State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
2.
Guanzhong Plain Ecological Environment Change and Comprehensive Treatment National Observation and Research Station, Xi'an 710061, China
3.
Department of Biological Sciences, Northern Arizona University, Flagstaff Arizona 86011, USA
4.
Institute of Biological and Environmental Sciences, School of Biological Sciences, University of Aberdeen, Aberdeen AB24 3UU, UK
5.
Department of Biology, University of New Mexico, Albuquerque New Mexico 87131, USA
6.
Department of Soil Science of Temperate Ecosystems, Department of Agricultural Soil Science, University of Goettingen, Göttingen 37077, Germany
7.
Peoples Friendship University of Russia (RUDN University), Moscow 117198, Russia
8.
Department of Ecology and Conservation Biology, Texas A & M University, College Station Texas 77843, USA
9.
Institute of Global Environmental Change, Department of Earth and Environmental Science, School of Human Settlements and Civil Engineering, Xi'an Jiaotong University, Xi'an 710049, China
Microbial carbon use efficiency (CUE), a key regulator of soil organic carbon (SOC) dynamics, reflects carbon allocation between microbial growth and respiration. Separate investigation of microbial growth and respiration helps to clarify the role of CUE in the carbon balance and consequently, in the carbon cycle in soil. First, in terms of microbial resource acquisition, the drivers of microbial growth and respiration differ: microbial growth is primarily regulated by synergistic availability of carbon, nitrogen, and phosphorus, whereas respiration is more strongly influenced by substrate quality, such as the carbon-to-nitrogen ratio. Second, synchronized responses of microbial growth and respiration rates under climate change (e.g., warming, drought, elevated CO2) often mask underlying CUE regulatory mechanisms. Thus, we propose: (1) explicitly representing microbial growth and respiration in models to raise the precision of SOC dynamics predictions; and (2) applying approaches such as isotope probing and metagenomic functional annotation to resolve CUE mechanisms from the community to the single-species level. Overall, decoupling CUE into its growth and respiration components establishes a mechanistic framework that explicitly links CUE to microbially mediated SOC dynamics.
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Zhou J., Liu J., Hungate B. A., et al. (2026). Digging deeper into microbial carbon use efficiency in soil: Perspectives from microbial growth and respiration. The Innovation Geoscience 4:100183. https://doi.org/10.59717/j.xinn-geo.2026.100183
Zhou J., Liu J., Hungate B. A., et al. (2026). Digging deeper into microbial carbon use efficiency in soil: Perspectives from microbial growth and respiration. The Innovation Geoscience4:100183. https://doi.org/10.59717/j.xinn-geo.2026.100183
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Zhou J., Liu J., Hungate B. A., et al. (2026). Digging deeper into microbial carbon use efficiency in soil: Perspectives from microbial growth and respiration. The Innovation Geoscience 4:100183. https://doi.org/10.59717/j.xinn-geo.2026.100183
Zhou J., Liu J., Hungate B. A., et al. (2026). Digging deeper into microbial carbon use efficiency in soil: Perspectives from microbial growth and respiration. The Innovation Geoscience4:100183. https://doi.org/10.59717/j.xinn-geo.2026.100183
The conceptual diagram illustrates the necessity and promising solutions of decoupling microbial carbon use efficiency (CUE) into growth and respiration components.