Chin J Plant Ecol ›› 2024, Vol. 48 ›› Issue (12): 1692-1707.DOI: 10.17521/cjpe.2023.0221  cstr: 32100.14.cjpe.2023.0221

• Research Articles • Previous Articles    

Effects of warming on phyllosphere and rhizosphere bacterial communities in Picea asperata and Fargesia nitida

LI Yun-Yi1,2, ZHENG Jin1, YAN Xiao-Yan1,3, LI Shuang1, LUO Lin4, TONG Jin1, ZHAO Chun-Zhang1,*()   

  1. 1State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, College of Ecology and Environment, Chengdu University of Technology, Chengdu 610051, China
    2Meishan Pharmaceutical College, Meishan, Sichuan 620200, China
    3Sichuan Keshengxin Environmental Technology Company, Chengdu 610100, China
    4Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu 610041, China
  • Received:2023-08-01 Accepted:2024-04-08 Online:2024-12-20 Published:2024-12-20
  • Contact: ZHAO Chun-Zhang
  • Supported by:
    National Natural Science Foundation of China(32271688);National Natural Science Foundation of China(31570477)

Abstract:

Aims Leaf and root are sensitive to environmental changes. There are many studies about the responses of leaf and root to climate warming, but the effects of warming on phyllosphere and rhizospheric soil bacterial communities remain unclear.

Methods Two dominant species (Picea asperata and Fargesia nitida) of subalpine coniferous forest in the eastern Qingzang Plateau were selected, and the compositional and functional characteristics of phyllosphere and rhizosphere soil bacterial community between the two species and their responses to simulated warming were studied.

Important findings The results showed that the Chao index and Shannon-Wiener index of bacterial communities in rhizosphere soil were significantly higher than those in phyllosphere of both species. The bacterial diversity in P. asperata was decreased by warming, but that in F. nitida was increased under warming conditions. There were significant differences in bacterial community composition and structure between phyllosphere and rhizosphere. Rhizobiales (41%-46%) were the dominant order of phyllosphere bacterial community, and Vicinamibacterales were the dominant bacterial order in rhizosphere soil. The relative abundance of Burkholderiales and Corynebacteriales increased by about two times in P. asperata phyllosphere, and Acidobacteriales in F. nitida phyllosphere were also increased under warming conditions. However, the rhizosphere bacterial community composition of the two species was less affected by warming. The complexity of rhizosphere bacterial co-occurrence network was higher than that of phyllosphere in both species. The number of links in co-occurrence networks of P. asperata phyllosphere and rhizosphere bacterial community were increased by warming, but this index was decreased in F. nitida phyllosphere and rhizosphere under warming conditions. According to FAPROTAX, the relative abundance of bacterial groups involved in carbon cycling and nitrogen fixation in rhizosphere were significantly higher than those in phyllosphere. The predictive functions of phyllosphere bacteria were more sensitive to warming than those of rhizosphere, and warming increased urealysis function of phyllosphere bacteria community of both species, but significantly decreased the phyllosphere predictive functions of nitrogen respiration, nitrate reduction and nitrate respiration in F. nitida and that of nitrogen fixation in P. asperata. Therefore, there were significant differences in structure and function of bacterial community between rhizosphere and phyllosphere, and the phyllosphere bacterial community was more sensitive to warming than those in the rhizosphere soil.

Key words: phyllosphere, rhizosphere, warming, bacterial community, Qingzang Plateau