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Acta Prataculturae Sinica ›› 2025, Vol. 34 ›› Issue (8): 123-131.DOI: 10.11686/cyxb2024476

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Composition and carbon-fixation pathways of carbon-fixing microorganisms in soils of a typical steppe and desert steppe in Inner Mongolia

Hao PENG1,2(), Bao-zhu DONG3, Li-juan MA4, Xiao-dong YU3, Yi-fan ZHANG1, Xiao-fang LI1   

  1. 1.College of Resources and Environmental Economics,Inner Mongolia University of Finance and Economics,Hohhot 010070,China
    2.Resource Utilization and Environmental Protection Coordinated Development Academician Expert Workstation in the North of China,Inner Mongolia University of Finance and Economics,Hohhot 010070,China
    3.School of Life Sciences,Inner Mongolia University,Hohhot 010020,China
    4.College of Resources and Environmental Sciences,Inner Mongolia Agricultural University,Hohhot 010040,China
  • Received:2024-11-26 Revised:2024-12-30 Online:2025-08-20 Published:2025-06-16
  • Contact: Hao PENG

Abstract:

Autotrophic soil microbes can assimilate atmospheric CO2 and fix carbon into the soil. The relative contributions of soil microorganisms to carbon fixation are greater in arid regions than in humid ecosystems. However, current carbon-fixation models mainly focus on plant functions and often neglect the roles of soil autotrophs. Therefore, such models cannot accurately predict carbon sequestration in the soil of arid ecosystems. In this study, we focused on the soil microorganisms of the typical steppe and desert steppe in Inner Mongolia, and analyzed differences in the composition and metabolic pathways of carbon-fixing microbial communities in those soils. The main results were as follows: 1) There were 14 carbon-fixing microbial groups (classes) in soils of both categories of steppe, among which Acidimicrobiia, γ-Proteobacteria, and Chloroflexi showed significantly higher abundance in the desert steppe soil than in the typical steppe soil; 2) The relative abundance of genes related to the reductive citric acid (rTCA) cycle and the 3-hydroxypropionate (3-HP) cycle was significantly higher in the desert steppe soil than in the typical steppe soil; 3) The abundance of genes encoding key enzymes in the rTCA pathway [EC (1.2.7.1) and EC (1.2.7.3)] and the 3-HP pathway [EC (6.4.1.2) and EC (6.4.1.3)] was higher in the desert steppe soil than in the typical steppe soil. Clearly, the abundance of carbon-fixing microorganism classes, carbon-fixation pathways, and genes encoding their key enzymes was higher in the desert steppe soil of Inner Mongolia than in the typical steppe soil, indicating that the desert steppe soil microorganisms have stronger potential for atmospheric CO2 fixation.

Key words: grassland soil, carbon-fixing microorganisms, carbon-fixation pathways, metagenomics, relative abundance