PulseExploreJournal ClubDebatesTrendingResearchersJournals
Instagram
HomeExploreJournal ClubTrending
Synapse
⌘+K
Synapse
March 14, 2026Sustainability0 citationsOpen Access

Functional Microbes Mediate the Impact of Soil Depth and Anthropogenic Activities on Greenhouse Gas Fluxes in the Yellow River Delta, China

View Full Paper
ZCZhengxi CaiQMQ. W. MengJSJian Sun

Key Points

  • The study aims to understand how soil depth and human activities influence greenhouse gas emissions and the role of functional microbes in this process.
  • Investigated seven human-impacted sites in the Yellow River Delta
  • Utilized in vitro microcosm cultivation and molecular biology techniques
  • Applied multivariate statistical analysis to assess GHG fluxes
  • Significant differences in GHG fluxes were found among various anthropogenic activities and soil depths (p < 0.05)
  • Positive N2O fluxes observed in sewage irrigation (20.98–35.08 mg N2O-N m−2 hr−1) and tourism areas (12.52–23.87 mg N2O-N m−2 hr−1)
  • Natural areas showed positive CH4 fluxes (25.02–55.54 mg CH4-C m−2 hr−1 in surface soil) while other areas displayed predominantly negative values

Abstract

Coastal wetlands represent significant sources of greenhouse gases (GHGs) and serve as crucial ecological interfaces between terrestrial and marine environments, substantially contributing to global biogeochemical cycles. However, GHG emission fluxes are strongly influenced by complex anthropogenic activities, yet their underlying microbial mechanisms remain poorly understood. This study investigated seven representative human-impacted sites within the Yellow River Delta. Employing a combined approach of in vitro microcosm cultivation, molecular biology, and multivariate statistical analysis, we investigated the integrated mechanisms controlling nitrous oxide (N2O) and methane (CH4) fluxes, with consideration of soil depth, environmental factors, microbial communities, and functional microbes. The results indicated that significant differences in GHG fluxes among different anthropogenic activities and soil depths (p < 0.05). Surface soil N2O fluxes were positive within sewage irrigation areas (20.98–35.08 mg N2O-N m−2 hr−1) and tourism development areas (12.52–23.87 mg N2O-N m−2 hr−1), while mariculture areas displayed negative fluxes. CH4 fluxes were positive exclusively in natural areas (surface soil: 25.02–55.54 mg CH4-C m−2 hr−1; deep soil: 8.38–356.68 mg CH4-C m−2 hr−1), while other areas predominantly showed negative values (surface soil: −130.98–44.32 mg CH4-C m−2 hr−1; deep soil: −106.16–65.24 mg CH4-C m−2 hr−1). Furthermore, a structural equations model highlighted the pivotal role of key functional microbes in soil carbon–nitrogen cycling (e.g., nirK, nosZII, and SRB) involved in soil carbon–nitrogen cycling in negatively regulating N2O and CH4 fluxes. The study also revealed distinct microbial responses across diverse habitats, underscoring the significant role of Proteobacteria in wetland soil. This research enhances our understanding of GHG dynamics in coastal wetlands and provides scientific evidence and potential regulatory pathways for enhancing soil biological mitigation functions and achieving carbon neutrality and sustainability within wetland ecosystems.

Ask AI
Helpful
Bookmark
Share
View Full Paper

Cite This Study

Cai et al. (2026) studied this question.

synapsesocial.com/papers/69b4fc6ab39f7826a300d4cbhttps://doi.org/10.3390/su18062798
Ask AI
Helpful
Bookmark
Share
View Full Paper