Evidence map›Paper›PMID 41647559›Full record

ReviewFundamental research2026

Research progress and perspectives on ecological processes and carbon feedback in permafrost wetlands under changing climate conditions.

Changchun Song, Alain N Rousseau, Yanyu Song, Yang Ou, Ning Chen, Xianwei Wang, Li Sun, Yuedong Guo, Hao Zhang, Zhengang Zhang and 1 more

Abstract readReview
In one paragraph

Review in Fundamental research, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

1 citing paper in PubMed.

  1. Review
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

11 authors.

Changchun SongSchool of Hydraulic Engineering, Dalian University of Technology, Dalian 116024, China.
Alain N RousseauNational Institute for Scientific Research - Water Earth Environment Center (INRS-ETE), University of Quebec, Quebec, QC G1K 9A9, Canada.
Yanyu SongKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China.
Yang OuKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China.
Ning ChenKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China.
Xianwei WangKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China.
Li SunKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China.
Yuedong GuoKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China.
Hao ZhangKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China.
Zhengang ZhangKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China.
Zhuohang XinSchool of Hydraulic Engineering, Dalian University of Technology, Dalian 116024, China.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Permafrost wetlands are closely related to potential greenhouse gas emissions under climate warming. In recent decades, climate change and human activities have induced extensive permafrost degradation, severely influencing the stability of wetlands in permafrost regions. The widely observed significant changes in vegetation cover, hydrological conditions, and soil carbon stability are strongly affecting the carbon cycle and the carbon sources/sinks of permafrost wetlands. In this review, research progress on the response and feedback mechanisms of wetland ecological processes to permafrost degradation under the influences of climate change is first explored, including the impacts of permafrost degradation on the vegetation dynamics, hydrological processes, soil carbon decomposition, greenhouse gas emissions, and carbon feedback. In addition, several questions regarding recent advances are raised and some suggestions are provided for future related research pertaining to the following issues: (i) linkages and response relationships between permafrost degradation and the vegetation-hydrology-carbon cycle in permafrost wetlands, (ii) stabilization mechanisms of their carbon sink function, (iii) accurate estimation of the carbon sequestration rate and sink potential, and (iv) carbon feedback in permafrost wetlands under future climate change scenarios. The findings will provide critical scientific evidence and data support for protecting wetland ecosystems in permafrost regions under changing climate conditions and the implementation of carbon peaking and carbon neutrality strategies.

Indexed as

Carbon feedbackCarbon sink functionClimate changeEcological processesPermafrost wetland

Identifiers

PMID41647559
PMCPMC12869778

What OpenQuestion holds

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LicenceCC BY-NC-ND
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Registered trials

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.