PulseExploreJournal ClubDebatesTrendingResearchersJournals
Instagram
HomeExploreJournal ClubTrending
Synapse
⌘+K
Synapse
September 10, 2025The ISME Journal0 citationsOpen Access

Distinct Microbial Communities Within and On Seep Carbonates Support Long-term Anaerobic Oxidation of Methane and Divergent pMMO Diversity

View Full Paper
MMMagdalena J. MayrSPSergio ParraSCStephanie A. Connon

Key Points

  • Exponential reactivation of anaerobic methane oxidation (AOM) was observed in carbonate samples from low activity seeps after 24 months.
  • Surface-associated microbial communities showed distinct variability, influencing the carbonate's AOM rates and precipitation processes.
  • Ca. Methanophaga dominated carbonate interiors, co-existing with sulfate-reducing bacteria, indicating potential for syntrophic partnerships in methane oxidation.
  • Single-cell analyses indicated variability in microbial activity levels within carbonate interiors, suggesting some microbes may enter dormancy.

Abstract

Abstract At methane seeps worldwide, syntrophic anaerobic methane-oxidizing archaea and sulfate-reducing bacteria promote carbonate precipitation and rock formation, acting as methane and carbon sinks. Although maintenance of anaerobic oxidation of methane (AOM) within seep carbonates has been documented, its reactivation upon methane exposure remains uncertain. Surface-associated microbes may metabolize sulfide from AOM, maintain carbonate anoxia, contribute to carbonate dissolution, and support higher trophic levels; however, these communities are poorly described. We provide insights into microbial diversity, metabolism, activity, and resiliency within and on seep carbonates through amplicon and metagenomic sequencing, incubations, and non-canonical amino acid tagging combined with fluorescence in situ hybridization (BONCAT-FISH). Ca. Methanophaga (ANME-1) dominated the carbonate interiors in active and low activity seeps, co-occurring with Ca. Desulfaltia as main sulfate reducer, potentially a new syntrophic partner in AOM. Single-cell BONCAT-FISH revealed variability in ANME-1 activity, suggesting potential dormancy in carbonates from low activity seep sites. However, incubations with carbonates from low activity seeps (≥24 months) showed exponential AOM reactivation (~44-day doubling), suggesting these carbonates retain the potential as long-term methane sinks under dynamic seepage conditions. Surface-associated microbial communities were heterogeneous and distinct from the carbonate interior and other seep habitats. Anaerobic methane-oxidizing biofilms and sulfide-oxidizing mats were associated with carbonates with high and intermediate AOM rates potentially influencing carbonate precipitation/dissolution. Shared aerobic methanotrophs between carbonate surfaces and invertebrates indicated carbonate surfaces may represent animal epibiont reservoirs. Recovered particulate methane monooxygenases included both aerobic methanotrophs and divergent forms associated with the Methylophagaceae, suggesting a new function in this group.

Ask AI
Helpful
Bookmark
Share
View Full Paper

Cite This Study

Mayr et al. (2025) studied this question.

synapsesocial.com/papers/68c193f19b7b07f3a0617f7ehttps://doi.org/10.1093/ismejo/wraf153
Ask AI
Helpful
Bookmark
Share
View Full Paper