Evidence map›Paper›PMID 34728618›Full record

ArticleNature communications2021

Distinct methane-dependent biogeochemical states in Arctic seafloor gas hydrate mounds.

Scott A Klasek, Wei-Li Hong, Marta E Torres, Stella Ross, Katelyn Hostetler, Alexey Portnov, Friederike Gründger, Frederick S Colwell

Open access · goldAbstract read
In one paragraph

Article in Nature communications, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing papers in PubMed
1.9field-weighted citation impact, top 16% 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

3 citing papers in PubMed, 23 citations in OpenAlex.

  1. Article
  2. Article
  3. Article
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

8 authors at 5 institutions in 4 countries.

Scott A Klasek *Department of Microbiology, Oregon State University, Corvallis, OR, USA.
Wei-Li Hong *Department of Geological Sciences, Stockholm University, Stockholm, Sweden. wei-li.hong@geo.su.se.ORCID http://orcid.org/0000-0002-7247-1827
Marta E TorresCollege of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, USA.
Stella RossCollege of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, USA.
Katelyn HostetlerDepartment of Microbiology, Oregon State University, Corvallis, OR, USA.
Alexey PortnovCentre for Arctic Gas Hydrate, Environment and Climate (CAGE), Department of Geosciences, UiT The Arctic University of Norway, N-9037, Tromsø, Norway.
Friederike GründgerCentre for Arctic Gas Hydrate, Environment and Climate (CAGE), Department of Geosciences, UiT The Arctic University of Norway, N-9037, Tromsø, Norway.ORCID http://orcid.org/0000-0002-7386-3603
Frederick S ColwellDepartment of Microbiology, Oregon State University, Corvallis, OR, USA.
Oregon State University · USAarhus University · DKCentre for Arctic Gas Hydrate, Environment and Climate · NOStockholm University · SEUniversity of Wyoming · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Archaea mediating anaerobic methane oxidation are key in preventing methane produced in marine sediments from reaching the hydrosphere; however, a complete understanding of how microbial communities in natural settings respond to changes in the flux of methane remains largely uncharacterized. We investigate microbial communities in gas hydrate-bearing seafloor mounds at Storfjordrenna, offshore Svalbard in the high Arctic, where we identify distinct methane concentration profiles that include steady-state, recently-increasing subsurface diffusive flux, and active gas seepage. Populations of anaerobic methanotrophs and sulfate-reducing bacteria were highest at the seep site, while decreased community diversity was associated with a recent increase in methane influx. Despite high methane fluxes and methanotroph doubling times estimated at 5-9 months, microbial community responses were largely synchronous with the advancement of methane into shallower sediment horizons. Together, these provide a framework for interpreting subseafloor microbial responses to methane escape in a warming Arctic Ocean.

Identifiers

PMID34728618
PMCPMC8563959
OpenAlexW3208065108

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.