Skip to main navigation Skip to search Skip to main content

Environmental Controls on Carbon Stability in Peatlands: Integrating Microbial, Geochemical, and Organic Matter Variation

  • Amelia Oakeshott
  • , Mike Vreeken
  • , Megan Jenkins
  • , Yiming Zhang
  • , Simon Cheung
  • , Juan Carlos Benavides Duque
  • , Paola Alarcon Prado
  • , Frank Kansiime
  • , Ellen Kayendeke
  • , Carol Kagaba
  • , Angela Gallego-Sala
  • , Richard Pancost
  • , Casey Bryce

Research output: Contribution to conferencePosterpeer-review

Abstract

Peatlands are significant terrestrial ecosystems that play a large role in regulating many global processes, resulting in a high social, environmental, and cultural importance. Despite this global distribution, these systems are far from uniform with differences in their hydrology, geochemistry, vegetation, and microbial communities, all shaping carbon processing pathways. This study investigates how contrasting peatland types across tropical and temperate zones differ in their biogeochemical characteristics, and to identify the dominant environmental and microbial drivers underpinning this variation. We examined microbial community composition, nutrient profiles, dissolved porewater gases, and detailed organic matter (OM) characterisation of eight peatlands from Colombia (n=4), Uganda (n=1), and the United Kingdom (n=3) to determine the influence on carbon cycling. First, we find that peat, which serves as microbial substrate, becomes enriched in aromatic and alkyl macromolecules with depth, which correlates with an increase abundance of Bathyarchaea and Spirochaeta, whilst a decrease in Methanobacterium and Burkholderia. This is consistent with a shift towards more processed OM and decreased substrate availability. Results also indicate a pH control, in relation to peatland type, on the abundance of Acidobacteriota. Sites with lower pHs (~ 4) are observed to have more Acidobacteriota in comparison to higher sites (~ 6) where Chloroflexi dominate more. Together, these results suggest that local geochemistry exerts a stronger influence on microbial community structure than latitude, further influencing OM decomposition pathways and carbon preservation. Overall, our data indicates that peat carbon stability is governed primarily by site-specific geochemistry rather than regional climate alone, highlighting the need for process-based constraints in predicting peatland carbon emissions under future environmental changes.

Original languageEnglish
DOIs
StateAccepted/In press - 14 Mar 2026
EventEGU General Assembly 2026 - Viena, Austria
Duration: 03 May 202608 May 2026

Conference

ConferenceEGU General Assembly 2026
Country/TerritoryAustria
CityViena
Period03/05/2608/05/26

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action
  2. SDG 15 - Life on Land
    SDG 15 Life on Land

Fingerprint

Dive into the research topics of 'Environmental Controls on Carbon Stability in Peatlands: Integrating Microbial, Geochemical, and Organic Matter Variation'. Together they form a unique fingerprint.

Cite this