Microbial carbon fixation is strongly regulated by microclimates: temperature shaped elevational variations of CO2 fixation pathways and potential in warm-temperate forests
Jingjing Wang , Hongyi He , Haibo Li , Yang Liu , Yu Wang , Siyuan Huangfu , Baixue Zhang , Huinan Ma , Haoqin Ma , Xinyue Wang , Xiongzhi Zhang , Huifang Zhang , Yaru Wang , Jieyan Yang , Houjuan Song , Xiuqing Yang
Journal of Forestry Research ›› 2026, Vol. 37 ›› Issue (1) : 176
Soil microbial CO2 fixation plays a pivotal role in the global terrestrial carbon cycle. In forest ecosystems, the changes in the pathways and potential of microbial CO2 fixation as well as their underlying mechanisms along environmental gradients remain unclear, particularly considering the effects of variations in forest microclimates. To address this gap, this study employed metagenomic sequencing and 13C stable isotope labeling to investigate CO2-fixing microorganisms, pathways, potential, and their relationships with environmental factors across elevations from 894 to 2200 m. The results showed that the dominant CO2-fixing microorganisms were Proteobacteria, Actinobacteria and Acidobacteria in this study, while their compositional proportions showing clear disparities, ranging from 30.88 to 48.17%, 16.02 to 30.75% and 13.55 to 23.52% with elevations, respectively. Among the 6 pathways detected, the dicarboxylate–hydroxybutyrate (DC/4-HB) and 3-hydroxypropionate (3-HP) cycles dominated CO2 fixation at low elevations, and the reductive citrate (rTCA) cycle prevailed at high elevations. Soil microbial CO2 fixation rates ranged from 22.46 to 78.99 mg m–2 d–1, with significantly higher values at high elevations than that at middle–low elevations. As proxies for forest microclimates, air and soil temperatures were the main drivers of elevational changes in CO2 fixation pathways and potential. Moreover, they indirectly inhibited the abundance of CO2-fixing microorganisms and pathways by curbing the accumulation of soil nutrients (microbial biomass carbon, ammonium nitrogen, reactive organic carbon and available potassium), thereby weakening microbial CO2 fixation potential (path coefficient = 0.78). Microclimates also directly and significantly reduced the microbial CO2 fixation potential (path coefficient = –0.67). Our results revealed the elevational variations and microclimate-driven mechanisms of microbial CO2 fixation, with implications for soil carbon cycling and ecosystem responses to climate warming.
Forest microclimates / Soil microorganisms / CO2 fixation pathways / CO2 fixation potential / Elevational variation
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Northeast Forestry University
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