Evidence map›Paper›PMID 26029170›Full record

ArticleFrontiers in microbiology2015

Shifts in methanogenic community composition and methane fluxes along the degradation of discontinuous permafrost.

Susanne Liebner, Lars Ganzert, Andrea Kiss, Sizhong Yang, Dirk Wagner, Mette M Svenning

Open access · goldAbstract read
In one paragraph

Article in Frontiers in microbiology, 2015. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 21 papers.

0numbers the graph read from it
0cells of the map it votes in
21citing papers in PubMed
4.7field-weighted citation impact, top 5% of its field
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

21 citing papers in PubMed, 96 citations in OpenAlex.

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  13. Dynamics of microbial communities and COJournal of microbiology (Seoul, Korea) · 2019
    Review
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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

6 authors at 2 institutions in 2 countries.

Susanne LiebnerSection of Geomicrobiology, GFZ German Research Center for Geosciences, Potsdam Germany.
Lars GanzertDepartment of Experimental Limnology, IGB Leibniz-Institute of Freshwater Ecology and Inland Fisheries, Stechlin Germany.
Andrea KissSection of Geomicrobiology, GFZ German Research Center for Geosciences, Potsdam Germany.
Sizhong YangSection of Geomicrobiology, GFZ German Research Center for Geosciences, Potsdam Germany.
Dirk WagnerSection of Geomicrobiology, GFZ German Research Center for Geosciences, Potsdam Germany.
Mette M SvenningDepartment of Arctic and Marine Biology, UiT The Arctic University of Norway, Tromsø Norway.
Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences · DEUiT The Arctic University of Norway · NO

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The response of methanogens to thawing permafrost is an important factor for the global greenhouse gas budget. We tracked methanogenic community structure, activity, and abundance along the degradation of sub-Arctic palsa peatland permafrost. We observed the development of pronounced methane production, release, and abundance of functional (mcrA) methanogenic gene numbers following the transitions from permafrost (palsa) to thaw pond structures. This was associated with the establishment of a methanogenic community consisting both of hydrogenotrophic (Methanobacterium, Methanocellales), and potential acetoclastic (Methanosarcina) members and their activity. While peat bog development was not reflected in significant changes of mcrA copy numbers, potential methane production, and rates of methane release decreased. This was primarily linked to a decline of potential acetoclastic in favor of hydrogenotrophic methanogens. Although palsa peatland succession offers similarities with typical transitions from fen to bog ecosystems, the observed dynamics in methane fluxes and methanogenic communities are primarily attributed to changes within the dominant Bryophyta and Cyperaceae taxa rather than to changes in peat moss and sedge coverage, pH and nutrient regime. Overall, the palsa peatland methanogenic community was characterized by a few dominant operational taxonomic units (OTUs). These OTUs seem to be indicative for methanogenic species that thrive in terrestrial organic rich environments. In summary, our study shows that after an initial stage of high methane emissions following permafrost thaw, methane fluxes, and methanogenic communities establish that are typical for northern peat bogs.

Indexed as

climate changediscontinuous permafrostmcrAmethanemethanogenspalsapeatland succession

Identifiers

PMID26029170
PMCPMC4428212
OpenAlexW1555511174

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

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.