MétaCan
Menu
Back to cohort
Record W4415820493 · doi:10.19189/001c.143644

Hydrological and Temperature Controls on CO <sub>2</sub> and CH <sub>4</sub> Exchange Between a Mid-Altitude Mountain Peatland and the Atmosphere

2025· article· en· W4415820493 on OpenAlexaff
Alexandre Lhosmot, Marc Steinmann, Adrien Jacotot, Philippe Binet, Robin Calisti, Edward A. D. Mitchell, Marie‐Laure Toussaint, Anne Boetsch, Fatima Laggoun‐Défarge, Guillaume Bertrand

Bibliographic record

VenueMires and Peat · 2025
Typearticle
Languageen
FieldEnvironmental Science
TopicPeatlands and Wetlands Ecology
Canadian institutionsUniversité de Montréal
FundersInstitut National de Recherche pour l'Agriculture, l'Alimentation et l'EnvironnementAgroParisTechCentre National de la Recherche Scientifique
KeywordsPeatGreenhouse gasTransectCarbon dioxideVegetation (pathology)Atmosphere (unit)Temperate climateMethaneHydrology (agriculture)

Abstract

fetched live from OpenAlex

The aim of the present study is to understand the variability and the environmental factors controlling the fluxes of carbonaceous greenhouse gases (GHGs), methane (CH 4 ) and carbon dioxide (CO 2 ) between a temperate Sphagnum -dominated mid-altitude mountain peatland and the atmosphere. We conducted monthly measurements of GHG fluxes over 20 months using the chamber method. Specifically, we assessed the effects of (1) air temperature and (2) water level (WL) on GHG emissions. Open Top Chambers (OTC) were used to simulate a warming effect by passive heating of the air above the soil. To assess the effect of WL, we studied a hydrological gradient along a 35 m long transect from a near-surface “WET” area, through an “INTER” area with an intermediate WL, to a “DRY” area with a lower WL. The WET area featured a higher cover of Sphagnum species while the vegetation cover in the DRY area contained more vascular plants. Although all plots showed the same seasonality of GHG fluxes, considerable variability was observed among them. Raising the temperature using OTCs, which increased annual average air temperature by 0.2 °C to 0.6 °C, did not significantly affect CH 4 and CO 2 respiration (Reco) fluxes. In contrast, hydrological conditions played an important role in explaining flux variability. CH 4 fluxes were significantly higher in the WET and INTER areas (median [95 % CI] values: 17.5 [14.2, 29.0] and 20.0 [14.8, 30.4] nmol m -2 s -1 ) compared to the DRY area (3.4 [1.9, 9.4] nmol m -2 s -1 ) during all hydrological periods, i.e., humid spring, humid summer and dry summer. Reco did not vary significantly along the hydrological gradient overall, but the fluxes were lower in the WET area under humid spring (0.4 [0.3, 0.6] µmol m -2 s -1 ) and summer (1.7 [1.25, 2.75] µmol m -2 s -1 ) conditions compared to the DRY area (1.6 [1.3, 2.0] µmol m -2 s -1 in spring and 3.8 [2.7, 4.6] µmol m -2 s -1 in summer). Conversely, greater fluxes (by ~ 0.5 µmol m -2 s -1 ) were observed in the WET area during summer drought. Given that Reco emissions are expected to be higher during droughts in the DRY area, we hypothesise a possible threshold effect, such as inhibition of phenoloxidase activity and/or other enzymatic activities, which would limit organic matter decomposition. Moreover, increasing WL in the WET and INTER areas led to a drastic drop in gross primary production (GPP) corresponding to Sphagnum immersion.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation 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 score0.041
Threshold uncertainty score0.735

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.001
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 head0.006
GPT teacher head0.220
Teacher spread0.214 · 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 teacher head, 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 routes1
Has abstractyes

Explore more

Same venueMires and PeatSame topicPeatlands and Wetlands EcologyFrench-language works237,207