decomposition by priming effects (PE), so as to increase the uncertainty of the feedback prediction between climate change and soil carbon pool. However, it is controversial about the direction and driving factors of the PE of surface SOC in the warming world.

Methods

In this meta-analysis, we investigated 1680 pairwise PE determined by 13C or 14C isotope labeling method in surface soils across cropland, grassland and forest from 39 warming experiments to generalize the direction and influencing factors of the warming effects on PE.

Results

The meta-analysis showed that warming decreased PE across different ecosystems. The decrease was much greater in forest (effect size: -6.2) than in cropland (effect size: -2.6) and grassland (effect size: -1.7) and was more severe in simple substrates (effect size: -12.1), i.e., small molecules such as glucose and amino acid than that in complex substrates (effect size: -1.7), including plant tissues, residues and pyrolysis products, etc. The effect size of warming on PE was positively correlated with soil clay and pH, while negatively correlated with SOC content, total nitrogen, soil C/N ratio and warming intensity.

Conclusions

These findings emphasize that warming will decrease the primed surface SOC loss, particularly in forest or organic matter-rich soils and larger warming intensity.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5

Similar content being viewed by others

Abbreviations

C:

Carbon

CO2 :

Carbon dioxide

PE:

Priming effects

SOC:

Soil organic carbon

TN:

Soil total nitrogen

C/N:

Soil carbon to nitrogen ratio

H/L:

High-low temperature ratio

ΔT:

The absolute temperature change

CI:

Confidence intervals

RR++ :

Mean effect size

References

Download references

Acknowledgements

This work was supported by the Science and Technology Research Program of Chongqing Municipal Education Commission (KJZD-K202003501, KJZD-K202001203), Chongqing Science and Technology Commission (cstc2020jcyj-msxmX0095), the Foundation of Intelligent Ecotourism Subject Group of Chongqing Three Gorges University (zhlv20221012) and the National Natural Science Foundation of China (31770592).

Author information

Authors and Affiliations

Authors

Corresponding authors

Correspondence to Junjie Lin or Dan Liu.

Additional information

Responsible Editor: Manuel T. Oliveira.

Publisher's note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Supplementary Information

Rights and permissions

Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Dong, H., Lin, J., Lu, J. et al. Priming effects of surface soil organic carbon decreased with warming: a global meta-analysis. Plant Soil (2022). https://doi.org/10.1007/s11104-022-05851-1

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s11104-022-05851-1

Keywords

Navigation