Evidence map›Paper›PMID 31952472›Full record

ArticleMicrobiome2020

Warming-induced permafrost thaw exacerbates tundra soil carbon decomposition mediated by microbial community.

Jiajie Feng, Cong Wang, Jiesi Lei, Yunfeng Yang, Qingyun Yan, Xishu Zhou, Xuanyu Tao, Daliang Ning, Mengting M Yuan, Yujia Qin and 13 more

Open access · goldAbstract readVideo-Audio Media
In one paragraph

Article in Microbiome, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 33 papers.

0numbers the graph read from it
0cells of the map it votes in
33citing papers in PubMed
10.5field-weighted citation impact, top 1% 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

33 citing papers in PubMed, 138 citations in OpenAlex.

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  20. Microscale drivers of summer COScientific reports · 2022
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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

23 authors at 11 institutions in 2 countries.

Jiajie FengInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Cong WangInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Jiesi LeiState Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, 100084, China.
Yunfeng YangState Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, 100084, China. yangyf@tsinghua.edu.cn.ORCID 0000-0001-8274-6196
Qingyun YanInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Xishu ZhouInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Xuanyu TaoInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Daliang NingInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Mengting M YuanInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Yujia QinInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Zhou J ShiInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Xue GuoInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Zhili HeInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Joy D Van NostrandInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Liyou WuInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Rosvel G Bracho-GarilloSchool of Forest Resources and Conservation, University of Florida, Gainesville, FL, 32611, USA.
C Ryan PentonCenter for Fundamental and Applied Microbiomics, Arizona State University, Mesa, AZ, 85212, USA.
James R ColeCenter for Microbial Ecology, Michigan State University, East Lansing, MI, 48824, USA.
Konstantinos T KonstantinidisSchool of Civil and Environmental Engineering, School of Biology, and Center for Bioinformatics and Computational Genomics, Georgia Institute of Technology, Atlanta, GA, 30332, USA.
Yiqi LuoCenter for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ, 86011, USA.
Edward A G SchuurCenter for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ, 86011, USA.
James M TiedjeCenter for Microbial Ecology, Michigan State University, East Lansing, MI, 48824, USA.
Jizhong ZhouInstitute for Environmental Genomics, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA. jzhou@ou.edu.
University of Oklahoma · USState Key Joint Laboratory of Environment Simulation and Pollution Control · CNNorthern Arizona University · USSun Yat-sen University · CNArizona State University · USCentral South University · CNGeorgia Institute of Technology · USGreat Lakes Bioenergy Research Center · USLawrence Berkeley National Laboratory · USMichigan State University · USUniversity of Florida · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

backgroundIt is well-known that global warming has effects on high-latitude tundra underlain with permafrost. This leads to a severe concern that decomposition of soil organic carbon (SOC) previously stored in this region, which accounts for about 50% of the world's SOC storage, will cause positive feedback that accelerates climate warming. We have previously shown that short-term warming (1.5 years) stimulates rapid, microbe-mediated decomposition of tundra soil carbon without affecting the composition of the soil microbial community (based on the depth of 42684 sequence reads of 16S rRNA gene amplicons per 3 g of soil sample).

resultsWe show that longer-term (5 years) experimental winter warming at the same site altered microbial communities (p < 0.040). Thaw depth correlated the strongest with community assembly and interaction networks, implying that warming-accelerated tundra thaw fundamentally restructured the microbial communities. Both carbon decomposition and methanogenesis genes increased in relative abundance under warming, and their functional structures strongly correlated (R

conclusionsOur results demonstrate that microbial responses associated with carbon cycling could lead to positive feedbacks that accelerate SOC decomposition in tundra regions, which is alarming because SOC loss is unlikely to subside owing to changes in microbial community composition. Video Abstract.

Indexed as

Carbon CycleGlobal WarmingMicrobiotaSoil MicrobiologyCarbonMethanePermafrostRNA, Ribosomal, 16SSeasonsSoilCarbonMethaneRNA, Ribosomal, 16SSoil

Identifiers

PMID31952472
PMCPMC6969446
OpenAlexW3013773288

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.