Evidence map›Paper›PMID 34440022›Full record

ArticleBiology2021

Microbial Involvement in Carbon Transformation via CH

Weronika Goraj, Anna Szafranek-Nakonieczna, Jarosław Grządziel, Cezary Polakowski, Mirosław Słowakiewicz, Yanhong Zheng, Anna Gałązka, Zofia Stępniewska, Anna Pytlak

Abstract read
In one paragraph

Article in Biology, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing 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

2 citing papers in PubMed.

  1. Article
  2. 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

9 authors.

Weronika GorajInstitute of Biological Sciences, The John Paul II Catholic University of Lublin, Konstantynów 1 I, 20-708 Lublin, Poland.ORCID 0000-0003-2234-5133
Anna Szafranek-NakoniecznaInstitute of Biological Sciences, The John Paul II Catholic University of Lublin, Konstantynów 1 I, 20-708 Lublin, Poland.ORCID 0000-0003-3257-0158
Jarosław GrządzielDepartment of Agricultural Microbiology, Institute of Soil Science and Plant Cultivation-State Research Institute (IUNG-PIB), Czartoryskich 8, 24-100 Puławy, Poland.ORCID 0000-0003-3028-1256
Cezary PolakowskiInstitute of Agrophysics, Polish Academy of Sciences, Doświadczalna 4, 20-290 Lublin, Poland.ORCID 0000-0002-1658-8334
Mirosław SłowakiewiczFaculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warszawa, Poland.ORCID 0000-0001-6623-8968
Yanhong ZhengState Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China.
Anna GałązkaDepartment of Agricultural Microbiology, Institute of Soil Science and Plant Cultivation-State Research Institute (IUNG-PIB), Czartoryskich 8, 24-100 Puławy, Poland.ORCID 0000-0001-5504-5706
Zofia StępniewskaDepartment of Biochemistry and Environmental Chemistry, The John Paul II Catholic University of Lublin, Konstantynów 1 I, 20-708 Lublin, Poland.
Anna PytlakInstitute of Agrophysics, Polish Academy of Sciences, Doświadczalna 4, 20-290 Lublin, Poland.

Funding

Narodowe Centrum Nauki DEC-2014/15/N/NZ8/00315
6 · The paper itself

Abstract

Methane and carbon dioxide are one of the most important greenhouse gases and significant components of the carbon cycle. Biogeochemical methane transformation may occur even in the extreme conditions of deep subsurface ecosystems. This study presents methane-related biological processes in saline sediments of the Miocene Wieliczka Formation, Poland. Rock samples (W2, W3, and W4) differed in lithology (clayey salt with veins of fibrous salt and lenses of gypsum and anhydrite; siltstone and sandstone; siltstone with veins of fibrous salt and lenses of anhydrite) and the accompanying salt type (spiza salts or green salt). Microbial communities present in the Miocene strata were studied using activity measurements and high throughput sequencing. Biological activity (i.e., carbon dioxide and methane production or methane oxidation) occurred in all of the studied clayey salt and siltstone samples but mainly under water-saturated conditions. Microcosm studies performed at elevated moisture created more convenient conditions for the activity of both methanogenic and methanotrophic microorganisms than the intact sediments. This points to the fact that water activity is an important factor regulating microbial activity in saline subsurface sediments. Generally, respiration was higher in anaerobic conditions and ranged from 36 ± 2 (W2

Indexed as

aerobic respirationanaerobic respirationBacillusmethanemethane oxidationmethanogenesismicrobial communityNGSsaline environments

Identifiers

PMID34440022
PMCPMC8389658

What OpenQuestion holds

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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.