Microbial controls over soil priming effects under chronic nitrogen and phosphorus additions in subtropical forests.

@article{Li2023MicrobialCO,
  title={Microbial controls over soil priming effects under chronic nitrogen and phosphorus additions in subtropical forests.},
  author={Jian Li and Zhanfeng Liu and M. Jin and Wei Zhang and Hans Lambers and Dafeng Hui and Chao Liang and Jing Zhang and Donghai Wu and Jordi Sardans and Josep Pe{\~n}uelas and Daniel F. Petticord and David W Frey and Yong-Guan Zhu},
  journal={The ISME journal},
  year={2023},
  url={https://api.semanticscholar.org/CorpusID:263264485}
}
Positive PE was associated with increased microbial C utilization, accompanied by an increase in microbial community activity, nutrient-related gene abundance, and enzyme activities, and the balance between soil available N and P effects on the PE, was dependent on rhizosphere microbial community composition.
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29 Citations

29 Citations

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64 References

Microbial carbon use efficiency and priming effect regulate soil carbon storage under nitrogen deposition by slowing soil organic matter decomposition

Nitrogen availability mediates the priming effect of soil organic matter by preferentially altering the straw carbon-assimilating microbial community.

Microbes changed their carbon use strategy to regulate the priming effect in an 11-year nitrogen addition experiment in grassland.

Phosphorus addition alters the response of soil organic carbon decomposition to nitrogen deposition in a subtropical forest

Microbial carbon use efficiency in grassland soils subjected to nitrogen and phosphorus additions

The Response of Critical Microbial Taxa to Litter Micro-Nutrients and Macro-Chemistry Determined the Agricultural Soil Priming Intensity After Afforestation

The results showed that soil priming was accelerated by different litter addition which varied from 24 to 74% of SOC mineralization, suggesting that priming intensity was relatively flexible and highly affected by litter quality, while micro-chemistry indirectly influences priming via alteration to dominant bacterial taxa.

Shifts in priming partly explain impacts of long‐term nitrogen input in different chemical forms on soil organic carbon storage

Evidence is provided that shifts toward higher graminoid abundance and changes in soil microbial abundance mediated by N chemical forms are key drivers for priming effects and SOC pool changes, thereby linking human interference with the N cycle to climate change.

Carbon and phosphorus addition effects on microbial carbon use efficiency, soil organic matter priming, gross nitrogen mineralization and nitrous oxide emission from soil

Root influence on soil nitrogen availability and microbial community dynamics results in contrasting rhizosphere priming effects in pine and spruce soil

The decomposition of SOM can either be stimulated or suppressed by living plant roots, and this rhizosphere priming effect (RPE) potentially plays an important role in regulating soil C storage and nutrient mineralization.

Microbial community structure and functional genes drive soil priming effect following afforestation.

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