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Record W4408439681 · doi:10.5194/egusphere-egu25-4987

Greenhouse gas balance of thermokarst fens and bogs in the discontinuous permafrost zone during extreme drought years

2025· preprint· en· W4408439681 on OpenAlexaffabout
Kasha Kempton, David Olefeldt

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsUniversity of Alberta
Fundersnot available
KeywordsThermokarstPermafrostBogEnvironmental scienceGreenhouse gasClimatologyHydrology (agriculture)GeologyPeatPhysical geographyEarth scienceGeographyGeotechnical engineeringOceanographyArchaeology

Abstract

fetched live from OpenAlex

The greenhouse gas (GHG) balance of northern peatlands is being influenced by the combined effects of rapid permafrost thaw and increasing frequency and severity of droughts. Our soil chamber flux measurements revealed that thermokarst fens in the discontinuous permafrost zone of boreal western Canada (Lutose, Alberta) acted as stronger net sources of carbon dioxide (CO2) and consistently emitted more methane (CH4) than thermokarst bogs during two extreme-drought years. Peatlands in the discontinuous permafrost zone store large amounts of soil carbon, but thawing permafrost results in changes to hydrology and vegetation, which have the potential to substantially impact their greenhouse gas balance. As permafrost thaws, thermokarst bogs and fens develop and expand, further modifying GHG dynamics. Although thermokarst fens account for approximately 30% of peatlands in the discontinuous zone, they have received little attention, and there is limited understanding of how the GHG balance varies along the trophic gradient from poor fens to extreme-rich fens.This study explored the spatial and temporal variability of greenhouse gas fluxes across four sites, including a thermokarst bog, poor fen, rich fen, and an extreme-rich fen. Trophic status of each site was classified based on pH, electrical conductivity (EC), vegetation, and concentrations of magnesium (Mg) and calcium (Ca). Fluxes were measured over two growing seasons and one winter (June 2023 to October 2024). Controls on greenhouse gas fluxes were explored using data on vegetation composition, water chemistry, hydrology, and climatic conditions. Our analysis showed that CH4 emissions generally increased along the trophic gradient, with the exception of the extreme-rich fen, where high sulfate concentrations suppressed emissions. Non-growing season CH4 emissions were also a significant contributor to annual emissions across all sites.Overall, our findings indicate that trophic status plays an important role in determining the greenhouse gas balance of thermokarst bogs and fens following permafrost thaw. Understanding the drivers of the carbon dioxide balance and methane emissions in these ecosystems during extreme drought years is essential for refining models of peatland carbon dynamics and predicting their future role in the global carbon cycle as climate change continues.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.286
Threshold uncertainty score0.568

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.033
GPT teacher head0.235
Teacher spread0.202 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2025
Admission routes2
Has abstractyes

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