EGU23-7993
https://doi.org/10.5194/egusphere-egu23-7993
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Microbial carbon use efficiency in soil under N deposition: Meta-analysis of 13C and 18O approaches

Yakov Kuzyakov1, Junxi Hu2, Congde Huang2, and Shixing Zhou2
Yakov Kuzyakov et al.
  • 1University of Goettingen, Soil Science, Goettingen, Germany (kuzyakov@gwdg.de)
  • 2Sichuan Agricultural University, Chengdu, China

The carbon use efficiency (CUE) of soil microorganisms is a critical parameter for the first step of organic carbon (C) transformation by and incorporation into microbial biomass and shapes C cycling in terrestrial ecosystems. As C and nitrogen (N) cycles interact closely and N availability affects microbial metabolism, N addition to soil may shift the microbial CUE. We conducted a meta-analysis (100 data pairs) to generalize information about the microbial CUE response to N addition in soil based on the two most common CUE estimation approaches: (i) 13C-labelled substrate addition (13C-substrate) and (ii) 18O-labelled water addition (18O-H2O).

The mean microbial CUE in soils across all biomes and approaches was 0.37. The effects of N addition on CUE, however, were depended on the approach: CUE decreased by 12% if measured by the 13C-substrate approach, while CUE increased by 11% if measured by the 18O-H2O approach. These differences in the microbial CUE response depending on the estimation approach are explained by the divergent reactions of microbial growth to N addition: N addition decreases the 13C incorporation into microbial biomass (this parameter is in the numerator by CUE calculation based on the 13C-substrate approach). In contrast, N addition slightly increases (although statistically insignificant) the microbial growth rate (in the numerator of the CUE calculation when assessed by the 18O-H2O approach), significantly raising the CUE. We explained these N addition effects based on CUE regulation mechanisms at the metabolic, cell, community, and ecosystem levels. Consequently, the differences in the microbial responses (microbial growth, respiration, C incorporation, community composition, and dormant or active states) between the 13C-substrate and 18O-H2O approaches need to be considered. Thus, these two CUE estimation approaches should be compared to understand microbially mediated C and nutrient dynamics under increasing anthropogenic N input and other global change effects.

Reference

Hu J, Huang C, Zhou S, Kuzyakov Y 2022. Nitrogen deposition affects microbial carbon use efficiency: Meta-analysis of similarities and differences in 18O and 13C approaches. Global Change Biology 28 (16), 4977-4988. http://doi.org/10.1111/gcb.16226

How to cite: Kuzyakov, Y., Hu, J., Huang, C., and Zhou, S.: Microbial carbon use efficiency in soil under N deposition: Meta-analysis of 13C and 18O approaches, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-7993, https://doi.org/10.5194/egusphere-egu23-7993, 2023.